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雅思阅读如何巧用文章标题

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雅思阅读如何巧用文章标题（精选7篇）由网友“赵赵被偷了”投稿提供，下面小编为大家整理后的雅思阅读如何巧用文章标题，希望能帮助大家!

雅思阅读如何巧用文章标题

篇1：雅思阅读如何巧用文章标题

雅思阅读：如何巧用文章标题

也就是就说学生平均每道题只能用1分30秒的时间去读懂题目,在文章中定位,确定答案并把答案写到答题纸上,因此对于雅思考生来说速度就是分数.

然而在雅思考试中,经常出现考生答不完题的情况,也就是学生经常反映的考试时间不够用的问题.很多考生以为雅思阅读考试的三篇文章的难度是递增的,因此在考试过程中就按照雅思试卷所给出的文章顺序去解题,结果要么第一篇文章花费过多时间(雅思要求每篇文章20分钟答完题);

要么第二篇花费过多时间,结果导致第三篇文章尽管非常简单,却没有时间去做了,最终只能匆匆忙忙把答案猜上去,甚至有的考生连猜答案的时间都没有,只能后悔莫及.

也因此很多考生总是疑惑,雅思阅读考试的三篇文章的难度到底是怎样的呢?是难度递增呢还是难度递减呢?在雅思阅读考试中到底应该如何决定文章的难易程度?

考生们可以从文章标题入手.雅思阅读考试的文章,其内容为学术类科普读物,主要选自世界各大主要媒体的文章改写而成,涉及经济、教育、科技、医学、环境、能源、地质、海洋、动植物等.

虽然文章题材不同,但都以大众题材为主,不涉及专业性很强的文章,以免给不同专业的考生造成优势或劣势.而文章标题是文章的中心思想和主题的提炼.

因此,建议考生们可以利用文章标题来判断自己对该篇文章的背景信息是否熟悉.如果考生对该篇文章的背景信息相当熟悉,那做该篇文章的题目当然也就得心应手,而不会出现文章内容根本一窍不通,无法答题的情况.甚至有的题目考生们可以利用自己对文章背景信息的了解直接答题,而无需在题目中划出定位词,到文章中定位再确定答案了.

当然如果考试文章的标题看不懂怎么办?或者说文章根本没有文章标题怎么办?其实考生们根本不需要担心,首先如果出现考试文章的标题难以理解,考官考虑到考生可能看不懂,会在文章标题旁插入一幅图片,帮助考生理解该文章的标题.

如剑7第一套题中阅读部分的第一篇文章的文章标题为Going to Bats,而考官考虑到考生们可能不认识Bats一词,在标题旁就插入一幅蝙蝠的图片,因此考生也就很容易判断出该篇文章应该主要是关于蝙蝠的了.

而这套题的第二篇文章的文章标题为Making Every Drop Count,仅仅看标题,考生们也无法准确确定该篇文章的主要内容,因为drop只能翻译为每一滴;考虑到这一点,考官也在文章的文章标题旁插入一幅自来水水龙头的图片,因此考生们也就可以很容易判断出该篇文章主要内容是关于珍惜水资源的.

在此提醒考生们,如果雅思阅读考试文章既没有给出文章标题,也没有插入图片,那考生们可以快速阅读该篇文章每一段的第一句话,即可以快速确定该篇文章的主题和背景信息了.

雅思阅读语言文化类话题解析

就像雅思口语话题一样，雅思阅读考试也同样有很多经常出现的话题，只要对其分类总结，然后根据这些常见的文章类型着重了解雅思阅读中的这些题材，便能达到事半功倍的效果。

雅思文章的出处有很多，其中最实用的、便于积累背景知识的雅思文章来源是new scientist网站, 这个网站是雅思出题方公布的出题来源，包括了太空领域、环境、生物地理物理等科学以及社会科学与人类健康等各方面的科学知识，而以下提到的雅思文章的三大类都可以在这里找到相关的文章。

地理类话题是阅读文章中常常摘选的内容，不过相比于上面的生物类，地理类的文章难度较高，因为地理现象涉及的专业名称更多、地名和各种地质现象也更加复杂，在积累地理类知识时，工作量是比较大的。

地理类知识范围很广，常见的有厄尔尼诺现象、气象观测、沙漠化、欧洲冰川等。我们可以在以上提到的那个网站中查到这些内容，当然，也不要拘泥于一个雅思文章的来源，可以多参阅一些与科学相关的英文报纸、杂志和网站。

雅思阅读人文科学类的第二大话题就是语言文化类。

从全年来看，主要涉及到语言的传播，笔译，国际公司的外语策略培训，语言对商业的作用，语言的起源，语言的消失，对语言发展的态度。在上半年来看，语言类话题主要有交流与文化，语义的理解，双语学习的利弊。

从去年到今年上半年，语言文化类话题主要涉及到了语言对商业，文化等的影响，语言的保护以及语言与教育的结合。这类型话题在剑桥雅思真题集中也有广泛分布，比如：剑桥4 Test2 Passage1 Lost for Words, 这篇文章主要讲解了少数语言的消亡，探讨了语言消亡的原因以及相应的解决办法。除此之外，剑桥4 Test3 Passage3 Obtaining Linguistic Data也是关于语言的，这篇文章相对比较专业化，讲述了获取语料的方法并讨论了这些方法的利弊，但即使这样做这篇文章时也不需要理解那些专业化的词汇。剑桥5 Test2 Passage3 The Birth of Scientific English, 这篇文章结合了语言与发展史，讲述了科学英语的诞生及发展。烤鸭们在遇到这类型的话题时，很多都会觉得相当困难，除非有些烤鸭们的专业就是语言学专业。因为语言学本身就包括了很多分支比如语音学，词汇学，句法学等等。每一个分支都会有很多相关的专业术语，烤鸭们尤其是还在读高中的小烤鸭们会觉得异常难懂，但是要记住一点：雅思考试的一大特色就是“非专业性”。

也就是说，虽然考试中会考到很多有关语言学的内容，但是大多是关于语言传播方式，如何保护语言等等比较简单易懂的方面，并不会出现太专业性的内容。即使有专业词汇出现，也应该感到高兴，因为它们不会涉及同意转换。

篇2：雅思阅读段落标题模拟题

雅思(IELTS)阅读模拟练习题：段落标题题【1】

Volcanoes-earth-shattering news

When Mount Pinatubo suddenly erupted on 9 June 1991, the power of volcanoes past and present again hit the headlines

Volcanoes are the ultimate earth-moving machinery. A violent eruption can blow the top few kilometres off a mountain, scatter fine ash practically all over the globe and hurl rock fragments into the stratosphere to darken the skies a continent away.

But the classic eruption―cone-shaped mountain, big bang, mushroom cloud and surges of molten lava―is only a tiny part of a global story. Vulcanism, the name given to volcanic processes, really has shaped the world. Eruptions have rifted continents, raised mountain chains, constructed islands and shaped the topography of the earth. The entire ocean floor has a basement of volcanic basalt.

Volcanoes have not only made the continents, they are also thought to have made the world's first stable atmosphere and provided all the water for the oceans, rivers and ice-caps. There are now about 600 active volcanoes. Every year they add two or three cubic kilometres of rock to the continents. Imagine a similar number of volcanoes smoking away for the last 3,500 million years. That is enough rock to explain the continental crust.

What comes out of volcanic craters is mostly gas. More than 90% of this gas is water vapour from the deep earth: enough to explain, over 3,500 million years, the water in the oceans. The rest of the gas is nitrogen, carbon dioxide, sulphur dioxide, methane, ammonia and hydrogen. The quantity of these gases, again multiplied over 3,500 million years, is enough to explain the mass of the world's atmosphere. We are alive because volcanoes provided the soil, air and water we need.

Geologists consider the earth as having a molten core, surrounded by a semi-molten mantle and a brittle, outer skin. It helps to think of a soft-boiled egg with a runny yolk, a firm but squishy white and a hard shell. If the shell is even slightly cracked during boiling, the white material bubbles out and sets like a tiny mountain chain over the crack―like an archipelago of volcanic islands such as the Hawaiian Islands. But the earth is so much bigger and the mantle below is so much hotter.

Even though the mantle rocks are kept solid by overlying pressure, they can still slowly 'flow' like thick treacle. The flow, thought to be in the form of convection currents, is powerful enough to fracture the 'eggshell' of the crust into plates, and keep them bumping and grinding against each other, or even overlapping, at the rate of a few centimetres a year. These fracture zones, where the collisions occur, are where earthquakes happen. And, very often, volcanoes.

These zones are lines of weakness, or hot spots. Every eruption is different, but put at its simplest, where there are weaknesses, rocks deep in the mantle, heated to 1,350℃, will start to expand and rise. As they do so, the pressure drops, and they expand and become liquid and rise more swiftly.

Sometimes it is slow: vast bubbles of magma―molten rock from the mantle―inch towards the surface, cooling slowly, to show through as granite extrusions (as on Skye, or the Great Whin Sill, the lava dyke squeezed out like toothpaste that carries part of Hadrian's Wall in northern England). Sometimes―as in Northern Ireland, Wales and the Karoo in South Africa―the magma rose faster, and then flowed out horizontally on to the surface in vast thick sheets. In the Deccan plateau in western India, there are more than two million cubic kilometres of lava, some of it 2,400 metres thick, formed over 500,000 years of slurping eruption.

Sometimes the magma moves very swiftly indeed. It does not have time to cool as it surges upwards. The gases trapped inside the boiling rock expand suddenly, the lava glows with heat, it begins to froth, and it explodes with tremendous force. Then the slightly cooler lava following it begins to flow over the lip of the crater. It happens on Mars, it happened on the moon, it even happens on some of the moons of Jupiter and Uranus. By studying the evidence, vulcanologists can read the force of the great blasts of the past. Is the pumice light and full of holes? The explosion was tremendous. Are the rocks heavy, with huge crystalline basalt shapes, like the Giant's Causeway in Northern Ireland? It was a slow, gentle eruption.

The biggest eruptions are deep on the mid-ocean floor, where new lava is forcing the continents apart and widening the Atlantic by perhaps five centimetres a year. Look at maps of volcanoes, earthquakes and island chains like the Philippines and Japan, and you can see the rough outlines of what are called tectonic plates―the plates which make up the earth's crust and mantle. The most dramatic of these is the Pacific 'ring of fire' where there have been the most violent explosions―Mount Pinatubo near Manila, Mount St Helen's in the Rockies and El Chichón in Mexico about a decade ago, not to mention world-shaking blasts like Krakatoa in the Sunda Straits in 1883.

But volcanoes are not very predictable. That is because geological time is not like human time. During quiet periods, volcanoes cap themselves with their own lava by forming a powerful cone from the molten rocks slopping over the rim of the crater; later the lava cools slowly into a huge, hard, stable plug which blocks any further eruption until the pressure below becomes irresistible. In the case of Mount Pinatubo, this took 600 years.

Then, sometimes, with only a small warning, the mountain blows its top. It did this at Mont Pelée in Martinique at 7.49 a.m. on 8 May, 1902. Of a town of 28,000, only two people survived. In 1815, a sudden blast removed the top 1,280 metres of Mount Tambora in Indonesia. The eruption was so fierce that dust thrown into the stratosphere darkened the skies, cancelling the following summer in Europe and North America. Thousands starved as the harvests faded, after snow in June and frosts in August. Volcanoes are potentially world news, especially the quiet ones.

篇3：雅思阅读段落标题模拟题

雅思(IELTS)阅读模拟练习题：段落标题题【2】

The Problem of Scarce Resources

Section A

The problem of how health-care resources should be allocated or apportioned, so that they are distributed in both the most just and most efficient way, is not a new one. Every health system in an economically developed society is faced with the need to decide (either formally or informally) what proportion of the community's total resources should be spent on health-care; how resources are to be apportioned; what diseases and disabilities and which forms of treatment are to be given priority; which members of the community are to be given special consideration in respect of their health needs; and which forms of treatment are the most cost-effective.

Section B

What is new is that, from the 1950s onwards, there have been certain general changes in outlook about the finitude of resources as a whole and of health-care resources in particular, as well as more specific changes regarding the clientele of health-care resources and the cost to the community of those resources. Thus, in the 1950s and 1960s, there emerged an awareness in Western societies that resources for the provision of fossil fuel energy were finite and exhaustible and that the capacity of nature or the environment to sustain economic development and population was also finite. In other words, we became aware of the obvious fact that there were 'limits to growth'. The new consciousness that there were also severe limits to health-care resources was part of this general revelation of the obvious. Looking back, it now seems quite incredible that in the national health systems that emerged in many countries in the years immediately after the 1939-45 World War, it was assumed without question that all the basic health needs of any community could be satisfied, at least in principle; the 'invisible hand' of economic progress would provide.

Section C

However, at exactly the same time as this new realisation of the finite character of health-care resources was sinking in, an awareness of a contrary kind was developing in Western societies: that people have a basic right to health-care as a necessary condition of a proper human life. Like education, political and legal processes and institutions, public order, communication, transport and money supply, health-care came to be seen as one of the fundamental social facilities necessary for people to exercise their other rights as autonomous human beings. People are not in a position to exercise personal liberty and to be self-determining if they are poverty-stricken, or deprived of basic education, or do not live within a context of law and order. In the same way, basic health-care is a condition of the exercise of autonomy.

Section D

Although the language of 'rights' sometimes leads to confusion, by the late 1970s it was recognised in most societies that people have a right to health-care (though there has been considerable resistance in the United States to the idea that there is a formal right to health-care). It is also accepted that this right generates an obligation or duty for the state to ensure that adequate health-care resources are provided out of the public purse. The state has no obligation to provide a health-care system itself, but to ensure that such a system is provided. Put another way, basic health-care is now recognised as a 'public good', rather than a 'private good' that one is expected to buy for oneself. As the 1976 declaration of the World Health Organisation put it: 'The enjoyment of the highest attainable standard of health is one of the fundamental rights of every human being without distinction of race, religion, political belief, economic or social condition.' As has just been remarked, in a liberal society basic health is seen as one of the indispensable conditions for the exercise of personal autonomy.

Section E

Just at the time when it became obvious that health-care resources could not possibly meet the demands being made upon them, people were demanding that their fundamental right to health-care be satisfied by the state. The second set of more specific changes that have led to the present concern about the distribution of health-care resources stems from the dramatic rise in health costs in most OECD countries, accompanied by large-scale demographic and social changes which have meant, to take one example, that elderly people are now major (and relatively very expensive) consumers of health-care resources. Thus in OECD countries as a whole, health costs increased from 3.8% of GDP in 1960 to 7% of GDP in 1980, and it has been predicted that the proportion of health costs to GDP will continue to increase. (In the US the current figure is about 12% of GDP, and in Australia about 7.8% of GDR.)

As a consequence, during the 1980s a kind of doomsday scenario (analogous to similar doomsday extrapolations about energy needs and fossil fuels or about population increases) was projected by health administrators, economists and politicians. In this scenario, ever-rising health costs were matched against static or declining resources.

篇4：雅思阅读段落标题模拟题

雅思(IELTS)阅读模拟练习题：段落标题题【3】

Disappearing Delta

The fertile land of the Nile delta is being eroded along Egypt’s Mediterranean coast at an astounding rate，in some parts estimated at 100 metres per year.In the past，land scoured away from the coastline by the currents of the Mediterranean Sea used to be replaced by sediment brought down to the delta by the River Nile，but this is no longer happening.

Up to now, people have blamed this loss of delta land on the two large dams aI Aswan in the south of Egypt，which hold back virtually all of the sediment that used to flow down the river. Before the dams were built，the Nile flowed freely carrying huge quantities of sediment north from Africa's interior to be deposited on the Nile delta.This continued for 7,000 years，eventually covering a region of over 2 square kilometres with layers of fertile silt.Annual flooding brought in new, nutrient-rich soil to the delta region，replacing what had been washed away by the sea，and dispensing with the need for fertilizers in Egypt's richest food-growing area.But when the Aswan dams were constructed in the 20th century to provide electricity and irrigation，and to protect the huge population centre of Cairo and its surrounding areas from annual flooding and drought，most of the sediment with its naturaI fertilizer accumulated up above the dam in the southern， upstream half of Lake Nasser, instead of passing down to the delta.

Now, however, there turns out to be more to the story.It appears that the sediment-free water emerging from the Aswan dams picks up silt and sand as it erodes the river bed and banks on the 800-kilometre trip to Cairo.Daniel Jean Stanley of the Smithsonian Institute noticed that water samples taken in Cairo，just before the river enters the delta，indicated that the river sometimes carries more than 850 grams of sediment per cubic metre of water-almost half of what it carried before the dams were built.I'm ashamed to say that the significance of this didn't strike me until after I had read 50 or 60 studies，says Stanley in Marine Geology. There is still a lot of sediment coming into the delta，but virtually no sediment comes out into the Mediterranean to replenish the coastline. So this sediment must be trapped on the delta itself.

Once north of Cairo, most of the Nile water is diverted into more than 10,000 kilometres of irrigation canals and only a small proportion reaches the sea directly through the rivers in the delta.The water in the irrigation canals is still or very slow-moving and thus cannot carry sediment，Stanley explains.The sediment sinks to the bottom of the canals and then is added to fields by farmers or pumped with the water into the four large freshwater lagoons that are located near the outer edges of the delta.So very little of it actually reaches the coastline to replace what is being washed away by the Mediterranean currents.

The farms on the delta plains and fishing and aquaculture in the lagoons account for much of Egypt's food supply.But by the time the sediment has come to rest in the fields and lagoons it is laden with municipal，industrial and agricultural waste from the Cairo region, which is home is more than 40 million people.’Pollutants are building up faster and faster,’ says Stanley.

Based on his investigations of sediment from the delta lagoons, Frederic Siegel of George Washington University concurs. 'In Manzalah Lagoon, for example, the increase in mercury, lead, copper and zinc coincided with the building of the High Dam at Aswan, the availability of cheap electricity, and the development of major power-based industries,' he says. Since that time the concentration of mercury has increased significantly. Lead from engines that use leaded fuels and from other industrial sources has also increased dramatically. These poisons can easily enter the food chain, affecting the productivity of fishing and farming. Another problem is that agricultural wastes include fertilizers which stimulate increases in plant growth in the lagoons and upset the ecology of the area, with serious effects on the fishing industry.

According to Siegel, international environmental organisations are beginning to pay closer attention to the region, partly because of the problems of erosion and pollution of the Nile delta, but principally because they fear the impact this situation could have on the whole Mediterranean coastal ecosystem. But there are no easy solutions. In the immediate future, Stanley believes that one solution would be to make artificial floods to flush out the delta waterways, in the same way that natural floods did before the construction of the dams. He says, however, that in the long term an alternative process such as desalination may have to be used to increase the amount of water available. 'In my view, Egypt must devise a way to have more water running through the river and the delta,' says Stanley. Easier said than done in a desert region with a rapidly growing population.

篇5：文章标题如何优化

1.文章标题如何优化着去写才能容易让百度收录，文章标题要有关键词，并且关键词要突出，能够被百度蜘蛛抓取。文章标题一定要原创，要新...

1.文章标题如何优化着去写才能容易让百度收录。文章标题要有关键词，并且关键词要突出，能够被百度蜘蛛抓取。文章标题一定要原创，要新颖，也不能定太主要的关键词。如果标题的关键词较长，那么在标题里出现一次就够了。比如：www.51hlht.com飞信客户端下载这个站的标题的关键词还要记得在文章中也要出现3――5次为宜。

2.文章的描述应该怎样写。首先要明白的是，百度收录的描述和google不同，百度是通过蜘蛛自己抓取文章最有搜索价值的一段放在网站标题的下面作为描述，而google则是我们截取什么描述就显示什么描述。为了方便百度抓取，描述一定要长，把用户可能会搜到的关键词在描述里分几段放进去，

如果是长尾关键词不太好加的，可以将关键词拆开了放进去。只要拆开的关键词都在描述里，并且出现多次，也可以被百度抓取组合，但是关键词不能堆积，要自然地隔开加入到描述里。

3.要注意的是关键词的密度高低是按页面算的，这也就是为什么我们在写伪原创时要注意标题和描述里不能出现太多网站的主关键词，这样是优化过度。

4.看一个网站的收录情况好不好要查看该网站的百度快照是不是最新的。如果是，那么这个网站的收录肯定不错。我想，我们现在快照比较新，收录也很好的网站是不是要经常更新会比较好呢?

5.在写文章或是伪原创的时候，除了要注意标题和描述的关键词问题，我想，一些虽与文章标题和内容无关，但是流量较高的词是不是也可以放到文章里，作为另一种“关键词”来用呢?因为平时我们找文章的时候，其实在搜一个信息时可能会带出来其他的信息。但是这样的“关键词”我觉得不能出现得太多，不然会抢了文章主词的位置。