The Effect of a Hot–Wet Environment on Adhesively Bonded Joints Under a Sustained Load

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英语作文环境与自然

英语作文环境与自然

Natural disasters and human destruction
Floods and droughts
Extreme weather events such as floods and droughts can cause widespad damage to human settlements and infrastructure
• The impact of human activities on the environment
• Environmental protection measures and policies
01
Introduction
Thhis writing is focused on the relationship between the English writing environment and nature, exploring how the natural world influences and inspirations English writing
02
Analysis of current environmental issues
Global climate change
1 2
Rising global cultures
Caused by greenhouse gas emissions, leading to melting ice caps, rising sea levels, and extreme weather events
English Writing Environment and
Nature
目录
• Introduction • Analysis of current environmental issues • The impact of natural environment on human

The effects of climate change

 The effects of climate change

Climate change is a significant and rapidly growing global issue that is having major impacts on the environment, economy, and human health. The effects of climate change are wide-ranging and can be felt across the world, with consequences including extreme weather events, rising sea levels, and changes in ecosystems. In this essay, we will explore the various effects of climate change and their implications for our planet.One of the most visible effects of climate change is the increased frequency and intensity of extreme weather events. Heatwaves, droughts, hurricanes, and heavy rainfall are becoming more common, leading to widespread devastation and loss of life. These extreme weather events are particularly harmful to vulnerable populations and have a significant economic impact, as infrastructure and agriculture are often damaged or destroyed.Rising sea levels are another consequence of climate change, driven by the melting of polar ice caps and glaciers. As sea levels continue to rise, coastal areas and low-lying islands are at risk of being inundated, leading to displacement of communities and loss of valuable land. Additionally, saltwater intrusion into coastal aquifers can contaminate freshwater sources, impacting both human and ecological systems.Changes in ecosystems are also a significant effect of climate change, with shifts in temperature and precipitation patterns altering habitats and disrupting species' life cycles. This can lead to loss of biodiversity, as some species are unable to adapt to changing conditions and face extinction. In addition, thespread of invasive species and diseases can further destabilize ecosystems, leading to negative impacts on agriculture and food security.The effects of climate change extend beyond the environment and into the realm of human health. Rising temperatures can exacerbate air pollution and worsen respiratory conditions, while changes in precipitation patterns can lead to waterborne diseases and food insecurity. Additionally, extreme weather events can cause physical injury and mental health issues, particularly for those who are displaced or directly impacted by disasters.The economic impact of climate change is substantial, with costs associated with extreme weather events, loss of infrastructure, and damage to agriculture and fisheries. This can strain national economies and lead to increased poverty and inequality, particularly in developing countries that lack the resources to adapt to and mitigate the effects of climate change.In response to the effects of climate change, it is crucial that we take action to reduce our greenhouse gas emissions and adapt to the changes that are already occurring. This includes transitioning to renewable energy sources, improving energy efficiency, and implementing policies to reduce deforestation and promote sustainable land use. Additionally, it is important to invest in climate-resilient infrastructure and technologies, and to support vulnerable communities in adapting to the impacts of climate change.In conclusion, the effects of climate change are far-reaching and have significant implications for the environment, economy, and human health.Addressing this global challenge requires urgent and coordinated action at all levels, from individual efforts to national and international policies. By working together to mitigate the effects of climate change and adapt to its impacts, we can build a more sustainable and resilient future for our planet.。

人类对气候的影响英语作文

人类对气候的影响英语作文

人类对气候的影响英语作文英文回答:Climate change is one of the most pressing issues facing our planet today. Human activities are the primary driver of climate change, and we have a responsibility to take action to mitigate its effects.The burning of fossil fuels for energy and transportation releases greenhouse gases into the atmosphere. These gases trap heat and cause the planet to warm. The effects of climate change are already being felt around the world in the form of rising sea levels, extreme weather events, and changing plant and animal life.We can take action to reduce our greenhouse gas emissions and mitigate the effects of climate change. We can switch to renewable energy sources, such as solar and wind power. We can drive less and more efficiently, and we can improve the energy efficiency of our homes andbusinesses.Taking action on climate change is essential to protect our planet and our future. We all have a role to play in reducing greenhouse gas emissions and building a more sustainable future.中文回答:气候变化是当今地球面临的最紧迫的问题之一。

焓湿图(中英文)开放版

焓湿图(中英文)开放版

CLM believes that it is incumbent on manufacturers to serve the industry by regularly disseminating information gathered through laboratory research, testing programs, and field experience.The CLM Air Conditioning Clinic series is one means of knowledge sharing. It is intended to acquaint a technical audience with various fundamental aspects of heating, ventilating, and air conditioning (HVAC). We have taken special care to make the clinic as uncommercial and straightforward as possible. Illustrations of CLM products only appear in cases where they help convey the message contained in the accompanying text.This particular clinic introduces the reader to psychrometry, the science concerned with the physical laws that govern air – water mixtures.CLM认为,制造商有责任通过定期传播通过实验室研究,测试程序和现场经验收集的信息来为行业服务。

CLM空调章节系列是知识共享的一种方式。

气候变化对环境的影响英语作文

气候变化对环境的影响英语作文

气候变化对环境的影响英语作文Climate change is a pressing issue that has significant impacts on the environment. 气候变化是一个紧迫的问题,对环境有着重大影响。

One of the most noticeable effects of climate change is the rise in global temperatures. 气候变化最引人注目的影响之一是全球气温的上升。

This increase in temperature leads to melting ice caps and glaciers, resulting in rising sea levels. 这种温度上升导致冰川融化,海平面上升。

Rising sea levels threaten coastal communities and ecosystems, as well as increasing the risk of flooding. 上升的海平面威胁到沿海社区和生态系统,增加了洪水的风险。

In addition, extreme weather events, such as hurricanes and typhoons, are becoming more frequent and severe due to climate change. 此外,由于气候变化,极端天气事件,如飓风和台风,变得更加频繁和严重。

Furthermore, climate change also affects biodiversity, leading to the loss of habitats and species extinction. 此外,气候变化还影响生物多样性,导致栖息地的丧失和物种灭绝。

The disruption of ecosystems dueto climate change can have far-reaching consequences for the foodchain and overall ecosystem stability. 由于气候变化而导致生态系统的破坏可能对食物链和整体生态系统稳定性产生深远影响。

温室效应英文

温室效应英文

查看文章英文演讲稿环保温室效应the responsibility of the youth2009-08-25 20:22Good evening ladies and gentlemen,Today I want to talk about the responsibility of the youth on the environment issues.When I was young, I always dreamed about traveling around the world. One of the places that I want to visit most is the Great Barrier Reef in Australia. In my imagination, that must be a warm and clean place full of beautiful coral reefs, fishes like Nemo, kind and understanding dolphins, colorful sea turtles. They said that the Great Barrier Reef can even be seen from outer space! However, it is also said that due to the climate change mass coral bleaching events occurred in the summer of 1998,2002 and 2006, Beautiful scenery will vanish in the year 2050. That means when I am ready to pay a visit to Australia with my beautiful wife maybe, I can only see the faded coral reefs which are whiter than white.Throughout history, the young have been the driving force in social change. Now more than ever is the time for youth across the country to become global warming activists and join the movement. Youth should take the responsibility to help solve the problem as soon as possible.At a United Nations World summit on the world economy, Ex Premier Zhu Rongji said “economic development and environmental protection are interlinked and can not be separated from each other.” He also said, “A new pattern that guarantees a clean environment must replace the traditional pattern. That the new one is called sustainable development.”But as individuals, what we can do to bid our effort in it ?Here are some tips :1. Change the lightReplacing one regular bulb with a compact fluorescent light bulb will save 150 pounds of carbon dioxide a year.2. Recycle moreIt is said that in Japan, people are requested to separate the waste in different kinds. And the trash man would only collect one kind of waste each day. That can be a perfect way to recycle.3. Use less hot waterIt takes a lot of energy to heat water. Use less hot water by installing a low flow showerhead and washing your clothes in cold or warm water.4. Adjust your air conditionerMoving your air conditioner just 2 degrees in winter and up 2 degrees in summer. You could save about 2,000 pounds of carbon dioxide a year with this simple adjustment.5. Plant a treeA single tree will absorb one ton of carbon dioxide over its lifetime.6. Turn off electronic devicesSimply turning off your television, DVD player and computer when you’re not using t hem will save you thousands of pounds of carbon dioxide a year.Global warming has already been a very serious problem in the world. Even in our generation, varieties of birds singing are silenced, beautiful coral reefs are no longer be seen. It is a real pity that when I’m telling my son about the dream when I was young. He can never know a place named Great Barrier Reef.Thank you very much.英文资料-温室效应!The Greenhouse EffectThe greenhouse effect is a naturally occurring process that aids in heating the Earth's surface and atmosphere. It results from the fact that certain atmospheric gases, such as carbon dioxide, water vapor, and methane, are able to change the energy balance of the planet by absorbing longwave radiation emitted from the Earth's surface. Without the greenhouse effect life on this planet would probably not exist as the average temperature of the Earth would be a chilly -18° Celsius, ratherthan the present 15° Celsius.As energy from the sun passes through the atmosphere a number of things take place (see Figure 7h-1). A portion of the energy (26 % globally) is reflected or scattered back to space by clouds and other atmospheric particles. About 19 % of the energy available is absorbed by clouds, gases (like ozone), and particles in the atmosphere. Of the remaining 55 % of the solar energy passing through the Earth's atmosphere, 4 % is reflected from the surface back to space. On average, about 51 % of the sun'sradiation reaches the surface. This energy is then used in a number of processes, including the heating of the ground surface; the melting of ice and snow and the evaporation of water; and plant photosynthesis. The heating of the ground by sunlight causes the Earth's surface to become a radiator of energy in the longwave band (sometimes called infrared radiation). This emission of energy is generally directed to space (see Figure 7h-2). However, only a small portion of this energy actually makes it back to space. The majority of the outgoing infrared radiation is absorbed by the greenhouse gases (see Figure 7h-3 below).Figure 7h-3: Annual (1987) quantity of outgoing longwave radiationabsorbed in the atmosphere.(Image created by the CoVis Greenhouse Effect Visualizer).Absorption of longwave radiation by the atmosphere causes additional heat energy to be added to the Earth's atmospheric system. The now warmer atmospheric greenhouse gas molecules begin radiating longwave energy in all directions. Over 90 % of this emission of longwave energy is directed back to the Earth's surface where it once again is absorbed by the surface. The heating of the ground by the longwave radiation causes the ground surface to once again radiate, repeating the cycle described above, again and again, until no more longwave is available for absorption. The amount of heat energy added to the atmosphere by the greenhouse effect is controlled by the concentration of greenhouse gases in the Earth's atmosphere. All of the major greenhouse gases have increased in concentration since the beginning of the Industrial Revolution (about 1700 AD). As a result of these higher concentrations, scientists predict that the greenhouse effect will be enhanced and the Earth's climate will become warmer. Predicting the amount of warming is accomplished by computer modeling. Computer models suggest that a doubling of the concentration of the main greenhouse gas, carbon dioxide, may raise the average global temperature between 1 and 3° Celsius. However, the numeric equations of computer models do not accurately simulate the effects of a number of possible negative feedbacks. For example, many of the models cannot properly simulate the negative effects that increased cloud cover would have on the radiation balance of a warmer Earth. Increasing the Earth's temperature would cause the oceans to evaporate greater amountsof water, causing the atmosphere to become cloudier. These extra clouds would then reflect a greater proportion of the sun's energy back to space reducing the amount of solar radiation absorbed by the atmosphere and the Earth's surface. With less solar energy being absorbed at the surface, the effects of an enhanced greenhouse effect may be counteracted.A number of gases are involved in the human caused enhancement of the greenhouse effect (see Table 7h-1 below). These gases include: carbon dioxide (CO2); methane (CH4); nitrous oxide (N2O); chlorofluorocarbons (CFxClx); and tropospheric ozone (O3). Of these gases, the single most important gas is carbon dioxide which accounts for about 55 % of the change in the intensity of the Earth's greenhouse effect. The contributions of the other gases are 25 % for chlorofluorocarbons, 15 % for methane, and5 % for nitrous oxide. Ozone's contribution to the enhancement ofgreenhouse effect is still yet to be quantified. Concentrations of carbon dioxide in the atmosphere are now approaching 360 parts per million (see Figure 7a-1). Prior to 1700, levels of carbon dioxide were about 280 parts per million. This increase in carbon dioxide in the atmosphere is primarily due to the activities of humans. Beginning in 1700, societal changes brought about by the Industrial Revolution increased the amount of carbon dioxide entering the atmosphere. The major sources of this gas include fossil fuel combustion for industry, transportation, space heating, electricity generation and cooking; and vegetation changes in natural prairie, woodland, and forested ecosystems. Emissions from fossil fuel combustion account for about 65 % of the extra carbon dioxide now found in our atmosphere. The remaining 35 % is derived from deforestation and the conversion of prairie, woodland, and forested ecosystems primarily into agricultural systems. Natural ecosystems can hold 20 to 100 times more carbon dioxide per unit area than agriculturalsystems.Artificially created chlorofluorocarbons are the strongest greenhouse gas per molecule. However, low concentrations in the atmosphere reduce their overall importance in the enhancement of the greenhouse effect. Current measurements in the atmosphere indicate that the concentration of these chemicals may soon begin declining because of reduced emissions. Reports of the development of ozone holes over the North and South Poles and a general decline in global stratospheric ozone levels over the lasttwo decades has caused many nations to cutback on their production and use of these chemicals. In 1987, the signing of the Montreal Protocol agreement by forty-six nations established an immediate timetable for the global reduction of chlorofluorocarbons production and use. Since 1750, methane concentrations in the atmosphere have increased by more than 140 %. The primary sources for the additional methane added to the atmosphere (in order of importance) are rice cultivation, domestic grazing animals, termites, landfills, coal mining, and oil and gas extraction. Anaerobic conditions associated with rice paddy flooding results in the formation of methane gas. However, an accurate estimate of how much methane is being produced from rice paddies has been difficult to obtain. More than 60 % of all rice paddies are found in India and China where scientific data concerning emission rates are unavailable. Nevertheless, scientists believe that the contribution of rice paddies is large because this form of crop production has more than doubled since 1950. Grazing animals release methane to the environment as a result of herbaceous digestion. Some researchers believe the addition of methane from this source has more than quadrupled over the last century. Termites also release methane through similar processes. Land-use change in the tropics, due to deforestation, ranching, and farming, may be causing termite numbers to expand. If this assumption is correct, the contribution from these insects may be important. Methane is also released from landfills, coal mines, and gas and oil drilling. Landfills produce methane as organic wastes decompose over time. Coal, oil, and natural gas deposits release methane to the atmosphere when these deposits are excavated ordrilled.The average concentration of nitrous oxide in the atmosphere is now increasing at a rate of 0.2 to 0.3 % per year. Sources for this increase include land-use conversion; fossil fuel combustion; biomass burning; and soil fertilization. Most of the nitrous oxide added to the atmosphere each year comes from deforestation and the conversion of forest, savanna and grassland ecosystems into agricultural fields and rangeland. Both of these processes reduce the amount of nitrogen stored in living vegetation and soil through the decomposition of organic matter. Nitrous oxide is also released into the atmosphere when fossil fuels and biomass are burned. However, the combined contribution of these sources to the increase ofthis gas in the atmosphere is thought to be minor. The use of nitrate and ammonium fertilizers to enhance plant growth is another source of nitrous oxide. Accurate measurements of how much nitrous oxide is being released from fertilization have been difficult to obtain. Estimates suggest that the contribution from this source may represent from 50 % to 0.2 % of nitrous oxide added to the atmosphere annually.Ozone's role in the enhancement of the greenhouse effect has been difficult to determine scientifically. Accurate measurements of past long-term (more than 25 years in the past) levels of this gas in the atmosphere are currently unavailable. Concentrations of ozone gas are found in two different regions of the Earth's atmosphere. The majority of the ozone (about 97 %) found in the atmosphere is localized in the stratosphere at an altitude of 15 to 55 kilometers above the Earth's surface. In recent years, the concentration of the stratospheric ozone has been decreasing because of the buildup of chlorofluorocarbons in the atmosphere (see Lecture 7e). Since the late 1970s, scientists have discovered that total column ozone amounts over Antarctica in the springtime have decreased by as much as 70 %. Satellite measurements have indicated that the zone from 65° North to 65° South latitude has had a 3 % decrease in stratospheric ozone since 1978. Ozone is also highly concentrated at the Earth's surface. Most of this ozone is created as an artificial by product of photochemical smog.In summary, the greenhouse effect causes the atmosphere to trap more heat energy at the Earth's surface and within the atmosphere by absorbing and re-emitting longwave energy. Of the longwave energy emitted back to space,90 % is intercepted and absorbed by greenhouse gases. Without the greenhouse effect the Earth's average global temperature would be -18° Celsius, rather than the present 15° Celsius. In the last few centuries, the activities of humans have directly or indirectly caused the concentration of the major greenhouse gases to increase. Scientists predict that this increase may enhance the greenhouse effect making the planet warmer. Some experts estimate that the Earth's average global temperature has already increased by 0.3 to 0.6° Celsius, since the beginning of this century, because of this enhancement. Predictions of future climates indicate that by the middle of the next century the Earth's global temperature may be 1 to 3° Celsius higher than today.Table 7h-1: Gases involved in the Greenhouse Effect: past and presentconcentration and sources.Greenhouse GasConcentration1750Concentration1995Percent Change Natural and Anthropogenic SourcesCarbon Dioxide 280 ppm 360 ppm 29 % Organic decay; Forest fires; Volcanoes;Burning fossil fuels; Deforestation; Land-use change Methane 0.70 ppm 1.70 ppm 143 % Wetlands; Organic decay; Termites; Natural gas & oil extraction; Biomass burning; Rice cultivation; Cattle; RefuselandfillsNitrous Oxide 280 ppb 310 ppb 11 % Forests; Grasslands; Oceans; Soils; Soil cultivation; Fertilizers; Biomass burning; Burning of fossil fuels Chlorofluorocarbons (CFCs) 0 900 ppt Not Applicable Refrigerators;Aerosol spray propellants; Cleaning solventsOzone Unknown Varies with latitude and altitude in the atmosphere Global levels have generally decreased in the stratosphere and increased near the Earth's surface Created naturally by the action of sunlight on molecular oxygen and artificially through photochemical smog productionGreenhouse EffectA worldwide greenhouse effect might produce a dangerously warmer world.Since the late 19th century, the average global temperature has increased between0.54° F and 1.08° F (0.3° C and 0.6 ° C). Internationally, 1990 was the hottestyear on record since official weather records first started being kept by the Britishin about 1860.Estimates (估计) of global average temperatures have projected (突出) anincrease of as much as 9° F(5° C) before the year 2100. Such a rise in global temperature would pr oduce new patterns (模式) and extremes of drought (干旱) and rainfall, which would seriously disrupt (破坏) food production. This could potentially (潜在地) cripple (削弱) the North American corn belt (北美生产玉米的地带), which produces much of the world's grain, leading to much higher food prices, and even less food for the Third World than they already have. However, it would also mean that some countries which are further north would be able to grow crops they had never been able to before, although there is less land as you move north from the corn belt.The other serious worry is that rising sea levels from the melting of the polar (极地的) ice caps could severely flood many countries. A rise in sea levels of one metre, which many ex perts are predicting (预言) by the year 2100 (and some as soon as 2030), would flood 15 percent of Egypt, and 12 percent of Bangladesh (孟加拉国) . The Maldives (马尔代夫) in the Indian Ocean would almost completely disappear. Most of the countries which would su ffer most from a rise in sea levels are the poor island states, so the islands in the Caribbean (加勒比海), South Pacific, Mediterranean and Indian Ocean have formed the Alliance (联盟) of Small Island States, AOSIS, so they have a louder voice in internatioanl politics and can ma ke the richer developed world listen to their problems. Closer to home, Britain would lose most of East Anglia (英格兰的拉丁名称), and to protect the coast line would cost an estimated 5 to 10 billion pounds.温室效应英语作文本文来自作文地带:/daxue/20071220/740.htmlGlobal Warming 全球暖化温室效应导致全球变暖global warming“温室效应”是指地球大气层上的一种物理特性。

Effect of pH and Temperature on Enzyme Activity

Effect of pH and Temperature on Enzyme Activity

Effect of pH and Temperature on EnzymeActivityEnzymes are biological catalysts that speed up chemical reactions in living organisms. They are essential for many biochemical processes, such as digestion, metabolism, and DNA replication. Enzyme activity is affected by many factors, including pH and temperature. In this article, we will discuss the effect of pH and temperature on enzyme activity.Effect of pH on Enzyme ActivitypH is a measure of the acidity or basicity of a solution. Enzymes have an optimal pH range at which they function most efficiently. This optimal pH range varies for different enzymes. For example, the optimal pH for pepsin, an enzyme found in the stomach that breaks down proteins, is around 2.0, which is very acidic. In contrast, the optimal pH for alkaline phosphatase, an enzyme found in the liver and bones, is around 9.0, which is very basic.When the pH of the environment deviates from the optimal pH range for an enzyme, the enzyme's activity decreases. This is because enzymes are sensitive to changes in pH. At low pH levels, the enzyme may denature or lose its shape, making it unable to bind to its substrate and catalyze the reaction. At high pH levels, the enzyme may become too alkaline, which can also cause denaturation.Effect of Temperature on Enzyme ActivityTemperature is another critical factor that affects enzyme activity. Enzymes have an optimal temperature range at which they function best. For most enzymes, this optimal temperature is around 37°C, which is body temperature. However, there are exceptions to this rule. For example, enzymes in psychrophiles, organisms that thrive in extreme cold, have an optimal temperature range of 0-15°C.When the temperature of the environment deviates from the optimal temperature range for an enzyme, the enzyme's activity decreases. At low temperatures, enzymes have less kinetic energy, which means they move more slowly. This slows down the rate of the reaction and reduces enzyme activity. On the other hand, high temperatures can cause enzymes to denature and lose their shape, rendering them inactive.pH and Temperature InteractionThe effect of pH and temperature on enzyme activity can also interact with each other. Enzymes may have different optimal temperature ranges depending on the pH of the environment. For example, acid phosphatase, an enzyme found in the prostate gland, has an optimal temperature range of 30-40°C at pH 4.5, but an optimal temperature range of 55-60°C at pH 7.0.ConclusionIn conclusion, pH and temperature are critical factors that affect enzyme activity. Enzymes have optimal pH and temperature ranges at which they function most efficiently. Deviations from these optimal ranges can reduce enzyme activity by causing denaturation or slowing down the reaction. The effect of pH and temperature on enzyme activity can also interact with each other, meaning optimal temperature ranges may change depending on the pH of the environment. Understanding the effect of pH and temperature on enzyme activity is essential for researchers and scientists studying biochemistry and biology.。

学术综合英语下作文全球变暖

学术综合英语下作文全球变暖

学术综合英语下作文全球变暖英文回答:Global Warming: A Pressing Issue.Global warming, a pressing issue of our time, has been gaining widespread recognition and concern. Its effects are far-reaching, impacting various aspects of our planet and human well-being.One of the primary consequences of global warming is the alteration of weather patterns. As the Earth's temperature rises, it results in more frequent and intense extreme weather events, such as hurricanes, heatwaves, droughts, and floods. These events wreak havoc on communities, causing widespread destruction, loss of life, and economic disruption.Another significant impact is the rise in sea levels. As glaciers and polar ice caps melt due to warmingtemperatures, the volume of water in the oceans increases. This surge in sea levels poses a serious threat to coastal populations, particularly low-lying areas that are vulnerable to flooding and erosion.Furthermore, global warming poses significant threats to ecosystems and biodiversity. The changing climatic conditions disrupt the delicate equilibrium of ecosystems, affecting species' habitats, distribution, and survival. Some species may struggle to adapt to the altered conditions, leading to population declines or extinction.The consequences of global warming are not limited to environmental impacts; they also have profound implications for human health. Extreme weather events, such as heatwaves and storms, can cause heat-related illnesses, respiratory problems, and injuries. Air pollution levels often rise during these events, exacerbating respiratory issues and contributing to cardiovascular diseases.The economic ramifications of global warming are also substantial. Damage caused by extreme weather events canlead to billions of dollars in losses for infrastructure, property, and agriculture. Rising sea levels and coastal erosion can displace populations and disrupt economic activities in coastal regions.Addressing global warming requires a concerted global effort. Transitioning to renewable energy sources, promoting energy efficiency, and reducing carbon emissions are crucial steps towards mitigating the effects of climate change. Sustainable practices, such as deforestationcontrol and responsible land use, can help preserve ecosystems and reduce greenhouse gas emissions.Furthermore, adaptation strategies are essential to cope with the inevitable impacts of global warming. Implementing early warning systems for extreme weather events, strengthening infrastructure resilience, and investing in research and development to improve climate adaptation technologies are important measures for reducing vulnerabilities.Global warming poses a significant threat to our planetand the well-being of humanity. By understanding its causes and effects, we can take collective action to mitigate its impacts and build a more sustainable and resilient futurefor all.中文回答:全球变暖,一个紧迫的问题。

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This article was downloaded by: [Tulane University]On: 03 June 2014, At: 20:14Publisher: Taylor & FrancisInforma Ltd Registered in England and Wales Registered Number: 1072954 Registered office: Mortimer House, 37-41 Mortimer Street, London W1T 3JH, UKThe Journal of AdhesionPublication details, including instructions for authors andsubscription information:/loi/gadh20The Effect of a Hot–Wet Environmenton Adhesively Bonded Joints Under aSustained LoadX. Han a b , A. D. Crocombe a , S. N. R. Anwar a c , P. Hu b & W. D. Liba Department of Mechanical Engineering Science , University ofSurrey , Guildford , UKb School of Automotive Engineering , Dalian University ofT echnology , Dalian , PR Chinac Civil Engineering , University of Mataram , Mataram , IndonesiaPublished online: 10 Mar 2014.PLEASE SCROLL DOWN FOR ARTICLETaylor & Francis makes every effort to ensure the accuracy of all the information (the “Content”) contained in the publications on our platform. However, Taylor & Francis,our agents, and our licensors make no representations or warranties whatsoever as tothe accuracy, completeness, or suitability for any purpose of the Content. Any opinions and views expressed in this publication are the opinions and views of the authors,and are not the views of or endorsed by Taylor & Francis. The accuracy of the Content should not be relied upon and should be independently verified with primary sourcesof information. Taylor and Francis shall not be liable for any losses, actions, claims, proceedings, demands, costs, expenses, damages, and other liabilities whatsoever or howsoever caused arising directly or indirectly in connection with, in relation to or arising out of the use of the Content.This article may be used for research, teaching, and private study purposes. Any substantial or systematic reproduction, redistribution, reselling, loan, sub-licensing, systematic supply, or distribution in any form to anyone is expressly forbidden. Terms &D o w n l o a d e d b y [T u l a n e U n i v e r s i t y ] a t 20:14 03 J u n e 2014The Effect of a Hot–Wet Environment on Adhesively Bonded Joints Under aSustained LoadX.HAN 1,2,A.D.CROCOMBE 1,S.N.R.ANWAR 1,3,P.HU 2,and W.D.LI 21Department of Mechanical Engineering Science,University of Surrey,Guildford,UK 2School of Automotive Engineering,Dalian University of Technology,Dalian,PR China3Civil Engineering,University of Mataram,Mataram,IndonesiaThe aim of this research was to develop numerical modelling techniques for simulating the simultaneous effects of moisture,elevated temperature,and applied load on the performance of adhesively bonded joints.Associated experimental data are also reported.The degradation process of the joints was modelled using a fully-coupled approach,with the moisture concentration affecting the stress distribution and the stress state affecting the moisture diffusion analy-ses simultaneously.Further,the stress analysis contains a moisture-dependent creep model to accommodate viscous effects,and both swelling and thermal strains were included in the simulation.The gov-erning parameters adopted in the modelling procedure were deter-mined from experimental work based on the bulk adhesive.The joint response was monitored throughout the ageing process and good cor-relation was found between the experimental and numerical results.KEYWORDS Adhesion by diffusion;Ageing;Aluminium and alloys;Epoxy;Finite element analysis1.INTRODUCTIONAdhesives have been increasingly used in modern structural engineering with specific benefits including more joining flexibility and a better stressReceived 7August 2013;in final form 5October 2013.Address correspondence to A.D.Crocombe,Department of Mechanical Engineering Science,University of Surrey,Guildford,UK.E-mail:a.crocombe@Color versions of one or more of the figures in the article can be found online at /gadh.The Journal of Adhesion ,90:420–436,2014Copyright #Taylor &Francis Group,LLC ISSN:0021-8464print =1545-5823online DOI:10.1080/00218464.2013.853176420D o w n l o a d e d b y [T u l a n e U n i v e r s i t y ] a t 20:14 03 J u n e 2014distribution and fatigue resistance [1–3].One of the major concerns which inhibit a more widespread application of adhesive bonding is its prolonged durability in hostile service conditions,including moisture absorption,residual shrinkage,sustained mechanical,thermal,and swelling stresses,and the concomitant joint degradation [3–6].In earlier studies,Kinloch [7]stated that the mechanical performance of adhesive joints may be adversely affected when exposed to aqueous envir-onments,especially at an elevated temperature.Research by Adams et al.[1]revealed that thermal stresses coupled with the external loads influenced the mechanical behaviour of adhesive joints.Brewis et al.[8]studied single-lap joints (SLJs)bonded with an epoxide-polyamide adhesive exposed to a warm moist environment for up to 2500h and concluded that the moist-ure degradation was due to plasticisation of the adhesive.Crocombe [9]developed a framework (interfacial and cohesive)to assess the effect of environmental degradation and subsequent cohesive failure in adhesively bonded structures.Finite element simulation was carried out on joints bonded with FM1000(Cytec 1,New Jersey,USA)exposed to water over periods of time assuming Fickian moisture diffusion.Many subsequent researchers focused on the combined experimental–numerical method to investigate the performance of adhesive joints under a hot–humid environ-ment and developed a range of prediction methodologies [10–13].Liljedahl et al.[14]studied a sequentially coupled stress-diffusion analysis in bonded steel joints.It was found that the residual stresses relaxed significantly over time and did not further degrade the joint strength significantly.Sugiman et al.[15,16]presented a combined experimental–numerical approach to investigate the static and fatigue behaviour of adhesively bonded structures immersed in deionised water at 50 C for up to 2years.Experiments revealed that joint strength and fatigue life decreased with increasing moisture content and levelled off towards saturation.Hu et al.[17]investigated the effects of cyclic thermal loading with a cycle period of 2h on adhesively bonded joints for up to 8weeks.A degraded cohesive zone model was selected to simulate the degradation process in numerical modelling and good agreement was achieved with the experimental data.Banea et al.[18]discussed the effect of temperature on Mode I fracture toughness of adhesive joints through both experimental and numerical methods.Results showed that adhesives have mechanical properties that vary with temperature and the simulated predic-tions of the joint fracture toughness matched the experiment results well.Abdel Wahab et al.[19]developed an experimental–analytical–numerical method to study the moisture diffusion in adhesively bonded composite struc-tures under different degradation conditions (temperature,relative humidity).With the diffusion coefficients obtained from experiment,good agreement was found between the analytical and numerical results.However,to date,coupled situations where stress and moisture uptake occur simultaneously have not been studied.In this current work,prior toEffect of a Hot–Wet Environment 421D o w n l o a d e d b y [T u l a n e U n i v e r s i t y ] a t 20:14 03 J u n e 2014numerical simulation,experimental work was undertaken on bulk adhesive and adhesive joints to measure (a)the stress dependency of moisture diffusion,(b)the moisture-dependent adhesive stress–strain and creep com-pliance curves.Based on the measured adhesive material data,numerical modelling was then carried out to simulate the long-term degradation pro-cess in adhesively bonded joints under simultaneously combined thermal–hygro-mechanical loading conditions using a fully-coupled methodology.2.EXPERIMENTAL PROCEDURES AND RESULTS2.1.Specimen FabricationFM73(Cytec 1,New Jersey,USA)film adhesive with a knit carrier and nom-inal thickness of 0.18mm was utilised to make bulk adhesive dog bone and SLJ specimens.The required bulk adhesive specimens were obtained by stacking nine layers of FM73adhesive film.A specimen thickness of 1mm was maintained using steel spacers.The curing process was performed at the recommended curing temperature of 120 C [20].After curing,dumbbell specimens of overall length of 65mm and gauge length and width of 30and 5mm,respectively,were cut with a computer numerical control (CNC)machine.Details related to the curing process can be found elsewhere [15,21,22].Aluminium alloy 2024-T3was used as the substrates in the SLJs,shown in Fig.1.Prior to curing,the aluminium alloy substrates were surface treated to provide a durable interface.The treatment technique started with chromic acid etching (CAE)followed by phosphoric acid anodising (PAA)and then the application of corrosion inhibiting BR127(Cytec 1,New Jersey,USA)pri-mer [23,24].Two layers of adhesive film,having the same dimensions as the overlap area,were laid up on the pre-treated aluminium surfaces.The adhesive joints were then stacked one on top of the other and cured in a spring-loaded jig.A spacer 0.2mm thicker than the substrate was inserted between the specimens to maintain a bond line thickness of 0.2mm.The cur-ing procedures were the same as for the bulk adhesive described above.The detailed configuration of the SLJ is shown in Fig.1.FIGURE 1Configuration of the single-lap joint.422X.Han et al.D o w n l o a d e d b y [T u l a n e U n i v e r s i t y ] a t 20:14 03 J u n e 20142.2.Experimental Method2.2.1.B ULK ADHESIVEThe bulk adhesive dumbbell specimens were immersed in water at 50 C (both unloaded and at 25%of the static failure load)for 6months to obtain various material properties,including (a)moisture ingress under different loading levels,(b)the creep response,and (c)coefficient of hygroscopic expansion (swelling)(CHE).The loads were applied using the spring-loaded rig shown in Fig.2.This rig was placed in a tank containing the water,which in turn was placed in an oven at 50 C.A gravimetric method was used to obtain the adhesive moisture diffusion coefficients and equilibrium moisture uptake,assuming the Fickian diffusion model as expressed in Eq.(1)[25]:F x ¼ÀDd c d x:ð1ÞHere,F x is the flux of moisture in x -direction,D is the diffusion coefficient and d c =d x is the normalised moisture concentration gradient in the x -direction.Details of this procedure can be found elsewhere [26].Loaded specimens were periodically removed from the spring loaded rig for gravimetricmeasurements.FIGURE 2Loading jigs for the bulk adhesive degradation test.Effect of a Hot–Wet Environment 423D o w n l o a d e d b y [T u l a n e U n i v e r s i t y ] a t 20:14 03 J u n e 2014The creep extension of the adhesive was obtained by measuring the extension of the pre-compressed spring.This was generally undertaken immediately before removing the specimen for gravimetric testing.A power-law creep model was used in the subsequent modelling procedure as expressed in Eq.(2)[27]:_e¼Aq n t m :ð2ÞHere,_erepresents the creep strain rate,q is the equivalent stress,t is the time,and A ,n ,and m are coefficients based on a fitting procedure to the experimental data.Additional quasi-static tensile tests to failure have also been carried out on bulk adhesive specimens that had been pre-saturated to different levels [28].Moisture-dependent stress–strain curves were obtained from the result-ing data.The CTE of FM73adhesive was determined using strain gauges on both the adhesive and a reference material (aluminium 2024-T3with a CTE of 2.36E-5 C À1)[28].Both materials with strain gauges attached were placed in the oven to measure the strain variation with increased temperature in both specimens at the same time.The relationship between the CTEs for the adhesive and the reference material can be deduced from the following equation [29]:a A Àa R ¼e T =O =ðG =S ÞÀe T =O =ðG =R ÞÀÁD T:ð3ÞHere,a A and a R are CTEs for the adhesive and reference materials,e T =O =(G =S )and e T =O =(G =R )are strain outputs for adhesive and reference and D T is the temperature change from the initial reference temperature.The hygroscopic expansion in the adhesive was assumed to be isotropic and a micrometer was used to measure the increase in the thickness of the unloaded bulk adhesive dumbbell specimens during the degradation process [22,30].2.2.2.S INGLE-LAP JOINTCreep tests on adhesively bonded joints were carried out in similar spring-loaded jigs.However,with these tests each specimen was encased in a glass tube filled with de-ionised water and the resulting assembly placed in an oven at 50 C.Different loading levels (12.0%and 17.5%of the dry joint failure strength)were used to investigate the effect of stress on the joint response.The joint extension was determined by periodic measurement of the displacement of the pre-compressed spring.424X.Han et al.D o w n l o a d e d b y [T u l a n e U n i v e r s i t y ] a t 20:14 03 J u n e 20142.3.Experimental ResultsExperimental results based on bulk adhesive tests provided CTE,CHE,moisture-dependent stress–strain data,stress-dependent moisture diffusion,and moisture-dependent creep behaviour for the subsequent numerical modelling.The CTE and CHE for FM73adhesive were found to be 8.00E-5 C À1and 0.00463(%m w )À1(%m w being the percentage mass of water in the adhesive by weight),respectively.The effect of moisture on the adhesive Young’s modulus is given in Table 1.It can be seen that the Young’s modulus reduces by about 15%due to the presence of moisture.Young’s modulus and CTE used for the 2024-T3aluminium alloy are 70GPa and 2.36E-5 C À1,respectively.The dependency of the Fickian moisture diffusion parameters on the stress state are shown in Table 2.The moisture diffusion coefficients are sig-nificantly affected by the applied stress leading to a more rapid moisture uptake.Further,sustained loading is seen to increase the saturated mass uptake of water by over 25%from the unloaded condition.The increase in both parameters might be explained by the increase in the free volume of the bulk adhesive under load and =or the presence of crazes [31,32].Both aspects may be caused by the sustained loading these specimens experience.The creep properties of the adhesive in the ageing environment under 25%of the static failure load are shown in Table 3.These were determined based on the results from dry and pre-saturated bulk adhesive creep tests [27]and data from the gradually saturated bulk adhesive dumbbell specimen dis-cussed above.The gradually saturated bulk adhesive experimental and numerical creep–time curves are consistent with each other as presented in Fig.3.A two-phase (primary and secondary)creep model was used to provide better fitting with the experimental data.Creep behaviours based on adhesively bonded joints under two loading levels were obtained and used as a validation of the numerical simulation.TABLE 1Young’s Modulus for FM73at Various Moisture Concentrations Environment Moisture content (%)Young’s modulus (MPa)Dry =50 C01650Immersion =50 C3.751400TABLE 2Diffusion Parameters for FM73Immersed in 50 C Deionised Water at Different Loading Levels Stress (MPa)Temperature ( C)Saturation content (%)Diffusion coefficient (m 2=s)050 2.95 5.21E-1311.75503.757.18E-13Effect of a Hot–Wet Environment 425D o w n l o a d e d b y [T u l a n e U n i v e r s i t y ] a t 20:14 03 J u n e 2014The experimental creep strain–time curves are shown later in Fig.10(d),where they are compared with the predicted response.3.FINITE ELEMENT MODELLINGA 3D finite element (FE)model was built in the FE package Abaqus 1to simulate the fully-coupled degradation process of the adhesive joint carrying a sustained load in a hot–humid environment.Material parameters considered in this numerical modelling were obtained through the experi-ments discussed in Section 2and this section focuses on incorporating the relevant behaviours into the FE model.The numerical analysis was carried out assuming geometric nonlinear-ity.Figure 4shows a typical FEM mesh for the SLJ,with detailed refinement around the bonding areas,where large peel and shear stress gradients are located [33].Standard quadratic 3D stress elements (C3D20)were employed for the substrates around the bonding area to provide a more accurate stress description whilst reduced integration elements (C3D20R)were used for theTABLE 3Creep Parameters for FM73at 50 C (Force (N),Length (mm),Time (s),Stress (MPa))Phase Condition A n m Primary Dry5.774E-010 4.75À0.4764Primary Saturated 1.398E-009 4.75À0.397SecondaryPartial2.956E-0134.75FIGURE 3The numerical and experimental creep strain–time curves at 50 C and under 25%of the static failure load for FM73bulk adhesive.426X.Han et al.D o w n l o a d e d b y [T u l a n e U n i v e r s i t y ] a t 20:14 03 J u n e 2014rest of the substrate to reduce the computational cost.Quadratic 3D thermal-displacement-coupled elements (C3D20T)were used for the adhesive to include both moisture diffusion (using a heat transfer analogue)and stress.To obtain more accurate results,a higher mesh density (0.20mm Â0.20mm Â0.17mm)was adopted for the elements around the bonding area.One end of the substrate was assigned an encastre constraint,while a kinematic coupling was applied to impose the same axial displacement on all the nodes at the other end of the joint,with the displacements of these nodes in the other two directions constrained.A concentrated load was applied at the control point of the kinematic coupling to simulate the load supplied by the springs in the experiment procedure.Moreover to simulate an immersed environment,the exposed surfaces of the adhesive layer were assigned an initial normalised moisture concentration (temperature in Abaqus)boundary condition of 1at all exposed adhesive faces,as shown in Fig.4.3.1.Stress-Dependent Moisture DiffusionAn analogy between heat transfer and moisture diffusion was utilised in this model to simulate the moisture ingress process [34].Further details of the diffusion analysis can be found elsewhere [26].In order to simulate the simultaneous coupled effect of moisture and stress on each other,fully coupled thermal-displacement elements were utilised for the adhesive ing the Abaqus user subroutine USDFLD,the von Mises stress for each adhesive material (integration)point was defined as a field variable (FV1)and the diffusion coefficient was defined as being linearly dependent on FV1(the stress),as given in Table2.FIGURE 4FE mesh for the single-lap joint showing detailed refinement around the bonding area and boundary conditions.Effect of a Hot–Wet Environment 427D o w n l o a d e d b y [T u l a n e U n i v e r s i t y ] a t 20:14 03 J u n e 20143.2.Moisture-Dependent ElasticityAs found in the bulk adhesive tensile tests,the adhesive modulus is a function of moisture.In this model,the moisture-dependent adhesive modulus data shown in Table 1were incorporated by defining the moisture content as another field variable (FV2)in the user subroutine USDFLD.This is determined by the normalised moisture concentration,the stress-dependent saturation uptake (Table 2),and the von Mises stress.The Young’s modulus of the adhesive was defined as being linearly dependent on this field variable.3.3.Thermal and Swelling ExpansionsThe thermal expansion of both the adhesive and the substrate were introduced through the user subroutine UEXPAN which produces a total ‘‘expansion’’strain.A temperature drop of À50 C was defined as a predefined field variable (FV3)and used with the CTE to define the thermal strains.This temperature drop represents the decrease from the adhesive glass transition temperature (100 C)to the environmental testing temperature (50 C).Meanwhile,the swelling strain of the adhesive was defined as the product of the moisture con-tent (FV2)and the CHE.Values of the expansion coefficients are given at the beginning of Section 2.3.3.4.Moisture-Dependent Time-Hardening Creep As described in Section 2,a two-phase time-hardening power law creep model was used,and the parameters shown in Table 3were adopted to define the adhesive creep behaviour.These parameters are dependent on both moisture and the creep strain (transition at 48%from primary to secondary creep).With the moisture content defined as a field variable (FV2)and the creep strain as another field variable (FV4)in user subroutine USDFLD,the two-phase moisture-dependent creep model parameters were defined as being dependent on these field variables.The dependence was linear with moisture and stepwise at thetransition strain (primary to secondary creep).3.5.Concept Framework of the FE ModellingA general framework is shown in Fig.5,illustrating the modelling techniques outlined above.This should clarify what is a quite a complex modelling con-cept.It can be seen that the four field variables described above are deter-mined in increment N À1and imported into the next increment.Four adhesive behaviours (moisture diffusion,elasticity,creep,and thermal and swelling expansion)in increment N are considered and determined using the field variable values from the previous step.Then the FE calculation is carried out for the SLJ model,providing an updated stress and moistureD o w n l o a d e d b y [T u l a n e U n i v e r s i t y ] a t 20:14 03 J u n e 2014distribution which is then used to calculate the field variable values in the subsequent increment.This iterative process is repeated until the target simulation time (i.e.,3or 6months)is achieved.4.FE MODELLING RESULTS AND DISCUSSION Two steps were utilised in this Abaqus model to provide results data at the specific time points of 3and 6months during the environmental ageing pro-cess.The separate field-variable-dependent modelling aspects outlined in Sections 3.1–3.4were all validated successfully using simple benchmarking tests.In this paper,the focus is on the whole joint modelling,which incorpo-rates all these features rather than the validating benchmarking tests.Three simulations (unloaded,creep at 12.0%and at 17.5%of the static failure strength,respectively)were performed to investigate the effects of stress relaxation caused by moisture-dependent creep and thermal and swelling expansion.4.1.Moisture IngressNormalised moisture concentration,varying from 0to 1,is a dimensionless description of the moisture profile in the adhesive,with the completely dry condition corresponding to 0and the saturated condition to 1.The normal-ised moisture concentration contours on the adhesive mid-plane for thejoint FIGURE 5Concept framework of the FE modelling.D o w n l o a d e d b y [T u l a n e U n i v e r s i t y ] a t 20:14 03 J u n e 2014loaded at 12%of the static failure strength at initial,12,and 42days ageing are presented in Fig.6(a)–(c),respectively.It is observed that no moisture exists in the centre of the adhesive initially while after 12and 42days water diffuses into the adhesive layer and the normalised moisture concentrations in the centre reach around 0.4and 0.8,respectively.The distribution of the normalised moisture concentration along a path travelling through the centre of the adhesive in a widthwise direction is shown in Fig.6(d).It can be observed that the adhesive layer in the SLJ reaches full saturation after 3months exposure.The distributions of the actual (not normalised)moisture content (FV2)in both unloaded and loaded (12%of failure strength)conditions along the same path as Fig.6(d)are shown in Fig.7.It is observed that the stress-dependent moisture diffusion process is slowed in the absence of an external load.However,the unloaded moisture content level is not reduced by the amount suggested from the saturation mass uptakes in Table 2.This is due to the internal stress caused by the thermal and swelling expansion further clarified in Section 4.2.4.2.Stress Distribution The von Mises stress has been used to evaluate the variation of adhesive stress in the SLJ with time.The von Mises stress contours on the mid-plane of the adhesive at initial state,12days,and 42days are shown in Fig.8(a)–(c)forFIGURE 6The moisture concentration states of the adhesive loaded at 12%of the joint failure strength:moisture contours (a)initially,(b)after 12days,and (c)after 42days and (d)distribution along the overlap width.D o w n l o a d e d b y [T u l a n e U n i v e r s i t y ] a t 20:14 03 J u n e 2014FIGURE 7The moisture content distribution (loaded and unloaded)along the overlap width initially,after 12days,and after 42days.FIGURE 8The von Mises stress states of the adhesive (loaded):stress contours (a)initially,(b)after 12days,and (c)after 42days and (d)distribution along the overlap length.D o w n l o a d e d b y [T u l a n e U n i v e r s i t y ] a t 20:14 03 J u n e 2014the joint loaded at 12%of the static failure strength.Figure 8(d)shows the same stresses along a path in the middle of the adhesive layer running in the lengthwise direction initially,after 12days,and after 42days.It can be seen from Fig.8(d)that the stress concentration usually observed at the end of the bonding area is initially reversed (12days)and then largely reduced after 3months environmental degradation.The initial reversal can be explained by the rapid development of creep strains in the highly stressed region at the overlap ends.This increase in creep stains will reduce the elastic strains and hence the stresses.The subsequent smoothing of the von Mises stresses can be explained by a combination of the same mechanism and the fact that as the moisture diffuses further into the joint there is less resist-ance to the swelling by the dry inner core.As can be seen in Table 3,the creep parameters are dependent on the moisture content level and the stress and this leads to a much higher creep rate on the edges of the adhesive layer.Therefore,more stress relaxation occurs in the outer region thus averaging (or smoothing)the stress distribution in the bond.After 3months,the adhesive layer is essentially saturated and the stress is nearly uniform,thus the joint continues to creep at a broadly uniform rate across the entire adhesive layer.Similar investigation was also carried out on the joint model without any applied load and the von Mises stress contours on the mid-plane of the adhesive are shown in Fig.9(a)–(c).Also included are stresses along a path in the middle of the adhesive layer running in the lengthwise direction initially,after 12days,and after 42days as shown in Fig.9(d).It can be seenfromFIGURE 9The von Mises stress states of the adhesive (unloaded):stress contours (a)initially,(b)after 12days,and (c)after 42days and (d)distribution along the overlap length.D o w n l o a d e d b y [T u l a n e U n i v e r s i t y ] a t 20:14 03 J u n e 2014Fig.9(a)–(c)that the overall stress level is not significantly reduced when no mechanical load is applied.This is both because the mechanical load is only 12%of the static failure load and because some components of the mechanical and swelling =thermal stresses act in opposite directions.The residual stress in the adhesive layer is caused by the thermal and swelling expansion.The tem-perature difference imported initially into this model leads to non-negligible internal stress when the CTEs in the adhesive and substrate are dissimilar,whilst the swelling strains,which are proportional to the moisture content,exist throughout the ageing process.It can be seen from Figs.8(d)and 9(d)that a similar stress relaxation process is observed.However,the difference lies in that in the unloaded model the stress level keeps decreasing with accumu-lated creep and swelling expansion,whilst in the loaded model a certain lower limit can be achieved due to the applied load.4.3.Creep Behaviour The equivalent creep strain is used in this section to evaluate the joint defor-mation with time.The simulation of the creep behaviour,which is dependent on the moisture content in the adhesive as well as the stress,is a key factor in this modelling concept.The equivalent creep strain contours on the adhesive mid-plane at initial state,3months,and 6months are illustrated in Fig.10(a)–(c)for the joint loaded at 12%of the static failure strength.It is found (see Fig.10d)that the creep strain increases much faster in the first 3months than the latter 3months which is reasonable based on the moisture diffusion and creep models which develop more rapidly initially.Further,as thecreepFIGURE 10The equivalent creep strain contours (a)initially,(b)after 3months,and (c)6months,and (d)creep strain–time curves under different loading levels.D o w n l o a d e d b y [T u l a n e U n i v e r s i t y ] a t 20:14 03 J u n e 2014。

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