Spontaneus pion emission during fission - a new nuclear radioactivity

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原虫概论阿米巴

原虫概论阿米巴
×1000
3、生活史
经口
四核包囊 小肠下段脱囊 4个核滋养体
核分裂
8个单核小滋养体
肠粘膜
邹褶或隐窝,二分裂繁(以细菌粘膜 肠内容

已消化食物为食) 胞质分泌囊液
虫体团缩形成囊前期 包囊
包囊→滋养体→包囊为疾病阿米巴生活史型
在一定条件下
抵抗力下降
滋养体侵入肠粘膜组织
肠腔内
组织内(肠壁、肝脑) 、
染色后胞核形态特征是医学原虫病 原诊断的重要依据
致病特点
1、增殖作用:大量增殖到一定数量后引起 损害,血液、体液及分泌物中原虫的检查 可为临床诊断提供可靠信息。
2、播散作用:由于快速增殖而具有的全身 播散的倾向。病原学诊断不仅要考虑原发 病灶,而且还要考虑到继发病灶乃至全身 各器官。
3、机会致病:有些原虫对健康宿主不表现 出明显致病性,但当宿主免疫功能低下时, 可导致严重甚至致死性的感染。
常见医学原虫分类
1、生物学分类:隶属于4个纲: 动鞭纲 叶足纲 孢子纲 动基裂纲 (鞭毛虫)(阿米巴)(孢子虫) (纤毛虫) 2、按寄生部位分类:腔道内寄生原虫(肠
道、阴道)和血液及组织内寄生原虫(红 细胞内、有核细胞内、肝、肺、脑及其他 组织内寄生)。
阿米巴概述
以伪足为运动细胞器,多数生 活史有滋养体和包囊两个时期, 滋养体期为运动、摄食、繁殖和 致病期,包囊为静止期,是阿米 巴传播期。
对成形粪便,用碘液染色法查包囊。包囊形成有 间歇,故检查时应隔日1次并连续3次以上送检 为宜。 (2)十二指肠液或胆汁检查滋养体 (3)肠检胶囊法。 (4)小肠活组织检查,利用纤维胃镜取小肠粘 膜组织检查。
五、流行
、分布: 1本病在发达与发展中国家均有流行,我国平均 感染率为2.65%

向日葵向太阳的原理写英语作文

向日葵向太阳的原理写英语作文

向日葵向太阳的原理写英语作文Heliotropism: The Sun-Tracking Behavior of Sunflowers.Sunflowers, with their vibrant yellow petals and towering heights, have captivated people for centuries with their unique ability to follow the sun's movement across the sky. This phenomenon, known as heliotropism, is an adaptive trait that maximizes the plant's exposure to sunlight, essential for its growth and survival.Light Sensing and Response.At the heart of heliotropism lies a specialized sensory system within the sunflower's young stem, called the pulvinus. The pulvinus perceives the direction of light through photoreceptors known as phytochromes. Phytochromes are light-sensitive pigments that absorb specific wavelengths, particularly red and far-red light.When exposed to sunlight, phytochromes in the pulvinusundergo conformational changes that trigger a cascade of physiological responses. These responses include the asymmetrical distribution of auxin, a plant growth hormone, which promotes cell elongation on the shaded side of the stem.Stem Curvature and Tracking.As the pulvinus responds to light, it initiates a growth response that results in the curvature of the sunflower's stem. The shaded side of the stem elongates more rapidly than the sunlit side, causing the stem to bend towards the light source.This bending response is continuous throughout the day, as the sunflower tracks the sun's position from east to west. The movement is driven by the continuous sensing of light and the subsequent redistribution of auxin within the pulvinus.Circadian Rhythm and Day-Night Cycle.In addition to light sensing, sunflowers also exhibit a circadian rhythm, an internal clock that regulates their physiological processes over a 24-hour period. This circadian rhythm influences the timing and direction of heliotropism.During the night, when light levels are low, sunflowers return to an upright position. This movement is facilitated by a drop in auxin levels on the shaded side of the stem. As dawn approaches, light sensing triggers theredistribution of auxin, initiating the heliotropic response once again.Adaptive Significance and Benefits.Heliotropism provides significant adaptive advantages to sunflowers. By maximizing their exposure to sunlight, sunflowers optimize their photosynthetic efficiency. Photosynthesis is the process by which plants convert sunlight into chemical energy, which is essential for growth, reproduction, and overall health.Furthermore, heliotropism helps sunflowers avoid photoinhibition, a condition that occurs when plants are exposed to excessive sunlight. By tracking the sun, sunflowers minimize the amount of direct sunlight hitting their leaves, reducing the risk of damage to their photosynthetic machinery.Applications and Beyond.The heliotropic behavior of sunflowers has inspired a range of applications in various fields, including robotics, solar energy, and architecture. Researchers have developed sunflower-inspired robots that can follow the sun's movement, providing potential applications in solartracking systems.In solar energy, heliotropic technology can be incorporated into solar panels to maximize their efficiency. By tracking the sun throughout the day, solar panels can harness more sunlight, increasing their energy output.In architecture, heliotropic principles can be appliedto the design of buildings that optimize natural light exposure. This can reduce energy consumption for lighting and heating, while also improving indoor air quality and occupant comfort.Conclusion.Heliotropism is a remarkable example of plant adaptation and resilience. The ability of sunflowers to follow the sun's movement is a testament to the intricate mechanisms that govern plant behavior. This sun-tracking behavior not only ensures optimal growth and survival but also has practical applications in various disciplines, demonstrating the interconnectedness between nature and technology. As we continue to explore and understand the complexities of heliotropism, we unlock new possibilities for innovation and a sustainable future.。

植物的光合作用英语

植物的光合作用英语

The Process of Photosynthesis in Plants Photosynthesis is a crucial process for the survival of plants, as it enables them to convert sunlight into energy. This process occurs in the green parts of plants, such as leaves, and involves various components and stages. In this document, we will explore the process of photosynthesis in plants and its significance in their growth and development.IntroductionPhotosynthesis is a biological process in which plants use sunlight, carbon dioxide, and water to produce glucose and oxygen. This energy-conversion process takes place in specialized structures within plant cells called chloroplasts. Chloroplasts contain a pigment called chlorophyll, which plays a vital role in capturing sunlight.The Stages of PhotosynthesisPhotosynthesis can be divided into two primary stages: the light-dependent reactions and the light-independent reactions, also known as the Calvin cycle.Light-Dependent ReactionsThe light-dependent reactions occur in the thylakoid membrane of the chloroplasts. These reactions require sunlight and involve the following steps:1.Absorption of Light: Chlorophyll in the thylakoid membrane absorbslight energy from the sun.2.Splitting of Water: Water molecules are split into oxygen, hydrogenions (H+), and electrons (e-). This process is known as photolysis.3.Formation of ATP: The energy from the absorbed light is used togenerate ATP molecules, which act as a source of energy to fuel the plant’smetabolic reactions.4.Generation of NADPH: NADPH (nicotinamide adenine dinucleotidephosphate) is produced by transferring the electrons derived from water to the molecule NADP+.Light-Independent Reactions (Calvin Cycle)The light-independent reactions occur in the stroma of the chloroplasts and do not require direct sunlight. These reactions utilize the products of the light-dependent reactions, including ATP and NADPH, to produce glucose. The Calvin cycle consists of the following steps:1.Carbon Dioxide Fixation: Carbon dioxide (CO2) is combined with afive-carbon sugar known as RuBP (ribulose bisphosphate) in a reactioncatalyzed by the enzyme RuBisCO.2.Formation of PGA: The resulting six-carbon compound immediatelysplits into two three-carbon compounds called PGA (phosphoglycerate).3.Reduction of PGA: ATP and NADPH produced during the light-dependent reactions are utilized to convert PGA into a higher-energy molecule called G3P (glyceraldehyde 3-phosphate).4.Regeneration of RuBP: Some G3P molecules are converted back intoRuBP, which enables the continuation of the Calvin cycle. The remaining G3P molecules are used to synthesize glucose and other carbohydrates.Significance of Photosynthesis in PlantsPhotosynthesis is essential for the survival and growth of plants due to its numerous key roles:1.Energy Production: The primary goal of photosynthesis is to convertsunlight into chemical energy in the form of glucose. This energy is essential for supporting various metabolic processes in the plant, including growth andreproduction.2.Oxygen Release: During photosynthesis, plants release oxygen as abyproduct. This oxygen is vital for the respiration of both plants and otherorganisms, including humans.3.Carbon Dioxide Reduction: Plants absorb carbon dioxide from theatmosphere and convert it into glucose through photosynthesis. This process helps to regulate the concentration of carbon dioxide in the environment and acts as a crucial mechanism in combating climate change.4.Food Production: Through photosynthesis, plants produce glucose,which is further transformed into other carbohydrates, such as starch andcellulose. These compounds serve as a source of energy and structuralmaterials for the plant and are also consumed by humans and other animals as food.5.Environmental Impact: Photosynthetic plants play a vital role inmaintaining the balance of ecosystems. They provide habitats for variousorganisms, contribute to the cycling of nutrients, and help in reducing soilerosion.ConclusionPhotosynthesis is a complex and essential process for plants, enabling them to convert sunlight into usable energy. Through the stages of light-dependent and light-independent reactions, plants produce glucose and oxygen, playing a critical role in their own growth and development, as well as in the overall functioning of ecosystems. Understanding the process of photosynthesis is crucial for appreciating the importance of plants and their impact on the environment.。

托福阅读TPO31(试题+答案+...

托福阅读TPO31(试题+答案+...

托福阅读TPO31(试题+答案+译文)第1篇:SpeciationinGeographicallyIsolatedPop为了帮助大家备考托福。

提高阅读成绩,打有准备的仗,下面小编给大家带来托福阅读TPO31(试题+答案+译文)第1篇:Speciation in Geographically Isolated Populations,希望大家喜欢。

托福阅读原文【1】Evolutionary biologists believe that speciation, the formation of a new species, often begins when some kind of physical barrier arises and divides a population of a single species into separate subpopulations. Physical separation between subpopulations promotes the formation of new species because once the members of one subpopulation can no longer mate with members of another subpopulation, they cannot exchange variant genes that arise in one of the subpopulations. In the absences of gene flow between the subpopulations, genetic differences between the groups begin to accumulate. Eventually the subpopulations become so genetically distinct that they cannot interbreed even if the physical barriers between them were removed. At this point the subpopulations have evolved into distinct species. This route to speciation is known as allopatry (“alio-” means “different”,and “patria” means “homeland”).【2】Allopatric speciation may be the main speciation route. This should not be surprising, since allopatry is pretty common. In general, the subpopulations of most species are separated from each other by some measurable distance. So even under normal situations the gene flow among the subpopulations is more of an intermittent trickle than a steady stream. In addition, barriers can rapidly arise and shut off the trickle. For example, inthe 1800s a monstrous earthquake changed the course of the Mississippi River, a large river flowing in the central part of the United States of America. The change separated populations of insects now living along opposite shore, completely cutting off gene flow between them.【3】Geographic isolation also can proceed slowly, over great spans of time. We find evidence of such extended events in the fossil record, which affords glimpses into the breakup of formerly continuous environments. For example, during past ice ages, glaciers advanced down through North America and Europe and gradually cut off parts of populations from one another. When the glacier retreated, the separated populations of plants and animals came into contact again. Some groups that had descended from the same parent population were no longer reproductively compatible—they had evolved into separate species. In other groups, however, genetic divergences had not proceeded so far, and the descendants could still interbreed—for them, reproductive isolation was not completed, and so speciation had not occurred.【4】Allopatric speciation can also be brought by the imperceptibly slow but colossal movements of the tectonic plates that make up Earth’s surface. About 5 million years ago such geologic movements created the land bridge between North America and South America that we call the Isthmus of Panama. The formation of the isthmus had important consequences for global patterns of ocean water flow. While previously the gap between the continents had allowed a free flow of water, now the isthmus presented a barrier that divided the Atlantic Ocean from the Pacific Ocean. This division set the stage for allopatric speciation among populations of fishes and other marine species.【5】In the 1980s, John Graves studied two populations of closely related fishes, one population from the Atlantic side of isthmus, the other from the Pacific side. He compared four enzymes found in the muscles of each population. Graves found that all four Pacific enzymes function better at lower temperatures than the four Atlantic versions of the same enzymes. This is significant because Pacific seawater is typically 2 to 3 degrees cooler than seawater on the Atlantic side of isthmus. Analysis by gel electrophoresis revealed slight differences in amino acid sequence of the enzymes of two of the four pairs. This is significant because the amino acid sequence of an enzyme is determined by genes.【6】Graves drew two conclusions from these observations. First, at least some of the observed differences between the enzymes of the Atlantic and Pacific fish populations were not random but were the result of evolutionary adaption. Second, it appears that closely related populations of fishes on both sides of the isthmus are starting to genetically diverge from each other. Because Graves’s study of geographically isolated populations of isthmus fishes offers a glimpse of the beginning of a process of gradual accumulation of mutations that are neutral or adaptive, divergences here might be evidence of allopatric speciation in process.托福阅读试题1.The word "promotes" in the passage is closest in meaning toA.describes.B.encourages.C.delays.D.requires.2.According to paragraph 1, allopatric speciation involves which of the following?A.The division of a population into subspecies.B.The reuniting of separated populations after they have become distinct species.C.The movement of a population to a new homeland.D.The absence of gene flow between subpopulations.3.Why does the author provide the information that "the subpopulations of most species are separated from each other by some measurable distance"?A.To indicate how scientists are able to determine whether subpopulations of a species are allopatric.B.To define what it means for a group of animals or plants to be a subpopulation.C.To suggest that allopatric speciation is not the only route to subpopulation.D.To help explain why allopatric speciation is a common way for new species to come about.4.The word "accumulate" in the passage is closest in meaning toA.Become more significant.B.Occur randomly.C.Gradually increase in number.D.Cause changes.5.In paragraph 2,why does the author mention that some insect populations were separated from each other by a change in the course of Mississippi River caused by an earthquake?A.To make the point that some kind of physical barrier separates the subpopulations of most species.B.To support the claim that the condition of allopatry cansometimes arise in a short time.C.To provide an example of a situation in which gene flow among the subpopulations of a species happens at a slow rate.D.To explain why insects living along opposite shores of the Mississippi River are very different from each other.6.According to paragraph 3,separation of subpopulations by glaciers resulted in speciation in those groups of plants and animals thatA.were reproductively isolated even after the glaciers disappeared.B.had adjusted to the old conditions caused by the glaciers.C.were able to survive being separated from their parent population.D.had experienced some genetic divergences from their parent population.7.The word "colossal" in the passage is closet in meaning toA.consistent.B.gradual.C.enormous.D.effective.8.According to paragraph 4, which of the following is true of the geologic movements that brought about the Isthmus of Panama?A.The movements brought populations of certain fishes and marine organisms into contact with one another for the first time.B.The movements transferred populations of fishes and other marine animals between the Pacific and Atlantic Oceans.C.The movements created conditions that allowed water to flow more freely between the Pacific and Atlantic Oceans.D.The movements created conditions for the formation ofnew species of fishes and other marine animals.9.The word "sequence" in the passage is closet in meaning toA.quality.B.order.C.function.D.number.10.According to paragraph 5, by comparing the enzymes from two related groups of fishes on opposite sides of the isthmus, Graves found evidence thatA.there were slight genetic divergences between the two groups.B.the Atlantic group of fishes were descended from the Pacific group of fishes.C.the temperature of water on either side of the isthmus had changed.D.genetic changes in the Atlantic group of fishes were more rapid and frequent than in the Pacific group of fishes.11.It can be inferred from paragraph 5 and 6 that the reason Graves concluded that some of the differences between the Pacific and Atlantic enzymes were not random was thatA.each of the Pacific enzymes works better in cooler waters.B.the Enzymes of the Atlantic fish populations had not changed since the formation of the Isthmus of Panama.C.gel electrophoresis showed that the changes benefited both the Atlantic and the Pacific fish populations.D.the differences between the enzymes disappeared when the two fish populations were experimentally switched to other side of the isthmus.12.Which of the sentence below best expresses the essential information in the highlighted sentence in the passage? Incorrectchoices change the meaning in important ways or leave out essential information.A.Graves's study provides evidence that isthmus fishes are in the process of becoming geographically isolated.B.Graves's study of mutating isthmus fishes yields results that differ from results of other studies involving allopatric speciation.C.Graves's study of isolated populations of isthmus fishes provides some evidence that allopatric speciation might be beginningD.Grave's study indicates that when isolated, populations of isthmus fished register neutral or adaptive mutations.13. Look at the four squares [■] that indicate where the following sentence can be added to the passage.Where would the sentence best fit? The formation of the isthmus had important consequences for global patterns of ocean water flow.Allopatric speciation can also be brought by the imperceptibly slow but colossal movements of the tectonic plates that make up Earth's surface. ■【A】 About 5 million years ago such geologic movements created the land bridge between North America and South America that we call the Isthmus of Panama. The formation of the isthmus had important consequences for global patterns of ocean water flow. ■【B】While previously the gap between the continents had allowed a free flow of water, now the isthmus presented a barrier that divided the Atlantic Ocean from the Pacific Ocean. ■【C】This division set the stage for allopatric speciation among populations of fishes and other marine species. ■【D】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 mostimportant ideas in the passage. Some sentences do not belong in the summary because they express ideas that are not presented in the passages or are minor ideas in the passage. This question is worth 2 points.Allopatric speciation takes place when physically separated populations of a single species gradually diverge genetically to the point of becoming unable to interbreedA.Allopatric speciation is common because the gene flow between subpopulations is generally limited and the barriers that completely separate subpopulations can arise in a variety of ways.B.During past ice ages, some, but not all, subpopulations separated by glaciers evolved into distinct species.C.Speciation does not need to take place through allopatry because subpopulations will form distinct species whenever there are adaptive advantages or notD.Physical barriers from glaciers and the movement of tectonic plates form so slowly that the subpopulations on either side of the barriers usually do not form distinct species.E.Graves's study of fish populations separated by the Isthmus of Panama may well provide a picture of the beginning stages of speciation.F.Graves's study of physically separated fish populations show that there must be large differences between the environments of the isolated populations if allopatric speciation is to take place.托福阅读答案1.promote本身是促进的意思。

environment-pollution-ppt

environment-pollution-ppt
Gaseous pollutants include oxides of sulfur, nitrogen(氮) carbon and organic compounds. Particulate pollutants are smoke, dust, soot 煤 烟 , fumes, aerosols 气 雾 剂 , liquid droplets, pollen花粉grains etc.
We hear various types of sounds everyday. Sound is mechanical energy from a vibrating source. A type of sound may be pleasant to someone and at the same time unpleasant to others. The unpleasant and unwanted sound is called noise.
The sources of air pollution are natural and man-made.
Natural Sources : They are volcanic eruptions, forest fires, sea salt sprays, biological decay, photo chemical oxidation of terpenes ,marshes, extra terrestrial bodies, pollen grains of flowers, spores,etc.
It is an atmospheric condition in which certain substances (including the normal constituents in excess) are present in concentrations which can cause undesirable effects on man and his environment. These substances include gaseous [ 'gæsɪəs] particulate matter, radioactive substances etc.

A review of the species of protozoan epibionts on crustaceans-11

A review of the species of protozoan epibionts on crustaceans-11

A REVIEW OF THE SPECIES OF PROTOZOAN EPIBIONTS ONCRUSTACEANS.I.PERITRICH CILIATESBYGREGORIO FERNANDEZ-LEBORANS and MARIA LUISA TATO-PORTODepartamento de Biologia Animal I(Zoologia),Facultad de Biologia,Pnta9a,Universidad Complutense,E-28040Madrid,SpainABSTRACTAn updated inventory of the peritrich(Protozoa,Ciliophora)epibiont species on crustaceans has been carried out.Data concerning268epibiont species,their taxonomic position,and the various crustacean basibionts were considered.The overview comprised in this study may be of use in further surveys of protozoan-crustacean epibiosis.RESUMENSe ha realizado un inventario actualizado de las especies de peritricos(Protozoa,Ciliophora) epibiontes en crustáceos.Se han considerado los datos concernientes a268especies epibiontes,su posición taxonómica,y los diferentes crustáceos visión general que comprende este estudio puede ser utilizada en futuras investigaciones sobre la epibiosis protozoos-crustáceos.INTRODUCTIONEpibiosis is a facultative association of two organisms:the epibiont and the basibiont(Wahl,1989).The term“epibiont”includes organisms that,during the sessile phase of their life cycle,are attached to the surface of a living substratum, while the basibiont lodges and constitutes a support for the epibiont(Threlkeld et al.,1993).Both concepts describe ecological functions(Wahl,1989).Several crustacean groups,cladocerans,copepods,cirripedes,isopods,amphi-pods,and decapods,include forms that are hosts for macroepibiont invertebrates (Ross,1983),and for protozoan microepibionts of the phylum Ciliophora:apos-tomatids,chonotrichids,suctorians,peritrichs,and heterotrichs(Corliss,1979; Small&Lynn,1985).The study of ciliate epibionts on crustaceans began in the last century.Bütschli(1887-89)made a compilation from former publications.After-wards,other authors(Keiser,1921;Kahl,1934,1935;Precht,1935;Raabe,1947; c®Koninklijke Brill NV,Leiden,2000Crustaceana73(6):643-683644G.FERNANDEZ-LEBORANS&M.L.TATO-PORTONenninger,1948)not only described epibiont species,but proposed explanations for the processes of epibiosis.A review of the protozoan epibionts found on de-capod crustaceans was carried out by Sprague&Couch(1971).Green(1974), in a study of the epibionts living on cladocerans,pays considerable attention to protozoan species.Ho&Perkins(1985)have focused on the epibionts found on copepods.In other contemporary and also earlier works,the following aspects have been taken into account:(1)speci city between ciliates and their crustacean basi-bionts(Evans et al.,1981;Batisse,1986,1992;Clamp,1991);(2)the morpholog-ical and physiological adaptations of the epibionts(D’Eliscu,1975;Batisse,1986, 1994;Fenchel,1987;Clamp,1991;Lom&De Puytorac,1994);(3)the effects pro-duced by the epibionts on the crustaceans(Herman et al.,1971;Turner et al.,1979; Kankaala&Eloranta,1987;Nagasawa,1988);(4)the possible use of epibionts for the assessment of water quality(Antipa,1977;Henebry&Ridgeway,1979;Scott &Thune,1986);(5)the implications of protozoan epibionts on cultures of vari-ous species of crustaceans(Overstreet,1973;Johnson,1977,1978;Lightner,1977, 1988;Couch,1978;Scott&Thune,1986;V ogelbein&Thune,1988;Camacho& Chinchilla,1989);and(6)the organization of the epibiont communities on plank-tonic crustaceans(Threlkeld et al.,1993).Despite the fact that there is a considerable amount of information about the protozoan epibionts on crustaceans,since the works of Sprague&Couch(1971), Green(1974),and Ho&Perkins(1985),which relate to speci c crustacean groups, no further general reviews have appeared.Several new species of protozoan ciliate epibionts have recently been described(Dovgal,1985;Batisse,1992;Fernandez-Leborans&Gomez del Arco,1996;Zhadan&Mikrjukov,1996;Fernandez-Leborans et al.,1996,1997),and some of these are peritrich ciliates(Matthes& Guhl,1973;Bierhof&Roos,1977;Jankowski,1986;Dale&Blom,1987;Clamp, 1990,1991;Threlkeld&Willey,1993;Hudson&Lester,1994;Stoukal&Matis, 1994;Foissner,1996).The purpose of this work is to provide an up-to-date review of the peritrich ciliates living as epibionts on crustaceans:268species have been considered in this compilation,which may contribute data for studies of epibiosis in crustaceans.CRUSTACEAN PROTOZOAN EPIBIONTS,I.PERITRICH CILIATES645RESULTS1)Phylum CILIOPHORA Do ein,1901Class OLIGOHYMENOPHOREA De Puytorac,Batisse,Bohatier,Corliss, Deroux,Didier,Dragesco,Fryd-Versavel,Grain,Grolière,Hovasse,Iftode,Laval,Roque,Savoie&Tuffrau,1974Subclass P ERITRICHIA Calkins,1933Order S ESSILIDA Kahl,1933Family Epistylididae Kahl,1935Genus Rhabdostyla Kent,1880( g.1)R.bosminae Levander,1907.On the cladoceran Bosmina sp.R.conipes Kahl,1935.On the cladoceran Daphnia sp.Fresh water.On the cladocerans Daphnia magna,D.longispina and Scapholeberis mucronata (cf.Green,1957,1974).R.cyclopis Kahl,1935.On the copepod Cyclops sp.Fresh water.R.cylindrica Stiller,1935.On the cladoceran Leptodora ke Balaton (Hungary).On the cladoceran Leptodora kindtii.Denmark(Green,1974).R.hungarica Stiller,1931.On the cladoceran Leptodora ke Balaton (Hungary).R.globularis Stokes,1890.On the cladoceran Bosmina longirostris and on Diaphanosoma brachyurum.Germany(Nenninger,1948).R.invaginata Stokes,1886.On the ostracod Cypris sp.R.sessilis Penard,1922.On the copepod Cyclops sp.Fresh water.R.pyriformis Perty,1852(cf.Kahl,1935;on Entomostraca).On the clado-ceran Daphnia longispina(cf.Nenninger,1948).On the cladoceran Daph-nia hyalina(cf.Sommer,1950).On Daphnia pulex and Ceriodaphnia reticu-lata(cf.Hamman,1952).On Daphnia magna,D.pulex,D.cucullata,Simo-cephalus vetulus,Ceriodaphnia reticulata,and Leptodora kindtii(cf.Green, 1953).On Daphnia magna(cf.Green,1955).On Daphnia magna andD.longispina(cf.Green,1957).On Daphnia atkinsoni,D.hyalina,D.lon-gispina,D.curvirostris,D.obtusa,Ceriodaphnia laticaudata,and C.pulchel-la(cf.Green,1974).R.vernalis Stokes,1887.On the copepod Eucyclops agilis(cf.Henebry& Ridgeway,1979).1)For authors and dates of species of Crustacea mentioned herein,see separate section,below.646G.FERNANDEZ-LEBORANS&M.L.TATO-PORTOFigs.1-2.1,Rhabdostyla(R.pyriformis,after Green,1957);2,Epistylis(E.gammari,after Precht,1935).Rhabdostyla sp.Bierhof&Roos,1977.Between the spines at the end of the telson on Gammarus tigrinus.Germany.Rhabdostyla sp.Weissman et al.,1993.On the copepod Acartia hudsonica. Genus Epistylis Ehrenberg,1832( g.2)E.anastatica(Linnaeus,1767)(cf.Kent,1881).Syn.:Vorticella anastatica L.,1767.On Entomostraca and freshwater plants.On cyclopoid copepods and Daphnia pulex(cf.Green,1974).E.astaci Nenninger,1948.Fresh water.On the gills of the decapod Astacusastacus(as A. uviatilis)(Germany).On A.leptodactylus(cf.Stiller,1971).On the gills of Austropotamobius torrentium(cf.Matthes&Guhl,1973).E.bimarginata Nenninger,1948.Fresh water.On the appendages of Astacusastacus(as A. uviatilis).Germany.E.branchiophila Perty,1852.Syn.:E.formosa Nenninger,1948.On theparasitic copepod Lernaea cyprinacea,in freshwater environments of South Africa(Van As&Viljoen,1984).E.breviramosa Stiller,1931.On the antennal lament of the cladoceran Daph-nia ke Balaton(Hungary).On the copepod Cyclops sp.,Czechoslovakia (Srámek-Husek,1948).On the cladocerans Bosmina longirostris and Alona af nis(cf.Green,1974).E.cambari Kellicott,1885.On the gills of the decapod Cambarus sp.(NE ofU.S.A.).On the maxillae of the cray sh Astacus leptodactylus(fresh water) (cf.Matthes&Guhl,1973).E.crassicollis Stein,1867.On freshwater Entomostraca and on the pleopodsand gills of cray sh.On the gills of Astacus astacus(as A. uviatilis),andCRUSTACEAN PROTOZOAN EPIBIONTS,I.PERITRICH CILIATES647 the maxillae,maxillipeds,and gills of A.leptodactylus,in Europe(Matthes& Guhl,1973).E.cyprinaceae Van As&Viljoen,1984.On the parasitic copepod Lernaea cyprinacea(fresh water,South Africa).E.daphniae Fauré-Fremiet,1905.On the cladoceran Daphnia sp.On Daphnia magna(cf.Nenninger,1948).On the copepod Boeckella triarticulata(New Zealand)(Xu&Burns,1990).On the cladoceran Moina macrocopa in an urban stream.E.diaptomi Fauré-Fremiet,1905.On the copepod Diaptomus sp.E.digitalis Ehrenberg,1838.On the copepod Cyclops sp.E.epibarnimiana Van As&Viljoen,1984.On the parasitic copepod Lernaea barnimiana(fresh water,South Africa).E.fugitans Kellicott,1887.On the cladoceran Sida crystallina.North America.E.gammari Precht,1935.On the antennae of the gammarid Gammarus sp. (Kiel channel).On the proximal part of the rst antenna and,less commonly, on the second antenna of Gammarus oceanicus and G.salinus.In the Baltic Sea and areas of Norway(Fenchel,1965).On the rst antenna of Gammarus tigrinus(cf.Stiller,1971).E.halophila Stiller,1942.On the cladocerans Daphnia longispina and D.pulex (Lake Cserepeser,Hungary).E.harpacticola Kahl,1933.On harpacticoid copepods in the Kiel channel. E.helenae Green,1957.On the cladocerans Daphnia pulex,D.magna,D.ob-tusa,D.longispina,D.curvirostris,Ceriodaphnia pulchella,C.reticulata, ticaudata,Moina macrocopa,M.micrura,Chydorus sphaericus,Simo-cephalus serrulatus,and S.vetulus(cf.Green,1957,1974).On Daphnia magna(cf.Nenninger,1948).On Ceriodaphnia reticulata and Simocephalus vetulus(cf.Matthes,1950).E.humilis Kellicott,1887.On the gammarid Gammarus sp.and other Ento-mostraca.custris Imhoff,1884.On the pelagic copepod Cyclops sp.On the buccal appendages of the branchiopod Lepidurus apus(freshwater areas near Vienna, Austria)(Foissner,1996).E.magna V an As&Viljoen,1984.On the parasitic copepod Lernaea cypri-nacea(fresh water,South Africa).E.niagarae Kellicott,1883.On the body surface of cray sh(Niagara River, U.S.A.).On the antennae and body of the European cray sh Astacus lep-todactylus,on Austropotamobius torrentium,and on Orconectes limosus(as Cambarus af nis)(cf.Matthes&Guhl,1973).On the surface of the copepod648G.FERNANDEZ-LEBORANS&M.L.TATO-PORTOEucyclops serrulatus,and on the cladocerans Daphnia pulex,D.rosea,Cerio-daphnia reticulata,and Scapholeberis mucronata(lakes of Colorado,U.S.A.) (Willey&Threlkeld,1993).E.nitocrae Precht,1935.On the third pereiopod of Gammarus tigrinus(cf.Bierhof&Roos,1977).E.nympharum Engelman,1862.On cladocerans(Nenninger,1948).On Cy-clops sp.(cf.Foissner&Schiffman,1974).On the branchiuran Dolops ra-narum(cf.Van As&Viljoen,1984).E.ovalis Biegel,1954.On the gnathopods of Gammarus tigrinus.On the thirdpereiopod of the gammarid Gammarus pulex,and on the spines at the end of the third uropod of Gammarus tigrinus(cf.Bierhof&Roos,1977).E.plicatilis Ehrenberg,1838.On the copepods Eucyclops agilis,Cyclopsvernalis,and C.bicuspidatus(Ashmore Lake,Illinois,U.S.A.)(Henebry& Ridgeway,1979).E.salina Stiller,1941.On the rst and second antennae,coxae,and gills of thegammarid Gammarus pulex(cf.Bierhof&Roos,1977).E.thienemanni Sommer,1951.On the gills of Gammarus tigrinus(cf.Bierhof&Roos,1977).E.zschokkei(Keiser,1921).Syn.:Opercularia zschokkei Keiser,1921.On thegnathopods of the gammarid Gammarus tigrinus and on other Entomostraca.On the cladoceran Acantholeberis curvirostris(cf.Nenninger,1948).Epistylis sp.Hutton,1964.On the decapod Penaeus duorarum(Florida,U.S.A.).Between the setae of the rst antenna of Gammarus tigrinus(cf.Bierhof& Roos,1977).Epistylis sp.Hutton,1964.On the decapod Ploeticus robustus(Daytona Beach, Florida,U.S.A.).Epistylis sp.Viljoen&Van As,1983.Two species on the thoracic appendages of a freshwater brachyuran,apparently erroneously identi ed as“Potamon sp.”(South Africa)[the genus Potamon does not occur in southern Africa].Epistylis sp.Pearse,1932.On the gills of the decapods Coenobita clypeatus, Geograpsus lividus,and Pachygrapsus transversus(Florida,U.S.A.).Epistylis sp.Hudson&Lester,1994.On the gills of the decapod Scylla serrata (Moreton Bay,Queensland,Australia).Epistylis sp.Turner et al.,1979.On the estuarine copepods Acartia tonsa andA.clausi(Escambia Bay,Florida,U.S.A.).Epistylis sp.Villarreal&Hutchings,1986.Fresh water.On the maxillipeds, pereiopods,and ventral portion of the abdomen of the decapod Cherax tenuimanus(Australia).CRUSTACEAN PROTOZOAN EPIBIONTS,I.PERITRICH CILIATES649 Family Lagenophryidae Bütschli,1889Genus Lagenophrys Stein,1852( g.3)L.aegleae Mouchet-Bennati,1932.Fresh water.On the branchial laments of the anomurans Aegla sp.,Aegla castro,and Aegla franca.Arroyo Miguelete, (Uruguay)and Parana River(Brazil).L.ampulla Stein,1851.Fresh water.On the gills of species of the genus Gammarus.L.andos(Jankowski,1986)(cf.Clamp,1991).Syn.:Circolagenophrys andos Jankowski,1986.Fresh water.On the decapod Parastacus chilensis(Chile).L.anticthos Clamp,1988.Fresh water.On the branchial laments of the decapods Parastacus pugnax,P.defossus,and P.saffordi(Chile,Brazil, Uruguay).L.aselli Plate,1886.On the branchial surface of the isopod Asellus aquaticus (Hamburg,Germany).L.awerinzewi Abonyi,1928.On the gills of the decapod Potamon uviatilis(as Telphusa uviatilis)(Africa).L.bipartita Stokes,1890.On the cladoceran Daphnia sp.(fresh water,U.S.A.).L.branchiarum Nie&Ho,1943.Fresh water.On the gills of the caridean shrimp Macrobrachium nipponense(as Palaemon nipponense)(Japan).L.callinectes Couch,1967.Marine and in estuaries.On the gills of the decapods Callinectes sapidus,C.bocourti,and C.maracaiboensis(Chesapeake Bay, Maryland,Virginia,and Gulf of Mexico).mensalis Swarczewsky,1930.Fresh water.On gammarids(Lake Baikal).L.darwini Kane,1965.On the branchial laments of the decapod Cherax quadricarinatus(stream near Darwin,Australia).L.dennisi Clamp,1987.Fresh water.On the decapods Orconectes illinoiensis, Cambarus bartonii bartonii,and C.chasmodactylus(North America).L.deserti Kane,1965.Fresh water.On the gills of the decapods Cherax tenuimanus and C.quinquecarinatus(SW rivers,Australia).L.diogenes(Jankowski,1986).Syns.:Circolagenophrys diogenes Jankowski, 1986,Lagenophrys incompta Clamp,1987.Fresh water.On the gills of the decapods Orconectes illinoiensis and Cambarus diogenes(Illinois,U.S.A.).L.discoidea Kellicott,1887(cf.Clamp,1990).Syns.:Lagenophrys labiata Wallengren,1900(a junior homonym of biata Stokes,1887(cf.Clamp, 1990));L.wallengreni Abonyi,1928;Circolagenophrys entocytheris Jankow-ski,1986.Fresh water.On ostracods.On the cray sh Cambarus sp.,C.chas-modactylus,C.bartonii bartonii,and Orconectes illinoiensis(Ontario,Canada and U.S.A.).650G.FERNANDEZ-LEBORANS&M.L.TATO-PORTOFigs.3-7.3,Lagenophrys(L.eupagurus,after Clamp,1989);4,Clistolagenophrys(C.primitiva, after Swarczewsky,1930);5,Setonophrys(munis,after Clamp,1991);6,Operculigera (O.asymmetrica,after Clamp,1991);7,Usconophrys(U.aperta,after Clamp,1991).L.dungogi Kane,1965.On the branchial laments of the decapod Euastacus sp.(stream near Dungog,Australia).L.engaei Kane,1965.On the branchial laments,basal areas of the gills, branchiostegite membrane and,more rarely,on the pleopods of the decapods Engaeus victoriensis and Austroastacus hemicirratulus(Victoria,Tasmania, and Melbourne,Australia).L.eupagurus Kellicott,1893(cf.Clamp,1989).Syns.:Lagenophrys lunatus Imamura,1940;Lagenophrys articularis Nie&Ho,1943.Marine,in estu-arine areas and fresh water.On the decapods Litopenaeus setiferus(as Pe-CRUSTACEAN PROTOZOAN EPIBIONTS,I.PERITRICH CILIATES651 naeus s.)(Penaeidea,Penaeidae),on the surface of the body,Litopenaeus van-namei(as Penaeus v.),on the surface of the body,Macrobrachium nipponense (Caridea,Palaemonidae)on antennae and pleopods,Macrobrachium ohione, on the surface of the middle of the pleura,Macrobrachium rosenbergii,on the gills,Palaemon paucidens(Caridea,Palaemonidae),Palaemonetes inter-medius(Caridea,Palaemonidae),Palaemonetes kadiakensis,Palaemonetes paludosus,Palaemonetes pugio,Palaemonetes varians,on the whole body, except on the gills,Palaemonetes vulgaris,Upogebia af nis(Thalassinidea, Upogebiidae),and Pagurus longicarpus(Anomura,Paguridae),on the gills (U.S.A.,Japan,Venezuela,Thailand).L.foxi Clamp,1987.Fresh water.On the gills of the gammarids Gammarus pseudolimnaeus,G.troglophilus,G.minus,and Gammarus sp.(Missouri, U.S.A.).L.in ata Swarczewsky,1930.On the distal areas of pleopods of the gammarid Gmelinoides fasciata(Lake Baikal).L.jacobi(Kane,1969).Syn.:Stylohedra jacobi Kane,1969.On freshwater decapods in Australia.L.johnsoni Clamp,1990.Syn.:Lagenophrys labiata Stokes,1887(partim). Fresh water.On the appendages and the surface of the carapace of the gammarids Gammarus fasciatus,G.daiberi,G.tigrinus,and Crangonyx gracilis(New Jersey,Michigan,and North Carolina,U.S.A.).biata Stokes,1887(cf.Clamp,1990).Fresh water.On the appendages and on the surface of the carapace of the gammarids Gammarus fasciatus, G.daiberi,G.tigrinus,and Cangronyx gracilis(New Jersey,Michigan,and North Carolina,U.S.A.).L.leniusculus(Jankowski,1986).Syns.:Circolagenophrys leniusculus Jan-kowski,1986;L.oregonensis Clamp,1987.Fresh water.On the carapace, gills,ventral surface of the abdomen,uropods,pereiopods,and pleopods of the decapod Pacifastacus leniusculus leniusculus,and on the gills of P.leniusculus trowbridgii and P.connectens(North America).L.lenticula(Kellicott,1885)(cf.Clamp,1991).Syns.:Stylohedra lenticula Kellicott,1885;S.lenticulata Kahl,1935;Lagenophrys lenticulata(Kahl, 1935)(cf.Thomsen,1945).Fresh water.Setae of the sixth and seventh pereiopods of the gammarids Hyalella azteca and H.curvispina(U.S.A., Canada,Mexico,and Uruguay).L.limnoria Clamp,1988.Syn.:Circolagenophrys circularis Jankowski,1986 (cf.Clamp,1991).On the isopod Limnoria lignorum.L.macrostoma Swarczewsky,1930.Fresh water.On gammarids(Lake Baikal). L.matthesi Schödel,1983.On the maxillipeds of the gammarids Gammarus pulex and Carinogammarus roeselii.652G.FERNANDEZ-LEBORANS&M.L.TATO-PORTOL.metopauliadis Corliss&Brough,1965.Fresh water.On the gills of the brachyuran Metopaulias depressus(endemic on Jamaica).L.monolistrae Stammer,1935.On the pleopods of the isopod Monolistra sp.L.nassa Stein,1852.Fresh water.On the pleopods of the gammarid Gammarus pulex.L.oblonga Swarczewsky,1930.On the antennae of the gammarid Gammarus hyacinthinus(Lake Baikal).L.orchestiae Abonyi,1928.On the amphipod Orchestia cavimana(Lake Balaton,Hungary).L.ornata Swarczewsky,1930.Fresh water.On ke Baikal.L.ovalis Swarczewsky,1930.Fresh water.On the thoracic appendages of ke Baikal.L.parva Swarczewsky,1930.On ke Baikal.L.patina Stokes,1887(cf.Clamp,1990).Syn.:Lagenophrys labiata Stokes, 1887(cf.Shomay,1955).(Corliss&Brough,1965;Clamp,1973).Fresh water.On the pereiopods and gills of the gammarids Gammarus sp.and Hyalella azteca.American continent.L.rugosa Kane,1965.Fresh water.On the gills of the decapod Geocharax falcata(Victoria,Australia).L.similis Swarczewsky,1930.On ke Baikal.L.simplex Swarczewsky,1930.On ke Baikal.L.solida Swarczewsky,1930.On ke Baikal.L.stammeri Lust,1950.On ostracods.Germany.(Lust,1950a).L.stokesi Swarczewsky,1930.On ke Baikal.L.stygia Clamp,1990.Syn.:Lagenophrys labiata Stokes,1887(cf.Jakschik, 1967).Subterranean water.On the gills of the cave-dwelling amphipod Bactrurus mucronatus(Illinois,U.S.A.).L.tattersalli Willis,1942.On European copepods.L.turneri Kane,1969.On freshwater decapods in Australia.L.vaginicola Stein,1852.Syn.:Lagenophrys obovata Stokes,1887.On the genital setae and thoracopods of the copepods Cyclops miniatus and Cantho-camptus sp.L.verecunda Felgenhauer,1982.On the decapod Palaemonetes kadiakensis (Illinois,U.S.A.).L.willisi Kane,1965.Fresh water.On the gills of the decapods Cherax destructor,C.albidus,and C.rotundus(Melbourne,New South Wales(e.g., Newcastle),and NW Australia).Genus Clistolagenophrys Clamp,1991( g.4)C.primitiva(Swarczewsky,1930)(cf.Clamp,1991).Syn.:Lagenophrys primi-tiva Swarczewsky,1930.On pereiopods and pleopods of the gammarid Pallasea cancellus(Lake Baikal).Genus Setonophrys Jankowski,1986(cf.Clamp,1991)( g.5)S.bispinosa(Kane,1965)(cf.Clamp,1991).Syn.:Lagenophrys bispinosa Kane,1965.On pereiopods of the decapod Cherax rotundus setosus.Stream near Newcastle(N.S.W.,Australia).munis(Kane,1965)(cf.Clamp,1991).Syn.:Lagenophrys communis Kane,1965.On the body surface(telson,pleopods,pereiopods,carapace...) of the decapod Cherax destructor.On the gills of the decapods C.rotundus,C.albidus,C.quadricarinatus,Euastacus armatus,and Engaeus marmoratus(Victoria,Melbourne,and Tasmania,Australia).S.lingulata(Kane,1965)(cf.Clamp,1991).Syn.:Lagenophrys lingulata Kane,1965.On the branchial laments and branchiostegite membrane of the decapods Cherax destructor, C.albidus,and C.rotundus(Victoria, Melbourne,and coastal and central areas of Australia).S.nivalis(Kane,1969)(cf.Clamp,1991).Syn.:Lagenophrys nivalis Kane, 1969.On freshwater decapods in Australia.S.occlusa(Kane,1965)(cf.Clamp,1991).Syn.:Lagenophrys occlusa Kane, 1965.On the anterior zone of the branchial cavity of the decapods Cherax destructor,C.albidus,and C.rotundus(Victoria and New South Wales, Australia).S.seticola(Kane,1965)(cf.Clamp,1991).Syn.:Lagenophrys seticola Kane, 1965.On the setae of the decapods Engaeus fultoni and Geocharax falcata (Victoria,Melbourne,and Templestowe,Australia).S.spinosa(Kane,1965)(cf.Clamp,1991).Syn.:Lagenophrys spinosa Kane, 1965.On the pleopods,carapace,and telson of the decapod Cherax destructor (Victoria,Melbourne,and Heathcote,Australia).S.tricorniculata Clamp,1991.On the pleopods of the decapod Geocharax falcata(Victoria,Grampian Mountains,and Wannon River,Australia). Genus Operculigera Kane,1969( g.6)O.asymmetrica Clamp,1991.On the base of the gills of the freshwater decapods Parastacus pugnax and Samastacus spinifrons(Concepción and Talcahuano,Chile).O.insolita Clamp,1991.On the base of the gills of the freshwater decapod Parastacus pugnax(Concepción,Talcahuano,Malleco,and Puren,Chile).O.montanea Kane,1969.On the freshwater decapod Colubotelson sp.(Aus-tralia).O.obstipa Clamp,1991.Pleopods of the isopod Metaphreatoicus australis (New South Wales,Australia).O.parastacis Jankowski,1986.On the base of the gills of the decapod Parastacus nicoleti(Isla Teja,Valdivia,Chile).O.seticola Clamp,1991.On the setae at the base of gills of the decapod Parastacus pugnax(Concepción,Chile).O.striata Jankowski,1986.On the decapod Parastacus chilensis.Chile.O.taura Clamp,1991.On the branchial laments of the freshwater decapod Parastacus pugnax(Concepción,Malleco,and Puren,Chile).O.velata Jankowski,1986.On the gills of the anomuran Aegla laevis.Chile.O.zeenahensis Kane,1969.On freshwater decapods in Australia.Family Usconophryidae Clamp,1991Genus Usconophrys Jankowski,1985(cf.Clamp,1991)( g.7)U.aperta(Plate,1889)(cf.Clamp,1991).Syns.:Lagenophrys aperta Plate, 1889;Usconophrys dauricus Jankowski,1986.On the gills and pleopods of the isopod Asellus aquaticus(Marburg and Hessen,Germany;North Carolina, U.S.A.;Brittany,Finisterre,Plougarneau,Pont-Menou,and Douron River, France).U.rotunda(Precht,1935)(cf.Clamp,1991).Syn.:Lagenophrys rotunda Precht,1935.On ostracods.Germany.Family Operculariidae Fauré-Fremiet,1979(in Corliss,1979)Genus Opercularia Stein,1854( g.8)O.allensi Stokes,1887.Syn.:O.ramosa Stokes,1887.On several living and inert substrata.On the body of the cray sh Astacus leptodactylus(cf.Matthes &Guhl,1973).O.asellicola Kahl,1935.On the isopod Asellus sp.Germany.O.coarctata Claparède&Lachmann,1858.On crabs(Buck,1961).O.crustaceorum Biegel,1954.On the gills of the cray sh Astacus astacus(asA. uviatilis).On the maxillae,maxillipeds,and pleopods of Austropotamo-bius torrentium(cf.Matthes&Guhl,1973).O.cylindrata Wrzesniowski,1807.On the copepod Cyclops sp.O.gammari Fauré-Fremiet,1905.Pereiopods of the gammarid amphipod Gammarus sp.O.lichtensteini Stein,1868.On various crabs and molluscs.O.nutans Ehrenberg,1838.Syn.:O.microstoma Stein,1854.On Entomostraca.On the cladoceran Alona af nis(cf.Matthes,1950).On the maxillipeds of the European cray sh Astacus leptodactylus(cf.Matthes&Guhl,1973).O.protecta Penard,1922.On the setae of pereiopods of the gammarid amphi-pod Gammarus pulex.O.reichelei Matthes&Guhl,1973.Found exclusively on the maxillipeds of the cray sh Astacus leptodactylus.O.stenostoma Stein,1868.On the isopod Asellus aquaticus.Genus Orbopercularia Lust,1950(cf.Lust,1950b)( g.9)O.astacicola(Matthes,1950)(cf.Matthes&Guhl,1973).Syn.:Opercularia astacicola Matthes,1950.Maxillipeds and pleopods of the cray sh Aus-tropotamobius torrentium.Genus Propyxidium Corliss,1979( g.10)P.aselli Penard,1922.On the isopod Asellus sp.P.asymmetrica Matthes&Guhl,1973.On the European cray sh Astacus astacus(as A. uviatilis).P.bosminae Kahl,1935.On the cladoceran Bosmina sp.P.canthocampti Penard,1922.On the pereiopods of the harpacticoid copepod Canthocamptus sp.Fresh water.P.cothurnioide Kent,1880.On the ostracod Cypris sp.P.hebes Kellicott,1888.On the pereiopods of the isopod Asellus aquaticus.P.henneguyi(Fauré-Fremiet,1905)(cf.Kahl,1935).Syn.:Opercularia hen-neguyi Fauré-Fremiet,1905.On the rst abdominal segment of the copepod Cyclops sp.Genus Ballodora Dogiel&Furssenko,1921( g.11)B.dimorpha Dogiel&Furssenko,1921.On Porcellio sp.and other terrestrialisopods.Genus Nuechterleinella Matthes,1990( g.12)N.corneliae Matthes,1990.On the ostracod Cypria ophthalmica.Genus Bezedniella Stoukal&Matis,1994( g.13)B.prima Stoukal&Matis,1994.Fresh water.On the ostracod Cypria sp.(Slovakia).Figs.8-14.8,Opercularia(O.nutans,after Foissner et al.,1992);9,Orbopercularia(O.astacicola, after Matthes&Guhl,1973);10,Propyxidium(P.canthocampti,after Penard,1922);11,Ballodora (B.dimorpha,after Dogiel&Furssenko,1921);12,Nuechterleinella(N.corneliae,after Matthes, 1990);13,Bezedniella(B.prima,after Stoukal&Matis,1994);14,Rovinjella(R.spheromae,afterMatthes,1972).Family Rovinjellidae Matthes,1972Genus Rovinjella Matthes,1972( g.14)R.spheromae Matthes,1972.On the marine isopod Sphaeroma serratum. Family Scyphidiidae Kahl,1933Genus Scyphidia Dujardin,1841( g.15)Scyphidia sp.Henebry&Ridgeway,1979.On the cladocerans Scapholeberis kingi,Alona costata,and Pleuroxus denticulatus(Ashmore Lake,Illinois, U.S.A.).Family Vaginicolidae De Fromentel,1874Genus Platycola Kent,1881( g.16)P.baikalica(Swarczewsky,1930).Syn.:Vaginicola baicalica Swarczewsky, 1930.Fresh water.On the gills of the gammarids Brandtia lata,Pallasea grubei,and Echinogammarus fuscus(Lake Baikal).P.callistoma Hadzi,1940.Fresh water.On the cave-dwelling isopod Microlis-tra spinosissima(former Yugoslavia).P.circularis Dons,1940.Marine.On the uropods of the isopod Limnoria sp.P.decumbens(Ehrenberg,1830).Syns.:Vaginicola decumbens Ehrenberg, 1830;Platycola ampulla De Fromentel,1874;P.regularis De Fromentel, 1874;P.striata De Fromentel,1874;P.truncata De Fromentel,1874;P.longicollis Kent,1882;P.intermedia Kahl,1935;P.re exa Kahl,1935;P.amphora Swarcezwsky,1930;P.amphoroides Sommer,1951.Fresh water.On several vegetable and animal substrata.On the gills of the gammarid Brachiuropus sp.(Lake Baikal)(Swarczewsky,1930).geniformis Hadzi,1940.Fresh water.On the cave-dwelling isopod Micro-listra spinosissima(former Yugoslavia).P.pala Swarczewsky,1930.Syn.:Vaginicola pala Swarczewsky,1930.On the gills of the gammarid Palicarinus puzyllii(as Parapallesa pazill)(Lake Baikal).Genus Cothurnia Ehrenberg,1831(cf.Claparède&Lachmann,1858)( g.17)C.angusta Kahl,1933.Brackish or fresh water.On ostracods(Kiel,Germany).C.anomala Stiller,1951.Fresh water.On the amphipod Corophium curvispi-num(Lake Balaton,Hungary).C.antarctica(Daday,1911)(cf.Warren&Paynter,1991).Syn.:Cothurniopsisantarctica Daday,1911.Marine.Epibiont on the ostracod Philomedes lae-vipes(Antarctic areas).C.astaci Stein,1854.Fresh water.On the pleopods and gills of cray sh.On the maxillae,maxillipeds,and pleopods of the cray sh Astacus astacus。

7. Emission and Absorption

7. Emission and Absorption
abs dPki = Bki wν (ν) (7.2) dt is proportional to the spectral energy density wν (ν) = n (ν)h ν of the radiation field (where n (ν) is the number of photons h ν per unit volume within the frequency interval ∆ν = 1 s−1 ). The proportionality factor Bki is the Einstein coefficient for absorption. Each absorption takes one photon from a specific mode of the radiation field (see Sect. 3.1) and therefore decreases the number of photons in this mode by one. The radiation field can also induce atoms in an excited state with energy E i to emit a photon with energy h ν = E i − E k into a specific mode of the radiation field and to go into the lower state E k . This process is called induced (or stimulated) emission. It increases by one the number of photons in this mode from which the inducing photon came. Since the two photons are in the same mode, they have identical propagation directions. The energy of the atom is reduced by ∆ E and that of

寄生虫学课件 利什曼阴道毛滴虫

寄生虫学课件 利什曼阴道毛滴虫

宫颈草莓样突起
阴道粘膜充血、出血
Ⅴ流行
呈世界性分布,以女性20~40岁年龄组感染 率最高,平均感染率为28%。 传染源:为滴虫性阴道炎患者和无症状带虫 者或男性感染者。 传染途径:
直接传播,主要通过性交传播。 间接传播,主要通过公共浴池、浴具、公 用游泳衣裤、坐式厕所而感染。
家庭聚集性
夫+ →妻+ 91% 妻+ →夫+ 31% 孩+ →父+44%,母+72%
抵抗力降低,泌尿道生理功能失调,月 经期后期、妊娠,pH近中性,血清存 在,有利于虫体和有害菌生长繁殖,此 期感染率、发病率高。
男性感染者一般无症状而呈带虫状态, 可招致配偶的连续重复感染。有时也相引 起尿道前列腺炎,出现夜尿增多,局部压 痛。 阴道毛滴虫能吞噬精子,分泌物阻碍 精子存活,因此有可能引起不孕症。
二 生活史
无鞭毛体 前鞭毛体 无鞭毛体 (人及动物体) (白蛉胃) (人及动物体)
Life cycle of Leishmania donovani
Life cycle main points 生活史小结
感染方式与感染阶段: 白蛉吸血注入前鞭毛体
寄生部位与致病虫期: 无鞭毛体(利杜体)寄生于肝、脾、骨 髓和淋巴结等处巨噬细胞内
人源型
犬源型 自然疫源型
传染源
病人
病犬
野生动物
媒介 中华白蛉(家栖) 中华白蛉(偏 吴氏白蛉
野栖)
亚力山大白蛉
易感者 地区
青少年,壮年
平原
儿童(10岁↓) 婴幼儿 (2岁↓)
丘陵山区 荒漠半开发区
分布
黄淮海地区 关中,疆南
西北,华北 东北丘陵山区
塔里木 额济纳旗
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a rXiv:n ucl-t h /3156v122Oct23SPONTANEOUS PION EMISSION DURING FISSION A NEW NUCLEAR RADIOACTIVITY D.B.Ion 1,Reveica Ion-Mihai 2,M.L.Ion 2and Adriana I.Sandru 11National Institute for Physics and Nuclear Engineering,IFIN-HH ,Bucharest,Romania 2University of Bucharest,Department of Atomic and Nuclear Physics ,Bucharest,Romania February 8,2008Abstract In this paper a short review of the theoretical problems of the pionic radioactivity is presented.The essential experimental results obtained in the 18years of existence of the nuclear pionic radioactivity are reviewed.Moreover,using the recent results on the spontaneous fission half lives T SF of the heavy nuclei with Z ≥100new predictions on the pionic yields in the region of superheavy elements are established.1INTRODUCTION In 1935Japanese physicist Hideki Yukawa predicted [1]the existence of a parti-cle -a meson -with a mass about 200times that of the electron,which mediated the nuclear forces.At first,the muon,discovered in 1937,looked like a good candidate for the meson,but soon it became clear that the muon’s properties did not match those predicted by Yukawa theory.Then,in 1947,Lates,Oc-chialini and Powell discovered [2]the π-meson,or pion,which did have the predicted meson properties.Today,we know that the muon is an elementary particle [3],cousin to the electron,-leptons and neutrinos,and that mesons (π,K ,η,etc.),including the pion,are combinations of quark and an antiquark.Everybody know that the discovery of -meson was an very important finding since this was in fact a fundamental step in the understanding the subatomic world.It heralded the beginning of a deep revision of the physical concepts on the structure of matter.However,who can tell us what exactly are those mesons?Also,it is well known that the pion as lightest of mesons has a finite1size,with a mean charge radius of0.66fm,and that the long range part of the nucleon-nucleon forces necessarily arises from one-pion-exchange.The traditional picture of the nucleus as a collection of neutrons and protons bound together via the strong force has proven remarkable successful in under-standing a rich variety of nuclear properties.However,it is a well grounded achievement of modern nuclear physics that not only nucleons are relevant in the study of nuclear dynamics but that pions and the baryonic resonances like ∆’s and N*play an important role too[4].So,when the nucleus is explored at short distance scales the presence of short lived subatomic particles,such as the pion and delta,are revealed as nuclear constituents.At even shorter distance scales the basic building blocks of matter,the quarks and gluons,are also re-vealed as nuclear constituents.The role of pions,deltas,quarks and gluons in the structure of nuclei is one frontier of modern nuclear physics.This modern picture of the nucleus bring us to the idea to search for new kind of natural radioactivities such as:(π,µ,∆,N∗etc.)-emission during the nuclearfission in the region of heavy and superheavy nuclei.Moreover,new mode of nuclear fission such as:deltonicfission an hyperfission,was also suggested and inves-tigated.So,in1985,D.B.Ion,M.Ivascu and R.Ion-Mihai initiated[5]the investigation of the nuclear spontaneous pion emission as a new possible nuclear radioactivity called nuclear pionic radioactivity(NPIR)with possible essential contributions to the instability of heavy and superheavy nuclei.In this paper we present a short review not only of the main theoretical problems of the NPIR but also of the essential experimental results obtained in these18years of existence of the nuclear pionic radioactivity.Moreover,in this paper by using the recent results on the spontaneousfission half lives T SF of the heavy nuclei with Z>100we present new prediction on the pionic yields in the region of superheavy elements.2FISSION-LIKE MODEL FOR PIONIC RA-DIOACTIVITYThe nuclear pionic radioactivity of a parent nucleus(A,Z)can be considered as an inclusive reaction of form:(A,Z)→π+X(1) where X denotes any configuration offinal particles(fragments,light neutral and charged particles,etc.)which accompany emission process.The inclusive NPIR is in fact a sum of all exclusive nuclear reactions allowed by the conservation laws in which a pion can be emitted by a nucleus from its ground state.The most important exclusive reactions which give the essential contribution to the inclusive NPIR(1)are the spontaneous pion emission accompanied by two body fission::A Z X→π+A1Z1X+A2Z2X(2)where2A=A1+A2Z=Z1+Z2+Zπ(3)Hence,the NPIR is an extremely complex coherent reaction in which we are dealing with a spontaneous pion emission accompanied by a rearrangement of the parent nucleus in two or manyfinal nuclei.Charged pions as well as neutral pions can be emitted during two body or many bodyfission of parent nucleus.The energy released in an exclusive nuclear reaction(1)is given byQπF=Q SF−mπ(4) where Q SF is the energy released during spontaneousfissionQ SF=m(Z,A)−m(Z1,A1)−m(Z2,A2)(5) Then the energy condition for the pionic radioactivity channel isQπF>0(6) orQ SF>mπ(7) Other interesting new natural radioactivities predicted at IFIN-Bucharest are as follows•Muonic radioactivity[25]is a nuclear process in which the lepton pair (µ±,υµ)is emitted during two or many bodyfission of the parent nucleus.For the the nuclear spontaneous emission of(µ±,υµ)in binaryfission we can writeA Z X→µ±+νµ+A1Z1X+A2Z2X(8)A=A1+A2Z=Z1+Z2+Zµ(9)•Lambdonic radioactivity[26]is just a nuclear reaction of formA Z X→Λ0+A1Z1X+A2Z2X(10)A=A1+A2Z=Z1+Z2(11)•Hyperonic radioactivities Σ−,Σ0,Σ+ are also the possible nuclear decays of formA Z X→Σ±,0+A1Z1X+A2Z2X(12) 3A=A1+A2Z=Z1+Z2+ZΣ(13)•Hyperfission or weakfission[27]is afission process in which in one of fragment is hypernucleus:A Z X→A1Z1X+A2Z2Xγ(14)A=A1+A2Z=Z1+Z2(15)•Deltonicfission[28]is also afission process in which in one of fragment contain a delta resonance:A Z X→A1Z1X+A2Z2X∆(16)A=A1+A2Z=Z1+Z2(17)Afission-like model(see Ref.[5])for the pionic radioactivity was regarded as a first stage in the development of an approximate theory of this new phenomenon that takes into account the essential degree of freedom of the system:π-fissility,π-fission barrier height,etc.Therefore,let us considerEπF C(0)=E0C−αmπ(18)EπF S(0)=E0S−(1−α)mπ(19) where E0C and E0S are the usual Coulomb energy and surface energy of the parent nucleus given byE0C=γZ2/A1/3(20)E0S=βA2/3(21) withβ=MeV andγ=0.71MeV.αis a parameter defined so thatαmπand (1−α)mπare the Coulombian and nuclear contributions to the pion mass.For α=1,the entire pion mass is obtained only from Coulomb energy of the parent nucleus.So,by analogy with binaryfission was introduced the pionicfissility XπF which is given byX(α)πF =EπF C(0)E0S−(1−α)mπ(22)4orZ2A−mπ1−(1−α)mπ/E0S(23)In the particular caseα=1we haveXπF=X SF−mπ5 2EπF S(0)−EπF C(0) =2ε2EπF S(0)λ[1+ε2P2(cosθ)+ε4P4(cosθ)+ε6P6(cosθ)+...](29)5whereε2=2.33(1−XπF)−1.23(1−XπF)2+9.50(1−XπF)3−8.05(1−XπF)4+...ε4=1.98(1−XπF)2−1.70(1−XπF)3+17.74(1−XπF)4+...ε6=−0.95(1−XπF)+...(30)R0is the spherical radius andλis a scale factor just as in binary spontaneous fission.In Fig.4and5we present the values of EπF(LD)as well as the nuclear configuration at the saddle point compared with those fromfission(F)or hy-perfission(HF).True barrier height for the pionicfission isEπF=EπF(LD)−∆EπF shell(s.p.)−∆E shell(g.s.)(31) where and∆EπF shell(s.p)and∆E shell(g.s)are correction due to shell effect at saddle point and ground state,respectively.Next,the essential ingredients used for the estimation of the relative pionic yieldsΓπF−37,5(32)AθπF= Z2γA2/3α−(1−α)E0C/E0Sfor parent nuclei with A-odd.For example in Fig.6we presented the experimental values of theτ(θ) compared with thefitted curve(37).Finally,by using(36)-(37)we obtain the following important predictionΓπT CSFδα(A,Z)(38) whereδα(A,Z)=∆θαγA2/3α−(1−α)E0C/E0SΓSF <1,Γπ0,±ΓSF calculated with(38)-(40)forα=1andα=0.75,for even-even and A-odd parent nuclei,are presented in Table2a,b.3EXPERIMENTAL SEARCH FOR NUCLEAR PIONIC RADIOACTIVITY3.1Experimental limits on NPIR-yieldThe pionic radioactivity was experimentally investigated by many authors[13]-[24].A short review of the results obtained on the spontaneous NPIR yields is presented in Table3.73.2Recent results from LIPPE-Obninsk(Russia) Recently Khryachkov et al.[24]presented a new high performance spectrometer for investigation of ternary nuclearfission.The measured characteristics of this spectrometer allow for its successful use in studies of ternaryfission with the emission ofα-particles,tritons,and protons as well as in the search for exotic nuclearfission accompanied by the emission of charged mesons(π±,µ±).This new spectrometer was tested with a reaction of spontaneous252Cf ternary fission.This choice was determined by the fact that this reaction is well studied and the available data can be employed for the performance check of this facility. So,a252Cf layer5mm in diameter with an activity of15fissions/s was placed inside the spectrometer.The measurements were carried out continuously1.5 months.A2D spectrum of the scintillator signals obtained in coincidence with fragments is shown here in Fig.8(see Fig.9in Ref.[24]).Analyzing spectrum in Fig.8has shown that,in the space between the elec-tron and proton regions there are events that cannot be explained by an external background or as effect of neutrons.A detailed analysis of the parameter SF does not allow us to assign these events to protons or electrons.We estimate these events as an indication of the possibility of existence of a ternary nuclear decay with the participation of charged mesons.Subsequently,it is suggested to study the meson emission during the spontaneousfission on this new facility which has a number of substantial advantages.4SUMMARY AND CONCLUSIONSThe experimental and theoretical results obtained on the NPIR can be summa-rized as follows:1.The best experimental limit forπ-yields has been reported for252Cf by Bellini et al.[19].They reached an upper limit of3·10−13,a value close to the theoretical prediction[8].2.The unusual background,observed by Wild et al.[33]in(∆E−E)-energy region below that characteristic for long range alpha emission from257F m was interpreted by Ion,Bucurescu and Ion-Mihai[9]as being produced by negative pions emitted spontaneously by257F m.Then,they inferred value of the pionic yield is:Γπ/ΓSF=(1.2±0.2)·10−3forπ−/fission.In a similar way,Janko and Povinec[22],obtained the yield:Γπ/ΓSF=(7±)·10−5forπ+/fission.3.The supergiant radiohalos(SGH),discovered by Grady and Walker[34] and Laemmlein[35]are interpreted[12]as being theπ−-radiohalos andπ+-radiohalos,respectively.Hence these radiohalos are experimental signatures of the integral record in time of the natural pionic radioactivity from radioactive inclusions in ancient minerals.4.A new interpretation of the experimental bimodalfission is obtained in terms of the unitarity diagrams.is obtained in Ref.[29]So,the presence of the symmetric mode in the fragment mass-distribution at transfermium nuclei can be interpreted as experimental signature of the pionic radioactivity.Hence,it8is expected that this new degree of nuclear instability can becomes dominant at SHE-nuclides.This idea is illustrated not only by the symmetrization of frag-ment mass-yields from SF of the heavy nuclei with98≤Z≤104experimentally observed in Fig.7but also by high values ofΓπ/ΓSF-yields obtained by using the theoretical prediction(38)-(39).5.The nuclides No with A=242−250are expected to be allπF-nuclides while the No-isotopes with A≥252are all SF-nuclides(see Table2a).High pionic yields are obtained for250No(6.67)as well as for258No(7.1·10−2)and 262No(1.2·10−2).6.The nuclides Lr and Rf are all predicted to be SF-nuclides(see Table 2a).7.The nuclides258Sg(1.3·107),259Sg(6.1·106),260Sg(1.2·108),261Sg (1.3·1011),263Sg(5.2·1027)as well as264Hs(1.2·102)all are predicted to be πF-nuclides.Finally,we note that dedicated experiments,using nuclei with theoretically predicted high pionic yields(e.g.258F m,259F m,258No,260No,254Rf,Sg and264Hs(1.2·102)),are desired,since the discovery of the nuclear pionic radioactivity is of fundamental importance not only in nuclear science(e.g., for clarification of high instability of SHE-nuclei)but also for geochemistry and cosmology.References[1]H.Yukawa,Proc.Phys.Math.Soc.Japan.17,48(1935).[2]tes,G.P.S.Occhiallini and C.F.Powell,Nature,100,453(1947).[3]Particle Data Group[4]Delta Cenni etc.Vezi Rep in st year...[5]D.B.Ion,R.Ion-Mihai,M.Ivascu,Ann.of Phys.(N.Y.)171,237(1986),and IPNE-preprint FT-266-1985,Bucharest1985.[6]D.B.Ion,R.Ion-Mihai and M.Ivascu,Rev.Roum.Phys.31,205,209,551(1986).[7]D.B.Ion and R.Ion-Mihai and M.Ivascu,Rev.Roum.Phys.32,299and1037(1987).[8]D.B.Ion and R.Ion-Mihai and M.Ivascu,Rev.Roum.Phys.33,1071and1075(1988).[9]D.B.Ion,D.Bucurescu and R.Ion-Mihai,Rev.Roum.Phys.34,261(1989).[10]D.B.Ion and R.Ion-Mihai,Rev.Roum.Phys.36,163and261(1991).[11]D.B.Ion,Rev.Roum.Phys.37,347(1992).9[12]D.B.Ion and R.Ion-Mihai.Phys.Lett.B338(1994)7.[13]D.Bucurescu et al.,Rev.Roum.Phys.32,849(1987).[14]M.Ivascu et al.,Rev.Roum.Phys.,32,937(1987).[15]J.R.Beene,C.M.Bemis,Jr.and M.L.Halbert,Phys.Rev.C38,569(1988).[16]S.Stanislaus,D.S.Armstrong and D.F.Measday,Phys.Rev.C39,295(1989).[17]C.Cerruti,J.M.Hisleur,J.Julien,L.Legrain,Y.Cassagnou and M.Ribrag,Z.Phys.A329,383(1989).[18]J.Julien et al.,Z.Phys.A332,473(1989).[19]V.Bellini et al.,Proceedings14-th Europhys.Conf.,Rare Nuclear Pro-cesses,Bratislava,22-26October1990,(Ed.P.Povinec),p.116.[20]J.N.Knudson,C.L.Morris,J.D.Bowman,W.C.Sailor and S.J.See-strom,Phys.Rev.C44,2869(1991).[21]Yu.V.Adamchuk,P.E.Vorotnikov,M.A.Voskanyan and G.V.Muradyan,Sov.J.Nucl.Phys.49,932(1989).[22]K.Janko and P.Povinec,Proceedings14-th Europhys.Conf.,Rare NuclearProcesses,Bratislava,22-26October1990,(Ed.Povinec),p.121.[23]H.Otsu,N.Sakamoto,H.Okamura and H.Sakai,Z.Phys.A342,(1992)483[24]Khryachkov et al.,Instr.Exp.Tech.45,615(2002).[25]D.B.Ion,R.Ion-Mihai and M.Ivascu,Rev.Roum.Phys.31,209(1986).[26]D.B.Ion and R.Ion-Mihai and M.Ivascu,Rev.Roum.Phys.33,109(1988).[27]D.B.Ion and R.Ion-Mihai and M.Ivascu,Rev.Roum.Phys.34,461(1989)..[28]D.B.Ion,A.C.D.Ion and R.Ion-Mihai,Rev.Roum.Phys.38,3(1993).[29]D.B.Ion and R.Ion-Mihai,Rom.Journ.Phys.43,179(1998).[30]D.B.Ion and R.Ion-Mihai,Rom.Journ.Phys.44,703(1999).[31]D.B.Ion,Rev.Roum.Phys.37,347(1992).[32]N.E.Holden and D.C.Hoffman,Pure Appl.Chem.,72,1525(2000).[33]J.F.Wild et al.,Phys.Rev.C32,488(1985).10[34]C.A.Grady and R.M.Walker,Proceedings Intern.Symposium on Super-heavy Elements,Lubbock,Texas,March9-14,1978,(Ed.M.A.K.Lodhi),Pergamon,New York(1978),p.191.[35]emmlein,Nature,155,724(1945).Table1:Definitions and characteristic features of(SF,πF,T)-nuclides.Type of Mass Half LivesYield Z2/A<42.5Unitarity(MD)SF-nuclideΓSF<1T SF>T C SF D SFT-nuclideΓSF=1T SF=T C SF DπF+D SFπF−nuclideΓSF>1T SF<T C SF a new phaseΓSF yields for heavy parent nucleiwith Z between Z=100and Z=108,obtained forα=1by using Eqs.(38)-(40)and T SF from Ref.[32].A T SF/T C SFΓπ0/ΓSFF m2422.259·10+003.30·10−021001.046·10−108.59·10−043.85·10−04 2453.080·10+049.32·10−14 1004.753·10−071.17·10−125.16·10−14 2481.017·10+081.48·10−18 1008.000·10−013.28·10−211.54·10−23 2521.114·10+136.12·10−23 1006.242·10−019.36·10−171.41·10−18 2562.948·10+074.84·10−11 1001.310·10+022.75·10−147.93·10−16 2581.045·10+009.46·10−01 1004.753·10−085.44·10−023.91·10−02 2601.130·10+015.95·10−02Md2457.001·10−031.58·10+12 1016.338·10−091.73·10−011.42·10−01 2558.401·10+066.27·10−14 1016.338·10−091.37·10−126.16·10−14 2594.536·10+049.04·10−08Table2a(continued)A T SF/T C SFΓπ0/ΓSFNo2507.061·10−016.67·10+001023.169·10−073.33·10−093.69·10−10 2522.542·10+043.96·10−181029.126·10−041.02·10−241.91·10−27 2561.525·10+061.64·10−161025.324·10−053.53·10−102.97·10−11 2583.389·10+007.06·10−021021.141·10−031.68·10−111.06·10−12 2602.994·10+022.08·10−051021.584·10−101.30·10−027.94·10−031034.183·10−061.39·10−252.14·10−28 2551.680·10+051.77·10−281036.274·10−051.25·10−161.96·10−18 2592.411·10+025.09·10−081037.415·10−052.85·10−111.84·10−121041.521·10−121.16·10−646.44·10−72 2546.496·10−022.96·10−691049.190·10−081.81·10−755.87·10−84 2561.751·10+012.47·10−241041.065·10−056.30·10−392.81·10−43 2583.954·10+018.74·10−141041.331·10−062.13·10−163.55·10−18 2605.648·10+017.16·10−101042.091·10−058.73·10−171.31·10−18 2625.931·10+033.27·10−15DbπF2556.223·10+014.08·10+11SgπF2588.190·10+001.27·10+041067.605·10−084.36·10+062.47·10+07πF2601.977·10+013.24·10+081068.239·10−087.76·10+101.39·10+12πF2632.100·10+015.17·10+271064.119·10−071.01·10−914.69·10−1021073.803·10−097.93·10−017.72·10−011086.338·10−111.08·10+021.84·10+02 2653.734·10−024.25·10−051083.169·10−093.84·10−013.44·10−0112Table2.b:Theoretical predictions of theΓπ0,±/ΓSF yields for heavy parentnuclei with Z between Z=100and Z=108,obtained forα=0.75by using Eqs.(38)-(40)and T SF from Ref.[32].A T SFΓπ−Γπ0Γπ+Cf2385.931·10+014.47·10−03 981.008·10−047.44·10−091.39·10−09 2424.148·10+092.03·10−10 981.800·10+031.39·10−121.20·10−13 2482.852·10+152.83·10−12 988.000·10+107.33·10−153.97·10−16 2501.515·10+153.46·10−11 988.600·10+013.74·10−096.58·10−10 2541.486·10+108.32·10−07 982.282·10−052.41·10−041.14·10−04 2531.546·10+143.18·10−11 992.600·10+035.73·10−091.04·10−09 1002.535·10−111.39·10−011.17·10−01 2449.320·10+001.67·10−02 1001.255·10−042.74·10−085.76·10−09 2464.236·10+041.15·10−07 1001.141·10−033.91·10−114.57·10−12 2507.130·10+109.94·10−13 1001.250·10+028.65·10−145.84·10−15 2545.563·10+103.47·10−10 1003.308·10−047.79·10−072.21·10−07 2573.216·10+109.03·10−09 1001.172·10−119.67·10−019.64·10−01 2591.167·10+011.76·10−01 1001.268·10−101.86·10−011.60·10−01 1012.852·10−111.02·10+074.33·10+07 2471.556·10+003.64·10−01 1013.422·10−021.84·10−083.73·10−09 2571.546·10+071.05·10−07 1011.848·10−046.98·10−052.96·10−05 1027.922·10−122.97·10+003.28·10+00 2517.779·10+011.31·10−05 1022.852·10−079.10·10−111.14·10−11 2548.134·10+071.26·10−14 1021.711·10−056.61·10−109.95·10−11 2571.307·10+043.11·10−06 1023.803·10−112.12·10−011.85·10−01 2592.800·10+055.01·10−07 1023.359·10−091.80·10−031.02·10−03 2621.412·10+017.79·10−02Table2.b(continued)A T SFΓπ−Γπ0Γπ+Lr2531.027·10+035.94·10−15 1036.845·10−041.12·10−164.17·10−18 2571.540·10+046.66·10−10 1039.823·10−075.96·10−052.49·10−05 2611.820·10+047.39·10−07Rf2533.734·10−046.18·10−37 1047.288·10−131.26·10−394.15·10−43 2552.256·10+013.04·10−43 1041.965·10−103.49·10−142.17·10−15 2572.614·10+031.50·10−22 1044.436·10−103.34·10−087.16·10−09 2593.267·10+021.02·10−09 1046.338·10−105.54·10−061.87·10−06 2615.134·10+035.64·10−10 1046.654·10−084.38·10−097.82·10−10 1052.535·10−073.41·10+061.31·10+07 2576.223·10+016.00·10+11 1053.169·10−072.93·10−205.21·10−22 2633.734·10+022.60·10−12Sg2588.190·10+001.78·10+02 1067.605·10−086.47·10+031.42·10+04 2601.977·10+014.86·10+04 1068.239·10−081.89·10+066.93·10+06 2632.100·10+012.31·10+15 1064.119·10−071.22·10−532.22·10−58 1073.803·10−098.76·10−018.66·10−01 1086.338·10−111.42·10+011.81·10+01 2653.734·10−024.15·10−03 1083.169·10−095.78·10−015.51·10−0114Table3:Experimental results on spontaneous NPIR-yieldsYear LaboratoryΓπ0/ΓSFnucleiD.B.Ion et al.259Md<10−5Romania1987IFIN-RomaniaRev.Roum.Phys.32,849M.Ivascu et al.252Cf<10−8Romania1988CEN-Saclay<10−8Z.Phys.A329,383J.R.Beene et al.252Cf1989CEN-Saclay France<10−12Z.Phys,A332,473Yu.Adamchuk et al.252Cf<5·10−8 1989IFIN-BucharestRev.Roum.Phys.34,261·10−3(π−) S.Stanislaus et al.252CfColumbia Canada1989University British<3.1·10−4 Phys.Rev.C39,295J.N.Knudson et al.252Cf1991CEN Saclay France<3·10−13 Bratislava ConferenceK.Janko et al.[22]Proc.257Fm<7·10−5Czechoslovakia1992Tokio UniversityZ.Phys.A342,483(π−)Khryachkov et al.252Cf NotRussiaFigure1:The energies Qπ=QπF calculated by using Eq.(3)and Tables of Wapstra and Audi.16Figure 2:The physical regions from the plane (A,Z)in which the parent nu-clei are able to emit pions by tunnelling pi-fission barr ˆier (++++)and without tunnelling πF −barrier (oooo)(see the text).Figure 3:Definition of πF −barrier as a function of distance between the frag-ments during the pionic fission.17Figure4:The values of the barrier height EπF(LD)for the neutral pion emission during spontaneousfissionfission.Figure5:The nuclear configuration at the saddle point for spontaneousfission (F),spontaneous hyperfission(HF)and spontaneous pionicfission(πF).18Figure6:The experimental values ofτ(θ)are compared wit the linearfit(35).Figure7:The predicted values ofΓπ0Figure8:The experimental results(see Fig.9in Ref.[27])on the light charged particle emission during the spontaneousfission of252Cf.20。

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