雅思基础阅读练习 这么练习你的雅思阅读也可以拿8分

今天，雅思无忧小编为关注雅思阅读的同学们准备了雅思基础阅读练习 这么练习你的雅思阅读也可以拿8分，下面一起来看一下吧。

这么练习你的雅思阅读也可以拿8分

您好，我是专注留学考试规划和留学咨询的小钟老师。在追寻留学梦想的路上，选择合适的学校和专业，准备相关考试，都可能让人感到迷茫和困扰。作为一名有经验的留学顾问，我在此为您提供全方位的专业咨询和指导。欢迎随时提问！
小钟老师的雅思栏目小编为您带来“这么练习你的雅思阅读也可以拿8分”，希望对大家备考雅思有所帮助。更多雅思相关内容请关注我们网站!
1. 模拟考试环境
考过雅思的同学都知道， 四科里面时间最紧的当属阅读， 很多人初次去考试都会答不完卷子。如果想在时间上做更好的掌控，计时练习就变得相当有必要了。大家给自己限定一小时时间，之后核对答案，看下最终分数。
另外友情提示下各位，一小时的时间还包括把答案转移到题纸的时间。 转移答案的时候大概会消耗两分钟左右， 如此看来时间就变得更加紧迫了!
2. 不计时完成三篇文章阅读
此方法为了提高大家的精读能力，不要为了做题而做题， 而是为了把题目读懂、吃透。 每个词、每个短语、每个句式的功能都分析清楚再去答题。
此方法适合备考时间较长的，同时对阅读期望分值比较高的同学。
3. 20分钟完成一篇文章
初期做阅读练习学生，整个阅读三篇文章一起读下来会有种大脑被掏空的感觉。适度练习起码不会起到逆反心理。
此方法适合不喜欢阅读的同学， 最前期适应练习。
4. 没有时间限制完成一篇文章
依旧还是一篇文章， 如果20分钟的计时导致时间紧迫造成错误率过高， 可采用此种方法。没有时间限制的阅读也是为了阅读而阅读， 提升总体阅读实力。
5. 一次只做一个题型
题刷多了之后他家会发现， 不同题型他对文章不同部分的考察点是不一样的。比如list of headings考察是段落理解能力，True/ False / Not given考察的是句子理解能力。有针对性的答题往往会总结出适合自己的答题规律。
此方法适合多次刷题， 但毫无题感的同学。
6. 在字典的帮助下答题
此方法可检测出阅读失分的原因， 究竟是因为生词? 句式复杂? 还是逻辑是的问题? 如果有了字典的帮助还是得不到高分，就和生词没有关系了
7. 只读文章不做题
没有压力的阅读， 会让你的阅读分数提升。 其实也是鼓励各位培养良好的阅读习惯。
8. 核对答案后分析答案
如果做题中一味只是为了核对答案而做题， 实际这题方法没有多大意义。很多阅读8分的学生在做题中更多的会思考出题者出题的角度是什么，得出规律。甚至有些学生在阅读完文章后，都会猜到部分题目考官考什么，或者他会挖什么陷阱。这其实就是我们所强调的，从考官角度思考问题。
9. 整理词汇表格及关键词表格
如何提高雅思阅读，其实整个雅思的考试就是一套同义替换的体系，阅读听力口语写作皆是如此。 阅读中的同义替换放到写作中当然也适用。毕竟都是学术用语。
上面给出了具体的雅思阅读提高方法，相信大家照着做一定会有提高，从此雅思阅读高分不是梦。
雅思阅读栏目推荐阅读:

雅思阅读语法攻略
雅思阅读词汇记忆技巧
雅思阅读填图题答题技巧
2023年雅思报名时间
雅思零基础如何备考雅思
2023雅思考试时间安排表
2023全国各地雅思考点汇总

希望以上的答复能对您的留学申请有所帮助。如果您有任何更详细的问题或需要进一步的协助，我强烈推荐您访问我们的留学官方网站 ，在那里您可以找到更多专业的留学考试规划和留学资料以及*的咨询服务。祝您留学申请顺利！

如何有效地练习雅思阅读？

你好，　1、题型多变，宏观战略要取巧：上个月没有出现的题型这个月有可能出现，同时难度实在加大的，尤其是Headings等题型的出现也体现了难度的上升。所以，不要急于做题，因为题型多变，整体做题的战略也要改变。要首先做三件事：
(1)标题：首先要看标题，包括：主标题、副标题、引言、图，他们都能在段时间内帮助我们知道文章的整体题材是什么，以及自己的知识结构是否适合整篇文章的。
(2)结构：要花时间看文章的结构，例如：剑4 P65，文章主要讲都给街头小型企业贷款。这篇文章的结构有很大的特点：机构可分为：引言、introduction、background，还有后面的一个合作关系、得到的经验教训、结论。这些对我们的大体定位很有帮助，因为结构清晰、明确，对我们解题很有帮助
(3)题型：三篇文章发下来后，一定花点时间看一下这些文章的题型，再决定先做哪篇。因为我们每个人擅长的题型是不一样的，不擅长的题型出现比较多的文章可以放在后面去做，而且本身就是客观题，对我们来讲可以有一些猜的成分在里面。
2、主流题型，时刻准备着。
(1)Summary(选词填空)
(2)判断题
Summary题和判断题，作为7月份的主流题型，题目数量是稳中有升的，这两个题型也是基本的拿分点。在7月份的考试中一共出了9道，其中有3道选词填空。
选词填空是常见的题型，它的难点体现在它的选项在原文中用同义替换来代替。如果对词汇掌握的不好，最起来就会比较困难。在解这类题的时候，除了注意在审题的时候出现重复选项，还要注意要把选项分析一遍，一是要看词性，二是看有没出现相对应或相反的词。
判断题的解题点有两个：一是在读完题后，要知道它的考点是什么，是数字考点还是比较级考点，是谓语动词考点还是绝对词考点。二是要采用猜题的技巧，比如Only、instant等绝对词。
(3)选择题(单选vs.多选)
选择题是大规模复苏的题型，而且在8月份的考试中出现的概率也是比较大的。选择题的多选基本上也没有什么技巧，拿分的可能性也不是很高。但是单选的技巧还是有一些的，比如说：要选择4个选项中与主题相近的那一个;两个相似选项一般选一个;选择与原文替换比较明显的选项，而不是原文中出现词最多的选项。
3、段落细节信息配对题
(1)做题顺序策略选择
(2)解题技巧取胜
(3)战略性放弃
这是唯一现在还在的配对题，也是最难的一种配对题。这种题首先采取的战略是：有的放矢地进行放弃。比如目标为6分或6.5分时，做这种题可以适当地放掉一半或者1/3，因为它很浪费时间，而且准确率相对较低。
如果想在这个部分拿分，需要首先注意顺序，不能上来就做这道题，因为要做好这道题，原文的每句话都要看，很明显，段时间内做不到这一点。所以一般来讲，要把题先精度一遍，读出句子中很有特点的词，并勾出来，之后再先做后面的题，然后再做前面的题，这样就能有一个事半功倍的效果。
4、简单题型作为得分点
简单题型包括：图形题、完成句子题、表格题、流程图、简答题，这些题都是Summary题的变体，所以把Summary题攻破了，这五种题也就非常简单。
(1)套题做题顺序：先做出现简单题的那一篇。
(2)简单题型作为基础拿分项。

更多雅思学习技巧请继续关注：

雅思阅读段落标题模拟题

雅思阅读段落标题模拟题

雅思考试的'阅读部分，因篇幅比较长时间有限，一直是考生们难以攻克的难题。为了帮助大家能顺利备考，下面我为大家带来雅思阅读段落标题模拟题，供大家参考学习，预祝大家考试顺利!

试题(一)

Volcanoes-earth-shattering news

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

A

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. Vulcani*, 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 *oking 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.

B

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.

C

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.

D

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 *all 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.

试题(二)

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 (*ogous 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.

试题(三)

Disappearing Delta

A

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.

B

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 22000 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.

C

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.

D

Once north of Cairo, most of the Nile water is diverted into more than 10,000 kilometres of irrigation c*s and only a *all proportion reaches the sea directly through the rivers in the delta.The water in the irrigation c*s is still or very slow-moving and thus cannot carry sediment，Stanley explains.The sediment sinks to the bottom of the c*s 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.

E

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.

F

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.

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以上就是雅思无忧小编为大家带来的雅思基础阅读练习 这么练习你的雅思阅读也可以拿8分，希望对大家有帮助，了解更多相关资讯请关注雅思无忧。

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