陸坡海水的 的英文怎麼說

中文拼音 [liùpōhǎishuǐde]
陸坡海水的 英文
bathypelagic
  • 陸 : 陸數詞（六的大寫） six （used for the numeral 六 on cheques, etc. to avoid mistakes or alterations）
  • 坡 : Ⅰ名詞（地面傾斜的地方） slope Ⅱ形容詞（傾斜） sloping; slanting
  • 水 : 名詞1 （由兩個氫原子和一個氧原子結合而成的液體） water 2 （河流） river 3 （指江、河、湖、海、洋...
  • 的 : 4次方是 The fourth power of 2 is direction
  • 海水 : seawater; brine; the sea海水剝蝕 [地質學] marine denudation; 海水淡化 desalination of sea water; ...
  1. This continental slope usually starts at a place somewhere near the 100 - fatheom mark and in the course of a few hundred miles reaches the true ocean floor at 2, 500 - 3, 500 fathoms

    大陸架慢坡一般是從差不多100英尋水深的地方開始的，一直延伸到幾百英里遠深達2 ， 500至3 ， 500的地方，那裡才是真正的海底。
  2. The topography and the physiognomy of the south china sea are very complex such as continental slop, continental shelves, seamounts, sea basin, etc. the south china sea lies between qingzang plateau, which is as the main driver of the variety of climate, and the western part of the pacific, which is called warm pool, and is influenced by some current systems, such as coastal current, kuroshi, etc. the south sea has considerable species

    南海具有陸坡、陸架、海溝、海盆等復雜的地形、地貌；南海位於作為地球氣候變化的主要驅動力的青藏高原和西太平洋暖池之間；南海受到沿岸流、南海暖流水、黑潮入侵水等流系的影響；南海具有豐富的物種分佈；上述因素共同影響南海生源要素的分佈、輸送和遷移。
  3. The company has a technical researching and developing department both in singapore, beijing and shanghai. experts from famous universities and research institutions work with employee of batf to develop reliable and new products to meet with different requirements of our customers throughout the world. and now it push more than 30 new categories of international standard latex

    公司擁有現代化專業化國際化的乳液研發機構，在新加坡北京上海建立了乳液研發中心和乳液應用研究所，聚集了一大批行業專家教授高級工程師和企業管理人才，陸續推出了30多種具有國際水準的乳液新品種。
  4. The condition of profiles in outer station did n ' t change much in spring cruise, but showed more variable in near - shore stations when observed in different time. fluorescent characteristic per cell can be obtained by flowcytometric analysis. based on fluorescence data of synechococcus of all stations, two distinctly pigment - containing cell types coexisting can be found in some stations of east china sea, which located in all depth of p3, mixlayer of e7, 40 - meter depth of e6 of autumn cruise and in mixlayer of p2 of spring cruise

    通過對流式細胞計測量的細胞熒光結果來看，在秋季的p3 、 e7整個混合層、 e6站40米層，春季的p2站均發現有兩群不同色素含量的聚球藻（ high一pe和low一pe ）共存現象，極有可能分別屬于不同品系，春季共存站位位置比秋季時更靠外，表明在秋季p3 、 e7等站位的共存是季節性現象，可能與此季節黑潮次表層水沿陸架坡涌升入侵到中陸架有關，水團的運動及混合使從外海遷移而來的high一pe與近岸的low一pe得以共存，在春季，由於長江沖淡水的日漸強盛，在中陸架區的共存區域有所外移。
  5. The carbonate source rocks of middle - upper ordovician in tarim basin are widely distributed in different sedimentary environments at the same period such as platform margin slope, platform inner sag, continental shelf, abyssal basin, etc

    摘要塔里水盆地中上奧陶統碳酸鹽巖烴源巖在同一時期不同的沉積環境（臺緣斜坡、臺地內凹陷、陸棚、深海盆地等）中均有發育。
  6. According to the differences of sedimentary facies and environment, the source rock are divided into four types such as lime - mud reef in platform margin, platform inner sag, deep - water flat slope or continental shelf, abyssal basin, the lime - mud reef type is distributed in platform margin of upper ordovician, the remained three types are widely distributed in cambrian - ordovician system

    根據沉積相帶與沉積環境的不同，可將烴源巖劃分為在不同沉積環境中的4種類型烴源巖；臺地邊緣灰泥丘型烴源巖、臺地內凹陷型烴源巖、深水緩坡與陸棚型烴源巖、深海盆地型烴源巖。
  7. The results show that kuroshio intrudes onto the continental shelf of east china sea in large scale and during its flow water is exchanged ceaselessly with outer sea along ryukyu island

    模擬結果表明黑潮在東海陸架有大規模的入侵，其在沿東海陸坡流動途中沿著沖繩島與外海不斷的進行水體交換。
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