淡水層 的英文怎麼說

中文拼音 [dànshuǐcéng]
淡水層 英文
fresh water aquifer
  • 淡 : 形容詞1 （液體或氣體稀薄） thin; light 2 （味道不濃; 不咸） tasteless; weak 3 （顏色淺） light; f...
  • 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...
  • 層 : i 量詞1 （用於重疊、積累的東西 如樓層、階層、地層） storey; tier; stratum 2 （用於可以分項分步的...
  • 淡水 : freshwater淡水湖 limn; freshwater lake; 淡水生物 freshwater organisms; 淡水養魚 freshwater piscic...
  1. A problem which is often attacked by resistivity measurements is to locate the depth at which saltwater invades fresh water in aquifers.

    經常用電阻率測量來攻克的問題是確定含水層中鹽水侵入淡水的深度。
  2. The salt water, being more dense, flows upstream under the fresh water which is flowing downstream.

    淡水在上層向下流動，比重更大的鹽水在下層逆流向上。
  3. Salaquifers have also been used for the storage of fresh water and natural gas.

    鹹水層也用來貯存淡水和天然氣。
  4. The site provides information resources focusing on limnology ， lake management and freshwater benthic ecology ， as well as the domain of sustainable development of freshwater and marine eco - systems ， including knowledge of limnology, eutrophication, pollutants, lake restoration, as well as other related information

    該網站重點提供有關湖沼學、湖泊管理和淡水底層生態學以及淡水和海洋生態系統可持續發展領域的信息資源，內容包括湖沼學、富營養化、污染物、湖泊恢復的知識以及其他有關的信息。
  5. In this paper, the nacre of hyriopsis cumingii ( lea ) which is one of the main freshwater pearl - forming mollusk in china is studied emphatically, as compared with the nacre of three species of saltwater pearl - forming mollusks, pinctada martensii ( dunker ), pinctada maxima ( jameson, and peteria penguin ( roding ). the basic characteristics of nacreous and prismatic layers are understood by powder x - ray diffraction analysis, trace elements analysis, amino acid composition of protein and differential thermal analysis

    本文以我國主要育珠蚌淡水三角帆蚌貝殼珍珠層為重點研究對象，以三種海水育珠貝馬氏珍珠貝、企鵝珍珠貝及大珠母貝貝殼珍珠層為對比研究對象，首先通過粉末x -射線衍射、微量元素分析、蛋白質氨基酸分析及差熱分析對珍珠層及其與之密切共生的稜柱層的基本特徵進行了初步研究。
  6. Touke stratum was laid down in the pliocene and early pleistocene epochs. it is some 1500 meters thick on average, and rich in fossils. the fossil beds of tsailiao creek in tsochen were made famous by the discovery there in 1971 of the skull of " tsochen man.

    也由於左鎮鄉的地質為上新世至更新世早期的頭?山層，平均厚度為一千五百公尺，此層中含有豐富的海相濱海相淡水相等各類化石群，隨著地殼隆起而露出成陸。
  7. 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。
  8. Both tidal mixing and wind stirring can weaken the vertical stratification induced by freshwater buoyancy, but different mechanisms dominate such a process : tidal mixing is accomplished through the upward dissipation of turbulent kinetic energy whereas wind stirring is in the opposite direction

    盡管潮汐混合和風的攪動作用均能削弱河流沖淡水浮力引起的垂直層化現象，但是其控制機制有所不同：潮汐混合是通過湍流動能自下向上的耗散來完成的，風攪動的方向恰好相反。
  9. Water quality ; design and use of quantitative samplers for benthic macro - invertebrates on stony substrata in shallow freshwaters iso 8265 : 1988 ; german version en 28265 : 1994

    水質.淺淡水中多石底層上水底大無脊椎動物的定量取樣
  10. Large scale salt - water intrusion has been occurred since late 1970 ' s due to freshwater exploitation by human activity

    20世紀70年代末期以來，隨著對地下淡水的過度開采，淡鹹水水頭壓力差減小，鹵水通過古河道砂層快速南侵。
  11. The integrated study of heavy mineral, palaeocurrent direction, and sedimentary facies distribution has disclosed that the detritus are derived chiefly from the southeast and east - northeast during the deposition of the yanchang formation in the late triassic. the variations in the palaeocurrent directions have consequences for the development and distribution of the sequence stratigraphy and sedimentary facies of the yanchang formation. the major and trace element analyses of the mudstones from the yanchang formation also show that the lake waters would be freshened to brackish

    初次通過泥巖常、微量元素測試資料和沉積學分析得出，延長期富縣探區湖泊水體屬于淡水-微鹹水，微量元素含量及其比值在剖面上的變化對延長期湖平面升降和氣候的演變具有良好的響應，湖平面升降、氣候演變對層序地層的發育有著直觀而又重要的影響。
  12. Water quality - biological methods - methods of biological sampling : guidance on the design and use of quantitative samplers for benthic macro - invertebrates on stony substrata in shallow freshwater

    水質.生物法.生物取樣法.淺淡水中多石底層上大無脊椎動物定量取樣器設計和使用指南
  13. The genetic types include weathering, regional meteoric corrosion, regional dolomitization regional paleokarstification, regional dedolomitization and regional fresh - water cementation and filling

    研究區存在包括風化、區域性大氣淡水溶蝕、區域性白雲巖化、區域性古巖溶、區域性去白雲巖化和區域性淡水膠結充填等6種巖溶作用的層序成因類型。
  14. Thirty - five percent is in rivers and lakes, and in aquifers deep under the ground

    35 %的淡水在河、湖及地下深處的蓄水層。
  15. Thirty - five percent is in the rivers and lakes and in aquifers, deep underground

    35 %的淡水儲存在河流、湖泊和地下深處的蓄水層中。
  16. The comprehensive geological characteristic has been fully studied in this paper. on the basis of this, closely combining production practice, the favorable gas developing regions have been determined with the methods of sedimentary facies and combination of generation, reservoir and caprock, and logging parameters interpretation maps and regression formulas have been established with logging data, as well as reprocessing, interpretation and identification of gas reservoir have been done with computer. integrating the information and results of geology, logging, testing and geophysics, the gas reservoir distribution regularity of structure of no. 1 sebei has been described and reserves in place of no. 1 ' sebei gas field have been recalculated, which have provided a basis for next step of development in research area

    在近十多年，通過提高地震資料處理精度、淡水聚合物泥漿的應用、數字測井技術的運用、並加強了低電阻層和差物性層的試氣及氣田擴邊鉆探，大大提高了對氣層的識別，大量增加了氣層的層數和厚度，擴大了氣田的含氣面積，使氣田儲量通過多次復查核算仍在不斷增加本論文充分研究了青海澀北一號氣田天然氣地質綜合特徵，並以此為基礎緊密結合生產實踐，應用沉積相與生儲蓋組合等方法確定氣藏有利發育區帶，應用測井資料建立測井參數解釋圖版並回歸公式，應用計算機重新處理、解釋和識別氣層，綜合地質、測井、試井、物探等多方面信息與成果，描述了澀北一號構造的氣層分佈規律，重新計算了澀北一號氣田的地質儲量，為研究區下一步開發提供了依據。
  17. Ecological considerations for the use of oilspill dispersants in freshwater and other inland environments, impermeable surfaces

    在淡水及其它內陸環境非滲透層上使用浮油分散劑的生態條件
  18. The paper has made a comprehensive study to marine carbonate oolitic reservoir in triassic of feixianguan group of intra - platform taphrogenic trough basin in north - east past of sichuan basin. according to the principle of high resolution stratigraphic sequence, combined with original results gained form the area, the author have built up the base level cycles and fades model of different stages based on the surface identification mark of base level cycle using the information of geology, seismic, logging, core and outcrops

    1 、依據層序地層學高解析度基準面旋迴原理與識別技術，建立了裂陷槽向上變淺直至露出水面過程中形成的基準面旋迴變化的7種特徵性識別標志，包括泥巖表面乾裂、淡水選擇性溶蝕、白雲化現象、白雲巖、石膏、伽瑪曲線高值、向上變厚、變粗序列、向上變細、變泥、變紅序列、向上值變低序列等。
  19. This condition is also true for e2 but inversely for e6, p2 and p1 station which declined about 10 times compared with data of last autumn. prochlorococcuswas found in p3, e7, e6, p2 during autumn cruise, and in p2, p1 during spring cruise

    在春季，僅在p2 、 p1站的混合層檢測到，位置相比秋季外移，可能與長江沖淡水在此季節逐漸強盛有關，原綠球藻較少分佈於低鹽度水體。
  20. The freshwaters, such as changjiang river and hangzhou bay, bring with abundant nutrients which result in significantly enhanced biological activities, and thus lead to pronouncedly increased consumption of co2

    東海夏季，雖然有長江、杭州灣等大量的高含量pco :淡水輸入，但在東海中部有大片區域的表層海水是大氣coz的匯區。
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