政策解讀
快速擇校
There are some earth phenomena you can count on, but the magnetic field, some say, is not one of them. It fluctuates in strength, drifts from its axis, and every few 100,000, years undergoes a dramatic polarity reversal—a period when north pole becomes south pole and south pole becomes north pole. But how is the field generated, and why is it so unstable?
Groundbreaking research by two French geophysicists promises to shed some light on the mystery. Using 80 metres of deep sea sediment (沉淀物) core, they have obtained measurements of magnetic-field intensity that span 11 polarity reversals and four million years. The analysis reveals that intensity appears to fluctuate with a clear, well-defined rhythm. Although the strength of the magnetic field varies irregularly during the short terra, there seems to be an inevitable long-term decline preceding each polarity reversal. When the poles flip—a process that takes several hundred thousand years—the magnetic field rapidly regains its strength and the cycle is repeated.
The results have caused a stir among geophysicists. The magnetic field is thought to originate from molten (熔化的) iron in the outer core, 3,000 kilometers beneath the earth's surface. By studying mineral grains found in material ranging from rocks to clay articles, previous researchers have already been able to identify reversals dating back 170 million years, including the most recent switch 730,000 years ago. How and why they occur, however, has been widely debated. Several theories link polarity flips to external disasters such as meteor (隕星) impacts. But Peter Olson, a geophysicist at the Johns Hopkins University in Baltimore, says this is unlikely if the French researchers are right. In fact, Olson says intensity that predictably declines from one reversal to the next contradicts 90 percent of the models currently under study. If the results prove to be valid, geophysicists will have a new theory to guide them in their quest to understand the earth's inner physics. It certainly points the direction for future research.
1.Which of the following titles is most appropriate to the passage?
A.Polarity Reversal: A Fantastic Phenomenon of Nature.
B.Measurement of the Earth's Magnetic-Field Intensity.
C.Formation of the Two Poles of the Earth.
D.A New Approach to the Study of Geophysics.
2.The word "flip" (Line6, Para, 2) most probably means "___".
A. decline
B. intensify
C. fluctuate
D. reverse
3.What have the two French geophysicists discovered in their research?
A.Some regularity in the changes of the earth's magnetic field.
B.Some causes of the fluctuation of the earth's magnetic field.
C.The origin of the earth's magnetic field.
D.The frequency of polarity reversals.
4.The French geophysicists' study is different from currently prevailing theories in____.
A.its identification of the origin of the earth's magnetic field
B.the way the earth's magnetic intensity is measured
C.its explanation of the shift in the earth's polarity
D.the way the earth's fluctuation rhythm is defined
5.In Peter Olson's opinion, the French experiment_____.
A.is likely to direct further research in the inner physics of the earth
B.has successfully solved the mystery of polarity reversals
C.is certain to help predict external disasters
D.has caused great confusion among the world's geophysicists
參考答案:A D A C A
特別聲明:①凡本網(wǎng)注明稿件來源為"原創(chuàng)"的,轉(zhuǎn)載必須注明"稿件來源:育路網(wǎng)",違者將依法追究責任;
②部分稿件來源于網(wǎng)絡,如有侵權(quán),請聯(lián)系我們溝通解決。
浙江同等學力申碩通過率較高,得益于免試入學的政策。大專及以上學歷可先參加課程學習,本科畢業(yè)有學位滿三年可申碩,申碩考試科目少、難度低,多種因素共同提升了通過率。
40歲讀在職研究生不晚。學習沒有年齡限制,40歲時通過在職研究生提升學歷、拓展能力,既能適配職場發(fā)展需求,又能實現(xiàn)自我成長,且在職學習可平衡工作與生活,年齡不是...
藝術(shù)學非全日制研究生備考攻略:核心目標為考點精準化、答題規(guī)范化和時間高效化。公共課(政治、英語)需抓重點:政治側(cè)重時政與高頻考點,強化答題框架;英語聚焦閱讀與寫...
歷史學在職研究生考什么科目?同等學力申碩和非全日制研究生各有特點?忌谶x擇報考方式時,應根據(jù)自身的實際情況,如專業(yè)基儲外語水平、備考時間和職業(yè)發(fā)展需求等,綜合...
教育學在職研究生考英語二嗎?不同招生方式的英語科目:非全日制研究生多數(shù)考英語二(少數(shù)可換小語種),同等學力申碩考申碩統(tǒng)考英語(難度低、60分合格),中外合作辦學...
生態(tài)學在職研究生報考院校有吉林農(nóng)業(yè)大學等,多為同等學力申碩模式,學制2年。同等學力申碩有入學靈活、邊工作邊學等優(yōu)勢,可參考院校專業(yè)、學費等選校,合理規(guī)劃提升深造...
評論0
“無需登錄,可直接評論...”