雅思阅读遇到生词你该这么办

雅思是一个没有考试大纲更没有词汇大纲的考试，所以 理论上来说，英语的几十万词汇都是可以出现在雅思阅读的考试中的。小编给大家带来了雅思阅读遇到生词你该这么办，希望能够帮助到大家，下面小编就和大家分享，来欣赏一下吧。

莫慌!雅思阅读遇到生词你该这么办

为了更好地表达文章的主旨，揭示所要诠释的思想，作者常常在文章中对一些比较重要的词汇vocabulary、概念concept和难懂的术语terminology等做出一些解释，这种解释称作针对性解释，它可以提供明确的信息，可以利用这些针对性解释来猜测词义。

雅思阅读猜词之根据定义

如果生词是句子或段落所解释的定义，理解句子或段落本身就是推断词义。

例如：1.Anthropology is the scientific study of man。由定义可知，anthropology(人类学)就是“研究人类的科学”。

2.In slang the term "jam" constitutes a state of being in which a person finds himself or herself in a difficult situation。

同样，从上下文的定义可知jam一词在俚语中的意思是“困境”。

定义句的谓语动词多为：be, mean, deal with, be considered, to be, refer to, be called, be known as, define, represent, signify, constitute等。

雅思阅读猜词之根据复述

虽然复述不如定义那样严谨、详细，但是提供的信息足以使阅读者猜出生词词义。复述部分可以是单词、短语或是从句。

例如：1.Semantics, the study of the meaning of words, is necessary if you are to speak and read intelligently。

此处注意同位语，逗号间短语意为“对词意义进行研究的学科”。该短语与前面生词semanties是同位关系，因此我们不难猜出semantics指“语义学”。

在复述中构成同位关系的两部分之间多用逗号连接，有时也使用破折号，冒号，分号，引号，和括号等。

2.Capacitance, or the ability to store electric charge, is one of the most common characteristics of electronic circuits。

由同位语我们很快猜出生词capacitance词义---电容量。

需要注意的是：同位语前还常有or, similarly, that is to say, in other words, namely, or other, say i. e. 等副词或短语出现。

3.定语从句Krabacber suffers from SAD, which is short for seasonal affective disorder, a syndrome characterized by severe seasonal mood swings。

根据生词SAD后面定语从句which is short for seasonal affective disorder和同位语a syndrome characterized by severe seasonal mood swings, 我们可以推断出 SAD含义，即“季节性情绪紊乱症”。

雅思阅读猜词之根据举例

恰当的举例能够提供猜测生词的重要线索。

例如：1.The consequences of epochal events such as wars and great scientific discoveries are not confined to a small geographical area as they were in the past。

句中“战争”和“重大科学发现”是生词的实例，通过它们我们可以猜出epochal的大致词义“重要的”，这与其确切含义“划时代的”十分接近。

雅思阅读中所出的文章范围广，领域涉及多面，因此，要考生完全读懂文章是不可能的。这就需要考生们要具有根据上下文或者关键词来猜测词义与长难句的能力。小“烤鸭”们，不要再害怕因读不懂文章而阅读低分了，只要掌握方法并且加强训练，相信每一位同学都可以在雅思阅读考试中获得好成绩!

雅思阅读素材积累： Runaway Devils Lake

Devils Lake is where I began my career as a limnologist in 1964, studying

the lake's neotenic salamanders and chironomids, or midge flies. Back then, the

lake covered about 80 square kilometers, had a maximum depth of about 3 meters

and held about 130,000 acre-feet of water. The lake has since risen 13 meters,

from a surface elevation of 430 meters above mean sea level to 443 meters.

Estimated lake volume is now 4.1 million acre-feet, or about 32 times greater

than it was in 1964, and about 370 times greater than it was in 1940 when the

lake stood at a record low elevation of 427 meters.

The Devils Lake Basin is an endorheic, or closed, basin covering about

9,800 square kilometers in northeastern North Dakota. The basin is at the

epicenter of an unprecedented wet period in the lake's modern-day history going

back to 1867, when the lake's surface elevation was first measured. Basin

climate has become substantially wetter since 1990, with the years 1990 through

2009 ranking as the wettest 20-year period in more than a century. The National

Weather Service has referred to this trend as "the new climate" for the Devils

Lake region, cautiously predicting that the current weather pattern may continue

for several decades and possibly intensify. Indeed, the agency has warned that

the region faces the strong possibility of an "unprecedented fourth consecutive

major spring flood threat in 2012."

Rising lake waters have flooded much of the region, engulfing hundreds of

homes and farmsteads, more than 650 square kilometers of productive farmland,

major highways and bridges, state parks, Native American tribal lands,

historical landmarks and more than half a million trees. Submerged too is the

North Dakota Biological Station, a two-story limnological facility established

in 1909 to study the lake's unusual ecology and biogeochemistry. Portions of

U.S. Highway 281 are now underwater, which has forced the relocation of this

principal north-south highway several kilometers to the west. Other roads and

highways are either extremely hazardous or simply impassable because of

encroaching floodwaters. Amtrak and the BNSF Railway may have to reroute their

trains over more southern lines as rising waters threaten to wash out roadbeds

and bridges. The small town of Minnewaukan, once located 13 kilometers west of

the lake, is now partly underwater, and many of its 300-plus residents have been

forced to abandon their homes. Only a handful of people remain in Churchs Ferry

and nearby Penn, communities established more than a century ago. The city of

Devils Lake, North Dakota's eleventh largest city with about 7,000 residents,

sits behind a U.S. Army Corps of Engineers levee that protects the community

from storm-generated waves that reportedly reach 2 meters or more in height.

Without the levee, 3 to 4 meters of water would now cover parts of the city. To

date, efforts by federal, state and local governments to control flooding and

protect communities exceed $1 billion, a cost that is rising as fatefully as

lake waters.

Ancient Lake Minnewaukan

Devils Lake owes its existence to a continental glacier that covered much

of North America during the Pleistocene Epoch. Carving a basin as it advanced

over the landscape, the glacier deposited excavated materials along its leading

edges, leaving terminal moraines marking the farthest extent of glacial ice

sheets. Near the end of the Pleistocene, roughly 11,000 years ago, the glacier

began its retreat. As the glacier withdrew, glacial meltwaters poured into the

basin, creating a vast proglacial lake dammed by morainal deposits. Native

Americans called this lake Minnewaukan, meaning, among other possible

interpretations, Bad Spirit Water. Recent flooding has perhaps given credence to

a legend told by those Native Americans, claiming that the lake once overflowed

and flooded the entire world.

Based on abandoned beaches, or strand lines, geologists estimate that the

ancestral lake reached a maximum surface elevation of between 444 and 445

meters. At that elevation, the lake covered about 1,050 square kilometers, held

about 5 million acre-feet of water and had a maximum depth of around 50 meters.

A natural outlet called Tolna Coulee, which allowed water to flow out of the

basin and prevented the lake from rising and expanding further, controlled the

maximum elevation. How often the lake has overflowed is uncertain, but

geologists believe it has happened at least twice over the past 4,000 years,

most recently around 2,000 years ago.

During the centuries that followed the lake's origin, climate shifts caused

water levels to fluctuate between 6 and 12 meters every few hundred years.

Sediment analyses by geologist Edward Callender, published in his 1968

University of North Dakota doctoral thesis, indicated that the lake might have

been completely dry 6,500 years ago. After the lake last rose to its maximum

elevation and began overflowing, water levels continued to fluctuate in response

to alternating dry and wet periods. A persistently dry climate 500 to 600 years

ago held levels at relatively low elevations for perhaps as long as 200 years.

Wetter conditions followed, raising the lake to levels that prevailed until the

late 1800s. Levels then began dropping precipitously, falling to the

lowest-recorded elevation by 1940 before rising again.

Whether Lake Minnewaukan was completely dry at times or not, periodic

drawdowns during dry conditions reduced its immense volume to numerous remnant

lakes scattered across the south-central region of the basin. Nonindigenous

people who settled the region beginning in the mid-1800s named the largest and

most prominent of these remnants "Devils Lake," perhaps because of the lake's

highly saline, undrinkable water, or perhaps in tribute to Sioux warriors whose

canoes were often capsized in the lake's treacherous, storm-tossed waters.

In 1964, Devils Lake consisted of three principal basins called West Bay,

Main Bay and East Bay. West Bay then was essentially dry and Main Bay covered

about 53 square kilometers. The Rock Island State Military Reservation separated

East Bay—which covered about 27 square kilometers—from Main Bay. According to T.

E. B. Pope of the U.S. Bureau of Fisheries, Main Bay and East Bay had become

isolated during the 1890s after lake levels dropped about 6 meters during the

previous 25 to 30 years. Besides Devils Lake, other major lakes nearby included

Pelican Lake to the west and, to the east, East Devils Lake, Swan Lake, West

Stump Lake and East Stump Lake, in that order.

Water Supply and Overflows

Devils Lake receives nearly all of its water from surface runoff and direct

precipitation. Most surface-water runoff originates from a chain of remnant

lakes located a few kilometers north of Devils Lake, although many of these

smaller lakes have now merged with Devils Lake as the water levels rise. (By

September 2007, for example, Devils Lake and all of the lakes to the

east—including the two Stump lakes—had completely merged.) Total annual inflows

ranged from near zero during the drought-stricken 1930s to nearly 400,000

acre-feet in 1993. Inflows, averaging 65,500 acre-feet annually between 1950 and

1993, rose to 317,000 acre-feet annually between 1993 and 2000, a fivefold

increase. The years 1993 to 1995 contributed 24 percent of all inflow to Devils

Lake between 1950 and 1995.

If Devils Lake rises approximately two additional meters and begins

overflowing, as scientists predict it will, lake waters will enter the Sheyenne

River. The Sheyenne, which originates 50 kilometers west of the river's juncture

with the Tolna Coulee outlet, meanders on an easterly course that lies about 15

kilometers south of the Devils Lake Basin. After turning south, the river is

impounded by a Corps of Engineers dam (Bald Hill Dam) located 20 kilometers

north of Valley City, a town of about 6,300 residents. The dam's narrow

reservoir (Lake Ashtabula) extends 43 kilometers upstream and contains about

71,000 acre-feet of water at full capacity. After passing through Valley City,

the river joins the Red River of the North near the city of Fargo. The Red River

flows northward before emptying into Canada's Lake Winnipeg.

Like climate predictions in general, predictions about when the current

lake will overflow are rife with uncertainty. For example, in a report published

in 2008, the U.S. Geological Survey predicted that the probability of the lake

exceeding 443 meters between years 2008 and 2015 was only 10 percent, but the

lake reached that elevation in 2011. Also predicted was a 50-percent probability

that the lake would not exceed an elevation of 442 meters between 2008 and 2040.

In fact, the lake had reached 442 meters by June 2009. Recent computer

simulations predict that the probability of the lake overflowing by 2030 is only

15 to 20 percent, even with planned man-made outlets in operation. That scenario

may prove to be far too optimistic, however, given that precipitation totals

during water year 2011 (October 1–September 30), which are forecast to continue,

raised the lake 0.7 meters.

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