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认知语言学第三章隐喻与转喻

认知语言学第三章隐喻与转喻

突显原则(principle of prominence)
人们的注意力更容易观察和记忆事物比较突显的方面。
相似原则&顺接原则是隐喻的认知原则。 接近原则&凸显原则是转喻的认知原则。
好的语言是一种圆满的实现,能表达人的感知本 身所不能表现的事情。——查理
语言学上,把由于两个事物的特征上所存在的某 一类似之处,而用指一个事物的词来指代另一个 事物的演变方式叫做隐喻(Metaphor)。
IDEAS (or MEANINGS) ARE OBJECTS LINGUISTIC EXPRESSIONS ARE CONTAINERS COMMUNICATION IS SENDING It’s hard to get that idea across to him. It’s difficult to put my ideas into words. ARGUMENT IS WAR He attacked every week point in my argument.
常规隐喻(conventional or dead metaphors)
“……通过长期建立的常规关系而无意识进入语 言的隐喻才是最重要的。”(Ungerer & Schmid 1996: 117)
莱考夫(1980)把隐喻看做是人们思维、行为和 表达思想的一种系统的方式,即隐喻概念 (metaphorical concept or conceptual metaphor)。
Metonymy has primarily a referential function, that is, it allows us to use one entity to stand for another. […] It also serves the function of providing understanding.

William-Faulkner

William-Faulkner





the idea of a "tale told by an idiot― Benjy’s version of the Compsons' story opens the novel Quentin and Jason’s narratives display their own respective varieties of idiocy the novel is recounting the death of a family, including some of its members, as well as the decline of the traditional upper-class Southern family. This is the significance of "The way to dusty death". Faulkner later says in his speech upon being awarded the Nobel Prize in Literature that people must write about things that come from the heart, or "universal truths". Otherwise, he states, the ideas published signify nothing.




Plot introduction in the fictional Yoknapatawpha County four sections 1. Benjy Compson, a thirty-three year old man with mental retardation. 2. is set eighteen years earlier than the other three Quentin Compson, a Harvard-educated student 3.cynical, embittered brother, Jason 4. Dilsey , a third-person-limited-omniscient narrative point-of-view Many passages are written in a stream of consciousness. This novel is a classic example of the unreliable narrator technique.

听力教程3第二版unit7听力原文

听力教程3第二版unit7听力原文

听力教程3第二版unit7听力原文UNIT 7Section one Tactics for ListeningPart 1 Spot DictationMeet Your ChiropractorThe doctor of chiropractic (D.C.) is a (1) well-recognized member of the health team who (2) considers the human body as a total functioning (3) unit and gives special attention to the spine, (4) muscles, nerves, circulatory and skeletal (5) systems. The chiropractor seeks to (6) relieve pain.The procedures utilized are primarily focused on the (7) spine. The chiropractor is concerned about the spine's relationship to the (8) nerve system, which controls important body functions. The chiropractor knows that a malfunctioning* spinal joint can not only cause (9) back pain or headaches, it can also (10) interfere with the nerves leading from the spine, thereby (11) affecting other portions of the body.Millions of Americans are chiropractic patients for a wide variety of (12) health disorders. They depend on their chiropractor as their (13) family doctor to help them maintain their health through proper (14) diagnosis, treatment, and referral when (15) necessary.A minimum of six years of college study including internships(16) goes into the making of a chiropractic physician. Many doctors of chiropractic choose to (17) limit their practices to certain specialties, such as (18) sports injuries, nutrition, orthopedics or radiology.As a (19) licensed and regulated member of the healing arts, the doctor of chiropractic must pass a state (20) licensing boardexamination in order to practice.Part 2 listening for GistLike the "Iron Age" volunteers, Paul has also chosen to cut himself off from many aspects of modem life, not, however, as an experiment but because he feels it is a more satisfactory way to live. He is talking about his small cottage in the Welsh mountains: "And that brings me to say what is primitive about it, namely, it is anything that has to be done, and there are obviously certain basic needs of life, is 'DIY' as they say: Do it yourself. There is no labor to be had nowadays in such a remote part. Er, there are no neighbors for most of the year and so you are on your own entirely. The place itself is extremely primitive. Er, I mentioned the water. I mentioned that we now have got electricity. Er, the building itself - it's impossible to keep it clean and it's stupid to try. We try to keep it tidy, and reasonably clean. It is very difficult to keep it warm, warm enough particularly in winter and that we do by an old kitchen range with coal and wood."ExerciseDirections: Listen to the passage and find its topic sentence.The topic sentence is "The place itself is extremely primitive."Section Two Listening ComprehensionPart1 DialogueA Healthy LifeDr Martin Answay writes a column in a popular women's magazine on health problems. He is also an expert on heart disease.Q: Is there a secret to good health? I mean, is there some way we can achieve it which is not generally known?A: It certainly isn't a secret. However, there is a great deal of ignorance, even among supposedly educated people, about howto be reasonably healthy.Q: Well, what advice do you give, then?A: Vh ... to begin with, take diet. I believe that one of the greatest dangers to health in Britain and other countries ... particularly developed countries ... is the kind of food we tend to prefer.Q: Such as?A: Such as that great national institution, the British breakfast, for example, ham and eggs. Or the kind of lunch so many people in this country have: sausage and chips! Or all the convenience foods like hamburgers. Or even things we regard as "healthy", such as full-fatmilk. Or Cheddar cheese. The list is endless.Q: What's wrong with those things?A: The excessive consumption of such things leads to the overproduction of cholesterol, which in turn results in heart attack ...Q: Excuse me, but what exactly is cholesterol?A: It's a ... wax-like substance ... yellowish ... and it's produced naturally in our livers. We all need some cholesterol for survival.Q: Well, if we need it, in what way is it bad for us?A: Too much of it is bad for us. It builds up in our arteries, causing them to get narrower, so that our blood supply has difficulty in getting through ... and this, of course, can eventually end in a heart attack or stroke. The point I'm trying to make here is that, even though we all need some cholesterol in order to insulate our nerves, and to produce cell membranes and hormones, the things many of us eat and even consider healthy lead to the overproduction of cholesterol. And this is very dangerous.Q: How can we avoid this overproduction of cholesterol?A: By cutting down our consumption of animal fats: things like red meat, cheese, eggs, and so on. And by increasing our consumption of fresh fruit and vegetables, and also by eating more potatoes, rice, pasta and bread.Q: Pasta? Potatoes? But ... aren't such things fattening?A: Nonsense. It isn't pasta, potatoes or bread that makes us fat. It's what we put on such things!Cheese, Butter, Meat!Q: So anything we like, anything that's delicious, is bad for us. Isn't that what you're saying? A: Rubbish! I'm simply saying we eat too much of these things. And there are many ways of preparing delicious food without using such large quantities of animal fats.Q: Last of all, what about exercise? You recently warned against certain forms of exercise, which you said could be dangerous.A: What I said was that if people aren't used to getting regular and vigorous exercise, they should begin slowly, and not try to do too much at the beginning! I also said that certain games, such as squash, can be dangerous, particularly if you aren't used to playing them. A number of injuries are due to sudden, twisting movements that games like squash involve. Q: What kinds of exercise do you recommend, then?A: Gentle jogging, swimming, cycling, brisk walking ... exercise that is rhythmic and gentle, and above all, sustained. That is, done for at least fifteen minutes uninterruptedly at least three times a week. We all need such exercise, and the fact is that far too few of us get enough of it, particularly if we live in large cities and regularly use cars.ExerciseDirections: Listen to the dialogue and complete the following grids.A. CholesterolB. ExercisePart 2 PassageAging of America1)The impending collision between the boomers and thenation's retirement system is naturally catching the eye of policymakers and the boomers themselves.2)Retirement income security in the United States has traditionally been based on the so-called three-legged stool: Social Security, private pensions, and other personal saving.3)Retirement planning takes time, and these issues need to be addressed sooner rather than later.4)One found that in 1991 the median household headed bya 65-69-year-old had financial assets of only $14,000, but expanding the measure to include Social Security, pensions, housing, and other wealth boosts median wealth to about $270,000.5)Only one or two generations of Americans have had lengthy retirements, and the crucialretirement issues keep changing rapidly, making long-term predictions even harder.The Baby Boom* generation - the roughly 76 million people born between 1946 and 1964-has been reshaping American society for five decades. From jamming the nation's schools in the 1950s and 1960s, to crowding labor markets and housing markets in the 1970s and 1980s, to affecting consumption patterns almost continuously, boomers have altered economic patterns and institutions at each stage of their lives.Now that the leading edge of the generation has turned 50, the impending collision between the boomers and the nation's retirement system is naturally catching the eye of policymakers and the boomers themselves.Retirement income security in the United States has traditionally been based on the so-called three-legged stool: Social Security, private pensions, and other personal saving. SinceWorld War II the system has served the elderly well: The poverty rate among elderly households fell from 35 percent in 1959 to 11 percent in 1995 .Are the baby boomers making adequate preparations for retirement? In part, the answer depends on what is meant by "adequate". One definition is to have enough resources to maintain pre-retirement living standards in retirement. A rule of thumb* often used by financial planners is that retirees should be able to meet this goal by replacing 60-80 percent of pre-retirement income. Retired households can maintain their pre-retirement standard of living with less income because they have more leisure time, fewer household members, and lower expenses. Taxes are lower because retirees escape payroll taxes and the income tax is progressive. And mortgages have, for the most part, been paid off. On the other hand, older households may face higher and more uncertain medical expenses, even though they arecovered by Medicare.From a public policy perspective, assuring that retirees maintain 100 percent of pre-retirement living standards may be overly ambitious. But should policymakers aim to ensure that they maintain 90 percent of their living standards? Or that they stay out of poverty? Or use some other criterion? Retirement planning takes time, and these issues need to be addressed sooner rather than later.A second big question is how to measure how well baby boomers are preparing for retirement. Studies that focus only on personal saving put aside for retirement yield bleak conclusions. One found that in 1991 the median household headed by a 65-69-year-old had financial asset of only $14,000. But expandingthe measure to include Social Security, pensions, housing, and other wealth boosts median wealth to about $270,000.A third issue - crucial but as yet little explored - is which baby boomers are not provided adequately for retirement and how big the gap is between what they have and what they should have. Some boomers are doing extremely well, others quite poorly. Summary averages for an entire generation may not be useful as descriptions of the problem or as suggestions for policy.The uncertain prospects for the baby boomers in retirement are particularly troubling because, as a society, we as yet understand little about the dynamics of retirement. Only one or two generations of Americans have had lengthy retirements, and the crucial retirement issues - health care, asset markets, Social Security, life span - keep changing rapidly, making long-term predictions even harder.Exercise A Pre-listening QuestionAs China's aging population is increasing rapidly, there should be a well-funded pension system put in place. However, the country's pension system only covers a fraction of the work force. It predicts that China will have an elderly population of about 400 million by 2040, which will be a large burden on the economy if an effective pension system is not established.The Chinese government, aware that the old pension system in the planned economy could not keep pace with the market economy, started to reform a purely "pay-as-you-go" pension system in 1997 and introduced one that combines a basic pension with personal savings accounts. The accounts are jointly paid into by employers and employees, as saving to support employees' retirements. The state is considering expanding a reformed pension insurance system nationwide.China is also accelerating the reform of China's pension system.It has been trying to find appropriate ways to invest pension funds in the capital market rather than simply putting them in banks or buying treasury bonds.It has also been trying to find appropriate ways to invest pension funds in the capital market overseas.To ensure the maintenance and appreciation of the pension pool, more investment tools should be allowed, with sound governance and parallel reform in the financial sector to ensure returns.Exercise B Sentence DictationDirections: Listen to some sentences and write them down. You will hear each sentence three times.Exercise C Detailed ListeningDirections: Listen to the passage and choose the best answer to complete each of the following sentences.l.D 2.D 3. B 4.B 5.C 6.C 7.A 8.CExercise D After-listening DiscussionDirections: Listen to the passage again and discuss the following questions.1)The boomers have altered economic patterns from jamming the nation's schools in the 1950s and 1960s, to crowding labor markets and housing markets in the 1970s and 1980s, to affecting consumption patterns almost continuously.2)(Open)Section 3 NewsNews item 1You are what you eat, the saying goes. And now it appears you are also what your mother ate.Researchers are learning more about how a pregnant mother’s diet can affect her child’s health long after the child is born. The latest research shows that some of those effects can begin within days of conception.Women are encouraged to starting taking prenatal vitamins and watching what they eat as soon as they learn they are pregnant, to help ensure a healthy baby. But it appears that maternal health before pregnancy also has an impact.Professor Tom Fleming and his colleagues fed mice and rats a low-protein diet for three-and-a-half days after the animals had mated.Fleming compared their offspring to the babies of animals fed a normal, higher-protein diet for those three and a half days. The young rodents from the low-protein group had higher blood pressure and were more hyperactive than the control group.Another study found that animals with vitamin B deficiencies in the very early days of pregnancy also has offspring with higher blood pressure. These young animals tended to be obese and were at risk for diabetes. So F leming says it’s best to eat right if you’re even thinking about getting pregnant.This news item is about the impact of mother’s diet on baby even before pregnancy.T F F T F T T FNews item2UN VaccineWhile the latest vaccines are available to children in the developed world, the situation is very different in poorer countries. According to a joint report by the World Health Organization, the World Bank and the UN Children’s Fund, just 50% of children in sub-Saharan Africa are immunized in their firstyear of life against diseases like tuberculosis, measles, tetanus, and whooping cough.The report says in some developing countries fewer than one in twenty children arevaccinated.Dr. Paul Fife of UNICEF says many developing countries are not able to buy vaccines that are widely available and even discounted in the industrialized world. He says UNICEF, the single largest buyer of vaccines for children, is also finding difficulty locating the needed medicines.The head o f the World Health Organization’s vaccine program, Dr. Daniel Tarantola, says one way to address the vaccine shortage is for more production in the developing world.The report says that although the market for vaccines in developing countries is potentially huge, with more than 130 million children born there each year, drug companies target most of their vaccines to the countries of the developed world.This news item is about the shortage of vaccines in developing countries.Vaccines are not available to children in many developing countries, just 50 percent of children in sub-Saharan Africa are immunized in their first year of life against diseases. In some developing countries fewer than one in twenty children are vaccinated.Many developing countries are not able to buy vaccines that are widely available, and even discounted in the industrialized world. One way to address the vaccine shortage is for more production in the developing countries.Although the market for vaccines in developing countries is potentially huge, with more than 130 million children born thereeach year, drug companies target more of their vaccine to the countries of the developed world.News item3Closer to home…an experimental AIDS vaccine has proved partly effective in a test involving 16000 volunteers in Thailand.For a variety of reasons, HIV--- the virus that causes AIDS--- has stymied efforts to develop a vaccine, and this new vaccine was only about 31 percent effective, according to the researchers. Tha t’s not great, but it is the best result yet, and the limited success may help researchers improve its effectiveness.U.S. Ambassador to Thailand Eric John noted the significance of the vaccine trial.“There will be more studies of this vaccine regimen, an d perhaps other vaccines tested…. This trial will be recognized as a testament to Thailand’s ability to successfully execute a complicated vaccine trial, the largest ever attempted, that ended with a credible conclusion, and that brought us one step closer to an HIV vaccine.”Even if the vaccine only modestly reduces a person’s risk of developing AIDS, it could play an important role in combating the disease, which the United Nations estimates killed two million people in 2007.Exercise A: Listen to the news item and complete the summary.This news item is about an AIDS vaccine test in Thailand which shows some promise in combating the disease.Exercise B: Listen to the news again and answer the following questions.1. What has an experiment AIDS vaccine proved in a test in Thailand?An experimental AIDS vaccine has proved partly effective ina test in Thailand.2. Why is it not easy to develop a vaccine?Because of a variety of reasons. HIV has stymied efforts to develop a vaccine.3. To what extent was this new vaccine effective according to the researchers?This new vaccine was only about 31 percent effective.4. What may the limited success help researchers do?The limited success may help researchers improve its effectiveness.5. Is this vaccine trial the largest ever attempted?Yes, it is the largest ever attempted.6. How many people were likely by AIDS in 2007?The United Nations estimates that AIDS killed two million people in 2007.。

A high resolution record of vegetation and environmental variation

A high resolution record of vegetation and environmental variation

A high resolution record of vegetation and environmental variation through the last ∼25,000years in the western part of the Chinese Loess PlateauH.N.Wu a ,b ,Y.Z.Ma c ,Z.-D.Feng a ,d ,⁎,A.Z.Sun e ,C.J.Zhang a ,F.Li a ,J.Kuang aaMOE Key Laboratory of West China's Environmental System,Lanzhou University,Lanzhou 730000,China bGansu Provincial Water Resources and Hydropower School,Lanzhou 730020,China cState Key Laboratory of Earth Surface Processes and Resource Ecology,Beijing Normal University,Beijing 100875,China dDepartment of Geology,Baylor University,Waco,TX 76798,USA eSchool of Geography Science,Southwest University,Chongqing 400715,Chinaa b s t r a c ta r t i c l e i n f o Article history:Received 30July 2008Received in revised form 12December 2008Accepted 21December 2008Keywords:Loess plateau MIS 2Holocene Pollen recordVegetation historyWe present a high-resolution reconstruction of vegetation and environmental changes from a 40-m thick section in the western part of the Chinese Loess Plateau in attempt to reveal the details of the MIS 2and MIS 1climate variations.Our data show that a desert steppe occupied the landscape between ∼24,500and ∼13,60014C yr BP.Two episodes of further vegetation deteriorations occurred between ∼20,000and ∼17,10014C yr BP and between ∼15,100and ∼13,60014C yr BP,corresponding to the Heinrich events 2and 1.The late glacial stage between ∼13,600and ∼988014C yr BP included four sub-stages that correspond chronologically and climatologically to the European deglacial sub-stages.The first sub-stage (∼13,600to ∼12,40014C yr BP)corresponds to the Bølling warm period;the second sub-stage (∼12,400to ∼11,50014C yr BP)to the Older Dryas cold period;the third sub-stage (∼11,500to ∼10,70014C yr BP)to the Allerød warm period;and the fourth Sub-stage (∼10,700to ∼988014C yr BP)to the Younger Dryas cold period.The early –mid Holocene (∼9880to ∼437014C yr BP)was a period when a forest steppe dominated the landscape under a warm and wet climate.During this period,eight cool and dry spells occurred at ∼972014C yr BP (E1),∼938014C yr BP (E2),∼887014C yr BP (E3),∼866014C yr BP (E4),∼844014C yr BP (E5),∼8240to ∼806014C yr BP (E6),∼7120to ∼655014C yr BP (E7),and ∼5640to ∼512014C yr BP (E8).After a major deterioration in vegetation between ∼4370to ∼327014C yr BP,the study area experienced improved moisture conditions between ∼3270to ∼145014C yr BP,followed by a persistent deterioration of vegetation under a drying climate during the past ∼1500years.©2009Elsevier B.V.All rights reserved.1.IntroductionThe past ∼25,000years,which covers the last two complete marine isotope stages (i.e.,MIS 2and MIS 1),witnessed the most dramatic climatic changes of global scale during recent geologic history.Speci fically,the Earth's climatic systems of the past 25,000years experienced the Last Glacial Maximum at ∼20,000yr BP,the extremely unstable late glacial climatic oscillations between ∼15,000and ∼10,000yr BP,and then the Holocene Climatic Optimum at ∼6000yr BP (Bradley,1999;Ruddiman,2008).Although we have learned a lot about the climate changes of this period through several international programs (e.g.,CLIMAP,1981;COHMAP,1988),we need to further improve our understanding of regional climatic variations (Ruddiman,2008).In that regard,the Chinese Loess Plateau,where the study area (i.e.,the Zulihe River Basin)is located,is situated at an extremely important location.First,the high-latitudinal continent-originated winter monsoon is considered to have dominated the interactions between the winter and summer monsoons during MIS 2(from ∼25,000to ∼10,000yr BP)(Zhou et al.,1996).Second,the low-latitudinal ocean-originated summer monsoon is shown to have dominated the interactions during MIS 1(the past ∼10,000years)(An et al.,2000).Third,violent interactions between the winter and summer monsoons are considered to have characterized the late glacial period between ∼15,000and ∼10,000yr BP,although only few records support this characterization (e.g.,Zhou et al.,1999).In addition,the climatic systems of this period are also demonstrated to have changed on millennial –centennial scales (Bond et al.,1997,2001)and these changes have been well documented in the North Atlantic area at higher latitudes (McManus et al.,1994;Oppo et al.,2003)and also in the Yangtze River Basin at lower latitudes (Wang et al.,2001,2005).It is apparent that the need is pressing to investigate regional responses to these millennial –centennial scale climate changes in the western part of the Chinese Loess Plateau in middle latitudes to explore the geographic coherence of these changes.Environmental and vegetation changes have been one of the foci for studying the global conditions within and between differentPalaeogeography,Palaeoclimatology,Palaeoecology 273(2009)191–199⁎Corresponding author.Department of Geology,Baylor University,Waco,TX 76798,USA.Tel.:+12547102194;fax:+12547102673.E-mail address:zhaodong_feng@ (Z.-D.Feng).0031-0182/$–see front matter ©2009Elsevier B.V.All rights reserved.doi:10.1016/j.palaeo.2008.12.023Contents lists available at ScienceDirectPalaeogeography,Palaeoclimatology,Palaeoecologyj o u r n a l h om e p a g e :w w w.e l sev i e r.c o m /l o c a t e /p a l a e oclimate states and also for assessing land–air interactions under different vegetation conditions during different climate states(Bridg-man and Oliver,2006).Unfortunately,high-resolution and well-dated pollen records are rarely available from the Chinese Loess Plateau, especially for the period between25,000and10,000years.The best early pollen work was undertaken by Sun et al.(1995),who analyzed over300pollen samples(with6conventional14C dates and2TL dates)for the period covering the last∼100,000years from a Weinan loess section(34.4°N and109.5°E)in the southeastern part of the Chinese Loess Plateau.Recently,Feng et al.(2007)analyzed over260 pollen samples covering the period between∼50,000and ∼10,000years(with20AMS14C dates)from a Jingning lacustrine–wetland–eolian section(35.5°N and105.9°E)in the western part of the Chinese Loess Plateau.MIS1of the Chinese Loess Plateau is better palynologically studied than MIS2.Li et al.(2003)established a high-resolution Holocene pollen sequence from a Yulin sand–loess–peat section(37.5°N and 108.5°E)in the northeastern part of the Chinese Loess Plateau with 120pollen samples and23AMS14C dates.In the western part of the Chinese Loess Plateau,three high-resolution and well-dated Holocene loess–paleosol sequences have been recently established by Feng and his colleagues(Feng et al.,2004,2006;Sun et al.,2007).First,105 pollen samples with a chronological support of8AMS14C dates were analyzed at a Dingxi Lacustrine–wetland and loess–paleosol sequence (32.5°N and104.5°E).Second,250pollen samples with a chronological support of9AMS14C dates were analyzed at a Qin'an(i.e.,DDW site in Fig.1)wetland–fluvial and loess–paleosol sequence(35.1°N and105.9°E).Third,210pollen samples with a chronological support of9AMS14C dates were analyzed at a Haiyuanfluvial–loess–paleosol sequence.Here,we present a high-resolution reconstruction of environ-mental variations and associated vegetation changes,based on711pollen samples and1914C dates,from a40-m thick lacustrine–fluvial–eolian sequence at Xiaogou section(36.1°N and104.9°E)in the western part of the Loess Plateau(Fig.1)in attempt to reveal the details of the MIS2climate changes and to further confirm the temporal patterns of the Holocene climatic changes documented at other sites. It is expected that this research will add a piece of valuable infor-mation to improving our understanding of the large-scale mechanisms that control or modulate the climate changes during recent geologic history.2.Physiographic settingsThe study area is the Zuli River Basin where the Zuli River is joined by the major branch(namely Guanchuan River)and then drains to the Yellow River.The studied section(i.e.,Xiaogou section)is located on the river near the outlet of the basin(Fig.1).The terrain of the study area is undulating with the elevations ranging from1500to2000m. The climate is characterized by cold and dry winters and warm and wet summers.The mean annual temperature is∼9°C at the lowest (northern)end of the basin and gradually decreases to∼4°C at the highest(southern)end.The mean annual precipitation is more than 500mm in the southern end and gradually decreases northward to only250mm at the northern end.All of natural forests and most of natural shrubs have been cleared and the present vegetation is basically a mixture of the remnant natural and introduced grasses.The remaining natural herb component includes Stipa spp.,Agropyron cristatum,Artemisia frigida and Thymus mongolicus,and the remaining natural shrub component mainly consists of Ajania fruticulosa,Lycium chinensis,Nitraria sibirica and Reaumuria soongarica.There are small patches of secondary forest(primarily Populus davidiana,Betula platyphylla,Pinus tabulaeformis,and Picea crassifolia)in the nearby mountains(e.g.,Huajialing Ridge and Quwu Mountain)wheretheFig.1.Map of the western part of Chinese Loess Plateau and location of the studied section(i.e.,Xiaogou section)within the major trunk watershed of the Zulihe River Basin(dashed-line circled area).192H.N.Wu et al./Palaeogeography,Palaeoclimatology,Palaeoecology273(2009)191–199available moisture is higher than the surrounding low-elevation loess terrains (Wu,1980;Huang,1997)boratory methods and stratigraphy boratory methodsThe sampling interval was 6cm for pollen analysis and 4cm for grains-size and total organic carbon analyses.For pollen analysis of 711samples,exotic Lycopodium tablets were first added for calculation of pollen concentration (Moore et al.,1991;Wang et al.,1995),and the samples were then treated with HCl (10%)and HF(39%).More than 300pollen grains (excluding spores)were counted and identi fied for most samples.The raw pollen data are expressed as percentages of the sum of terrestrial pollen and are plotted against depth using Grapher 2.0(Duane et al.,1990).The particle size of bulk samples was measured using a Malvern laser diffraction grain size analyzer and the total organic carbon (TOC)content was measured with titration methods (see Singer and Janitzky,1987).3.2.Stratigraphy and chronologyThe 40-m thick studied section (i.e.,Xiaogou section)is a natural exposure of a lacustrine –fluvial –eolian sequence and the lacustrine –fluvial portion (4000–256cm deep)was formed at the outlet of the basin between ∼25,000and ∼145014C yr BP under a completely closed terminal lake when the Zuli River was dammed by a massive landslide,according to our field investigations.The eolian portion ofthe section (256–0cm deep)was formed during the past ∼1500years (Fig.2).We obtained 9AMS 14C dates on charcoal samples (Table 1)that were measured at the NSF-AMS Facility at the University of Arizona (USA)and 10conventional 14C dates of bulk organic-rich samples (Table 2)that were measured at the MOE Key Laboratory of Lanzhou University (China).It should be particularly mentioned that four charcoal AMS 14C dates from the top portion (0–1300cm)seem to be in a perfect order and five bulk conventional 14C dates from the bottom portion (2600–4000cm)are reasonably acceptable (Fig.2).But,we were originally frustrated by the five similar charcoal AMS 14C dates between 2100and 2900cm (i.e.,open diamonds in Fig.2).The dates vary very little,ranging between ∼9170and ∼981014C yr BP within the 8-m thick sediment (2100–2900cm).We then dated five bulk organic-rich samples between 1600and 2600cm (filled diamonds in Fig.2)and again the dates refused to vary withdepth,Fig.2.Diagram showing the stratigraphy and associated 14C dates of the Xiaogou lacustrine –fluvial –eolian section.Also included are photos of six representative segments,medium grain size data (μm)and 14C dates-based age-depth model.Table 1AMS 14C dates of Xiaogou section Lab no.Depth (cm)δ13C (‰)14C age (yr BP)AA64267152–154−20.0803±40AA64268674–675−19.54033±44AA642701036–1037−23.06412±56AA642721258–1259−24.08039±72AA642752132–2133−26.79171±50AA642762226–2228−26.69292±79AA642772475–2478−25.39393±49AA642782674–2676−26.69210±110AA642792874–2876−25.89807±52193H.N.Wu et al./Palaeogeography,Palaeoclimatology,Palaeoecology 273(2009)191–199ranging between∼9780and∼11,26014C yr BP within the10-m thick sediment(1600–2600cm).We thought of the possibility that the organic-rich sediments formed at∼10,00014C yr BP in the entire basin or along the river banks might have been the source of the dated organic-rich sediments and the sediments between1600and2900cm were just reworked from the source sediments.However,our speculation was immediately rejected by the fact that the sediments between1600and2900cm are well-laminated(see photo at ∼2200cm in Fig.2)and regularly-interbedded(see photo at ∼2500cm in Fig.2).That is,it is naturally impossible that the organic-rich sediments formed at∼10,00014C yr BP were impulsively re-transported from the source area(s)and rhythmically re-deposited in the closed terminal lake to form organic-rich and organic-poor alternating layers in this loess hilly area where upslope loess can be easily eroded and transported to the terminal lake.Our thought then went to the report that the atmosphericΔ14C instability at∼10,00014C yr BP can result in large14C-date uncertainties(Kromer and Becker, 1992;Hughen et al.,1998;Wang and Jian,1999).Whatever the reasons might be for the near-constant dates of the portion of the sediment (1600–2900cm deep),ourfield investigation excluded the possibility that this portion(1300-cm thick)of sediment was suddenly deposited from an outburst of upstream lake or from megaflood erosion of previously-deposited organic-rich layer.Subsequently,we established an age-depth model by taking these four actual AMS14C dates (solid line-indicated in Fig.2)at their face values for the upper portion (0–1300cm)and by using the polynomial regression-produced model ages(dashed line-indicated in Fig.2)for the lower portion(1300–4000cm).The model is expressed as Age=1E−06(Depth)3−0.0053 (Depth)2+11.334(Depth).It should be noted that,although all of19 dates participated in the age-depth model construction,thosefive AMS14C dates within the depths between2100and2900cm and also thosefive conventional14C dates within the depths between1600and 2600cm were greatly discounted simply because they are so clustered.In other words,those clustered10dates statistically act like one or two dates in the polynomial regression model.The section can be divided into six sediment units from the bottom to the top(Fig.2).Sediment Unit1(4000–3000cm;∼24,500to∼13,30014C yr BP) consists of interbedded layers alternating between light-grey sandy silt and brown-grey silt.It has an average medium grain size of23µm and an average deposition rate of0.09cm/yr.The unit is interpreted to be afluvially-reworked loess-dominated lacustrine–fluvial complex formed under shallow-water conditions.Sediment Unit2(3000–2000cm;∼13,300to∼947014C yr BP) consists of four interbedded∼250cm thick layers alternating between light-grey silt and brown-grey silty clay.It has an average grain size of 14µm and an average deposition rate of0.26cm/yr.The unit is interpreted to be a lacustrine facies-dominated lacustrine-fluvial complex formed under deeper-water conditions.Sediment Unit3(2000–1260cm;∼9470to∼805014C yr BP) consists of eight interbedded thin layers(∼100cm each)alternating between light-grey silt and brown-grey clayey silt.It has an average grain size of17µm and an average deposition rate of0.52cm/yr.Unit3 is also interpreted to be a lacustrine-dominated lacustrine-fluvial complex.However,there are two major differences from Sediment Unit2.First,each of the interbedded layers is thinner in Unit3than in Unit2.Second,the color is lighter and the average deposition rate is higher than that of the Unit2,probably suggesting that the upstream erosion was increased either due to increased precipitation or due to decreased vegetation coverage.Sediment Unit4(1260–780cm;∼8050to∼473014C yr BP) consists of four interbedded layers(∼125cm each)alternating between light-grey clayey silt and brown-grey or bluish silty clay.It has an average grain size of15µm and an average deposition rate of 0.14cm/yr.It is our interpretation that the brown-grey or bluish silty clay layers were formed under deeper-water conditions(see Photo of 9–10m in Fig.2)and the light-grey clayey silt layers arefluvially-reworked loess layers formed under shallower-water conditions.Sediment Unit5(780–256cm;∼4730to∼145014C yr BP)isfluvially-reworked loess-dominated lacustrine–fluvial complex containing wet-land-facies lenses(e.g.,at∼300cm depth)and has an average grain size of18µm and an average deposition rate of0.16cm/yr.Sediment Unit6(256–0cm;∼1450to∼014C yr BP)is a massive loess unit with an average grain size of16µm and an average deposition rate of0.18cm/yr.4.Pollen data and interpretation4.1.A brief review of modern pollen assemblagesA survey of modern pollen assemblages within the study area is limited in their ability to interpret fossil pollen records simply because the natural vegetation has been severely disturbed.Therefore,our interpretation of the fossil pollen records has to rely on the modern pollen-vegetation studies from other areas in China where human disturbance is minimal.The pollen spectra of a temperate deciduous forest are dominated by deciduous arboreal taxa including Quercus, Betula,Alnus,Acer,Ulmus,and Populus(9.0–50.0%)and also by Pinus (5.9–54.6%),accompanied by Artemisia(3.9–58.8%),Gramineae(1.1–10.0%)and Chenopodiaceae(1.0–11.5%)(Wang et al.,1996;Zhao et al., 1998;Xu et al.,2000,2007).It should be noted that Ulmus is normally under-represented and Quercus is proportionately represented in the modern pollen spectra of temperate deciduous forest(Zhao et al., 1998;Li et al.,2000;Ma et al.,2004;Xu et al.,2007).In a temperate steppe forest,the pollen spectra are co-dominated by the herb com-ponent(20.0–80.0%)and the arboreal component(15.0–40.0%).The arboreal component includes Pinus(5.1–42.2%),Quercus(1.1–11.9%) and Betula(0.6–17.0%),and the herb component includes Artemisia (20.8–50.6%),Chenopodiaceae(6–15.0%),and Gramineae(2.1–8.6%) (Liu et al.,1999;Ma,2004;Xu et al.,2007;Ma et al.,2008).The modern pollen spectra of temperate steppe are absolutely dominated by the herb component(62.0–93.0%)with a minor Pinus-dominated arboreal component(7.0–28.0%).The herb component includes Artemisia(36.5–80.0%),other Compositae(10–20%),Cheno-podiaceae(14.9–46.6%),and Gramineae(2.2–10.0%)(Li,1998;Liu et al.,1999).High percentages of Artemisia(20.6–55.8%)and Cheno-podiaceae(23.1–48.6%)fairly represent the dominance of these two herbaceous taxa in a temperate desert steppe where Stipa(Grami-neae)is normally under-represented(Yan and Xu,1989;Li,1998).Finally,we want to discuss the pollen representation of coniferous trees(e.g.,Pinus and Picea).Pinus pollen is normally over-represented and even up to30%of its pollen can not be interpreted as a reflection of local presence of a forest or a forest-steppe if other tree taxa are lacking(Li,1998;Ma et al.,2004).However,published data show that Picea pollen has a more realistic representation than Pinus pollen because the former(Picea pollen)is less suitable for long-distance wind transport.It is subsequently demonstrated that a relatively high percentage of Picea pollen in a terminal lake sediments of any arid orTable2Conventional14C dates of Xiaogou sectionLab no.Depth(cm)14C age(yr BP)LUG06-451426–142810,870±98LUG06-461636–16399782±118LUG06-471992–199610,487±123LUG06-482132–21369572±129LUG06-492360–236411,981±157LUG06-502628–263211,259±107LUG06-512924–292813,501±162LUG06-1003260–327219,421±191LUG06-1013720–373222,811±246LUG06-1023990–400023,243±272194H.N.Wu et al./Palaeogeography,Palaeoclimatology,Palaeoecology273(2009)191–199semiarid basin indicates that the coniferous pollen grains were fluvially transported from the montane coniferous forests within the basin (Li,1998;Zhu et al.,2001a,b;Xu et al.,2004).4.2.Pollen data and interpretationAs shown in Fig.3,the pollen spectra are dominated by Pinus ,and the average percentage of the coniferous component reaches 70.6%.The Quercus -dominated deciduous component reaches only 7.1%and the total shrub percentage (including Ephedra ,Rosaceae,Nitraria ,Elaeagnus ,Leguminasae and others)is even lower.The herb com-ponent retains its secondary representation (after the conifers)throughout the section except for Sediment Unit 6in which the herbs share dominance with the conifers.The herbs include Cheno-podiaceae,Artemisia,Aster-type,Taraxacum-type,Anthemis-type,Gramineae,Polemonium ,Polygonum ,Plumbaginaceae and Stellera.Six climate phases were reconstructed based on six pollen assemblage zones (PZs)which were recognized by visual inspection and CONISS analysis (Grimm,1987).PZ 1(4000–3045cm;∼24,500to ∼13,60014C yr BP)corresponds to the Sediment Unit 1(4000–3000cm),and the pollen assemblage is absolutely dominated by the coniferous component (mean=91%).It is noticeable that Picea shares the dominance with Pinus in this zone with an upward increasing trend of Pinus and a corresponding decreasing trend of Picea .This zone has merely detectable deciduous and shrubs with a very low percentage of herbs and with a low pollen concentration (mean=893grains/g),suggesting that a desert steppe occupied the landscape within the basin.The higher Picea percentage relative to Pinus percentage in this zone in comparison with other zones seems to suggest that coniferous tree patches might have developed in upper-stream higher-elevation areas.The climate was generally cold and dry.PZ 2(3045–2180cm;∼13,600to ∼988014C yr BP)approximately corresponds to Sediment Unit 2(3000–2000cm).The pollen assemblage is characterized by a sudden appearance of some herbs and shrubs (e.g.,Ephedra ,Chenopodiaceae,Artemisia and Taraxacum-type)and also by considerable increases of some other herbs and shrubs (e.g.,Polygonum ,Plumbaginaceae,and Stellera ).It is noticeable that the pollen concentration increased remarkably with notable fluctuations.This zone can be divided into four sub-zones.Sub-zone 2-1(3045–2844cm;∼13,600to ∼12,40014C yr BP)is typi fied by a sudden increase in herbs (including Polygonum,Plumbaginaceae,Artemisia ,Taraxacum-type,Anthemis-type and Stel-lera )at the expense of the coniferous component and also by the absence of the deciduous component.It is noticeable that the pollen concentration increased (mean=1831gains/g)relative to the PZ 1and that the coniferous component retains its dominance.This pollen assemblage and the relatively high pollen concentration re flect the replacement of the former desert steppe (PZ 1)by steppe under ameliorated climatic conditions in the basin and the coniferoustreeFig.3.Chronostratigraphy and the main pollen-types percentage diagram and the total pollen concentration diagram of Xiaogou section.195H.N.Wu et al./Palaeogeography,Palaeoclimatology,Palaeoecology 273(2009)191–199patches in the higher-elevations.The decline of Picea may suggest a milder climate,and the sudden increases in herb component and the increased pollen concentration may indicate a wetter climate.Sub-zone2-2(2844–2678cm;∼12,400to∼11,50014C yr BP)is marked by a sharp increase in Chenopodiaceae(up to20%)at the expenses of other herbs.Although the pollen concentration remains the same as that in Sub-zone2-1,the climate seems to have deteriorated as indicated by(1)a sharp increase in Chenopodiaceae, (2)an observable decrease in total herb pollen percentage,and(3)a decrease in the diversity of the detected species.This pollen assemblage is interpreted to represent a Chenopodiaceae-dominated steppe or even a Chenopodiaceae-dominated desert steppe.The climate again changed to cold and dry,probably being only slightly milder and wetter than that during PZ1.Sub-zone2-3(2678–2447cm;∼11,500to∼10,70014C yr BP)has a greater diversity of herb species than Sub-zone2-2.The considerable increases in Quercus,Ephedra and Artemisia and the corresponding drastic increase in pollen concentration(mean=5837grains/g)make this sub-zone outstanding among all of sub-zones in PZ2.This pollen assemblage is interpreted to represent a Quercus-dominated woodland steppe under a milder and wetter climate.The drastically increased coniferous pollen concentration suggests that the coniferous forests or tree patches also expanded in higher-elevation areas.Sub-zone2-4(2447–2180cm;∼10,700to∼988014C yr BP)is similar to the Sub-zone2-1in the composition of the herb component except that Chenopodiaceae and Ephedra pollen percentages are higher.Two other distinguishable features are the dramatic decrease in the pollen concentration and the nearly completely disappearance of Quercus.It seems that the woodland steppe(i.e.,Sub-zone2-3)deteriorated to a dry steppe under a colder and drier climate.The coniferous forests or tree patches in higher-elevation areas also shrank in response to the deteriorated climate.PZ3(2180–1408cm;∼9880to∼824014C yr BP),approximately corresponding to Sediment Unit3(2000–1260cm),is unequivocally characterized by a persistently high Quercus pollen percentage and also by a continuous appearance of pollen of other deciduous trees (e.g.,Betula,Corylus,Ulmus and Juglans)at the expense of the coniferous component.The pollen concentrationfluctuates dramati-cally between∼200and∼15,000grains/g with a relatively high mean (∼5000grains/g).The dramatic increase in the deciduous component and the extremely high pollen concentration are interpreted to represent a forest–steppe vegetation under a warm and wet climate.It is also noticeable that Aster types and Gramineae pollen percentages are considerably higher than those in the PZ2and that Chenopodia-ceae and Artemisia pollen percentages are also higher than those in the PZ2.The increase in the herb component(e.g.,Gramineae,Aster types,Chenopodiaceae and Artemisia)may indicate that the studied site was within the northern(i.e.,drier)portion of a forest steppe.It is also noted that there arefive intervals when both the pollen concen-tration and the percentage of deciduous component drop consider-ably,suggestingfive cool and dry spells.Thesefive cool and dry spells occurred at∼9760to∼967014C yr BP(2130–2090cm),∼9430to ∼933014C yr BP(1981–1934cm),∼8920to∼882014C yr BP(1727–1680cm),∼8700to∼862014C yr BP(1617–1580cm),∼8470to ∼840014C yr BP(1507–1475cm).PZ4(1408–725cm;∼8240to∼437014C yr BP),approximately corresponding to the Sediment Unit4(1260–780cm),is typified by an upward increasing trend of the coniferous component and a corresponding decreasing trend of the deciduous component.Shrubs (e.g.,Ephedra)and some herbs(e.g.,Chenopodiaceae,Artemisia and Gramineae)are also considerably reduced in comparison with those in the PZ3.Again,like in the PZ3,the pollen concentrationfluctuates dramatically between∼100and∼16,000grains/g with a relatively high mean(∼5000grains/g).The assemblage is also interpreted to represent a forest steppe.However,the increase in the coniferous component and the corresponding decreases in other components (deciduous,shrubs and herbs)relative to PZ3seem to suggest that the temperature was reduced and the available moisture might thus be elevated.The data indicate that there were three intervals when both the pollen concentration and the percentage of deciduous component dropped drastically,suggesting three cool and dry spells that occurred at∼8240to∼806014C yr BP(1408–1333cm),∼7120to∼655014C yr BP(1133–1055cm),and∼5640to∼512014C yr BP(918–840cm).PZ5(725–256cm;∼4370to∼145014C yr BP),approximately corresponding to the Sediment Unit5(780–256cm),is characterized by a dramatic decrease in the pollen concentration and nearly com-pletely disappearance of the deciduous component,accompanied by a slight increase in herb component.Apparently,the previous forest steppe(i.e.,PZ4)had deteriorated to a steppe under a cold and dry climate.The fact that Picea/Abies and Tsuga pollen percentages increase considerably seems to suggest an expansion of coniferous forests or tree patches in high-elevation areas.According to the secondary variation of pollen concentration and herbs composition, two sub-zones are recognized:Sub-zone5-1and Sub-zone5-2.Sub-zone5-1(725–550cm;∼4370to∼327014C yr BP)is typified by a dramatically reduced pollen concentration(mean=1009grains/g) and by a significantly increased herb component(including Cheno-podiaceae,Artemisia,Plumbaginaceae,and Stellera),suggesting that a relatively cold and dry climate prevailed.Sub-zone5-2(550–256cm;∼3270to∼145014C yr BP)is characterized by an increase in the coniferous component(mainly Pi-nus,Picea,Abies,Tsuga)and also by an increase in total pollen con-centration(mean=2219grains/g),probably suggesting an improved moisture condition relative to Sub-zone5-1.PZ6(256–0cm;∼1450to∼014C yr BP),exactly corresponding to the eolian portion of the sequence(Sediment Unit6),is charac-terized by a significant increase in the herb component(including Chenopodiaceae,Artemisia,Taraxacum-type,Aster-type,Gramineae, Polemonium,Polygonum,Plumbaginaceae and Stellera)at the expense of the coniferous component(including Pinus,Picea,Abies,Tsuga) and also by an extremely low pollen concentration(mean=635 gains/g)with the continued absence of the deciduous component. Although the biodiversity of the detected species of herbs is rather high in this zone,the extremely low pollen concentration suggests that the previous steppe vegetation(PZ5)had further deteriorated and the studied site was probably within the northern (drier)portion of a steppe.The further deterioration of the vegetation since∼48014C yr BP is most likely a result of severe human disturbances.5.Discussion and conclusions5.1.MIS2The period between∼24,500and∼13,60014C yr BP,represented by PZ1,is characterized by the following four features:(1)lowest pollen concentration(∼900gains/g);(2)the highest percentage of coniferous component(mean=91%);(3)the coarsest particle size of the sediments(mean=23μm),and(4)a rather low TOC content in the entire section(Fig.4).It means that the vegetation coverage was low in a desert steppe under a cold and dry climate.The reconstructed desert steppe vegetation further deteriorated twice during this period. Thefirst deterioration occurred between∼20,000and∼17,10014C yr BP,and the second deterioration between∼15,100and∼13,60014C yr BP.Considering the uncertainties in14C dates,these two deteriora-tions mostly likely correspond to the North Atlantic-documented (McManus et al.,1994)and Chinese Hulu cave stalagmite-corrobo-rated(Wang et al.,2001)Heinrich events H2(∼21,00014C yr BP) and H1(∼14,30014C yr BP).Thesefindings(H2and H1)are well collaborated by the pollen record from nearby Jingning lacustrine–wetland–eolian sequence(i.e.,Suancigou section)(Li et al.,2006;Feng et al.,2007).196H.N.Wu et al./Palaeogeography,Palaeoclimatology,Palaeoecology273(2009)191–199。

三体中的名词术语英文 刘宇昆

三体中的名词术语英文 刘宇昆

三体中的名词术语英文刘宇昆The Three-Body Problem by Liu Cixin has captivated readers around the world with its intricate plot and rich scientific concepts. One of the unique aspects of this acclaimed science fiction novel is the author's introduction of various specialized terms and jargon related to the fictional "Three-Body" universe. These terms not only add depth and authenticity to the narrative but also challenge readers to delve deeper into the complex ideas presented. In this essay we will explore some of the key English terminology used in The Three-Body Problem and examine their significance within the context of the story.One of the most prominent terms in the novel is "Trisolaris" which refers to the fictional three-star planetary system that serves as the primary setting for much of the narrative. The word "Trisolaris" is a combination of the prefix "tri-" meaning three and the word "solaris" meaning related to the sun. This term encapsulates the core premise of the story where a planet orbits not one but three suns, leading to extreme climatic instability and unpredictability. The chaotic nature of the Trisolaris system is a key driver of the plot as it sets the stagefor the extraterrestrial civilization's attempts to flee their doomed homeworld and seek refuge on Earth.Another important term is "sophon" which describes the mysterious and highly advanced microscopic probes sent by the Trisolarians to infiltrate and monitor human civilization. The word "sophon" is derived from the Greek word "sophos" meaning wise or intelligent. This term effectively conveys the incredible technological capabilities of the Trisolarian civilization, as these sophons are able to manipulate the fundamental particles of the universe to gather information and even influence human affairs. The sophons serve as a constant threat and source of tension throughout the narrative, highlighting the asymmetry of power between the Trisolarians and humanity.A crucial concept introduced in the novel is that of "the Sphere" which represents the boundary of the Trisolaris system's influence. This term refers to an imaginary three-dimensional sphere within which the Trisolarian civilization can effectively exert its control and disrupt the normal laws of physics. The Sphere is a crucial plot device as it defines the limits of the Trisolarians' technological superiority and the extent to which they can intervene in human affairs. The constant struggle to expand or maintain the Sphere is a central theme in the novel, as both the Trisolarians and humanity attempt to gain the upper hand in this cosmic chess match.Another notable term is "dark forest" which describes the author's vision of a hostile and unforgiving universe where civilizations must remain hidden and silent to avoid annihilation. This metaphor is used to convey the idea that in a universe teeming with intelligent life, the safest strategy for survival is to avoid drawing attention to oneself, much like a hunter hiding in a dark forest. The "dark forest" concept is a key driver of the Trisolarians' decision to seek out and destroy humanity, as they believe that by remaining hidden, they can avoid the fate that has befallen countless other civilizations.The term "cosmic sociology" is also introduced in the novel to describe the study of the relationships and interactions between different civilizations on a cosmic scale. This field of study is central to the Trisolarians' understanding of the universe and their attempts to navigate the treacherous landscape of interstellar politics. The term "cosmic sociology" highlights the novel's exploration of the broader implications of humanity's first contact with an alien civilization, and the potential challenges and consequences that such an encounter may bring.Another intriguing term is "supra-quantum computer" which refers to the Trisolarians' most advanced computing technology. This term suggests a level of computational power that transcends the limitations of traditional quantum computers, allowing theTrisolarians to perform feats of calculation and simulation that are beyond the reach of human technology. The supra-quantum computer is a crucial plot device, as it enables the Trisolarians to model and manipulate the behavior of human civilization with uncanny precision.Finally, the term "Wallfacer" is used to describe a select group of individuals tasked with devising strategies to defend Earth against the Trisolarian invasion. The word "Wallfacer" evokes the image of a defensive wall or barrier, suggesting the critical role these individuals play in protecting humanity from the extraterrestrial threat. The Wallfacers are imbued with immense power and resources, but their true plans and motivations remain shrouded in mystery, adding to the suspense and intrigue of the narrative.These are just a few of the many specialized terms and concepts that are integral to the world-building and storytelling in The Three-Body Problem. Each of these terms serves to deepen the reader's understanding of the complex scientific and philosophical ideas that underpin the novel's narrative. By exploring these terms and their significance, we gain a deeper appreciation for the richness and depth of Liu Cixin's imaginative vision, and the ways in which he has seamlessly blended scientific speculation with captivating storytelling.。

1993英语考研真题

1993英语考研真题

1993年考研英语真题精解精析1993年全国硕士研究生入学统一考试英语试题按照《1993年全国硕士研究生入学统一考试英语考试大纲(非英语专业)》要求命制,体现了《大纲》的考核目标、形式和内容。

1993年试题题型与1992年相比,题型相同,难度维持在一个水平线上。

Section ⅠCloze Test【文章综述】本文首先指出室内设计发展成一个专门领域的时间不长,但却已经很重要。

接着分析原因:一是建筑物往往具有很多功能;二是人们大部分时间是在室内度过,因此希望其环境舒适宜人。

最后介绍室内设计者关注的基本问题是室内空间的功能。

【英汉对照】Although interior design has existed since thebeginning of architecture, its development into aspecialized field is really quite recent. Interior designershave become important partly because of the manyfunctions that might be 46 in a single large building.The importance of interior design becomes 47when we realize how much time we 48 surrounded byfour walls. Whenever we need to be indoors, we wantour surroundings to be 49 attractive and comfortable aspossible. We also expect 50 place to be appropriate toits use. You would be 51 if the inside of yourbedroom were suddenly changed to look 52 the insideof a restaurant. And you wouldn’t feel 53 in abusiness office that has the appearance of a school.It soon becomes clear that the interior designer’smost important basic 54 is the function of the particular 55. For example, a theater with poor sight lines, poorsound-shaping qualities, and 56 few entries and exitswill not work for 57 purpose, no matter howbeautifully it might be 58. Nevertheless, for any kindof space, the designer has to make many of the samekind of 59. He or she must coordinate the shapes,lighting and decoration of everything from ceiling tofloor. 60 addition, the designer must usually selectfurniture or design built-in furniture, according to thefunctions that need to be served.尽管室内设计自建筑业出现之初业已存在,但它发展成为一个专门的领域的历史却不长。

Feminist movement女权运动


THREE STAGES
• First wave: 18th—early 20th centuries, women’s suffrage, end with Nineteenth Amendment to the United States Constitutions (1919)
• Second wave:1960s—1980s,gender inequality in laws and culture, “The Personal and Political” • Third wave: early 1990s, response to the perceived failures of the second wave.
This movement originated in Europe, and also it had its own background . Because at that time the European women 'status were so low. Therefore before the 17th century ,the married women in England had the right which stem from their husbands
Thank you for listening.
The second wave
• The second women’s movement in the 1960s was started by three groups of women and an accident. • 1. The first was a group of professional women who were appointed to a Commission on the Status of Women by President Kennedy in 1961. • 2. The second group were mostly white housewives and mothers who read Betty Friedan's book, The Feminine Mystique, published in 1963. 3. The third group were young activists in the civil rights and anti-war movements.

英文专业词汇学考试复习资料---精品管理资料

Chapter 1 The Basic Concepts of Words and Vocabulary1、The Definition of a WordLexicology focuses on the study of meanings and origins of words。

According to semanticists(语义学家), a word is a unit of meaning.A word is a minimal(最小的)free form of a language that has a given sound,meaningand syntactic function(句法功能).2、 VocabularyAll the words in a language make up what is generally known as its vocabulary。

3、 Sound and MeaningThe relationship between sound and meaning is no logic4、 Sound and FormThere was more agreement between sound and form in Old English than in Modern English。

With the development of the language,more and more differences arose between sound and form.(1)、What is the relationship between sound and meaning? Give examples to illustrate it.The relationship between sound and meaning is arbitrary and conventional。

雅思阅读 英文标题类填词

雅思阅读英文标题类填词Fill in the Blank: IELTS Reading Passage with English Title.Instructions: Fill in the blanks in the following IELTS Reading passage with the correct words or phrases from the options provided. Write your answers in the spaces provided after each blank.Passage:The Importance of Sleep.Sleep is essential for maintaining our physical, mental, and emotional well-being. It allows our bodies to rest and repair themselves, and it helps to clear our minds and improve our cognitive function.There are two main types of sleep: rapid eye movement (REM) sleep and non-rapid eye movement (NREM) sleep. REMsleep is characterized by rapid eye movements, increased brain activity, and dreaming. NREM sleep is divided into three stages, each with its own unique characteristics.The first stage of NREM sleep is the lightest and shortest stage. It is often referred to as the "transition stage" because it occurs as we fall asleep. The second stage of NREM sleep is slightly deeper and is characterized by slower brain waves. The third stage of NREM sleep is the deepest and longest stage. It is often referred to as "slow wave sleep" because it is characterized by very slow brain waves.The length and quality of our sleep can be affected by a number of factors, including our age, genetics, and lifestyle. As we age, our sleep patterns tend to change. We tend to get less sleep as we get older, and our sleep is often more fragmented. Genetics also plays a role in our sleep patterns. Some people are simply more likely to get a good night's sleep than others. Finally, our lifestyle can also have a significant impact on our sleep. Stress, anxiety, and lack of exercise can all interfere with ourability to get a good night's sleep.Getting enough sleep is essential for maintaining our overall health and well-being. It can help to improve our mood, boost our energy levels, and enhance our cognitive function. It can also help to reduce our risk of developing chronic diseases such as heart disease, stroke, and diabetes.Fill in the Blank:1. The two main types of sleep are REM sleep and__________________.2. The first stage of NREM sleep is often referred to as the __________________.3. The deepest and longest stage of NREM sleep is often referred to as __________________.4. As we age, our sleep patterns tend to__________________.5. ___________ can also have a significant impact on our sleep.Answer Key:1. non-rapid eye movement sleep.2. transition stage.3. slow wave sleep.4. change.5. Lifestyle.中文回答:1. 睡眠主要分为两类,快速眼动睡眠和非快速眼动睡眠。

Aquatic Animal Embryonic Stage

Aquatic Animal Embryonic Stage Embryonic development in aquatic animals is a fascinating and complex process that plays a crucial role in the survival and evolution of these species. From the moment of fertilization to hatching, aquatic animal embryos undergo a series of intricate changes that ultimately determine their growth and development into mature individuals. In this discussion, we will explore the various stages of embryonic development in aquatic animals, the factors that influence this process, and the significance of understanding these stages for conservation and research purposes. The first stage of embryonic development in aquatic animals begins with fertilization, where sperm and egg cells unite to form a zygote. This initial step is crucial for the creation of a genetically unique individual and sets the foundation for all subsequent developmental processes. In many aquatic species, fertilization occurs externally, in the water, while others may have internal fertilization mechanisms. The timing and location of fertilization can varygreatly among different aquatic animals, depending on their reproductivestrategies and environmental conditions. Following fertilization, the zygote undergoes rapid cell division through a process known as cleavage. During this stage, the embryo does not increase in size but instead divides into smaller cells called blastomeres. Cleavage is essential for the formation of a multicellular embryo and sets the stage for the next developmental processes, including gastrulation and organogenesis. The timing and pattern of cleavage can vary among different aquatic animals, reflecting their evolutionary history and ecological adaptations. Gastrulation is a critical stage in embryonic development where the three primary germ layers – ectoderm, mesoderm, and endoderm – are established. This process involves the migration and rearrangement of cells to form distinct tissue layers that will give rise to different organs and structures in the developing embryo. The formation of these germ layers is essential for the differentiation and specialization of cells, ultimately leading to the development of complex body structures in aquatic animals. The precise mechanisms of gastrulation can vary among different species, reflecting their unique developmental pathways and evolutionary relationships. Organogenesis is the next stage in embryonic development, where the rudimentary organs and structures beginto form and take shape. During this process, the cells within the germ layers differentiate and specialize to give rise to specific tissues and organs, such as the nervous system, muscles, and digestive system. Organogenesis is a highly coordinated and regulated process that is influenced by a combination of genetic and environmental factors. Disruptions or abnormalities during organogenesis can lead to developmental defects and impairments in aquatic animals, highlighting the importance of understanding the underlying mechanisms of this stage. As the embryo continues to develop, it undergoes further growth and maturation, leading up to the final stage of hatching or birth. The timing and process of hatching can vary greatly among different aquatic animals, depending on their species-specific adaptations and environmental conditions. Some aquatic animals may hatch fromtheir eggs as larvae, while others may undergo direct development and emerge as miniature versions of the adult. The hatching process is a critical transition point in the life cycle of aquatic animals, marking the beginning of their independent existence outside the protective confines of the egg. In conclusion, embryonic development in aquatic animals is a complex and dynamic process that shapes the growth and evolution of these species. From fertilization to hatching, aquatic animal embryos undergo a series of intricate stages that determine their ultimate form and function. Understanding the mechanisms and factors that influence embryonic development in aquatic animals is essential for conservation efforts, research initiatives, and the overall appreciation of the diversity and complexity of life in aquatic environments. By studying and preserving the embryonic stages of aquatic animals, we can gain valuable insights into their biology, behavior, and ecological roles, ultimately contributing to the conservation and sustainability of these fascinating creatures.。

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Figure 1. Quantum Key Distribution
3. Kak’s Three-Stage Protocol In [4], S. Kak proposed a new quantum key distribution protocol based on secret unitary transformations (Figure 2). His protocol, like BB84, has three stages, but unlike BB84, it remains quantum across all three stages. In the first stage, Alice manipulates the message X , which is simply one of two orthogonal stages (e.g. α|0 + β |1 and β |0 − α|1 ) by means of a unitary transformation UA , known only to her. Bob receives the new state, and in the second stage, applies his own secret transformation UB , which is both a unitary transformation, and one that commutes with UA , and sends the result back to Alice. In the third stage, Alice applies the † Hermitian conjugate of her transformation, UA , and sends the result back to Bob. † † Since UA UB UA (X ) = UB (X ), Bob simply applies UB and obtains the previously unknown state, X . 4. The Man in the Middle Attack The Suceptability of both BB84 and Kak’s three-stage protocol to man in the middle attacks has been documented [e.g. 5,6], and various methods to counter these attacks have been proposed [e.g. 7,8]. In such an attack, the eavesdropper, Eve, can attempt to thwart the communication between Alice and Bob in one of the following ways (Figure 3).
12Leabharlann JAMES HAROLD THOMAS
ensured by transmitting it via such low-tech solutions as clandestine meetings or trusted couriers. The need for better transmission protocols is obvious.
Figure 3. Man in the Middle Attack
VARIATIONS ON KAK’S THREE STAGE QUANTUM CRYPTOGRAPHY PROTOCOL
JAMES HAROLD THOMAS Abstract. This paper introduces a variation on Kak’s three-stage quanutm key distribution protocol which allows for defence against the man in the middle attack. In addition, we introduce a new protocol, which also offers similar resiliance against such an attack.
VARIATIONS ON KAK’S THREE STAGE QUANTUM CRYPTOGRAPHY PROTOCOL
3
Figure 2. Kak’s Three-Stage Protocol (1) Eve receives the message from Alice by impersonating Bob. Eve then decodes Alice’s message, and, now impersonating Alice, duplicates this message to Bob. In this scenerio, both Eve and Bob obtain the secret message. (2) Eve impersonates Bob and decodes Alice’s message as in scenerio 1, but instead of relaying the actual message to Bob, Eve relays a different message of her own choosing. In this scenerio, only Eve obtains the secret message. (3) Eve impersonates Bob, but is not able to decode Alice’s message. Instead, she impersonates Alice and sends her own message to Bob. In this scenerio, communication between Alice and Bob is blocked, but no secret message is comprimised.
arXiv:0706.2888v1 [cs.CR] 19 Jun 2007
1. Introduction In the relatively new field of quantum information science, there have been limited numbers of true breakthroughs. The quantum computer remains a machine on paper only, for a working realization has proved elusive. For one of the most powerful tools that the quantum computer would provide, namely the reduction of the factorization problem to polynomial time by Shor’s algorithm, the most successful implementation to date has been to factor the number 15 into 3 times 5 [1]. The quantum computer might remain unrealized for years to come. Indeed, Kak has suggested that the current quantum circuit model for quantum computers is fundamentally flawed and new models must be developed to tackle the problem [2]. While there have been limited strides in some areas of quantum information science, one area in particular has produced realizable solutions in the field of cryptography. Quantum key distribution protocols have been successfully implemented and have produced commercially available products. In this paper, we will discuss a new protocol proposed by Kak called the “Three Stage Protocol.” To Kak’s protocol, we will introduce a modification which allows for greater security against man in the middle attacks. In addition, we introduce a new single stage protocol which similarly allows for security against such attacks. 2. Quantum Key Distribution The usefulness of quantum key distribution lies in the properties of the qubit, the quantum unit of information. Since a qubit is an object representing a quantum superposition state, the qubit cannot be copied. This is commonly called the nocloning theorem [3]. This property ensures that during qubit data transmission, it is impossible for an evesedropper (Eve) to simply make copies of the qubits being sent, and thus manipulate these copied qubits to obtain the message. This useful property allows quantum data transmission to be used effectively in key distribution protocols as shown in [3]. When a private key can be transmitted securly along a quantum channel, then secure classical communication between the two parties (Alice and Bob) can be achieved using the private key (Figure 1). One private key cryptosystem in use today is the Vernam cipher, also called the one time pad. According to Nielsen and Chuang, the security of the private key used in the Vernam cipher is sometimes
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