Constraints on the Formation and Evolution of Circumstellar Disks in Rotating Magnetized Cl

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陆国强词汇学讲稿第三章-理据

陆国强词汇学讲稿第三章-理据

第三章词的理据词的理据(motivation)指的是事物和现象获得名称的依据,说明词义与事物或现象的命名之间的关系。

第一章中提到词的音与义之间的关系实际上就涉及到了词的理据。

自然派认为音与义之间存在着必然的联系,而习惯派则认为音与义的联系是约定俗成。

第二章中在分析实义形位和语法形位时也涉及到了词的理据。

如chopper和doorman分别由chop-加-er和door-加-man构成,这是一种语法型的理据词。

本章拟将词的理据分成以下几种:I.拟声理据(onomatopoeic motivation)英语中有些词是通过声音的模仿构成的,这种构词称之为拟声构词(onomatopoeia)。

Stephen Ullmann把拟声构词分为两种。

一、基本拟声(primary onomatopoeia)基本拟声指音与义的相似,引志音与音之间联想,如buzz, crack, growl, hum, plop, squeak, squeal, whiz等。

鸟兽之类动物的叫声也属于这一范畴。

例如:Apes gibber Asses brayBears growl Beetles droneBulls bellow Camels gruntCats mew (purr)Ducks quackEagles scream Flies buzzFrogs croak Geese cackle (gabble)Goats bleat Hoses neigh (snort)Hens cluck Larks warbleLions roar Magpies chatterMice squeak Owls hoot(screech)Pigeons coo Pigs squeal (grunt)Puppies yelp Ravens croakSnakes hiss Thrushes whistleTurkeys gobble Wolves howl拟声法是一种修辞手段。

语言学提纲(学生)

语言学提纲(学生)

语⾔学提纲(学⽣)语⾔学复习I. Define the following terms 名词解释1. allomorphs2.suprasegmental features3. The semantic triangle4.cultural transmission (as a defining feature of human language)5. phonemic contrast (give an example)6. context7. sense8. relational opposites (give an example)9. perlocutionary act10. ReferenceII.Answer the following questions. 回答问题1. Take the following pairs of words:kill coal / kin cone / kit coatThe k in the first column is not identical with that in the second since its point of articulation is different: it is a forward k whereas the other is a backward k.How do phoneticians and linguists view this difference?Consider now the following pairs:cap gap / came game / coal goalHow do linguists view this difference?2. Sometimes a grammatically correct sentence can make no sense. For example: Sincerity shook hands with a brown apple. Q: How can you explain this phenomenon? (You should answer this Q by mentioning sentence meaning, grammaticality and selectional restriction.) Then analyze this sentence.3. Q: What are the four maxims of Cooperative Principle?Consider the following conversation:A: Where is Jack?B: He?s gone to the library. He said so when he left.Q: Which maxim does B’s response violate? What possible conversational implicature does B’s words have?III. Choice1. Antonyms are divided into several kinds. Which of the following is NOT a kind of antonyms?A. complementaryB. relationalC. polysemic2. In terms of predication analysis, the utterance “Is it going to snow this afternoon?” isa __________.A. one-place predicationB. two-place predicationC. three-place predicationD. no-place predication3. “I bought some roses” __________ “I bought some flowers”.A. entailsB. presupposesC. is inconsistent withD. is synonymous with4. Y?s utterance in the following conversation exchange violates the maxim of __________.X: Who was that you were with last night?Y: Did you know that you were wearing odd socks?A. qualityB. quantityC. relationD. manner5. “Sweets” and “candy” are used respectively in Britain and in America, but refer to the same thing. The words are__________ synonyms.A. collocationalB. dialectalC. completeD. stylistic6. There are di fferent types of affixes or morphemes. The affix “ed” in the word “learned” is known as a(n) __________.A. derivational morphemeB. free morphemeC. inflectional morphemeD. free form7. English consonants can be classified into stops. fricatives, nasals, etc. , in terms of __________.A. manner of articulationB. openness of mouthC. place of articulationD. voicing8. The study of how words are combined to form sentences is called __________.B. morphologyC. syntaxD. semantics9. Of the three branches of phonetics, the longest established, and until recently the most highly developed, is __________ phonetics.A. auditoryB. acousticC. articulatoryD. none of the above three10. What the element “-es” indicates is third person singular, present tense, the element “-ed”past tense, and “-ing”progressive aspect. Since they are the smallest unit of language and meaningful, they are also __________.A. phonemesB. morphemesC. allophonesD. phones11. The famous quotation from Shakespeare?s play “Romeo and Juliet” …A rose by any other name would smell as sweet? well illustrates _______.A. the arbitrariness of languageB. the productivity of languageC. the duality of languageD. the cultural transmission of language12.Of the following sound combinations, only _______ is permissible according to the sequential rules in English.A. rcudB. bkilC. echtD. gnav13. The term _______ linguistics may be defined as a way of referring to the approach which studies language at some point of time in history.A. synchronicB. diachronicC. comparativeD. historical comparative14.______ is NOT a design feature of human language.A. Cultural transmissionB. DisplacementC. Duality of structureD. Prescriptivism15. The consonant [f] in English can be correctly described as having the following phonetic features: ______.A. voiceless, bilabial, stopB. voiceless, labiodental, fricativeC. voiced, bilabial, stopD. voiced, labiodental, fricative16. The illocutionary point of the ______ is to commit the speaker to something?s being the case, to the truth of what has been said.A. representativesB. commissivesC. expressivesD. directives17. Which following pair of antonyms belong to complementary antonyms?A. good : badB. hit : missC. lend : borrowD. above : below18. Which of the following sentences doesn?t belong to one-place predication?A. The room is small.B. Is he making any trouble?C. It is raining heavily.D. The flower grows well.19. The relationship between furniture and wardrobe is ______.A. HyponymyB. SynonymyC. PolysemyD. Homonymy20. Conjunctions, prepositions, article, and pronouns consists of the grammatical word,they can be called ______.A. open class wordB. bound morphemesC. free morphemesD. closed class wordIV. Fill in the blanks (The first letter is given) 10%1. In F. de Saussure's dichotomy, l________ refers to the abstract linguistic system shared by all the members of a speech community; p is its realization inactual use. This distinction is similar to the distinction between c________ and p________, proposed by Chomsky.2. If a linguistic study describes and analyzes the language people actually use, it is said to be d________.3. Hyponymy is the relationship which obtains between specific and general lexical items. The word that is more general in meaning is called s________.4. The study of the linguistic meaning of words, phrases, and sentences is called Syntax .5. C________ are statements that either state or describe, and are thus verifiable; p________ are sentences that don?t statea fact or describe a state and are not verifiable.6. When two words are identical in both sound and spelling, they are complete h________.7. Clear l and dark l are a________ of the same one phoneme /1/. They never take the same position in sound combinations, thus they are said to be in c________ distribution.8. A r________ is often seen as part of a word, but it can never stand by itself although it bears clear, definite meaning.9. An essential difference between consonants and vowels is whether the air coming up from the lungs meets with anyo________ when a sound is produced.10.The morphemes that cannot be used by themselves, but must be combined with other morphemes to form words are called b________ morphemes.11.In the semantic analysis of a sentence, the basic unit is called p .12.The basic difference between pragmatics and traditional semantics is that pragmatics considers meaning in c________ and traditional semantics studies meaning in isolation from use.13. “Interviewer” and “interviewee” are a pair of r_______ opposites.14. R________deals with the relationship between the linguistic element and non-linguistic world of experience.15. Conversational i________may arise as a result of a speaker?s violation of the cooperative principle.V. Judge whether the following statements are T/F 10%( ) 1.A general difference between phonetics and phonology is that phonetics is focused on the production of speech sounds while phonology is more concerned with how speech sounds distinguish meaning.( ) 2. Modern linguistics is mainly diachronic.( ) 3. In classifying the English consonants and vowels, the same criteria can be applied.( ) 4. We can always tell by the words a compound contains what it means because the meaning of a compound is always the sum of the meanings of its parts.( ) 5. Beat and bit are not a minimal pair.( ) 6. Tense and reference are two terms often encountered in the study of meaning. ( ) 7. Sentences are not formed by randomly combining lexical items, but by following a set of syntactic rules that arrange linguistic elements in a particular order.( ) 8. The maxim of quality requires that a participant?s contribution be relevant to the conversation.( ) 9. A coordinate sentence contains two clauses joined by a linking word, such as “and”, “but”, “or”.( ) 10. The conceptualist view of meaning holds that there is no direct link between a symbol and reference, i.e. between language and thought.( ) 11. In the history of any language the writing system always came into being before the spoken form.( ) 12. In English, long vowels are also tense vowels because when we pronounce a long vowel such as /i:/, the larynx is in a state of tension.( ) 13. A compound is the combination of only two words.( ) 14. The word “photographically” is made up of 4 morphemes.( ) 15. The smallest meaningful unit of language is word.( ) 16. If a Chinese speaker pronounces the /l/ sound in the word feel not as a dark [l], but as a clear [l], he will be misunderstood by a native speaker as saying something else. ( ) 17. “He saw a child” entails “He saw a girl”.( ) 18. The conceptualist view of meaning holds that there is no direct link between a symbol and reference.( ) 19. The maxim of quality requires that a participant?s contribution be relevant to the conversation..( ) 20. Sentence meaning is concrete and context-independent .KEYSIV. Define the following terms (5*5分=25%)I.定义题1. Allomorphs: The variant forms of a morpheme are called its allomorph. For example, the morpheme used to express indefiniteness in English has two forms: a before a word that begins with a consonant and an before a word that begins witha vowel: an orange, an hour; a building, a minute. So a, an are the allomorph of the morpheme indefiniteness2. The phonemic features that occur above the level of the segments are called suprasegmental features; these are the phonological properties of such units are syllable, the word, and the sentence. The main suprasegmental features include stress, intonation and tone.3. The semantic triangle: There is no direct link between a linguistic form and what it refers to(i.e. between language and the real world); rather, in the interpretation of meaning they are linked through the mediation of concept in the mind. This is best illustrated by the classic semantic triangle suggested by Ogden and Richards.4. The details of any language system are not genetically transmitted, but have to be taught and learned. Language is passed on from one generation to the next through teaching and learning rather than by instinct, a feature which animals do not have.5. Phonetically similar sounds can form a contrast if they are two distinctive phonemes. Such pair of sounds can occur in the same environments and they distinguish meaning, and they are in phonemic contrast. For example, /p/ in rope and /b/ in robe are in phonemic contrast as the two similar sounds are in the same position yet distinguish meaning.6. Context is essential to the pragmatic study of language, and is considered as constituted by the knowledge shared by the speaker and hearer. The shared knowledge is of two types: the knowledge of the language they use and the knowledge about the world.7. Sense is concerned with the inherent meaning of the linguistic form. It is the collection of all features of the linguistic form and is abstract and decontextualized.8. As a form of antonymy, relational opposites refer to pairs of words that exhibit the reversal of a relationship between the two items such as doctor and patient.9. Perlocutioary act is the act performed by or resulting from saying sth; it is the consequence of, or the change brought about by the utterance; it is the act performed by say something.10. Reference means what a linguistic form refers to in the real, physical world; it deals with the relationship between the linguistic element and the non-linguistic world of experience.II.回答问题1. To the phonetician, the two k-s are not the same, since in the first column the k is followed by a front vowel and in the second by a back vowel.To the linguists, the difference is of secondary importance since to substitute a forward k for a b ackward k won?t cause the difference of the meaning, so they are not separate phonemes but so called allophones of the k phoneme.However, in the second case, we can seen a clear phonetic difference: that between a voiced and voiceless plosive at the same point. But to linguists, this difference is of vital importance. K and g are distinctive phonemes, and differentiate betweenmeaning.2. The meaning of a sentence has two parts: grammatical meaning and semantic meaning. Grammatical meaning refers to the grammatical well-formedness of a sentence, which is governed by the grammatical rules of the language. Semantic meaning is governed by selectional restrictions, constraints on what lexical items can go with others. Thus, some sentences may be grammatically correct, but may not be semantically meaningful, as they violate the selectional restrictions.In Sincerity shook hands with a brown apple, although this sentence is grammatically well-formed, it is obvious that it violates selectional restrictions. How can sincerity shake hands? How can one shake hands with a brown apple? How can an apple have brown color?3. There are four maxims under Cooperative Principle: the maxim of quantity, the maxim of quality, the maxim of relation, the maxim of manner.B?s response violates the maxim of quantity, which includes “Do not make your contribution more informative than is required”. B?s response has two parts. In fact, only the first part is enough to answer A?s question, but B has said the second part. He wants to imply that he is not sure whether Jack has really gone to the library because it is only what Jack told him.IV、填空题1. langue parole competence performance2. descriptive3. superordinate4. syntax5. constatives performatives6. homonyms7. allophone complementary 8. root 9. obstructed 10. bound 11. predication 12. context 13. relational 14. Reference 15. implicature。

Thermodynamical properties of the Undulant Universe

Thermodynamical properties of the Undulant Universe

a rXiv :0805.0635v 1 [a s t r o -p h ] 6 M a y 2008Thermodynamical properties of the Undulant UniverseTian LanDepartment of Astronomy,Beijing Normal University,Beijing,100875,ChinaTong-Jie Zhang ∗Department of Astronomy,Beijing Normal University,Beijing,100875,China.Recent observations show that our universe is accelerating by dark energy,so it is important to investigate the thermodynamical properties of it.The Undulant Universe is a model with equation of state ω(a )=−cos(b ln a )for dark energy,where we show that there neither the event horizon nor the particle horizon exists.However,as a boundary of keeping thermodynamical properties,the apparent horizon is a good holographic screen.The Universe has a thermal equilibrium inside the apparent horizon,so the Unified First Law and the Generalized Second Law of thermodynamics are satisfied.As a thermodynamical whole,the evolution of the Undulant Universe behaves very well in the current phase.However,when considering the unification theory,the failure of conversation law at the epoch of the matter dominated or near singularity need some more consideration for the form of the Undulant Universe.PACS numbers:95.36.+x,98.80.Cq,98.80.-k,04.20.Dw,04.70.-sI.INTRODUCTIONGeneral relativity (GR)is the theory of spacetime and gravitation formulated by Einstein in 1915.To admit a static,homogeneous solution for the Universe,Einstein modified his equation as follows (µ,ν=1,2,3,4):R µν−1∗Electronicaddress:tjzhang@known so little.In order to get more understanding of DE,many researchers have discussed it from thermody-namical viewpoints widely,such as thermodynamics of DE with constant ωin the range −1<ω<−1/3[5],ω=−1in the de Sitter spacetime and anti-de Sitter spacetime [6],ω<−1in the Phantom field [7,8],and ω=ω0+ω1z [9],the generalized chaplygin gas [10]and so on.More discussions on the thermodynamics of DE can be found in [11,12,13,14,45,46].In this paper,we also investigate a model from the thermodynamical viewpoints to explore some more interesting properties of DE.Usually we treat the Universe as a whole,a global spacetime,so it is analogous to black hole (BH),and some conclusions on BH can be used to the Universe.Hawking temperature,BH entropy,and BH mass satisfy the First Law of thermodynamics dM =T dS [15].In terms of the “rationalized area”[16],if a charged BH is rotating,solv-ing dM ,we get dM =(κ/8π)d A +Ω0dJ +V 0dQ ,where κ,A ,Ω0,J ,V 0,Q are the surface gravity,area,dragged ve-locity,angular momentum,electric potential and charge of a BH respectively.This expression is analogous to the First Law of thermodynamics dE =T dS −P dV .There-fore,it is suggestive of a connection between thermody-namics and BH physics in general,and between entropy and BH area in particular.Bekenstein conjectured these analysis at first [17],and Hawking discovered that the BH can emit particles according to the Planck spectrum,so we get the effective temperature on the horizon of the BH,T =κ/2π[18],and the entropy,S =A /4[19].Af-ter that,one can study many gravitational systems in the framework of thermodynamics.Consequently,the Uni-verse can be considered as a thermodynamical system [19,20,21,22],and the thermodynamical properties of BH can be generalized to spacetime enveloped by the cos-mological horizon.In other words,the thermodynamical laws should be satisfied.The principle of holography was first developed byHungarian scientist Dennis Gabor around1947-48while improving the resolution of an electron microscope[23].G.’t Hooft combined quantum mechanics with gravity tofind that the3-dimensional world is to be an image of data that can be stored on a2-dimensional holographic film,and they called the information on the projection “hologram”[24].Later,Fischler and Susskind applied it to the standard cosmological context[25].They con-sidered the world as a hologram[26],whose entire infor-mation about the global3+1-dimensional spacetime can be stored on particular hypersurfaces(called holographic screens).In other words,the degrees of freedom of a spa-tial region reside on the surface of the region.The total number of the degrees of freedom does not exceed the Bekenstein-Hawking bound,a universal entropy bound within a given weakly gravitational volume[27].Fur-thermore,the holographic principle requires the number of degrees of freedom per unit area to be no greater than 1per Planck area.Consequently,the entropy of a re-gion must not exceed its area in Planck units,wherefore, the maximum number of degrees of freedom in a volume should be proportional to the surface area[28].Even with a short distance cutoff,the information content of a spa-tial region would appear to grow with the volume.The holographic principle,on the other hand,implies that the number of fundamental degrees of freedom is related to the area of surfaces in spacetime.We will show that the holographic principle is coincidence with the analysis of the Unified First Law,and corresponds to the General-ized Second Law of thermodynamics of the Universe. We use the Planck units c=G=k B= =1,where G is Newton’s constant, is Planck’s constant,c is the speed of light,and k B is Boltzmann’s constant respec-tively.The Planck units of energy density,mass,temper-ature,and other quantities are converted to CGS units. This paper is organized as follows:In Sec.II,we re-view the introduction to the Undulant Universe.In Sec. III,we discuss the cosmological horizons of the Undulant Universe.Then we demonstrate the Unified First Law of thermodynamics and the Generalized Second Law of thermodynamics on the apparent horizon respectively in Sec.IV and Sec.V.In Sec.VI,we present conclusions and discussions.II.INTRODUCTION TO THE UNDULANTUNIVERSEParticle physicists contemplate the possibility of an en-ergy density inherent in the vacuum that is defined as the state of lowest attainable energy.Now we believe we have measured the vacuum energy.However,from the measurement,wefind that the cosmological constant has a discrepancy of large orders of magnitude in energy scale to the vacuum energy,and some reviews can been seen from Sahni and Starobinski2000,Carroll2001,or Peebles and Ratra2003.What is worse,there is a co-incidence scandal between the observed vacuum energy and the current matter density.Our homogeneous and isotropic Universe follows the dynamics of an expanding Robertson-Walker(RW)spacetime(i,j=1,2):ds2=g ij dx i dx j+r∗2dΩ2(3) =dt2−a2(t)(dr21−κr2.(4)The evolution of the Universe is governed by the Fried-mann equation:H2=˙a23ρ−κ8πG.(7)The weight of observational evidence,extended by de-tailed observations[29],points to aflat Universe,in-cluding0.05ordinary matter and0.22nonbaryonic dark matter,but dominated by DE.The densities in matter and vacuum are of the same order of magnitude.Fur-thermore,the traditional vacuum energy density does not vary with time,while matter and radiation density change rapidly with the expansion of the Universe.The phase of the Universe transferred from radiation domi-nated to matter dominated in the past,and recently,at z∼1.5,the vacuum energy is ly,if the vacuum becomes dominated at any epoch,the Uni-verse would have evolved completely different history.To solve this cosmic coincidence problem,some researchers put forward the anthropic idea[30].According to this idea,there are many universes with different values of the vacuum energy,and most of them don’t allow life to develop.Meanwhile,many nonanthropic ideas have also been proposed.These ideas make the vacuum en-ergy track the matter density in a certain way such thatthe ratio is not so large[31],but all of them involvefinetuning problem in some way.[32]Considering all of these challenges to our understand-ing of DE,we investigate Undulant Universe character-ized by alternating periods of acceleration and deceler-ation[33].The Undulant Universe is the case of thevacuum energy varying with time,specifically with thenumber of e-foldings of the scale factor.Its EOS is:ω(a)=−cos(b ln a),(8)and the Hubble parameter:3H2(a)=H20(ΩM0a−3+ΩΛ0a−3exp[sin(b ln a)].(10)bThere are two quite different horizon concepts in cos-mology satisfying our definition and cosmologists have atvarious times devoted their attention to these horizons.Firstly,an event horizon(EH),for a given fundamentalobserver A,is a hypersurface in spacetime dividing allevents into two non-empty classes:those that have been,are,or will be observable by observer A,and those thatare forever outside observer A’s possible powers of obser-vation[36].Such that,for a global observer,the radiusof spacetime EH at cosmic time t can be written as:R E=a(t) t f t dt= +∞a da H0a0.5exp[1.5a(t)(PH),for any given fundamental observer B and cosmic instant t is a surface in the instantaneous3-space,divid-ing all fundamental particles into two non-empty classes: those that have already been observable by observer B at time t and those that have not[36].The radius of spacetime PH at cosmic time t can be written as:R P=a(t) t t i dta(t)= a0da H0a0.5exp[1.5bsin(b ln a)].(17)The radius of spacetime AH depends on the details of the matter distribution in the Universe.In generic situation, the AH evolves in time,and visibility of the outside anti-trapped region depends on the time development of the AH.Because there is no EH,the spatial region outsideFIG.2:The radius of spacetime AH in units of H−1as func-tion of a within three different large ranges,which are in dif-ferent starting points or end points,corresponding to three differentωin FIG.1respectively.of the horizon at a given time might be observed.The change of the radius varying with time during a Hubble time t H is:t Hd ln r∗AFIG.3:t H d ln r∗A/dt as function of a in different starting points or end points,corresponding to three differentωin FIG.1respectively.The amount of energyflux[40]crossing the AH within the time interval dt isdE A=4πr∗2A Tµνuµuνdt=4πr∗2A(ρ+P)dt=1.5H−1a0.5[1−cos(b ln a)]×exp[−1.5bsin(b ln a)]da.(24)Comparing Eq.(21)with Eq.(24),we have proved the re-sult dE A=T A dS A,so the Unified First Law of thermo-dynamics on the AH is confirmed,and the work can be done is zero indeed.From the FIG.4,wefind no periodic variation in any periods ofω.Some details in the top panel of FIG.4have been demonstrated in FIG.5.We find in different starting points or end points,even if in small ranges,the basic feature of the change of energy is similar,and T A dS A and−dE A are symmetrically dis-tributed around the level line.Actually,because of the of H−1(dashed line)as function of a in different starting points or end points,corresponding to three differentωin FIG.1respectively.And the level line is the change of energy in the Standard Universe(dotted line).oscillation ofω,the variation of energy is somefluctua-tion of the Standard Universe.We chooseΛCDM with ΩΛ0=1andΩM0=0as the Standard Universe. However,considering unification theory,the matter term and k=0should be added to the dynamics of the Undulant Universe.As discussed above,the Unified First Law is broken when the Universe is deceleration or the curvature generally becomes large near the singularity. To make sure that the Unified First Law is satisfied,we speculate that the DE has other form,e.g.,scalar vector form near the singularity[45].V.THE GENERALIZED SECOND LA W OFTHERMODYNAMICS ON THE APPARENTHORIZONFrom holography we know that the preferred screen is the cosmological horizon.As the discussion mentioned above,the AH is a good cosmological horizon,and the successful Unified First Law of thermodynamics give us the chance to continue to discuss the Generalized Second Law of thermodynamics.The Generalized Second Law:The common entropy in the BH exterior plus the BH entropy never deceases. This statement means that we must regard BH entropy as a genuine contribution to the entropy content of the Universe.Similarly,we now state a version of the cosmic holographic principle based on the cosmological AH:the particle entropy inside the AH can never exceed the AH gravitational entropy,i.e.the entropy inside the AH plus the AH gravitational entropy never deceases[41].FIG.5:T A dS A(thick line)in units of H−1and−dE A inunits of H−1(dashed line)as function of a in different starting points or end points,which demonstrate some details in the top panel of FIG.4.And the level line is the change of energy in the Standard Universe(dotted line).We can obtain the entropy of the Universe inside the AH through the Unified First Law of thermodynamics inside the horizon:T dS i=dE i+P dV=V dρ+(ρ+P)dV,(25)thereinto Eq.(25),the energy inside the AH is E i= 4πr∗3Aρ/3,and the volume is V=4πr∗3A/bin-ing Eq.(6)with Eq.(7),and differentiatingρ=ρΛ,we get dρ=3HdH/4π.According to the Zeroth Law of thermodynamics[42],we know on a stationary surface in the thermodynamical equilibrium,the temperature is constant Hawking temperature.However,the tempera-ture of the viscous matter were higher than the Hawking temperature.At the same time,because the Universe expands and DE is dominant,the temperature declines more rapidly.Such that we might define T=uT H[43], where u is a real constant,0<u≤1.Indeed the param-eter u shows the deviation from Hawking temperature. Therefore we obtaindS i=V dρ+(ρ+P)dVuT H(26)=1.5H−1bsin(b ln a)]da.(27)When u=1,dS i is minimum,so we just need to study how the minimal differential entropy evolves.For the FIG.6:dS i(thick dotted green line),dS A(thick solid line), and dS i+dS A=dS total(thick dashed line)in units of H−20 as functions of a in different starting points or end points, corresponding to three differentωin FIG.1respectively.The differential entropy of the Standard Universe is the level line (thin dotted line).entropy of the AH,we obtaindS A=dr∗Absin(b ln a)]da.(28)The total differential entropy is dS total=dS A+dS i, and all of the variation of the entropy vary with a.As shown in FIG.6,dS i≤0all the time,but dS A≥0and dS total≥0too.All of these cases in different start-ing points or end points are similar,even if in the small ranges.Because of smallfluctuation in the evolution,as presented in FIG.7,there is dS i≥0locally.However, the minimal total differential entropy is dS total≥0all the time,so the real total differential entropy should not decrease.In conclusion,the Generalized Second Law of thermodynamics is confirmed on the AH.We conclude from[45,46],thatω(a)<−1is physi-cally meaningless because of the negative entropy,while ω(a)=−cos(b ln a)>−1should be satisfied all the time. Therefore the confirmation of the Generalized Second Law of the Universe is another support to this conclu-sion.VI.CONCLUSIONS AND DISCUSSIONSThe properties of DE have been studied since long time ago,and many models have been put forward.Although there is no evidence to present an exact model in accord with the real world,researchers have been successful inFIG.7:dS i(thick dotted line),dS A(thick solid line),and dS i+dS A=dS total(thick dashed line)in units of H−2as functions of a within three different small ranges,and in dif-ferent starting points or end points,which demonstrate some details in the top panel of FIG.6.The differential entropy of the Standard Universe is the level line(thin dotted line).many aspects.In this paper,we study the Undulant Universe on its thermodynamical properties,and all of these conclusions demonstrate wonderful results.We have shown that the Undulant Universe is a model to solve the cosmic coincidence problem withoutfine tun-ing,i.e.current phase of the Universe is not a particular one.In other words,we can come from any phase in the past,and go to any phase in the future.In the discussions of the cosmological horizon,neither the EH nor the PH exists in the Undulant Universe,which is a direct result from the solution.However,wefind another cosmological horizon,the AH,in the Universe as a whole.According to topology,the FOTH is a3-manifold,and the AH is the outer boundary of a connected component of a trapped region.Locally in time,it is a2-dimensional surface.We choose a special expression for the AH,whose evolution can be seen from FIG.2.There is no periodicity,but no matter how the Universe evolves,we can alwaysfind a AH,and all of their evolution are similar.Whereafter, we consider the Universe as a thermodynamical system inside the AH.Because of no change significantly over one Hubble scale,as shown in FIG.3,the equilibrium thermodynamics can be applied within the AH.The Four Laws of BH thermodynamics[42]are suc-cessful,whether these conjectures are confirmed in the Universe should be proved.The thermodynamical First Law dM=T dS converted to the AH,is dE A=T A dS A. Because the work might be done is zero at infinity,we have ignored the work term P dV.From our deduction, the Unified First Law of thermodynamics is satisfied per-fectly.As shown in FIG.4,there is no periodic variation in any periods ofω,and the basic feature of the change ofis similar in different starting points or end points, if in small ranges.As presented in FIG.5,due to the ofω,there is somefluctuation in the variation energy comparing with the Standard Universe.One of the most popular theory,holography,is a beau-information theory.We would applied it to the stan-cosmological context,such that the world can be as a hologram,and entire information about global3+1-dimensional spacetime can be stored on hypersurfaces.The connection between en-and information is well known[44].The entropya thermodynamical system in equilibrium is realizedit measures the uncertainty or inaccessibility of in-as to the actual internal configuration of theThe information is compatible with its macro-thermodynamical parameters(temperature,pres-etc.).Whenever new information about the system available,it can be considered as imposing some constraints on the entropy.This process leads to a de-crease in the entropy function.The entropy of a thermo-dynamical system,being in not equilibrium approaching equilibrium,increases because information about the in-ternal configuration of the system is missing during its evolution.The missing is due to the washing out of the effects of the initial conditions,and it would be expected to be reflected in the gradual increase in the entropy of its surface.An exterior observer is likely to cause a de-crease in the entropy of a system by acquitting infor-mation about the internal configuration of the system. But information is never free.During acquiring informa-tion about the system,the observer causes an increase in the entropy of the rest of the Universe inevitably.This increase exceeds the decrease.Accordingly,the total en-tropy of the Universe increases in the process.Coming back to the thermodynamics of the Universe, we obtain the entropy inside the AH by the Unified First Law of thermodynamics,and the temperature of the DE dominated Universe is not higher than the Hawking tem-perature.So we choose the maximal temperature to get the minimal total differential entropy dS total.Associ-ated with the differential entropy on the AH,we get dS total=dS A+dS i.The temperature of the cosmo-logical material will decline as the Universe expands,so dS i≤0.The accompanying loss of energy can cause a back reaction on the cosmic dynamics.The reaction will lead to increase the horizon area,so dS A≥0.We might expect the rise in entropy associated with this increase to more than offset the decrease,which is due to the other processes discussed above.Wefind that the total entropy of the AH does not decrease with time,i.e.dS total≥0. The entropy of the visible Universe decreases in the pro-cess,in spite of dS i≥0locally due to smallfluctuation in the evolution.In a word,the Generalized Second Law of thermodynamics is satisfied on the AH.As shown in FIG.6and FIG.7,whenever and wherever the Universe evolves,the variation of the entropy is similar.Although we just discuss the minimal total differential entropy,the real one remains confirmed.In conclusion,the AH of the Undulant Universe is a good holographic screen,and as a boundary of keeping thermodynamical properties.The Universe has a ther-mal equilibrium within the AH.The Undulant Universe behaves very well in its evolution,and in spite of some undulant departure from the Standard Universe,it solves some coincidence problem in the Standard Universe.In summary,from the thermodynamical viewpoints, the investigation to the Universe is interesting,however, there are some problems.In fact,the acceleration of our Universe is temporary,and there ever was and will be a matter dominated phase or singularity.Therefore we should consider matter dominated or large curvature case due to unification theory.We have assured that the conversation law is confirmed all the time,however, when the Universe is deceleration or near singularity,the conversation law is broken.This bad result means that the energy in the Undulant Universeω(a)=−cos(b ln a) maybe some other form in the matter dominated epoch or near singularity,such that the conversation law can not be violated.Another possibility is that the entropy should be redefined.However,the success of our stan-dard deduction encourages the definition in the Undulant Universe.Furthermore,thermodynamical properties de-mand to be explored more deeply in the future,and there are some more cosmological horizons expected to be stud-ied.VII.ACKNOWLEDGMENTSWe are very grateful to the anonymous referee for his valuable comments that greatly improve this pper.Tian Lan would like to thank Prof.Canbin Liang for his pa-tient and valuable teaching,and Yongping Zhang for her discussion and suggestions,all the students in her lab for their valuable comments and help.This work was supported by the National Science Foundation of China (Grants No.10473002)and the Scientific Research Foun-dation for the Returned Overseas Chinese Scholars,State Education Ministry.[1]A.G.Riess et al,Astron.J.116(1998)1009.[2]C.L.Bennett et al.,Astrophys.J.Supp.Ser.148(2003)1;D.N.Spergel et al.,ApJS,170,377(2007).[3]D.J.Eisenstein et al.Astrophys.J.633(2005)560.[4]A.G.Riess et al.,Astrophy.J.607(2004)665.[5]B.Wang,Y.G.Gong,E.Abdalla,Phys.Rev.D74,083520(2006).[6]A.Frolov and L.Kofman,JCAP.05(2003)09;BunchT.S and Davies P.C,Quantumfield theory in de Sitter space(Proc.R.Soc.A360,1978).[7]Raphael Bousso,Phys.Rev.D71,064024(2005).[8]Jens Kujat,Robert J.Scherrer and A.A.Sen,Phys.Rev.D74,083501(2006).[9]Yongping Zhang,Zelong Yi,Tong-Jie Zhang,WenbiaoLiu,Phys.RevD.77.023502(2008).[10]Y.G.Gong,B.Wang and A.Z.Wang,JCAP0701(2007)024.[11]I.Brevik,S Nojiri,S.D.Odintsov and L.Vanzo,Phys.Rev.D70(2004)043520.[12]S.Nojiri and S.D.Odintsov.Phys.Rev.D70(2004)103522.[13]M.R.setare and S.shafei,JCAP09(2006)011;M.R.Settare,JCAP0701(2007)023.[14]F.C.Santos,M.L.Bedran and V.soares.Phys.lett.B636(2006)86.[15]J.M.Bardeen,B.carter and S.W.Hawking,Commum.Math.Phys.31,161(1973).[16]D.Christodoulou Phys.Rev.Lett.25,1596(1970); D.Christodoulou Ph.D.thesis,Princeton University,1981 (unpublished).[17]J.D.Bekenstein,Phys.Rev.D7,2333(1973).[18]S.W.Hawking,Commun.Math.Phys.43,199(1975).[19]G.W.Gibbons and S.W.Hawking,Phys.Rev.D15(1977)2738.[20]M.D.Pollock and T.P.Singh,class.Quantum.Grav.6(1989)901.[21]A.V.Frolov and L.kofman,JCAP0305(2003)009.[22]T.Jacobson,Phys.Rev.Lett.75,1260(1995).[23]Collier,R.,Burckhardt,C.,Lin,L.,”Optical Hologra-phy”,1971,Academic Press,Inc.,New York.[24]G.’t Hooft,Dimensional Reduction in Quantum Grav-ity,in’Salamfest’pp.284-296(World Scientific Co,Sin-gapore,1993).[25]W.Fischler and L.Susskind,hep-th/9806039.[26]L.Susskind,J.Math.Phys.36,6377(1995).[27]J.D.Bekenstein,Phys.Rev.D49,1912(1994),and ref-erences therein.[28]L.Susskind,J.Math.Phys.(N.Y.)36,6377(1995);G.’t Hooft,gr-qc/9310026.[29]C.L.Bennett et al.,Astrophys.J.Suppl.Ser.148,1(2003).[30]S.Weinberg,Rev.Mod.Phys.61,11989.[31]R.R.Caldwell,R.Dave,and P.J.Steinhardt,Phys.Rev.Lett.80,15821998.[32]A.Vilenkin,hep-ph/0106083and A.Vilenkin,Phys.Rev.D61,023*******;S.Bludman,Nucl.Phys.A2000.J.Garriga and A.Vilenkin,Phys.Rev.D64,023517 2001.E.D.Stewart,in Cosmo2000:Proceedings of the Fourth International Workshop on Particle Physics and the Early Universe,Korea,2000.[33]Gabriela Barenboim,Phys.Rev.D71,063533(2005).[34]Deepak Jain,Abha Dev,and J.S.Alcaniz,Phys.lett.B656(2007)15.[35]Raphael Bousso,Rev.Mod.Phys.74(2002)825-874.[36]W.Rindler,Mon.Not.Roy.Astr.Soc.116,662-677(1956).[37]Abhay Ashtekar Phys.Rev.D68,104030(2003)[38]R.G.Cai and L.M.Cao,Phys.Rev.D75,064008(2007).[39]Sean A.Hayward,Class.Quant.Grav.15(1998)3147.[40]Raphael Bousso,Phys.Rev.D71,064024(2005).[41]Dongsu Bak and Soo-Jong,Class.Quant.Grav.17(2000)L83.[42]J.M.Bardeen B.Carter and S.W.Hawking,Commun.math.Phys.31,161-170(t973).[43]P C W Davies,Class.Quantum Grav.4(1987)L225-L228(1987).[44]L.Brillouin,Science and Information.[45]Shinichi Nojiri,Sergei D.Odintsov,Phys.Rev.D70.103522(2004).[46]J.A.S.Lima,J.S.Alcaniz,Phys.lett.B600191-196(2004).。

托福阅读TPO27-2 The Formation of Volcanic Islands

托福阅读TPO27-2 The Formation of Volcanic Islands

The Formation of Volcanic IslandsEarth’s surface is not made up of a single sheet of rock that forms a crust but rather a number of “tectonic plates” that fit closely, like the pieces of a giant jigsaw puzzle. Some plates carry islands or continents others form the seafloor. All are slowly moving because the plates float on a denser semi-liquid mantle, the layer between the crust and Earth’s core. The plates have edges that are spreading ri dges (where two plates are moving apart and new seafloor is being created), subduction zones (where two plates collide and one plunges beneath the other), or transform faults (where two plates neither converge nor diverge but merely move past one another). It is at the boundaries between plates that most of Earth’s volcanism and earthquake activity occur.Generally speaking, the interiors of plates are geologically uneventful. However, there are exceptions. A glance at a map of the Pacific Ocean reveals that there are many islands far out at sea that are actually volcanoes----many no longer active, some overgrown with coral----that originated from activity at points in the interior of the Pacific Plate that forms the Pacific seafloor.How can volcanic activity occur so far from a plate boundary? The Hawaiian Islands provide a very instructive answer. Like many other island groups, they form a chain. The Hawaiian Islands Chain extends northwest from the island of Hawaii. In the 1840s American geologist James Daly observed that the different Hawaii islands seem to share a similar geologic evolution but are progressively more eroded, and therefore probable older, toward the northwest. Then in 1963, in the early days of the development of the theory of plate tectonics. Canadian geophysicist Tuzo Wilson realized that this age progression could result if the islands were formed on a surface plate moving over a fixed volcanic source in the interior. Wilson suggested that the long chain of volcanoes stretching northwest from Hawaii is simply the surface expression of a long-lived volcanic source located beneath the tectonic plate in the mantle. Today’s most northwest island would have been the first to form. They as the plate moved slowly northwest, new volcanic islands would have forms as the plate moved over the volcanic source. The most recent island, Hawaii, would be at the end of the chain and is now over the volcanic source.Although this idea was not immediately accepted, the dating of lavas in the Hawaii (and other) chains showed that their ages increase away from the presently active volcano, just as Daly had suggested. Wilson’s analysis of these data is now a central part of plate tectonics. Most volcanoes that occur in the interiors of plates are believed to be produced by mantle plumes, columns of molten rock that rise from deep within the mantle. A volcano remains an active “hot spot” as long as it is over the plume. The plumes apparently originate at great depths, perhaps as deep as the boundary between the core and the mantle, and many have been active for a very long time. The oldest volcanoes in the Hawaii hot-spot trail have ages close to 80 million years. Other islands, including Tahiti and Easter Islands in the pacific, Reunion and Mauritius in the In dia Ocean, and indeed most of the large islands in the world’s oceans, owe their existence to mantle plumes.The oceanic volcanic islands and their hot-spot trails are thus especially useful for geologist because they record the past locations of the plate over a fixed source. They therefore permit the reconstruction of the process of seafloor spreading, and consequently of the geography of continents and of ocean basins in the past. For example, given the current position of the Pacific Plate, Hawaii is above the Pacific Ocean hot spot. So the position of The Pacific Plate 50 million years ago can be determined by moving it such that a 50-million-year-oil volcano in the hot-spot trail sits at the location of Hawaii today. However because the ocean basins really are short-lived features on geologic times scale, reconstruction the world’s geography by backtracking along the hot-spot trail works only for the last 5 percent or so of geologic time.Paragraph 1: Earth’s surface is not made up of a single shee t of rock that forms a crust but rather a number of “tectonic plates” that fit closely, like the pieces of a gain jigsaw puzzle. Some plates carry islands or continents, others form the seafloor. All are slowly moving because the plates float on a denser sem-iliquid mantle, the layer between the crust and Earth’s core. The plates have edges that are spreading ridgescollide and one plunges beneath the other), or transform faults (where two plates nor diverge but merely move past one another). It is at the boundaries between plates that most of Earth’s volcanism and earthquake activity occur.1.The author mentions “spreading ridges”, “subduction zones”, and “transform faults” in order toO illustrate that the boundaries of tectonic plates are neat, thin linesO explain why some tectonic plates carry islands or continents while others form the seafloorO explain the complex nature of the edges of tectonic platesO provide examples of areas of tectonic plates where little geologic action occursO expandO formO riseO move closer3.which of the sentences below best expresses the essential information in the highlighted sentence in the passage? Incorrect choices change the meaning in important ways or leave out essential information O Volcanic activity is responsible for the formation of the Pacific seafloor in the interior of the Pacific Plate.O Many volcanoes in the Pacific Ocean are no longer active and have become islands that supportcoral.O There are many islands in the Pacific Ocean that originated as volcanoes in the interior of the Pacific Plate.O The map of the Pacific Ocean reveals fewer volcanic islands than there truly are because many are no longer active and some are completely overgrown with coral.volcanic activity occur so far from a plate boundary? The Hawaiian islandsChain extends northwest from the island of Hawaii. In the 1840s American geologist James Daly observed that the different Hawaii islands seem to share a similar geologic evolution but are progressively moreand therefore probable older, toward the northwest. Then in 1963, in the early days of the development of the theory of plate tectonics. Canadian geophysicist Tuzo Wilson realized that this age progression could result if the islands were formed on a surface plate moving over a fixed volcanic source in the interior. Wilson suggested that the long chain of volcanoes stretching northwest from Hawaii is simply the surface expression of a long-lived volcanic source located beneath the tectonic plate in the mantle. Today’s most northwest island would have been the first to form. They as the plate moved slowly northwest, new volcanic islands would have forms as the plate moved over the volcanic source. The most recent island, Hawaii, would be at the end of the chain and is now over the volcanic source.O clearO detailedO informativeO familiarO worm downO scatteredO developedO deserted6.In paragraph 3, what is the relationship between the scientific contribution of James Daly and Tuzo Wilson?O Wilson provided an explanation for the observations made by Daly.O Wilson challenged the theory proposed by Daly.O Wilson found numerous examples of island chains that supported Daly’s theory.O Wilson popularized the explanation of volcanic island formation formulated by Daly.Paragraph 4: Although this idea was not immediately accepted, the dating of lavas in the Hawaii (and other) chains showed that their ages increase away from the presently active volcano, just as Daly had suggested. Wilson’s analysis of these data is now a central part of plate tectonics. Most volcanoes thatoccur in the interiors of plates are believed to be produced by mantle plumes, columns of molten rock that rise from deep within the mantle. A volcano remains an active “hot spot” as long as it is over t he plume. The plumes apparently originate at great depths, perhaps as deep as the boundary between the core and the mantle, and many have been active for a very long time. The oldest volcanoes in the Hawaii hot-spot trail have ages close to 80 million years. Other islands, including Tahiti and Easter Islands in the pacific, Reunion and Mauritius in the India Ocean, and indeed most of the large islands in the world’s oceans, owe their existence to mantle plumes.7.Why does the author provide the informatio n that “the dating of lavas in the Hawaii (and other) chains showed that their ages increase away from the presently active volcano”?O To point out differences between the Hawaii island chain and other volcanic island chainsO To question the idea that all the islands in an island chain have been formed by volcanic activity O To explain why Wilson hypothesis was initially difficult to acceptO To provide evidence in support of Daly’s and Wilson’s ideas about how the Hawaii islands were formed8.According to paragraph 4, which of the following is true of mantle plumesO They exist close to the surface of tectonic plates.O They cause most of the volcanic activity that occurs in the interiors of plates.O They are rarely active for long period of time.O They get increasingly older away from the present hot spots.Paragraph 5: The oceanic volcanic islands and their hot-spot trails are thus especially useful for geologist because they record the past locations of the plate over a fixed source. They therefore permit thePacific Ocean hot spot. So the position of The Pacific Plate 50 million years ago can be determined by moving it such that a 50-million-year-oil volcano in the hot-spot trail sits at the location of Hawaii today. However because the ocean basins really are short-lived features on geologic times scale, reconstruction the world’s geography by backtracking along the hot-spot trail works only for the last 5 percent or so of geologic time.9.According to paragraph 5, volcanic islands help geologists toO reconstruct past geographyO detect changes in mantle plumesO measure the rigidity of tectonic platesO explain why the seafloor spreads10.What can be inferred about the Pacific Plate from paragraph 5?O The hot spots on the Pacific Plate are much older than the ones located on the other tectonic plates.O Most of the volcanic sources beneath the Pacific Plate have become extinct.O The Pacific Plate has moved a distance equal to the length of the Hawaiian Island chain in the past 80 million years.O The Pacific Plate is located above fewer mantle plumes than other plates are.O originalO idealO relativeO present12.According to paragraph 5, why are geologists unable to trace back the entire geologic of continents from hot-spot trails?O Hot spots have existed for only about 5 percent of geologic time.O Hawaii did not exist 50 millions years ago.O Oceanic basins that contained old hot-spot trails disappeared a long time ago.O Hot-spot trails can be reconstructed only for island chains.Paragraph 3: How can volcanic activity occur so far from a plate boundary? The Hawaiian islands provide a very instructive answer. ■Like many other island groups, they form a chain. ■The Hawaiian Islands Chain extends northwest from the island of Hawaii. ■In the 1840s American geologist James Daly observed that the different Hawaii islands seem to share a similar geologic evolution but are progressively more eroded, and therefore probable older, toward the northwest. ■Then in 1963, in the early days of the development of the theory of plate tectonics. Canadian geophysicist Tuzo Wilson realized that this age progression could result if the islands were formed on a surface plate moving over a fixed volcanic source in the interior. Wilson suggested that the long chain of volcanoes stretching northwest from Hawaii is simply the surface expression of a long-lived volcanic source located beneath the tectonic plate in the mantle. Today’s most northwest island would have been the first to form. They as the plate moved slowly northwest, new volcanic islands would have forms as the plate moved over the volcanic source. The most recent island, Hawaii, would be at the end of the chain and is now over the volcanic source.13.Look at the four squares [■] that indicate where the following sentence could be added to the passage.This pattern remained unexplained for a long time.Where would the sentence best fit?14 Directions: An introductory sentence for a brief summary of the passage is provided below. Complete the summary by selecting the THREE answer choices that express the most important ideas in the passage. Some sentences do not belong in the summary because they express ideas that are not presented in the passage or are minor ideas in the passage. This question is worth 2 points.Although volcanic activity is concentrated on the edge of tectonic plates, such activity can occur in the interiors of plates as well.Answer Choices●●●O Our understanding of islands comes from Daly’s and Wilson’s observations of the Hawaiian Islands, which was later confirmed by plate-tectonic theory.O The hot-spot trails formed by volcanic island chains indicate the positions of tectonic plates as for back as the present ocean basins have existed.O Whereas volcanic islands formed by mantle plumes are typically small, most of the world’s largest islands are formed at the edges of tectonic plates.O It has only recently been discovered that tectonic plates are closely fitting rather than loosely constructed, as geologist previously believed.O Volcanic island chains such as the Hawaiian Islands form in the interior of a tectonic plate as the plate moves over a fixed volcanic source in the mantle.O The Pacific Plate has existed for as long as the Hawaiian Islands have existed, namely for more than 80 million years.参考答案1.○32.○43.○34.○35.○16.○17.○48.○29.○110.○311.○412.○313.○414. Our understanding of islands comes…Whereas volcanic islands…It has only recently been…。

constrains on nature selection

constrains on nature selection

constrains on nature selectionConstraints on Nature SelectionIntroduction•Nature selection refers to the process by which the environment, through various mechanisms, determineswhich traits are advantageous and allow organisms tosurvive and reproduce.•However, there are certain constraints that affect the outcomes of natural selection and shape the evolution of species.•In this article, we will explore some of the key constraints on nature selection and their implicationsfor biological diversity and adaptation.Genetic Constraints1.Genetic Variation:–Limited genetic diversity within a population can constrain the potential for adaptation.–Lower genetic variation reduces the pool ofavailable traits for selection to act upon.2.Genetic Trade-offs:–Organisms often face trade-offs when allocating resources to different traits.–Selection for one beneficial trait may hinder the development or maintenance of other traits.3.Genetic Drift:–Random changes in allele frequencies can occur due to genetic drift, especially in small populations.–Genetic drift can lead to the fixation of neutral or deleterious alleles, limiting adaptation. Environmental Constraints1.Physical Limitations:–Organisms are constrained by physical limitations imposed by their environment.–For example, the size and shape of beaks in birds may be constrained by their feeding habits andavailable food sources.2.Resource Availability:–Limited availability of resources, such as food, water, or shelter, can restrict the extent ofadaptation.–Competition for resources can influence theselection pressures acting on different traits. 3.Coevolutionary Interactions:–Coevolution with other species can imposeconstraints on natural selection.–Organisms may evolve traits that are advantageous in their interactions with specific partners,limiting their adaptation in other contexts. Developmental Constraints1.Developmental Plasticity:–Organisms exhibit various degrees of developmental plasticity, allowing them to respond toenvironmental cues.–Developmental constraints can limit the range of possible phenotypes that can be produced inresponse to selection.2.Developmental Trade-offs:–Developmental processes may be subject to trade-offs, making it difficult to simultaneouslyoptimize multiple traits.–This can constrain the direction and extent of natural selection.3.Developmental Constraints on Evolutionary Transitions:–Some evolutionary transitions, such as thetransition from aquatic to terrestrial habitats,are constrained by developmental limitations.–The need for functional intermediates can slow down the process of adaptation and the emergence of newspecies.Conclusion•Constraints on nature selection play a crucial role in shaping the patterns of biological diversity andadaptation.•Genetic, environmental, and developmental constraints interact to determine the direction and pace ofevolutionary change.•By understanding these constraints, we can gain insights into the limitations and possibilities of naturalselection and appreciate the remarkable diversity oflife on Earth.Implications for Conservation•Understanding the constraints on natural selection is essential for conservation efforts.•Conservation strategies need to take into account the limitations and vulnerabilities of species in theirresponse to changing environments.Future Directions•Further research is needed to better understand the interconnectedness of genetic, environmental, anddevelopmental constraints.•Exploring the adaptive potential of organisms under different constraints can provide insights into theirevolutionary resilience.Ethical Considerations•Recognizing the constraints on natural selection raises ethical questions about human responsibility andintervention in evolutionary processes.•It is important to balance conservation efforts with respect for natural processes and the preservation ofbiodiversity.Conclusion•Constraints on natural selection shape the course of evolution and determine the patterns of biodiversity andadaptation.•Genetic, environmental, and developmental constraints define the limits and possibilities of natural selection. •By studying and understanding these constraints, we can gain a deeper appreciation for the intricacies of thenatural world and make more informed decisions regardingconservation and preservation.。

银川海派英语【托福阅读】文章的结构类型你了解吗

银川海派英语【托福阅读】文章的结构类型你了解吗

银川海派英语【托福阅读】文章的结构类型你了解吗当一篇文章对话题进行分类讨论,文章总体结构就属于分类。

官方指南《Aggression》这篇文章就是典型的分类文章。

文章的话题是“攻击性行为”。

文章从第二段开始分成了三大类,分别是三种理解“攻击性行为”的方法:The Biological Approach(生物学方法),The Psychodynamic Approach(心理动力学方法)和The Cognitive Approach(认知方法)。

不仅如此,生物学方法里面还讨论一个分支:Sociobiology(社会生物学)。

这篇文章的结构一目了然,因为文章本身就把每种方法用粗体字的方式标示出来。

除了《Aggression》之外,我们会发现官方指南的《Geology and Landscape》、TPO13的《Types of Social Groups》、TPO16的《Planets of Our Solar Systems》、TPO17的《Symbiotic Relationships》还有TPO20的《Fossil Preservation》,文章的大体结构都是分类。

其实当我们把上面的文章读完之后,就会发现《Types of Social Groups》和《Planets of Our Solar Systems》这两篇文章只分出两类,结构更接近比较,因为文章内容对分出的两种类型在很多方面都做了不同的比较。

当一篇文章有两个话题,并且对两个话题在诸多方面做了比较,文章的总体结构属于比较。

官方指南的《Applied Arts and Fine Arts》是典型的比较文章。

文章的话题分别是“应用艺术”和“精细艺术”,主要的内容就是对这种两种艺术在不同方面进行比较。

《Artisan and Industrialization》是比较文章,比较的是工业化之前技工(artisan)的工作状况和工业化之后工人(worker/laborer)的工作状况。

托福TPO阅读39原文+题目

托福TPO阅读39原文+题目

小编为托福考生们准备了托福阅读TPO39原文,希望各位考生们在TPO真题里能够得到锻炼,祝广大托福考生能够取得理想成绩。

Origins of the MegalithsSince the days of the earliest antiquarians, scholars have been puzzled bythe many Neolithic (~4000 B.C.~2200 B.C.) communal tombs known as megalithsalong Europe's Atlantic seaboard. Although considerable variations are found inthe architectural form of these impressive monuments, there is a generaloverriding similarity in design and, particularly, in the use of massivestones.The construction of such large and architecturally complex tombs byEuropean barbarians struck early prehistorians as unlikely. The Bronze Ageseafaring civilizations that lived in the region of the Aegean Sea (~ 3000 B.C.~ 1000 B.C.), among whom collective burial and a diversity of stone-built tombswere known, seemed a probable source of inspiration. It was suggested thatAegean people had visited Iberia in southwestern Europe in search of metal oresand had introduced the idea of collective burial in massive tombs, which thenspread northward to Brittany, Britain, North Germany, and Scandinavia.Radiocarbon dates for a fortified settlement of megalith builders at LosMillares in Spain appeared to confirm this picture, though dates for megalithsin Brittany seemed too early. When calibrated, however, it became clear thatradiocarbon dates were universally too early to support a Bronze Age Aegeanorigin. It is now clear that the megaliths are a western and northern Europeaninvention, not an introduced idea. Even so, they are still a subject ofspeculation and inquiry. What induced their builders to invest massive effortsin erecting such monumental tombs How was the necessary labor force assembled What underlies their striking similaritiesOne answer to the last question was proposed by Professor Grahame Clark,one of Britain's greatest prehistorians. Investigating the megaliths of southern Sweden, he noted that one group was concentrated in coastal locations from which deep-sea fish such as cod, haddock, and ling could have been caught in winter. Historically, much of the Atlantic was linked by the travels of people who fished, and this could well have provided a mechanism by which the megalith idea and fashions in the style of tomb architecture spread between coastal Iberia, Brittany, Ireland, western England and Scotland, and Scandinavia. The high concentrations of megaliths on coasts and the surprising number of megaliths found on small islands may support a connection with fishing.Professor Colin Renfrew of the University of Cambridge, England, however, views the similarities as similar responses to similar needs. At the structural level, the passage that forms a major element of many graves could have been devised independently in different areas to meet the need for repeated access to the interior of these communal tombs. Other structural resemblances could be due to similarities in the raw materials available. In answer to the question of why the idea of building monumental tombs should arise independently in a number of areas, he cites the similarities in their backgrounds.Most megaliths occur in areas inhabited in the postglacial period byMesolithic hunter-gatherers (~20000 B.C. ~ 18000 B.C.). Their adoption of agriculture through contact with Neolithic farmers, Renfrew argues, led to a population explosion in the region and consequent competition for farmland。

超基性岩同生镍矿典型:甘肃金川矿床

超基性岩同生镍矿典型:甘肃金川矿床

第3期曾昭光等:老挝仙诺晚三叠世火山岩年代学及地质意义25⑷(-13.SONG Shuhe. The magma source and classification of volcanic rocks [J]. Northwestern Geology, 1973,9(4) : 1-13.范蔚茗,彭头平,王岳军.滇西古特提斯俯冲-碰撞过程的岩浆作用记录[J].地学前缘,2009,11!) (91-302.FAN Weiming,PENG Touping,W AN G Yuejun. Triassic magmatism in the southern Lancangjiang zone,south­western China and its constraints on the tectonic evolu­tion of Paleo-Tethys [J].Earth Science Frontiers,2009,16(6):291-302.寇林林,钟康惠,唐菊兴,等.昌都-思茅构造带晚三叠世构造 环境的火山岩地球化学判别[J].西北地质,2009,42(1)=79-87.KOU Linlin,ZHONG Kanghui,TAN G Juxin, et al. Geo­chemistry Discrimination of Late Triassic Volcanic Rocks in Changdu-Simao Tectonic Zone [J]. North-w esternG eology,2009,42(1): 79-87.彭平头.澜沧江南三叠纪碰撞后岩浆作用、岩石成因及其构造意义[D].北京:中国科学院研究生院,2006.PENG Touping. The Triassic post-collisional magmatism for the Southern Lancangjiang tectonic zone,southwestern China:petrogenesis and its tectonic implications [D].Beijing :The Graduate School of Chinese Academy of Sciences,2006.云南省地质矿产局.云南省岩石地层[M].北京:中国地质出 版社,2008.Yunnan Bureau of Geological and Mineral Resources. The litho-stratigraphic of Yunnan province [ M]. Beijing:Geological Publishing H ouse,2008.B A LE Y J C. Geochemical criteria for a refined tectonic dis­crimination of orogenic anZesites [J]. Chem Geol& 1981,32:139-154.超基性岩同生镍矿典型:甘肃金川矿床成矿区带:阿拉善成矿带(E-18)。

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a r X i v :a s t r o -p h /9808140v 1 13 A u g 1998Constraints on the Formation and Evolution of CircumstellarDisks in Rotating Magnetized Cloud CoresShantanu Basu Canadian Institute for Theoretical Astrophysics,University of Toronto,60St.George Street,Toronto,Ontario M5S 3H8,Canada;basu@cita.utoronto.ca.ABSTRACT We use magnetic collapse models to place some constraints on the formation and angular momentum evolution of circumstellar disks which are embedded in magnetized cloud cores.Previous models have shown that the early evolution of a magnetized cloud core is governed by ambipolar diffusion and magnetic braking,and that the core takes the form of a nonequilibrium flattened envelope which ultimately collapses dynamically to form a protostar.In this paper,we focus on the inner centrifugally-supported disk,which is formed only after a central protostar exists,and grows by dynamical accretion from the flattened envelope.We estimate a centrifugal radius for the collapse of mass shells within a rotating,magnetized cloud core.The centrifugal radius of the inner disk is related to its mass through the two important parameters characterizing the background medium:the background rotation rate Ωb and the backgroundmagnetic field strength B ref .We also revisit the issue of how rapidly mass is deposited onto the disk (the mass accretion rate)and use several recent models to comment upon the likely outcome in magnetized cores.Our model predicts that a significant centrifugal disk (much larger than a stellar radius)will bepresent in the very early (Class 0)stage of protostellar evolution.Additionally,we derive an upper limit for the disk radius as it evolves due to internal torques,under the assumption that the star-disk system conserves its mass and angular momentum even while most of the mass is transferred to a central star.Subject headings:accretion,accretion disks -circumstellar matter -ISM:clouds -ISM:magnetic fields -MHD -stars:formation -stars:pre-main-sequence1.INTRODUCTIONEver since the discovery that the planets in our solar system have nearly circular and coplanar orbits,the presence of a gaseous circumstellar disk has been thought to be intimately associated with star and planet formation.At the present time,circumstellar disks can be detected around a large number of young stellar objects(YSO’s)by a variety of techniques,including infrared excess(e.g.,Cohen,Emerson,&Beichman1989;Strom et al. 1989),measurement of their millimeter and submillimeterflux(e.g.,Beckwith et al.1990; Adams,Emerson,&Fuller1990;Ohashi et al.1991;Osterloh&Beckwith1995),and even direct optical imaging of disk silhouettes in the Orion Nebula using HST(McCaughrean& O’Dell1996).The millimeter and submillimeter measurements,which are sensitive to the outer parts of the disk,usuallyfind disk radii∼<100AU.The radii of the Orion silhouettes range from25AU to500AU.Altogether,a disk radius of∼100AU is often taken to be a typical value.However,circumstellar disks of size∼1000AU are also found around some older stars such asβPictoris.Theoretically,disks are believed to be a natural consequence of the collapse of a rotating molecular cloud core.Therefore,in principle,one should be able to derive some physical properties of a circumstellar disk directly from the properties of a cloud core in which it is formed,or even from the properties of the ambient molecular cloud in which the core itself was formed.A crucial quantity that should be derived from a collapse model is the centrifugal radius for infalling mass shells;this quantity depends certainly on the existing density and angular velocity profile near a protostar at the time that it is formed. Previous estimates of the centrifugal radius have tended to use hydrodynamic models. For example,Terebey,Shu,&Cassen(1984)have derived a centrifugal radius r c under the assumption that the core is uniformly rotating and has the static density profile of a singular isothermal sphere at the moment that a central protostar is formed.In this paper,we estimate a centrifugal radius for the collapse of a rotating,magnetized core.We use results from numerical magnetohydrodynamic(MHD)models of the formation of cores by ambipolar diffusion and magnetic braking(Basu&Mouschovias 1994,1995a,1995b,hereafter BM94,BM95a,b)and their subsequent collapse once they have a supercritical mass-to-flux ratio.The nonrotating aspects of these MHD models are discussed in detail by Fiedler&Mouschovias(1992,1993,hereafter FM93)and Ciolek& Mouschovias(1993,1994,1995,hereafter CM93,CM94,CM95).In a previous paper,(Basu 1997),we used these numerical models to build a semianalytic model for the supercritical collapse phase.Our analytic expressions for the inner solution could be extrapolated to the instant that a central protostar is formed.At this moment,labeled t=0in the terminology of isothermal similarity solutions for cloud collapse(Larson1969;Shu1977;Hunter1977),the cloud core takes the form of aflattened envelope around the protostar, with a nonequilibrium power-law radial density profile(ρ∝r−2)and supersonic infall velocity.The core is also differentially rotating,with angular velocityΩ∝r−1in the innermost region.Although the semianalytic solution applies to the time period t<0,we can extrapolate to t>0for the purpose of estimating the centrifugal radius,since angular momentum should continue to be conserved in this more dynamical phase of accretion onto the central protostar.A centrifugal radius is expected to exist during the accretion phase (t>0),even though it does not exist during the earlier runaway collapse phase(t<0).We relate the centrifugal radius r c to the disk mass m though two fundamental parameters characterizing the ambient cloud:the background rotation rateΩb,and the background magneticfield strength B ref.The mass accretion rate˙m is dependent on two other fundamental parameters:the isothermal sound speed c s and the universal gravitational constant G.However,˙m is not expected to be constant for t>0,for reasons given by Basu(1997).This has been demonstrated by recent numerical models of magnetized clouds(Tomisaka1996;Ciolek&K¨o nigl1998).We discuss the implications of several recent papers(Basu1997;Saigo&Hanawa1998;Ciolek&K¨o nigl1998;Tomisaka 1996)on the mass accretion rate,and use them to place constraints on its likely value.Once formed,or perhaps during the formation period itself,the disk is expected to undergo significant angular momentum evolution in order to give birth to star-disk systems of the type that are observed.Given the current theoretical uncertainties in understanding these processes,we present a constraint on the disk evolution if driven by internal torques (e.g.,viscous or gravitational).Regardless of the details of the process,wefind an upper limit to the disk radius if its mass and angular momentum are conserved.We also discuss how estimates of disk sizes in the early protostellar phases(before the protostar has assembled most of its mass)may help to distinguish between various collapse scenarios which yield different physical properties in the near-protostellar environment.In essence,wefind that a differentially rotating nonequilibrium pre-stellar core is necessary in order to obtain a significant centrifugal disk in the early(Class0)protostellar phase.2.Formation of an Inner Centrifugal Disk2.1.The Centrifugal RadiusIn the presence of dynamically significant magneticfields,star formation is expected to occur within aflattened cloud core aligned perpendicular to the mean magneticfield direction.FM93found that an initially magnetically subcritical(i.e.,mass-to-flux ratiobelow the critical value for collapse)cloud willfirst relax to equilibrium alongfield lines as it begins a quasistatic,ambipolar diffusion driven radial contraction toward a local density peak.This radial contraction becomes dynamic within a central region after it has achieved a supercritical mass-to-flux ratio;however,near-equilibrium is maintained alongfield lines.The supercritical regions,which are identified with molecular cloud cores,provide aflattened envelope within which stars form and grow by accretion.These disklike structures are in fact much larger(size up to∼10,000AU)than a possible inner centrifugally-supported disk,and are not in equilibrium(they are supercritical).They are also not to be confused with the“pseudodisks”of Galli&Shu(1993a,b),which form after the formation of a central protostar in a cloud that has the density profile of a singular isothermal sphere when the protostar is formed,and is threaded by a dynamically weak magneticfield.When magneticfields are dynamically significant,as implied by some Zeeman measurements(Goodman et al.1989;Crutcher et al.1993),the formation of the outer magnetic disk precedes star formation.The collapse of magnetic cores has been further investigated numerically by CM94, 95,and BM94,95a,95b,using the thin-disk approximation.Basu(1997)found analytic expressions for the inner profiles of physical variables in these collapsing cores.A natural limiting form for isothermal collapse is when a power-law density profile(established due to self-similarity in the innermost region)extends inward to radius r=0,creating a central singularity.Since afinite mass now exists at r=0,this moment is usually associated physically with the formation of a central protostar.1Basu(1997)shows that the magnetic collapse models of BM94,95a,95b typically lead to the limiting column density(integrated along the mean magneticfield direction)profilec2sσ(r)≃(2)B ref G1/2r(Basu1997),whereΩb is the ambient rotation rate of the cloud and B ref is a uniform background(or“reference”)magneticfield.This differential rotation profile is a resultof magnetic braking enforcing uniform rotationΩ≃Ωb until a critical column density is reached,and subsequent near angular momentum conservation during the rapid collapse phase,during which the column density profile of equation(1)is built up(BM94).Based on the BM94results,Basu(1997)showed that angular momentum conservation effectively begins at a column densityσcrit≃2B ref/µcrit,whereµcrit=(2πG1/2)−1is the critical mass-to-flux ratio for a magnetized thin disk(Nakano&Nakamura1978).The result is a rotation rate many orders of magnitude greater thanΩb near the cloud center.Equations (1)and(2)yield the following relation between specific angular momentum j=Ωr2and the enclosed mass m:Ωb G1/2j≃so that the integral equation for a thin-disk gravitationalfield(see equations[12]and[13] of BM94)yields g r=−2πc2s/r=−Gm/r2.When t>0,the inner near free-fall region has infall velocity v r∝r−1/2,and column densityσ∝r−1/2if the mass accretion rate˙M=−2πσrvris uniform in this region2.Theσ∝r−1/2profile does not yield the exact relation g r=−Gm/r2,but numerical integration shows that g r=−g0Gm/r2,whereg0≃0.7(Ciolek&K¨o nigl1998).Hence,during t≥0,when the column density profile isa combination of r−1/2and r−1,we expect g r=−g0Gm/r2,with g0falling in the range0.7−1.For the remainder of this paper,we simply use g r≃−Gm/r2,and not consider the multiplicative constant in front that is close to unity.Since the gravitationalfield increases less rapidly than the centrifugal acceleration during t>0,each mass shell(offixed j)hits a centrifugal barrier at a radius r c determined (to within a factor of order unity)by the relationj2r2c.(4) Incorporating equation(3),wefind the centrifugal radiusr c≃ Ωb10−14rad s−1 2 30µG1M⊙ AU.(6)The squared dependence onΩb and B ref means that r c can be quite sensitive to the actual ambient cloud conditions.The inverse dependence on B ref occurs since a stronger ambient magneticfield implies a longer subcritical phase during which magnetic braking can enforceΩ≃Ωb.The relation(5)should be used only when B ref is sufficiently strong that the core begins dynamic collapse from a magnetically critical state rotating at a background rateΩb.One may also choose to write equation(5)in terms of a critical column density σcrit(≃2B ref/µcrit;see§2.1)at which dynamical contraction begins.2.2.Self-Similarity and Dynamical Accretion from the Envelope2.2.1.Analysis of Self-Similar ProfilesThe mass m of the star-disk system grows by dynamical accretion from the nonequilibriumflattened envelope.The accretion rate(˙m)during the time t>0determines how rapidly the star-disk system is built up.Since the self-similar column density profile given by equation(1)is valid in at least an innermost region,it is worthwhile to see what predictions are made by self-similar solutions for the collapse from this profile.We make comparisons with self-similar models and discuss below the likely evolution of the mass accretion rate for t>0based on existing semianalytic and numerical models in the literature.An important property of equation(1)is that it represents a nonequilibrium column density profile,i.e.,the column density exceeds the equilibrium value.For comparison,the equilibrium solution for a non-magnetic thin disk,the singular isothermal disk(SID),isc2sσSID=gravity.The three papers by Shu&Li(1997),Nakamura&Hanawa(1997)and Basu (1997)all show that a M,T/g r=−µ−2,whereµis the mass-to-flux ratio in units ofµcrit=(2πG1/2)−1.However,theyfind slightly different values for a M,P/a T,although they are all essentially proportional toµ−2.The proportionality constant can vary due to different assumptions about the vertical structure of the cloud or inclusion in the magnetic pressure offinite-thickness corrections to the magnetic tension force,as pointed out by Shu&Li(1997).For example,Nakamura&Hanawa(1997)find that a M,P/a T=µ−2,but they do not include anyfinite thickness corrections to the magnetic tension force.Basu (1997)finds that a M,P/a T=2µ−2,since his magnetic pressure term actually incorporates afinite thickness correction term from the magnetic tension.Since the magnetic pressure force is itself an effect of thefinite-thickness of the disk,we consider the inclusion of the finite thickness magnetic tension term3a necessity.In the following discussion,we scale hydrodynamic thin-disk solutions using a M,P/a T=2µ−2,both for this reason and also because we are comparing results with the simulations of BM94,for which the analysis of Basu(1997)is most applicable.Given that detailed numerical simulations of core formation and evolution with ambipolar diffusion(e.g.,FM93;CM94;BM94)show thatµ(≃2)has approximate spatial uniformity during the late stages before protostar formation,we obtain the scaled magnetic equilibrium solution,the singular isothermal magnetic disk(SIMD),from the SID profile. Using the exact valueµ=2.1from the late stages of BM94’s standard model,wefind thatσSIMD=(1+2µ−2)2πGr≃1.88c2s3The leading term in thefinite thickness correction to the magnetic tension is proportional to B2z∇Z, where B z is the vertical component of the magneticfield,Z is the half-thickness,and∇is the gradient in the plane of the disk.This term exactly cancels out one of the terms in the total magnetic pressure,proportional to−∇(Z B2z).The canceled term is exactly−1/2times the total magnetic pressure in the late supercritical phase,so that the value of a M,P/a T calculated by Basu(1997)is exactly twice that estimated by Nakamura &Hanawa(1997).A detailed derivation of the thin-disk equations that were used by Basu(1997)can be found in CM93.4Centrifugal support is very negligible at this stage(BM94;Basu1997),and can be ignored when considering sources of support.(1969)and Penston(1969)for the runaway collapse phase(t<0),in which the density profile exceeds the SIS by the factor4.4.This solution has been extended to the accretion phase(t>0),when a central point mass exists,by Hunter(1977);we subsequently refer to the combined solution as the Larson-Penston-Hunter(LPH)solution.Given that there are an infinite number of spherical hydrodynamic similarity solutions,with the highly dynamic LPH solution and the static(at t=0)Shu solution at two extremes(Hunter 1977;Whitworth&Summers1985),it is remarkable that various numerical calculations show a convergence to the LPH solution near the cloud center(Larson1969;Hunter1977; Foster&Chevalier1993).The convergence to the LPH solution has been justified recently by Hanawa&Nakayama(1997),who performed a stability analysis of various solutions. Given this history in the hydrodynamic case,it is(at least in retrospect)not surprising that the MHD models also converge to a dynamic similarity solution.However,the similarity solution in this case is quantitatively different from LPH due to the distinctive character of self-gravity in thin-disk geometry.Basu(1997)used an approximate similarity solution(in which the self-similar profiles were predetermined by comparison with numerical simulations)to analyze the approach to self-similarity during t<0in a thin-disk magnetic cloud.There has also been recent progress infinding exact solutions to the self-similar equations for a thin disk.Here,we utilize these solutions to gain further insight into the collapse properties both before and after protostar formation.Li&Shu(1997)found a similarity solution for t>0which starts from a static SIMD profile(as given by eq.[10])at t=0,and is similar in spirit to the spherical similarity solution of Shu(1977)for the collapse of a cloud that has a static SIS profile at t=0.In contrast,Saigo&Hanawa(1998,hereafter SH)found hydrodynamic similarity solutions which exhibit dynamic collapse for t<0;they also extended these solutions to t>0.The magnetic solution can be recovered from the hydrodynamic one using the scaling laws given above.Their model also includes rotation,which leads to a centrifugally-supported inner region when t>0,as we expect based on the arguments given in§2.1.SH’s solutions all converge to a spatially uniform infall velocity and r−1 column density profile at t=0,and for t>0have an inner region with r−1/2profiles in infall velocity and column density,both characteristic of free-fall.The rotating models also have an innermost quasi-equilibrium region with zero infall velocity and r−1column density profile.The latter profile for an equilibrium centrifugal disk can also be inferred from the mass-radius relation of equation(5).SH’s solutions are parametrized by varying values of the rotation parameterω=c s j/ing equations(1)and(3),wefind that the appropriate value for a rotating,magnetized core isc sΩbω≃=0.026 c s10−14rad s−1 30µG(1−µ−2)c2s2πGr,(12)v r=−1.73(1+2µ−2)1/2c s≃−2.09c s.(13) The latter term in each case represents the scaled magnetic solution whenµ=2.1.The limiting profile of BM94(eq.[1])is within10%of the SH value,but over3times the equilibrium value.Hence,the inner regions of magnetized thin disks(where a similarity solution is expected to be valid)appear to converge to the dynamic similarity solution of SH rather than the static(at t=0)solution of Li&Shu(1997)during the approach to protostar formation The infall velocity of equation(13)agrees less well with the simulations in regions where the column density is in good agreement,but Basu(1997)points out that the infall velocity begins to converge to the self-similar value in a much smaller region(see his Figures3a and4b and associated discussion in§5.1.2).The maximum value of the infall velocity(≃−c s)does not appear to have yet reached a terminal value in the BM94 model.This late convergence of the infall velocity,relative to the column density,has also been noted by Nakamura et al.(1995,1998)In any case,a limiting infall velocity of v r≃−2c s is in agreement with the limiting(t=0−)velocity estimated by Basu(1997)if the central magnetic force becomes significantly less than thermal-pressure force,and is also in agreement with the limiting infall velocity obtained in the thin-disk magnetic collapse calculations of Nakamura et al.(1995)and the two-dimensional magnetic simulation of Tomisaka(1996).2.2.2.Expected Mass Accretion RatesThe late convergence of the infall velocity means that only the collapse of the innermost mass shells can be described by the similarity solution when extended to t>0;later mass shells will fall in at a lower rate since they start out with lower infall velocities at t=0(see further discussion in§5.1.3of Basu1997).A time-dependent accretion rate has been confirmed by Ciolek&K¨o nigl(1998)for an initially subcritical magnetic cloud in which ambipolar diffusion is operative.Additionally,Tomisaka(1996)shows that an initially supercritical magnetic cloud withflux-freezing also yields a time-dependent accretion rate. This feature was also seen in the hydrodynamic collapse calculations of Hunter(1977)and Foster&Chevalier(1993).The likely outcome of a time-dependent accretion rate has also been discussed recently by Henriksen,Andr´e,&Bontemps(1997),who present a simplified hydrodynamic model for its development.Given the reasonablefit of the SH solution,we estimate its predicted mass accretion rate for a magnetic cloud.SHfind that˙m(t<0)=6.27c3s,eff/G effand˙m(t>0)=10.96c3s,eff/G effin theirω=0solution.Therefore,scaling to to the magnetic solution usingµ=2.1yields˙m(t=0−)=6.27(1+2µ−2)3/2G≃14c3s(1−µ−2)c3sG(15)just afterwards.The former value is in good agreement with the limiting value˙m(t=0−)≃13c3s/G estimated by Basu(1997),but the latter value could not be obtained from his model which only applied to t<0.These values can be compared with the values˙m(t=0−)=29c3s/G and˙m(t=0+)=47c3s/G of the spherical hydrodynamic LPH solution.Equations(14)and(15)represent the limiting forms for the inner(where B z≫B ref) solution of BM94if the contraction continues withflux-freezing at a terminal valueµ=2.1,and also if full convergence to the scaled SH similarity solution is achieved.For comparison,if the solution converged to the SIMD profile implied byµ=2.1at t=0,the mass accretion rates would be˙m(t=0−)=0and(using the model of Li&Shu1997)˙m(t=0+)=1.05(1+H0)c3s/G≃2c3s/G,where1+H0=(1+2µ−2)/(1−µ−2)≃1.88is the overdensity factor supported by magneticfields(see eq.[10]).The t=0−limit of the BM94 simulation is betterfit by the scaled SH solution;the nonequilibrium column density is in good agreement and the magnitude of the infall velocity is far above zero,although still a factor∼2below the limiting SH value when the simulation ends.Despite the reasonable agreement of the BM94simulation with the scaled SH solution for t=0−,there is much important physics that is left out of aflux-frozen thin-disk similarity solution,as discussed below.In reality,ambipolar diffusion plays an important role in the supercritical collapse phase.Basu(1997)showed that the mass-to-flux ratio increases as a weak power of thecolumn density during t<0:µ∝σǫ,(16) whereǫ≃0.05when using the simplified ionization model of BM94.He also showed that this significantly reduces the level of magnetic support a M/|g r|∝σ−2ǫ,so that the contraction of the initially near-equilibrium core becomes increasingly dynamic.However, the estimate of equation(14),which assumes constantµ,is expected to be reasonably good since much of the innermost1M⊙in the supercritical core is in regions withµ≃2. When t>0,Ciolek&K¨o nigl(1998)have shown that ambipolar diffusion has an even more dramatic effect;an increased magnetic tension force in the vicinity of the newly formed protostar halts the inward advection of magneticfield lines and ions,even as the neutral particles tend to continue their infall.This results in a hydromagnetic shock at a larger radius where the ions and neutrals become better coupled(see also Contopoulos, Ciolek,&K¨o nigl[1998]for a semianalytic treatment).Ciolek&K¨o nigl(1998)find that ˙m(t=0+)≃6c3s/G.The discrepancy with the estimate on the far right hand side of equation(15)is accounted for by three factors:1)the mean mass-to-flux ratioµin their supercritical core is somewhat higher than in the model of BM94,2)the infall velocity magnitude is∼c s rather than∼2c s when the central zone is converted to a sink cell,and 3)the retarding effect of the ambipolar diffusion induced hydromagnetic shock.In regard to point2)above,Ciolek&K¨o nigl(1998)dofind that the maximum value of the infall velocity is still increasing when a sink cell is introduced at a central density n n,c≈1011 cm−3,when non-isothermal effects are expected to become significant.Hence,it has not yet reached a terminal value,as expected if full convergence to an isothermal similarity solution has occurred.This raises the interesting point that nature may not provide enough dynamic range between cloud core densities and the formation of a dense opaque core for the infall velocity to fully converge to that of the SH isothermal similarity solution.The previous discussion highlights the important fact that increasingly better understanding of the innermost regions of star-forming cores will depend crucially on detailed understanding of the microphysics of the attachment of neutral particles to the magneticfield and also of the conditions under which opacity effects become important and a hydrostatic stellar core is formed.This will lead to increasingly more accurate estimates of˙m at and near t=0.5Based on current thin-disk MHD numerical solutions, we conclude that the solutions are converging to a dynamic thin-disk similarity solution (approximately a scaled SH solution),but that the departure fromflux-freezing has two effects:1)it accelerates the collapse somewhat during t<0by increasing the mass-to-fluxratioµ(Basu1997),and2)it significantly decelerates infall during t>0for mass shells that start collapse outside the hydromagnetic shock caused by rapid ambipolar diffusion in the innermost region(Ciolek&K¨o nigl1998).All in all,the detailed physics is too complicated to be described by a single similarity solution.The numerical simulations must guide us in the right direction.It is also worth remembering that the vertical equilibrium assumption of the thin-disk approximation is expected to break down in the vicinity of the protostar,where dynamical infall takes place. Here,the mass accretion will occur in the vertical direction as well,so that the thin-disk accretion rates,including the simulated value of Ciolek&K¨o nigl(1998),must be regarded as lower limits to the actual value.Indeed,Tomisaka(1996)found a mass accretion rate ˙m(t=0+)≈40c3s/G in his two-dimensional axisymmetric MHD calculation,very close to the LPH value.This simulation does include vertical infall,and the initial cloud is magnetically supercritical,unlike the model of Ciolek&K¨o nigl(1998).Furthermore,it does not include ambipolar diffusion,which acts to significantly retard the accretion rate at this stage.Altogether,we believe that the true accretion rate must lie somewhere between the Ciolek&K¨o nigl(1998)and Tomisaka(1996)values,withc3s˙m(t=0+)∼>10K¨o nigl1998).The mass accretion rate can actually decrease even further if and when the core mass is exhausted.The mechanism for ultimately terminating the accretion,whether due to a limited mass supply or the effect of outflows from the YSO,remains an unsolved problem.3.Constraints on Disk EvolutionA centrifugal disk that is formed in the manner described in§2,with radius r c given by equation(5),will contain most of its matter in the outer disk.For typical parameters, less than1%of the mass will fall directly onto the star.Hence,star formation requires that the bulk of the protostellar material accrete through an initially self-gravitating centrifugal disk.In order to accrete onto the central star,most mass shells must shed the bulk of their angular momentum.Despite significant uncertainties in determining disk masses,or even the central star mass,various determinations yield YSO disk masses which are about an order of magnitude below the stellar mass(see reviews by Beckwith&Sargent1993;Mundy1997).This implies that the phase of a massive disk around a YSO is relatively short lived,and that an efficient process is available for transferring most of the system mass onto the central star.The accretion may be driven by angular momentum loss from the outer disk via a disk wind(e.g.,K¨o nigl1989;Pelletier&Pudritz1992).Alternatively,if outflows are generated within the innermost part of the disk,nearby or at the star-disk interface,then the outer mass shells mustfind some other means to shed their angular momentum.This can still be accomplished by internal redistribution of angular momentum within the disk.In the remainder of this paper,we assume that the disk evolution is driven by internal torques; either viscous or gravitational.Gravitational torques may dominate in the early stages, when the disk mass is greater than or comparable to the stellar mass.These can be driven by nonaxisymmetric spiral instabilities(e.g.,Cassen et al.1981;Heemskerk,Papaloizou,& Savonije1992;Laughlin&Bodenhiemer1994;Laughlin&Rozyczka1996),which may,if the instability is severe enough,also result in the formation of a secondary star,as argued by Adams,Ruden&Shu(1989).In contrast,viscous effects may induce a more gentle but steady accretion which will be the primary mover when the disk mass is less than the stellar mass.In the rest of this paper,we focus on the case of single-star formation. However,if disk instabilities lead to the formation of a close binary,the general feature of disk expansion discussed below should also be present in a circumbinary disk.In either the gravitational or viscous case,the inward transport of mass also requires。

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