Warm nuclei The transition from independent particle motion to collisional dominance

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气候的影响英语作文

气候的影响英语作文

Climate change is one of the most pressing global issues of our time,with farreaching implications for the environment,economy,and society.The effects of climate change are multifaceted and can be observed in various aspects of life on Earth.1.Environmental Impact:The most evident impact of climate change is on the environment.Rising temperatures have led to the melting of polar ice caps and glaciers, causing sea levels to rise.This not only threatens coastal cities and lowlying islands but also disrupts the habitats of many species,leading to a loss of biodiversity.Additionally, climate change has been linked to more frequent and severe weather events,such as hurricanes,floods,and droughts,which can devastate ecosystems and human settlements.2.Agricultural Effects:Agriculture is heavily dependent on stable climate conditions. Changes in temperature and precipitation patterns can lead to reduced crop yields, affecting food security globally.Droughts can decimate harvests,while floods can destroy crops and soil fertility.Moreover,warmer temperatures can shift the ranges of pests and diseases,complicating agricultural practices.3.Health Implications:Climate change can have direct and indirect effects on human health.Direct effects include heatrelated illnesses and deaths during heatwaves.Indirect effects are more complex and can include the spread of vectorborne diseases as warmer climates expand the habitats of diseasecarrying insects.Additionally,air quality can be affected by higher temperatures,exacerbating respiratory issues.4.Economic Consequences:The economic impacts of climate change are significant and varied.Industries such as agriculture,fisheries,and tourism are particularly vulnerable to the effects of climate change.Insurance costs may rise due to an increase in natural disasters,and infrastructure may require costly adaptations to withstand extreme weather events.On the other hand,some regions may experience economic benefits from a longer growing season or access to new shipping routes.5.Social and Political Ramifications:Climate change can exacerbate social inequalities and lead to political instability.Displacement of populations due to environmental disasters can create refugee crises,straining international relations and local resources. Additionally,competition for dwindling resources like water and arable land can lead to conflicts.6.Mitigation and Adaptation Efforts:In response to the impacts of climate change,there is a growing emphasis on mitigation and adaptation strategies.Mitigation involves reducing greenhouse gas emissions to slow the rate of climate change,while adaptation involves adjusting to the effects that are already occurring.This can include developingmore resilient infrastructure,investing in renewable energy,and implementing policies that promote sustainable development.cation and Awareness:Raising awareness about the impacts of climate change is crucial for driving societal and political cation plays a key role in informing the public about the science behind climate change,its consequences,and the steps that can be taken to mitigate its effects.8.International Cooperation:Addressing climate change requires a coordinated global response.International agreements,such as the Paris Agreement,aim to unite countries in efforts to reduce emissions and support those most vulnerable to climate change impacts.In conclusion,the impacts of climate change are widespread and interconnected, affecting every aspect of life on Earth.It is essential that individuals,communities,and nations work together to mitigate these effects and adapt to the changes that are already underway.。

2023年高考英语外刊时文精读专题14气候变化与珊瑚礁

2023年高考英语外刊时文精读专题14气候变化与珊瑚礁

2023年高考英语外刊时文精读精练 (14)Climate change and coral reefs气候变化与珊瑚礁主题语境:人与自然主题语境内容:自然生态【外刊原文】(斜体单词为超纲词汇,认识即可;下划线单词为课标词汇,需熟记。

)Human beings have been altering habitats—sometimes deliberately andsometimes accidentall y—at least since the end of the last Ice Age. Now, though, that change is happening on a grand scale. Global warming is a growing factor. Fortunately, the human wisdom that is destroying nature can also be brought to bear on trying to save it.Some interventions to save ecosystems are hard to imagine andsucceed. Consider a project to reintroducesomething similar to a mammoth(猛犸象)to Siberiaby gene-editing Asian elephants. Their feeding habits could restore the grassland habitat that was around before mammoths died out, increasing the sunlight reflected into space and helping keep carbon compounds(碳化合物)trapped in the soil. But other projects have a bigger chance of making an impact quickly. As we report, one example involves coral reefs.These are the rainforests of the ocean. They exist on vast scales: half a trillion corals line the Pacific from Indonesia to French Polynesia, roughly the same as the number of trees that fill the Amazon. They are equally important harbor of biodiversity. Rainforests cover18% of the land’s s urface and offer a home to more than half its vertebrate(脊椎动物的)species. Reefs occupy0.1% of the oceans and host a quarter of marine(海洋的)species.And corals are useful to people, too. Without the protection which reefs afford from crashing waves, low-lying islands such as the Maldives would have flooded long ago, and a billion people would lose food or income. One team of economists has estimated that coral’s global ecosystem services are worth up to $10trn a year. reefs are, however, under threat from rising sea temperatures. Heat causes the algae(海藻) with which corals co-exist, and on which they depend for food and colour, to generate toxins(毒素)that lead to those algae’s expulsion(排出). This is known as “bleaching(白化)”, and can cause a coral’s death.As temperatures continue to rise, research groups around the world are coming up with plansof action. Their ideas include identifying naturally heat-resistant(耐热的)corals and moving themaround the world; crossbreeding(杂交)such corals to create strains that are yet-more heat-resistant; employing genetic editing to add heat resistance artificially; transplantingheat-resistant symbiotic(共生的)algae; and even repairing with the bacteria and other micro-organismswith which corals co-exist—to see if that will help.The assisted evolution of corals does not meet with universal enthusiasm. Without carbon reduction and decline in coral-killing pollution, even resistant corals will not survive the century. Some doubt whetherhumans will get its act together in time to make much difference. Few of these techniques are ready for action in the wild. Some, such as gene editing, are so controversial that it is doubtful they will be approved any time soon. scale is also an issue.But there are grounds for optimism. Carbon targets are being set and ocean pollution is being dealt with. Countries that share responsibilities for reefs are starting to act together. Scientific methods can also be found. Natural currents can be used to facilitate mass breeding. Sites of the greatest ecological and economical importance can be identified to maximise benefits.This mix of natural activity and human intervention could serve as a blueprint (蓝图)for other ecosystems. Those who think that all habitats should be kept original may not approve. But when entire ecosystems are facing destruction, the cost of doing nothing is too great to bear. For coral reefs, at least, if any are to survive at all, it will be those that humans have re-engineered to handle the future.【课标词汇精讲】1.alter (通常指轻微地)改动,修改;改变,(使)变化We've had to alter some of our plans.我们不得不对一些计划作出改动。

冬天作文 英语

冬天作文 英语

Winter is a season of stark contrast and unique beauty.It is a time when the world is blanketed in a layer of frost,transforming landscapes into a serene tableau of white.The air turns crisp and the days grow shorter,yet the season offers a sense of tranquility and a break from the hustle and bustle of the warmer months.The Arrival of WinterWinter often arrives with the first frost,signaling the end of autumns colorful foliage. Trees shed their leaves,revealing their bare branches against the cold,clear sky.The transition can be abrupt,with temperatures dropping sharply and the first snowfall covering the ground in a pristine layer of white.The Chill of WinterThe cold is one of winters defining characteristics.It seeps into every corner,making it necessary to bundle up in warm clothing.The chill is not only felt in the air but also in the icy touch of the wind that bites at exposed skin.Despite the cold,winter can be a time of warmth,as families gather indoors,sharing meals and stories around the fireplace.Winter ActivitiesDespite the cold,winter offers a variety of activities.Skiing,snowboarding,and ice skating become popular pastimes,as people take advantage of the snowy conditions. Children build snowmen and engage in snowball fights,while adults might enjoy a quiet walk in the snow,admiring the winter scenery.The Beauty of WinterWinters beauty is often understated.The snowcovered landscapes can be breathtaking, with the sun casting a soft glow on the white expanse.The nights are long and dark,but they are also filled with the magic of the northern lights in some regions,a natural light display that dances across the sky in vibrant colors.Winter WildlifeAnimals too have their own ways of adapting to the winter season.Some hibernate,while others migrate to warmer climates.Those that remain must find ways to survive the harsh conditions,often seen foraging for food in the snow or huddling together for warmth.Winter Festivals and TraditionsCulturally,winter is a time for celebration.Holidays such as Christmas,Hanukkah,and New Years Eve bring people together in a spirit of joy and festivity.Decorations adorn homes and streets,and the scent of traditional winter foods fills the air.The End of WinterAs winter progresses,the days slowly begin to lengthen,and the promise of spring is on the horizon.The snow starts to melt,revealing the first signs of new life and growth. Winters end is a time of renewal and anticipation for the warmer months ahead.In conclusion,winter is a season of change,offering a different pace of life and a unique set of experiences.It is a time to appreciate the quiet beauty of nature,to enjoy the warmth of loved ones,and to look forward to the rebirth of spring.。

新视野大学英语读写教程三unit8

新视野大学英语读写教程三unit8

难句解释
In the wake of this announcement, governments hurried to draft guidelines for the unknown, a future filled with incredible possibilities.
译文:就在克隆宣告成功之后,为了一个未知世界,一 个充满各种不可思议的可能性的未来,各国政府立即起 草指导方针。
Word Using
1.implication n. (1)含义,暗示 (2)牵连,卷入,涉 及 (3)可能的影响(后果)
Something that is suggested
Translation
I resent your implication that my work is not satisfactory.
Para2 In the wake of this announcement, governments hurried to draft guidelines for the unknown, a future filled with incredible possibilities. President Clinton ordered a national commission to study the legal and moral implications of cloning. Leaders in Europe, where most nations already prohibit human cloning, began examining the moral implications of cloning other species.
The human cloning situations that experts consider most frequently fall into two broad categories: 1) parents who want to clone a child, either to provide transplants for a dying child or to replace that child, and 2) adults who for a variety of reasons might want to clone themselves.

2022年考研考博-考博英语-华南师范大学考试全真模拟易错、难点剖析AB卷(带答案)试题号:71

2022年考研考博-考博英语-华南师范大学考试全真模拟易错、难点剖析AB卷(带答案)试题号:71

2022年考研考博-考博英语-华南师范大学考试全真模拟易错、难点剖析AB卷(带答案)一.综合题(共15题)1.单选题Changing from solid to liquid, water takes in heat from all substances near it, and this()produces artificial cold surrounding it.问题1选项A.absorptionB.transitionC.consumptionD.interaction【答案】A【解析】考查名词词义辨析。

A: absorption “吸收”;B: transition “过渡,转变”;C: consumption “消费”;D: interaction “相互作用”。

句意:水从固体转变为液体,吸收了周围所有物质的热量,这种吸收产生了周围的人工寒冷。

根据语境和句意,这里所指的是吸热,因此A最合适。

2.单选题It is no wonder that they always hold()hope for the future because they are raised in the greenhouse.问题1选项A.exaggeratedB.amplifiedC.extravagantD.luxurious【答案】A【解析】考查形容词词义辨析。

A: exaggerated “夸大的,言过其实的” ;B: amplified “扩大;放大”;C: extravagant “过度的,过分的;浪费的”;D: luxurious “奢侈的”。

句意:难怪他们总是对未来抱有夸大的希望,因为他们是在温室里长大的。

结合语境,故A为正确答案。

3.单选题The man to whom we handed the forms pointed out that they had not been()filled in.问题1选项A.consequentlyB.regularprehensivelyD.properly【答案】D【解析】考查副词词义辨析。

风的形成原理英文名词解释

风的形成原理英文名词解释

风的形成原理英文名词解释The Formation Mechanism of Wind: An ExpositionIntroduction:Wind, a phenomenon found across the globe, is a constant presence in our lives. It shapes landscapes, influences climates, and affects our daily activities in numerous ways. But have you ever wondered how wind is formed? In this article, we delve into the intricate mechanisms that give rise to wind, shedding light on the fascinating processes and principles behind this natural phenomenon.Thermal Gradients and Differential Heating:At the core of wind formation lies the concept of thermal gradients and differential heating. Solar radiation, the primary source of energy that drives Earth's weather patterns, is unevenly distributed across the planet due to varying angles of incidence. As a result, different regions receive dissimilar amounts of heat, setting the stage for the formation of wind.Convection and the Atmospheric Circulation Cells:To understand convection, imagine placing a pot of water on a stove. As the heat rises from the stove, it warms the water at the bottom of the pot. The warm water expands, becomes less dense, and rises to the surface. Meanwhile, the cooler water at the surface sinks and replaces the rising warm water. This process creates a continuous circular flow, known as convection.Similarly, in the Earth's atmosphere, solar radiation warms the air near the surface. The warm air rises due to its lower density, creating a low-pressure area. As the warm air ascends, it moves toward higher altitudes, where it cools and eventually descends. This descending air creates a high-pressure area. These rising and sinking motions, combined with the rotation of the Earth, give birth to large-scale circulation patterns known as atmospheric circulation cells.Hadley Cell:One such atmospheric circulation cell is the Hadley cell, named after George Hadley, the British meteorologist who first described it. The Hadley cell is located near the equator and plays a crucial role in shaping the global wind patterns. It consists of three main components: the Intertropical Convergence Zone (ITCZ), the trade winds, and the subtropical high-pressure belts.The ITCZ, characterized by low atmospheric pressure, forms due to the convergence of trade winds from the northern and southern hemispheres. As warm, moist air ascends in the ITCZ, it cools, condenses, and forms clouds, resulting in heavy rainfall and thunderstorms.The trade winds, on the other hand, blow from the subtropical high-pressure belts towards the equator. These winds are responsible for carrying heat from the subtropics to the equatorial regions. They have been historically important for maritime trade routes, facilitating global exploration and commerce.Ferrel and Polar Cells:In addition to the Hadley cell, there are two other atmospheric circulation cells named after William Ferrel and the polar regions. The Ferrel cell exists between the Hadley and polar cells and plays a vital role in redistributing heat from the lower to higher latitudes. This cell features prevailing westerlies, which blow from west to east in mid-latitudes.Lastly, the polar cell encompasses the polar regions and involves the descent of cold air at the poles, leading to the formation of polar high-pressure belts. The circulating air from the polar region meets the westerlies from the Ferrel cell, resulting in polar easterlies blowing from east to west.Coriolis Effect and Wind Direction:The Coriolis Effect, a phenomenon arising from the Earth's rotation, influences the direction of wind. Due to the conservation of angular momentum, objects moving acrossthe Earth's surface are deflected to the right in the Northern Hemisphere and to the left in the Southern Hemisphere.The Coriolis Effect influences the wind direction by deflecting air masses as they move from areas of high pressure to areas of low pressure. This deflection, coupled with the pressure gradient force caused by pressure differences, contributes to the establishment of prevailing wind patterns, such as the trade winds, westerlies, and polar easterlies.Conclusion:Wind, a captivating natural phenomenon, is a product of complex interactions between solar radiation, convection, atmospheric circulation cells, and the Coriolis Effect. By understanding the mechanisms behind wind formation, we gain insight into the intricate workings of our planet's climate system. This knowledge not only deepens our appreciation for the forces of nature but also aids in studying and predicting weather patterns, benefiting diverse sectors ranging from agriculture to renewable energy.。

Globalwarming学习笔记

Globalwarming学习笔记

Global warmingThe vanishing(消失) northThere are benefits in the melting of the Arctic, but the risks are much greaterNOW that summer is here, the Arctic(北极地区)is crowded with life. Phytoplankton(浮游植物)are blooming in its chilly seas. Fish, birds and whales are gorging on(饱吃)them. Millions of migratory(流浪的)geese are in their northern breeding grounds(滋生地,繁殖地). AndBetween now and early September, when the polar(极地的)pack ice (浮冰块)shrivels(皱缩)to its summer minimum, they will pore over (注视,集中精力阅读)the daily sea ice reports of America’s National Snow and Ice Data Centre. Its satellite data will show that the ice has shrunk far below(远低于)the long-term average. This is no anomaly (异常,反常事物): since the 1970s the sea ice has retreated(撤退)by around 12% each decade. Last year the summer minimum was 4.33m square km (1.67m square miles)—almost half the average for the 1960s.The Arctic’s glaciers(冰川), including those of Greenland’s vast(广阔的) ice cap(冰盖), are retreating. The land is thawing(融化): the area covered by snow in June is roughly(概略的)a fifth less than in the 1960s. The permafrost(永久冻土)is shrinking. Alien plants, birds, fish and animals are creeping (爬行,慢慢移动)north: Atlantic mackerel (鱼类,鲭), haddock(黑线鳕)and cod(鳕鱼)are coming up in Arctic nets. Some Arctic species will probably die out(灭绝).is a stunning(极好的)illustration(例证)of global warming, the causeworld would be mad to ignore them.Less feedback, pleaseAs our special report(专题报道)shows in detail, the Arctic is warming roughly twice as fast as the rest of the planet. Since the 1950s the lower atmosphere has warmed by a global average of 0.7 degrees Celsius(摄氏度); Greenland’s air has warmed by 1.5 degrees. The main reason appears to be a catalytic warming effect, triggered by global warming. When snow or ice melt, they are replaced by darker melt-water pools, land or sea. As a result, the Arctic surface absorbs more solar heat. This causes local warming, therefore more melting, which causes morewarming, and so on. This positive feedback shows how even a small change to the Earth’s systems can trigger much greater ones.Some scientists also see a tipping-point—another feared term in the climatology lexicon—in the accelerating diminution of the sea ice. The term describes the moment at which the planet shifts from one environmental state to another: in this case, from an Arctic with summer sea ice to one without it. By the end of this century—perhaps much sooner—there will probably be frequent summers with no sea ice at all. Arctic peoples have also noticed what is going on. Inuit hunters are finding the sea ice too thin to bear their sleds. Arctic governments are starting to see a bonanza in the melt. The Arctic is stocked with minerals that were hitherto largely inaccessible, including an estimated 30% of undiscovered reserves of natural gas and 13% of undiscovered oil reserves. A combination of high commodity prices, proactive governments, technological progress and melting ice will help bring these to market. Encouraged by Arctic governments and dwindling reserves elsewhere, oil companies are flocking north like migrating geese to explore the continental shelves of Alaska, Canada, Greenland, Norway and Russia. Canada and Russia also hope to develop their Arctic shipping-lanes, which the melt is making accessible. Russia’s Northern Sea Route, hugging the Siberian coast, cuts the normal distance betweenEurope and Asia by more than a third. It will help ferry Russia’s Arct ic resources to Asian markets, and could one day be a wider boost to world trade.These exciting developments carry risks, however. Many fear for Arctic cultures—a Canadian Inuit argues despairingly for her “right to be cold”. Others foresee conflict between Arctic countries scrambling for the region’s resources. Greens warn of environmental risks in developing them: a big oil spill would be disastrous for fragile Arctic ecosystems. The igloos have goneSuch fears are reasonable, but often exaggerated. Traditional Arctic peoples have been changed far more by Westernisation than they will be by melting ice. None lives in an igloo these days. And everywhere except Russia their rights have been recognised. Nor is conflict much of a worry. The Arctic is no terra nullius. Most of it is demarcated, and Arctic countries have a commercial incentive to keep the peace. Last year Russia and Norway settled an old dispute over their maritime border; soon they will open the border region to oil firms.The risks of pollution from bilge water, mining effluent and spilt oil are real. Yet the Arctic is not unprotected: it is, by and large, among the most regulated oil provinces. Its development will also be slower and morecautious than greens fear. Even with little sea ice, the Arctic will remain forbiddingly cold, remote, stormy and therefore expensive to operate in. The worry that needs to be taken most seriously is climate change itself. The impact of the melting Arctic may have a calamitous effect on the planet. It is likely to disrupt oceanic circulation—the mixing of warm tropical and cold polar waters, of which the Gulf Stream is a part—and thawing permafrost will lead to the emission of masses of carbon dioxide and methane, and thus further warming. It is also raising sea levels. The Greenland ice sheet has recently shed around 200 gigatonnes of ice a year, a fourfold increase on a decade ago. If the warming continues, it could eventually disintegrate, raising the sea level by seven metres. Many of the world’s biggest cit ies would be inundated long before that happened. Some scientists argue that the perils are so immediate that mankind should consider geoengineering the atmosphere to avert them (see article). They may turn out to be right, but there could be enormous risks involved.A slower but safer approach would be to price greenhouse-gas emissions, preferably through a carbon tax, which would encourage the adoption of cleaner technologies (see article). That shift would be costly, but the costs of inaction are likely to be larger.In the end, the world is likely to get a grip on global warming. The survival instinct demands it. But it is likely to lose a lot of the unique Arctic first. That would be a terrible pity.。

尊重汇暖流的英语作文

尊重汇暖流的英语作文

Respecting the Warm Current is a profound concept that can be applied to various aspects of life,from personal relationships to global environmental issues.Heres an essay that explores the idea in depth:In the vast ocean of life,there exists a phenomenon known as the warm current,which is a metaphor for the positive and nurturing forces that flow through our existence.This warm current can be the kindness of a stranger,the support of a friend,or the love of a family member.It is essential to respect and cherish these warm currents,as they are the lifeblood of our emotional and social wellbeing.Understanding the Warm CurrentThe warm current is not a onetime event but a continuous flow of positive energy.It is the small acts of kindness that accumulate over time,creating a reservoir of goodwill and compassion.Recognizing the presence of this warm current in our lives is the first step towards respecting it.It requires us to be mindful and appreciative of the good that surrounds us,even in the midst of challenges and hardships.Cultivating Respect for the Warm CurrentRespecting the warm current involves more than just acknowledging its presence.It means actively nurturing and protecting it.This can be done by reciprocating kindness, showing gratitude,and fostering an environment where positive energy can thrive.It also involves standing up against negativity and promoting a culture of respect and understanding.The Impact of the Warm CurrentThe impact of the warm current is farreaching.It can transform individuals,communities, and even nations.When people come together in a spirit of cooperation and mutual respect,they can overcome adversity and create a more harmonious society.The warm current has the power to heal emotional wounds,bridge cultural divides,and inspire collective action towards common goals.Challenges to the Warm CurrentDespite its transformative potential,the warm current faces numerous challenges.These include apathy,selfishness,and the erosion of social bonds due to modern lifestyles.Tocounter these challenges,it is crucial to actively seek out and engage with the warm current.This can be done by participating in community activities,volunteering,and simply being there for others in times of need.The Role of Education and MediaEducation and media play a pivotal role in promoting respect for the warm current.They can help by raising awareness about the importance of kindness and compassion,and by showcasing positive role cational curricula should include lessons on empathy and social responsibility,while media outlets should highlight stories of unity and goodwill.ConclusionIn conclusion,respecting the warm current is not just about acknowledging the good in our lives but actively participating in its preservation and enhancement.It is a collective responsibility that requires us to be vigilant and proactive.By doing so,we can ensure that the warm current continues to flow,enriching the lives of all it touches.This essay serves as a reminder of the importance of recognizing and respecting the warm currents in our lives,which can lead to a more compassionate and connected world.。

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a rXiv:n ucl-t h /97943v122Sep1997Warm nuclei:The transition from independent particle motion to collisional dominance 1by Helmut Hofmann 2Physik Department,TUM,D-85747Garching Fedor A.Ivanyuk and Alexander G.Magner Institute for Nuclear Research,252028,Kiev-28Physik Department,TUM,D-85747Garching We study large scale collective dynamics of isoscalar type and examine the in-fluence of interactions residual to independent particle motion.It is argued that for excitations which commonly are present in experimental situations such inter-actions must not be neglected.They even help to justify better the assumption of locality,both in time as well as in phase space,which is necessary not only for such classic approaches to collective motion as the ”cranking model”but also for the more general picture of a transport process.With respect to dissipation,our results are contrasted with those of wall friction.PACS 21.60.Ev,21.60.Cs,24.10.Pa,24.75+i 1IntroductionAfter the discovery of the shell model it has become customary to base the descrip-tion of collective motion on the picture of single particles moving independently within a deformed mean field.This approach was introduced in the early 50’ties by A.Bohr andB.Mottelson to portray low energetic collective excitations,and to the present day there can be little doubt that this approximation is adequate for that regime.It is somewhat as-tonishing,however,that this picture still is vindicated by many groups even for situations where the nucleons are heated up to considerable amount,say to temperatures of a fewMeV.After all,in the very early days of nuclear physics collective motion of large scale was considered to be governed by dissipative processes,which in turn imply the presence offluctuating forces.Such a picture may be condensed into the one equation,which was suggested by Kramers[1]already in1940to describe nuclearfission.It reads∂∂Q P∂P dV(Q)∂P P∂P∂Pf(Q,P,t)(1)and has the structure typical of a Fokker-Planck equation.Actually,Kramers consider-ations strictly adhered to classical motion,in which case the diffusion coefficient is given by the Einstein relation D pp=γT;in the quantum case another term appears.As is well known,Kramers has used this equation to calculate the decay rate for a meta-stable situation likefission,in generalization of the famous Bohr-Wheeler formula.In these days the origin of dissipation was attributed to the strong”correlations”among the nucleons, as they can be understood within or follow from N.Bohr’s compound nucleus—and which by definition occur”incoherently”.In this lecture we want to look at this transition from”independent particle motion to collisional dominance”in the view of the”linear response approach”,a complete version of which can be found in[2].This discussion will be complemented by presenting new aspects in the relation to wall friction,following the more recent considerations of the group of W.J.Swiatecki,J.Blocki and others(see[3]).The applicability of linear response theory may be understood by the following arguments.First,one my note that the solution of (1)can be written in the following wayf(Q,P,t)= d Q0d P0K(Q,P,t;Q0,P0,t0)f(Q0,P0,t0)(2) where K(Q,P,t;Q0,P0,t0)is interpreted as the conditional probability for the system to move from Q0,P0at t0to Q,P at time t.On both sides of this relation the distribution f, the”joint probability”,may be replaced by conditional probabilities defining the transition say from a t0to thefinal time t through an intermediate step at t1.The resulting relation is nothing else but the Chapman-Kolmogorov equation.(For a discussion of such general properties we may refer to the book by van Kampen[4]).The procedure just described may be repeated as often as one likes.Starting from the given equation(1)one may introduce arbitrarily small time stepsδt in completely rigorous manner.The reason for this behavior is found in the fact that this equation(assumedly)describes a genuinely Markovian process.It is exactly at this stage where a possible justification of a linear response approach has to set in.In essence this requires two steps.First of all,if theδt may be chosen to be sufficiently small on the collective time scale one may construct the K(Q,P,t;Q0,P0,t0) by describing collective motion locally to harmonic order.Secondly,if theδt is large enough on the microscopic scale the dynamics of the intrinsic degrees of freedom does not have to be followed in complete ing such hypothesis it is possible to construct the form of K(Q,P,t;Q0,P0,t0)explicitly and to derive microscopic expressions for the individual transport coefficients.Moreover,this procedure even allows one to generalize Kramers’equation to include quantum effects,which show up,first of all,in generalized diffusion coefficients;for details see[2].One step necessary in this direction is to interpret the K(Q,P,t;Q0,P0,t0)from above as a”propagator”for Wigner functions.It is clear that this locally harmonic approximation(LHA)is closely related to prop-erties which one expects to hold true for Fokker-Planck equations.Nevertheless,there are various ways to check that the goal set at the beginning is actually reached in the very end.For instance,it is possible to see a)whether the local propagators observe Marko-vian behavior,or b)whether or not the process is indeed”diffusive”.As it turns out,the latter feature ceases to be given for unstable modes at low temperatures.We will not have time to go any further into these questions.We shall,however,be able to touch upon another condition for the LHA to be valid,the”smoothness”of the transport coefficients as function of the collective variables.2Linear response theory for collective motionIn the sequel let’s suppose to be given a HamiltonianˆH(ˆx i,ˆp i,Q)for the nucleons’dynamics in a deformed meanfield,with the deformation being parameterized by the shape variable Q,whose average ˆH(ˆx i,ˆp i,Q) represents the total energy of the system E tot (eventually including both the Strutinsky re-normalization as well as”heat”).The equation for average motion(EOM)for Q(t)can then be constructed from energy conservation. From Ehrenfest‘s equation it follows:0=d∂Q t≡˙Q ˆF(ˆx i,ˆp i,Q) t(3)All one needs to do to get the equation of motion for Q(t)is to express the average ˆF(ˆx i,ˆp i,Q) t as a functional of Q(t).Following the scheme of the LHA one may expandtheˆH(Q)around any given Q0to have:ˆH(Q(t))=ˆH(Q0)+(Q(t)−Q0)ˆF+1∂Q2(Q0) qs Q0,T0(4)The effects of the coupling term(Q(t)−Q0)ˆF may now be treated by linear response theory,exploiting as a powerful tool the causal response function˜χ˜χ(t−s)=Θ(t−s)idt E coll≡−d2˙q2+C(ω1)dtS(7)which correctly expresses the exchange between collective motion into heat.(Theω1 represents one of the possible(complex!)frequencies of the system,as determined from the secular equation).3Forced energy transfer to a system of independent particlesAs is clearly seen from(7),the friction force parameterizes that energy which is transfered irreversibly to the intrinsic system.Let us study this feature within a simple model,with the simplifications consistingfirst of all in neglecting self-consistency.This means that we take a nucleus at given deformation Q0which is exposed to a time dependent externalfield at somefixed polarization.We may thus use a Hamiltonian of the type given in(4),where theˆF is chosen to represent this polarization,but where the last term on the right is neglected.The Q(t)−Q0=q(t)is then a truly external quantity,which shall be called q(t)in the sequel,and which is not subject to a subsidiary condition of the type k ˆF t=q(t),which follows from(3)and(4).As another important simplification we will assume theˆH(Q0)to represent the ensemble of independent particles as given by the deformed shell model at zero temperature.Such a system has been studied in a series of papers which aimed at a new understand-ing of the physics of wall friction(see[3]and references given there).The time dependence of the q(t)was assumed to be of the form q(t)=q0sin(Ωt)and the system was followed for one period simulating the solutions of the Schr¨o diger equation numerically.Let us examine this problem within linear response theory.The energy transfered to the intrinsic degrees of freedom within one cycle may be evaluated from the following well known formula:∆E int with their∆E and calculate the total unperturbed energy E0as the sum over single particle energies.However,one may as well go ahead and introduce already here a friction coefficient by the following reasoning.As thedE int(2π/Ω)=Ω=γ(Ω)with v≡˙q,˙q0=Ωq0and≡Φ′′(Ω)(10)Ωwith the functionΦ′′(Ω)being the so called relaxation function.Notice that the frequency appearing here is the(real)one given by the externalfield.This is very different from the form indicated in(7).As mentioned there,theω1is the actual,complex frequency the collective motion has around the Q0.Incidentally,a form of the typeχ′′(Ω)/Ωmay appear (for friction)even within the linear response formulation as described before,but only if the coupling between collective and intrinsic motion is treated perturbatively,see section 3.3.2of[2].In case of small frequencies one may apply the so called zero frequency limit γ(Ω=0).In Figs.1and2we present numerical results for the quantity∆E/E0=a spherical deformation,the same situation which has been considered also in[6].Theone presented in Fig.2corresponds to a case where the unperturbed system has a sizableoctupole deformation ofα=0.3.In this case the wall formula is not recovered(at leastnot the one corresponding to the spherical configuration used in thefigure,whereas therecould be some small dependence on deformation).We may say that similar results areobtained for vibrations of other multi-polarity.As an interesting feature we may note that”macroscopic”friction is smaller the more complex the microscopic strength distributionis.We would not like to speculate whether or not this fact is related to an increase ofchaotic behavior of the nucleonic degrees of freedom.In[3]only forced vibrations around the sphere were considered.As can be seen fromtheir Fig.1,the simulations of the Schr¨o dinger equation indicate a straight behavior ofthe functional dependence of∆E/E0onηsomewhat below the wall formula.In such anon-perturbative calculation an average over a full cycle will differ in at least one respectfrom our procedure.Starting from formula(3)(which is a correct one),the ˆF(ˆx i,ˆp i,Q) t will no longer be a linear functional of q(s).If one still were expressing this quantity by anintegral like ∞−∞ds˜χ(t−s)q(s)the˜χ(t−s)itself would have to be a complicated functional of q(s).Apparently,it behaves such that the average over the amplitude of oscillation(in the deformation degree of freedom)in the end leads to a linear relation withη.It seems to us that this average may in a sense be considered analogous to our averaging in the spectrum,as is done in the Strutinksy method.As a matter of fact,experience tells one that averaging in energy e over an interval ofγav e=10MeV corresponds to an average in Q over aγav Q=γav e/e F≈1/4—which corresponds nicely to the amplitude chosen in[3]! 4The influence of collisional damping on transport propertiesFrom the discussion of the last section it is clearly seen that for nuclear collective mo-tion it is not possible to justify a local friction force within the mere picture of independentparticles.For such a model one has to employ averaging procedures of one kind or other.Moreover,we have observed that quite large intervals in the averaging parameters are in-volved if for the latter one chooses energy.This fact clearly hints to an inherent deficiencyof the underlying model:At the excitations which are at stake in common experimentalsituations the picture of particles moving in a meanfield without”collisions”does notapply!For this reason the notion of theˆH(Q0)to be simply given by the deformed shellmodel has been given up a long time ago whenever transport properties where calculatedwithin the linear response approach(see[2]for a detailed discussion).Instead it was as-sumed that the particles are dressed by self-energies having both real and imaginary parts:Σ(ω±iǫ,T)=Σ′(ω,T)∓i(¯hω−µ)2+π2T2(¯hω−e k−Σ′(ω))2+ Γ(ω)Γ0(for a detailed discussion see[6,2]).Let us demonstrate these features with the help of the zero frequency limit of friction.To sufficient accuracy the latter can be written asγ(0)=∂χ′′(ω)2T(12)On the very right the correlation function has been introduced which is related to the response function by the famousfluctuation dissipation theorem(FDT)¯hχ′′(ω)= tanh(¯hω/2T)ψ′′(ω).The definition ofψis similar to that given forχin(5),with two im-portant exceptions:The commutator is to be replaced by an anti-commutator and from the operatorˆF one has to subtract its unperturbed average value ˆF .The general microscopic expression forψ′′(ω)isψ′′(ω)=ψ02πδ(ω)+Rψ′′(ω)withψ0=T χT−χ(0) (13) with the Rψ′′(ω)being regular atω=0.TheχT is the isothermal susceptibility which measures how the(quasi-)static expectation value ˆF qs changes with Q if the temperature is kept constant.The singularity atω=0is called”heat pole”,in analogy to a similar pole in the density density strength distribution for infinite matter being responsible for heat diffusion there.A structure like that given in(13)is obtained only in the strict case of pure Hamiltonian dynamics(i.e.when the correlation function is formally calculated in the basis of exact eigen states).Within our approximation of collisional damping the heat pole changes like0ψ′′(ω)=ψ02πδ(ω)=⇒0ψ′′(ω)=ψ0¯hΓTΓTψ0ΓT χT−χ(0) (15)EstimatingχT−χ(0)simply in the independent particle model this component of friction turns into the one foundfirst by Ayik and N¨o renberg within the model of DDD[10].In [6]this form has been evaluated as function of temperature for all T.A slightly modified version is shown in Fig.4.The fully drawn line and the dashed one correspond the0γ(0)of(15)with the c of(11)put equal to c=20MeV and c→∞,respectively.The curve with the heavy dots corresponds to the contribution of the remaining part of the correlation function.As demonstrated in[6](see also[2]),the distinction of the two contributions can simply be made in terms of the matrix elements of the(one-body)operatorˆF with the shell model states.The0γ(0)is solely to be associated to the diagonal elements.That they may lead to dissipation,nevertheless,(and thus to entropy production)is due to the effects of”collisions”.From Fig.4it is seen that at smaller T the0γ(0)takes on very large values.They actually exceed several times that of wall friction(shown by the horizontal line),and they seem to be too large as required by experimental evidence(see[2]).The reason can be traced back to the following properties of static susceptibilities.Let usfirst rewrite the difference appearing inψ0as given by the left part of the following equation: 1ψ0=χT−χad(16)TThe difference of the adiabatic to the isothermal susceptibility can be seen to be small in the nuclear case;it is proportional to the square of the cross derivative of the free energy with respect to Q and T,a quantity which for the system underlying Fig.4even vanishes. So the culprit must be theχad−χ(0)!However,this difference is known to vanish for truly ergodic systems,namely systems whose states are non-degenerate.As an additional condition one only needs to have a sufficiently narrow distribution of the energies of the excited states.Apparently,these conditions are not met for the case shown in Fig.4,and most likely both of them are violated.First of all,the microscopic evaluation of the matrix elements is dominated by the model of independent particles,with all the many degeneracies ap-pearing there.Secondly,applying the canonical distribution to parameterize the thermal excitations of a nuclear system the spread in energy is exaggerated artificially.On the other hand,there is little doubt that the true compound configurations will remove these spurious contributions.First of all,because a consideration of the compound states will re-quire a more correct treatment of the residual interactions.In this way the many artificial degeneracies of the deformed shell model will be removed.Secondly,thermal excitations will have to be treated on the basis of the micro canonical ensemble.To simply simulate these effects one may just apply the reduction indicated in(16)to remove the unphysical contribution from the heat pole.6Dissipation within Landau theoryAs seen above,the friction coefficient tends to decrease with T at larger temperature. This feature is evident for the component0γ(0)(see(15)and Fig.4),but as discussed in [6]it will eventually hold true also for the other component(see also[11])under certain circumstances(like approximating the imaginary part of the self-energy in”common”relaxation time approximation(with c=∞)).Such a behavior with T reminds one of the two body viscosity of hydrodynamics. In[12]a model has been suggested in which the intrinsic dynamics is described by the Landau-Vlasov equation and where thefiniteness of the system exhibiting shape dynamics is introduced through special boundary conditions.In Fig.5we present a calculation of the friction coefficient(as function of T)for quadrupole vibrations about a sphere,done within an extension of this model.The dashed and the fully drawn lines correspond to the hydrodynamical limit,for two different choices of the parameter c entering the relaxation time used in the collision term of the Landau-Vlasov equation.The squares correspond to contributions from different peaks in the correlation function,where the full ones are suposed to correspond to the analog of the”heat pole”.Similarities with the behavior shown in Fig.4are evident.So far however,it is yet unclear exactly where the contribution comes from,solely from the differenceχT−χad as it should,or whether also in this model there is the spurious effect coming from a non-vanishing differenceχad−χ(0).Further studies are under way.7SummaryTo describe collective motion as a Markovian transport process one needs to be able to define transport coefficients which vary smoothly with the macroscopic variables,which by the way have to include the parameter which measures the thermal excitation.We have demonstrated that such a condition can hardly be fulfilled within the picture of the deformed shell model.On the other hand,we have shown that residual interactions may do the job,the better the larger the thermal excitation.At present the situation is less clear at smaller temperatures.Whether or not pairing alone will do is currently under investigation.It may well be,however,that even in this regime one may want to include more of the configurations as given by the nuclear compound model.References1)H.A.Kramers,Physica7(1940)2842)H.Hofmann,Phys.Rep.284(4&5),(1997)137-3803)J.Blocki,J.Skalski and W.J.Swiatecki,Nucl.Phys.A594(1995)1374)N.G.van Kampen:”Stochastic processes in physics and chemistry”,North-Holland,1981,Amsterdam5)D.Kiderlen,H.Hofmann and F.A.Ivanyuk,Nucl.Phys.A550(1992)4736)H.Hofmann,F.A.Ivanyuk and S.Yamaji,Nucl.Phys.A598(1996)1877)G.F.Bertsch,Z.Phys.A289(1978)1038)F.A.Ivanyuk,H.Hofmann,V.V.Pashkevich and S.Yamaji,Phys.Rev.C55(1997)17309)F.A.Ivanyuk and H.Hofmann,to be published10)S.Ayik and W.N¨o renberg,Z.Phys.A309(1982)12111)S.Yamaji,F.A.Ivanyuk and H.Hofmann,Nucl.Phys.A612(1997)112)A.G.Magner,H.Hofmann,V.M.Kolomietz and S.Shlomo,Phys.Rev.C51(1995)245713)A.G.Magner and H.Hofmann,to be publishedFigure captionsFig.1:Average energy transfer to a spherical system of independent particles by an external quadrupole perturbation,calculated within linear response.Otherwise the same picture is adopted as in[3].Fig.2:Same as for Fig.2but for a system with octupole deformation.Fig.3:Ratio of friction to inertia along thefission path of224Th(for details see text).Fig.4:The contribution of the”heat pole”to friction for collective quadrupole oscillations of a system of particles in a square well potential(see text).Fig.5:Friction for quadrupole oscillations calculated from a Landau-Vlasov approach to a finite nucleus.23456789T [M e V ]020040060080010001200/h。

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