问题 阅读理解与欣赏

阅读《雷雨》片断,完成小题。

周朴园 哦,侍萍!(低声)是你?

鲁侍萍 你自然想不到,侍萍的相貌有一天也会老得连你都不认识了。

周朴园不觉地望望柜上的相片,又望望侍萍。半晌。

周朴园 (忽然严厉地)你来干什么?

鲁侍萍 不是我要来的。

周朴园 谁指使你来的?

鲁侍萍 (悲愤)命,不公平的命指使我来的!

周朴园 (冷冷地)三十年的工夫你还是找到这儿来了

鲁侍萍 (悲愤)我没有找你,我没有找你,我以为你早死了。我今天没想到到这儿来,这是天要我在这儿又碰见你。

小题1:划线句“三十年的工夫你还是找到这儿来了”有言外之意,下列分析正确一项是(  )

A.三十年了,你还是念念不忘我。

B.三十年了,你终于还是找到我了,我还是没躲过你的追寻。

C.已经三十年了,你到我这里来,还有什么用呢?

D.你没有死,这将对我的名誉地位构成严重的威胁。小题2:鲁侍萍不止一次说到命运,“不公平的命指使我来的”,“这是天要我在这儿又碰见你”。对侍萍的命运观,分析正确的一项是(  )

A.侍萍不能解释自己三十年来为什么受那么多苦,不得不自认是“不公平的命”所使然。

B.鲁侍萍在苦难中挣扎,悲叹自己的“命苦”,她相信命运,但也表现出对世道不公的愤懑与不平。

C.她虽然一再说“命运”如何,但并无深意,只是客观反映了她对自己苦难一生的悲叹。

D.三十年的苦和恨,使被侮辱与被损害的侍萍觉醒了,她所说的“命”,从根本上看,是对不公平世道的控诉与抗争。小题3:下列课文语句的分析,错误的一项是(   )

A.3月14日下午两点三刻,当代最伟大的思想家停止思想了。

——“停止思想”讳饰的手法,表达了尊重之情同时突出了马克思是一个思想家,而且表达了恩格斯对马克思逝世的惋惜之情。

B.自由和平等的爽朗的秋天如不到来,黑人义愤填膺的酷暑就不会过去。

——“爽朗的秋天” 比喻黑人获得平等、自由和民主的时代, “酷暑”比喻美国黑人争取平等、自由和民主的的斗争精神和义愤填膺的反抗情绪。

C.他对这一切毫不在意,把它们当作蛛丝一样轻轻拂去。

——借代修辞,含蓄发人深思。它具有两方面的含义:一是说明敌人对马克思的攻击很多,但十分无力;二是说明马克思对敌人十分蔑视,表现了马克思崇高的思想境界。

D.100年后的今天,黑人仍生活在物质充裕的海洋中的一个贫困的孤岛上。100年后的今天,黑人仍然萎缩在美国社会的角落里,并且意识到自己是故土家园中的流亡者。——这两句话它深刻地揭示了美国黑人地位(“角落里”)低下,物质生活贫困(“贫困孤岛上)”和精神生活贫乏(“萎缩”)。

答案

小题1:D

小题2:B

小题3:C

小题1:

题目分析:潜台词是角色内心想表达而没有说出来的那部分意思。三十年了,你还是找来了。显然,周朴园不是要说自己的躲避,而是想说,三十年,没想到你没有死,你这一来,我的一切都将受到极大的威胁——名声、地位。

小题2:

题目分析:侍萍是广大不幸的底层人民的代表,他们从思想上还不能清楚地认识到造成自己命运悲剧的原因是什么,他们只有慨叹命运的不幸,当然,朦胧中,他们也深切的感受到种种不公,所以,在侍萍的话语中,既有对命运的悲吟,也有对生活不公的责问。

小题3:

题目分析:本句运用了比喻的修辞手法,而不是借代。

单项选择题
单项选择题

El Nino is the term used for the period when sea surface temperatures are above normal off the South American coast along the equatorial Pacific, sometimes called the Earth’s heartbeat, and is a dramatic but mysterious climate system that periodically rages across the Pacific.

El Nino means "the little boy" or "the Christ child" in Spanish, and is so called because its warm current is felt along coastal Peru and Ecuador around Christmas. But the local warming is just part of an intricate set of changes in the ocean and atmosphere across the tropical Pacific, which covers a third of the Earth’s circumference. Its intensity is such that it affects temperatures, storm tracks and rainfall around the world.

Droughts in Africa and Australia, tropical storms in the Pacific, torrential rains along the Californian coast and lush greening of Peruvian deserts have all been ascribed to the whim of EI Nino. Until recently it has been returning about every three to five years. But recently it has become more frequent--for the first time on record it has returned for a fourth consecutive year--and at the same time a giant pool of unusually warm water has settled down in the middle of the Pacific and is showing no signs of moving.

Climatologists don’t yet know why, though some are saying these aberrations may signal a worldwide change in climate. The problem is that nobody really seems sure what causes the El Nin o to start up, and what makes some per than others. And this makes it particularly hard to explain why it has suddenly started behaving so differently.

In the absence of EI Nino and its cold counterpart, La Nina, conditions in the tropical eastern Pacific are the opposite of those in the west. the east is cool and dry, while the west is hot and wet. In the east, it’s the winds and currents that keep things cool. It works like this. Strong, steady winds, called trade winds, blowing west across the Pacific drag the surface water along with them. The varying influence of the Earth’s rotation at different latitudes, known as the Coriolis effect, causes these surface winds and water to veer towards the poles, north in the northern hemisphere and south in the southern hemisphere. The surface water is replaced by colder water from deeper in the ocean in a process known as upwelling.

The cold surface water in turn chills the air above it. This cold dense air cannot rise high enough for water vapor to condense into clouds. The dense air creates an area of high pressure so that the atmosphere over the equatorial eastern Pacific is essentially devoid of rainfall.

In exploring the effect of EI Nino, the author mainly focuses on()

A. its violence

B. its conditions

C. its regularity

D. its features