2023年職稱英語(yǔ)理工類完形填空專項(xiàng)練習(xí)題

雕龍文庫(kù) 分享 時(shí)間: 收藏本文

2023年職稱英語(yǔ)理工類完形填空專項(xiàng)練習(xí)題

  第6部分:完形填空:考查應(yīng)試者正確把握文章內(nèi)容,以及在一定語(yǔ)境中準(zhǔn)確使用詞語(yǔ)的能力。本部分為1篇300~450詞的短文,文中有15處空白,每處空白給出4個(gè)選項(xiàng),要求應(yīng)試者根據(jù)短文的內(nèi)容從4個(gè)選項(xiàng)中選擇l個(gè)最佳答案。

  Earths Inner Core

  Scientists have long struggled to understand what lies at the planets center. Direct observation of its center is impossible, so researchers must (1) to other evidence.

  In 1889, a German scientist detected a severe earthquake in Japan. Geophysicists concluded that shock waves (2) jolts (晃動(dòng)) from one side of Earth through the center to the other side. Then in 1936, Danish geophysicist Inge Lehmann studied the waves (3) to determine that within Earths core of molten (熔化了的) iron lies a solid inner core - but (4) that core was made of eluded (難倒) her. Other geophysicists quickly determined that Lehmanns inner core was composed mostly (5) iron. Since then, Lehmanns discovery has (6) conventional Earth science.

  But now scientists are challenging traditional theory with new and radical (7). For example, Earths center could actually contain an inner core within the inner core, claim Ishii and colleague Adam Dziewonski.

  Analyzing hundreds of thousands of earthquake wave (8), they maintain that the inner core has at its heart a tiny, even more solid sphere (球體). This sphere may be the oldest fossil (9) from the formation of Earth, says Dziewonski.

  Dziewonski and Ishii speculate that shortly (10) Earth formed around 4.8 billion years ago, a giant asteroid (小行星) smashed into the young planet and nearly melted it. But Earths center didnt quite melt; it (11) mass as the planet cooled. The core within a core may be the kernel (核心) that endured. Its presence could change our basic ideas about the (12) of the planet, Dziewonski says.

  Dziewonskis idea is tame (溫和的) compared to the (13) theories of independent geophysicist J. Marvin Herndon. Earths inner core is made not of iron, he claims, but a (14) of nickel and silicon. Herndon has a truly revolutionary notion: Within the nickel silicide (硅化物) inner core is also an inner inner core - an 8 km-wide ball of the element uranium. Uranium is radioactive. Herndon thinks the uranium releases heat energy as its atoms (15) fission-split and crash into one another in a chain reaction. In other words, we may live on top of a gigantic, natural nuclear power plant.

  1 A try B leave C turn D point

  2 A create B receive C feel D overcome

  3 A work B solution C job D patterns

  4 A whether B what C why D how

  5 A from B within C of D to

  6 A followed B dominated C restored D opposed

  7 A ideas B demands C phenomena D movements

  8 A things B acts C methods D records

  9 A taken B benefited C left D kept

  10 A after B before C since D when

  11 A expanded B modified C gained D melted

  12 A size B origin C structure D shape

  13 A radical B traditional C classical D conventional

  14 A system B copy C model D compound

  15 A charge B last C experience D show

  參考答案:

  1. C 2. A 3. D 4. B 5. C 6. B 7. A 8. D 9. C 10. A 11. C 12. B 13. A 14. D 15. C

  

  第6部分:完形填空:考查應(yīng)試者正確把握文章內(nèi)容,以及在一定語(yǔ)境中準(zhǔn)確使用詞語(yǔ)的能力。本部分為1篇300~450詞的短文,文中有15處空白,每處空白給出4個(gè)選項(xiàng),要求應(yīng)試者根據(jù)短文的內(nèi)容從4個(gè)選項(xiàng)中選擇l個(gè)最佳答案。

  Earths Inner Core

  Scientists have long struggled to understand what lies at the planets center. Direct observation of its center is impossible, so researchers must (1) to other evidence.

  In 1889, a German scientist detected a severe earthquake in Japan. Geophysicists concluded that shock waves (2) jolts (晃動(dòng)) from one side of Earth through the center to the other side. Then in 1936, Danish geophysicist Inge Lehmann studied the waves (3) to determine that within Earths core of molten (熔化了的) iron lies a solid inner core - but (4) that core was made of eluded (難倒) her. Other geophysicists quickly determined that Lehmanns inner core was composed mostly (5) iron. Since then, Lehmanns discovery has (6) conventional Earth science.

  But now scientists are challenging traditional theory with new and radical (7). For example, Earths center could actually contain an inner core within the inner core, claim Ishii and colleague Adam Dziewonski.

  Analyzing hundreds of thousands of earthquake wave (8), they maintain that the inner core has at its heart a tiny, even more solid sphere (球體). This sphere may be the oldest fossil (9) from the formation of Earth, says Dziewonski.

  Dziewonski and Ishii speculate that shortly (10) Earth formed around 4.8 billion years ago, a giant asteroid (小行星) smashed into the young planet and nearly melted it. But Earths center didnt quite melt; it (11) mass as the planet cooled. The core within a core may be the kernel (核心) that endured. Its presence could change our basic ideas about the (12) of the planet, Dziewonski says.

  Dziewonskis idea is tame (溫和的) compared to the (13) theories of independent geophysicist J. Marvin Herndon. Earths inner core is made not of iron, he claims, but a (14) of nickel and silicon. Herndon has a truly revolutionary notion: Within the nickel silicide (硅化物) inner core is also an inner inner core - an 8 km-wide ball of the element uranium. Uranium is radioactive. Herndon thinks the uranium releases heat energy as its atoms (15) fission-split and crash into one another in a chain reaction. In other words, we may live on top of a gigantic, natural nuclear power plant.

  1 A try B leave C turn D point

  2 A create B receive C feel D overcome

  3 A work B solution C job D patterns

  4 A whether B what C why D how

  5 A from B within C of D to

  6 A followed B dominated C restored D opposed

  7 A ideas B demands C phenomena D movements

  8 A things B acts C methods D records

  9 A taken B benefited C left D kept

  10 A after B before C since D when

  11 A expanded B modified C gained D melted

  12 A size B origin C structure D shape

  13 A radical B traditional C classical D conventional

  14 A system B copy C model D compound

  15 A charge B last C experience D show

  參考答案:

  1. C 2. A 3. D 4. B 5. C 6. B 7. A 8. D 9. C 10. A 11. C 12. B 13. A 14. D 15. C

  

信息流廣告 周易 易經(jīng) 代理招生 二手車(chē) 網(wǎng)絡(luò)營(yíng)銷 旅游攻略 非物質(zhì)文化遺產(chǎn) 查字典 社區(qū)團(tuán)購(gòu) 精雕圖 戲曲下載 抖音代運(yùn)營(yíng) 易學(xué)網(wǎng) 互聯(lián)網(wǎng)資訊 成語(yǔ) 成語(yǔ)故事 詩(shī)詞 工商注冊(cè) 注冊(cè)公司 抖音帶貨 云南旅游網(wǎng) 網(wǎng)絡(luò)游戲 代理記賬 短視頻運(yùn)營(yíng) 在線題庫(kù) 國(guó)學(xué)網(wǎng) 知識(shí)產(chǎn)權(quán) 抖音運(yùn)營(yíng) 雕龍客 雕塑 奇石 散文 自學(xué)教程 常用文書(shū) 河北生活網(wǎng) 好書(shū)推薦 游戲攻略 心理測(cè)試 石家莊人才網(wǎng) 考研真題 漢語(yǔ)知識(shí) 心理咨詢 手游安卓版下載 興趣愛(ài)好 網(wǎng)絡(luò)知識(shí) 十大品牌排行榜 商標(biāo)交易 單機(jī)游戲下載 短視頻代運(yùn)營(yíng) 寶寶起名 范文網(wǎng) 電商設(shè)計(jì) 免費(fèi)發(fā)布信息 服裝服飾 律師咨詢 搜救犬 Chat GPT中文版 經(jīng)典范文 優(yōu)質(zhì)范文 工作總結(jié) 二手車(chē)估價(jià) 實(shí)用范文 古詩(shī)詞 衡水人才網(wǎng) 石家莊點(diǎn)痣 養(yǎng)花 名酒回收 石家莊代理記賬 女士發(fā)型 搜搜作文 石家莊人才網(wǎng) 鋼琴入門(mén)指法教程 詞典 圍棋 chatGPT 讀后感 玄機(jī)派 企業(yè)服務(wù) 法律咨詢 chatGPT國(guó)內(nèi)版 chatGPT官網(wǎng) 勵(lì)志名言 河北代理記賬公司 文玩 語(yǔ)料庫(kù) 游戲推薦 男士發(fā)型 高考作文 PS修圖 兒童文學(xué) 買(mǎi)車(chē)咨詢 工作計(jì)劃 禮品廠 舟舟培訓(xùn) IT教程 手機(jī)游戲推薦排行榜 暖通,電地暖, 女性健康 苗木供應(yīng) ps素材庫(kù) 短視頻培訓(xùn) 優(yōu)秀個(gè)人博客 包裝網(wǎng) 創(chuàng)業(yè)賺錢(qián) 養(yǎng)生 民間借貸律師 綠色軟件 安卓手機(jī)游戲 手機(jī)軟件下載 手機(jī)游戲下載 單機(jī)游戲大全 免費(fèi)軟件下載 石家莊論壇 網(wǎng)賺 手游下載 游戲盒子 職業(yè)培訓(xùn) 資格考試 成語(yǔ)大全 英語(yǔ)培訓(xùn) 藝術(shù)培訓(xùn) 少兒培訓(xùn) 苗木網(wǎng) 雕塑網(wǎng) 好玩的手機(jī)游戲推薦 漢語(yǔ)詞典 中國(guó)機(jī)械網(wǎng) 美文欣賞 紅樓夢(mèng) 道德經(jīng) 標(biāo)準(zhǔn)件 電地暖 網(wǎng)站轉(zhuǎn)讓 鮮花 書(shū)包網(wǎng) 英語(yǔ)培訓(xùn)機(jī)構(gòu) 電商運(yùn)營(yíng)
主站蜘蛛池模板: 五月婷婷在线免费观看| 韩国资源视频一区二区三区| 中文字幕日韩精品麻豆系列| 亚洲第一极品精品无码久久| 国产成人精品啪免费视频| 日日操夜夜操视频| 毛片在线高清免费观看| 精品亚洲456在线播放| 一二三四在线观看高清| 亚洲变态另类一区二区三区| 国产三区视频在线观看| 国产精品污WWW一区二区三区| 日本在线视频www色| 波多野结衣伦理视频| 色婷婷综合在线| 99热成人精品国产免国语的| 久久精品国产99久久久古代 | 久久99精品久久久久婷婷| 亚洲欧美另类一区| 另类小说图片综合网| 国产大陆xxxx做受视频| 国偷自产AV一区二区三区| 性色AV一区二区三区无码| 日韩毛片基地一区二区三区| 欧美黑人粗大xxxxbbbb| 看亚洲a级一级毛片| 老司机带带我懂得视频| 欧美色图在线播放| 田中瞳中文字幕久久精品| 97青青草原国产免费观看| a色毛片免费视频| 久久精品一本到99热免费| 免费看男人j放进女人j色多多| 国产伦精品一区二区三区免费迷 | 欧美成人黄色片| blacked欧美一区二区| 久久人人爽人人爽人人片AV高清| 亚洲小视频在线| 亚洲精品视频在线播放| 十八岁污网站在线观看| 噜噜噜噜天天狠狠|