鹽水湖 的英文怎麼說

中文拼音 [yánshuǐ]
鹽水湖 英文
lagoon
  • : 名詞1. (食鹽; 鹽類) salt 2. (姓氏) a surname
  • : 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...
  • : 名詞1 (被陸地圍著的大片積水) lake 2 (指湖州) short for huzhou3 (指湖南、湖北) a name referr...
  • 鹽水 : saline water; salting liquor; salt solution; brine solution; brine鹽水精製 salt refining; 鹽水選...
  1. Quite different from lake asphaltite, whose depression is twelve hundred feet below the sea, it contains considerable salt, and one quarter of the weight of its water is solid matter, its specific weight being 1170, and, after being distilled, 1000

    大鹹成分很大,固體的質占的總重量四分之一。的合重是一千一百七十,其中的重量是一千。所以在這樣的裡魚是無法生存的。
  2. The lacustrine carbonate rocks in the wudaoliang group consist of boundstone ( stromatolite ), micritic limestone, grainstone and micritic dolostone which were laid down in the shallow - water to bathyal, high - salinity and enclosed to semi - enclosed lake systems

    五道梁群相碳酸巖分為生物粘結灰巖(疊層石) 、泥晶灰巖、顆粒灰巖與泥晶白雲巖四大類,反映出沉積環境為一個具有淺半深、高度、半封閉封閉特點的綜合泊系統。
  3. Research on the production of magnesium sulfate from bittern in salt lake

    直接生產硫酸鎂的研究
  4. The chinese immersed their wood in sea water or salt lakes prior to use as a building material.

    中國人在把木材用作建築材料前,先將它浸泡在海中。
  5. The separation of calcium sulfate from water - mining carnallite by flotation for the production of kcl from chaerhan salt lake was studied

    摘要研究了青海察爾汗採光鹵石礦生產氯化鉀工藝中浮選除鈣的方法。
  6. Through the phase diagram analysis and calculation, a production method to improve the quality of carnallite by evaporating the bittern from which the sodium chloride has been eliminated by brine mixing method is presented in this paper

    摘要通過相圖分析及計算,介紹了一種「由兌鹵除氯化鈉后,首先獲得成礦鹵,然後對其蒸發制取質量較好光鹵石礦」的生產方法。
  7. Some land-locked waters such as the dead sea and the great salt lake contain waters that are nearly saturated with dissolved solids.

    有些內陸封閉的域,如死海及大,幾乎為飽和溶解固體的
  8. Abstract : based on the synthetical data from the remote images, geological section, geomorphologic landscape, ancient water system evolution and surface feature spectrum etc, the study indicates that there is an undersand lake in the northern peripberal belt of qarhan salt lakes of qaidam basin

    文摘:根據地球衛星遙感影象、地物波譜測定以及地貌景觀、古系演化和地面地質調查等資料的綜合研究表明,柴達木盆地察爾汗礦區北部外圍地帶存在一種新的成因類型的? ?沙下
  9. Besides, the sedimentary facies of upper ganchaigou and lower ganchaigou formation were also mapped in supersequences which are the main target strata for exploration. the high resolution sequence stratigraphic framework showed the genetic relationship between the distributions of sedimentary facies and their tectonic settings. the near - source sedimentary systems such as subaqueous alluvial fan and lake - floor fan are often deposed in rise - hemicycles in the steep slope background in the north, the coarse lithology of fan - delta prograded from north to south in fall - hemicycles, and the braided stream facies are formed in the rise - hemicycles in gentle slope background in the south, braided stream facies prograded from sorth to north in the fall - hemicycles, but the lacustrine facies and salt lake facies developed in the middle part of the area

    詳細的沉積相研究發現,紅獅地區第三系發育有沖積扇、下沖積扇、河流、三角洲、扇三角洲、泊和底扇7種主要沉積相類型,並對作為區內主要勘探目的層系的下乾柴溝組和上乾柴溝組進行了以超層序為單位的沉積相平面編圖,以較高的時間解析度揭示了區內沉積相帶的平面展布及其在不同構造背景中的分佈規律,比如在北部的凹陷陡坡背景下,上升半旋迴低位期通常發育有下扇、底扇等陡岸近源特徵的沉積體系,下降半旋迴高位期,扇三角洲相粗碎屑巖由北向南進積;在南部的凹陷緩坡背景下,上升半旋迴主要發育辮狀河流相,下降半旋迴辮狀河三角洲相由南向北進積;而中部紅柳泉一獅子溝一帶則為泊相沉積和類沉積。
  10. Research on producing lithium sulfate by intercrystalline brines from jilaier lake of xitai to salt out

    西臺吉乃爾晶間鹵兌鹵析制取硫酸鋰的研究
  11. Trend surface analysis on fluctuation of intercrystalline brine with time and space during the time of mining brine in qarhan salt lake

    察爾汗采鹵過程中晶間鹵位時空變化規律的趨勢面分析
  12. From studies of these characteristics of structures, palaeontology, drilling, well logging, seismic profile, salt chemistry and lacustrine sedimentary system, it is recognized that the new characteristics occur in of section pukou and in huaiyiri sag, and the huge thickness of salt rocks is formed by the crust salt materials upwelling along deep fracture in the form of hot bittern and entering lacustrine basin in this area

    通過該區構造、古生物、鉆井、測井、地震、巖化學及盆內沉積體系等特徵的研究,認為淮陰凹陷浦口組二段和三段的沉積構造有其特殊性,巨厚的巖層是殼深部類物質沿深大斷裂上涌以熱鹵形式進入盆的結果。
  13. The coqen basin in xizang lies between the bangong - nujiang suture zone and yarlung zangbo suture zone, and once extended northwards and southwards, respectively centred by the qiekan - goicang - asog rift zone as the center of deposition and subsidence during the middle jurassic to the early creatceous. ( 1 ) during the middle - late jurassic, the rift zone was occupied by deep - water turbidites, radiolarian siliceous rocks, shallow - water carbonate rocks, clastic rocks and basic - ultrabasic rocks, while both sides of it by littoral and shallow marine elastic rocks and carbonate rocks

    摘要位於班公怒江縫合帶與雅魯藏布江縫合帶之間的措勤盆地,在中侏羅世早白堊世期間具有以且坎古昌阿索裂谷帶為沉積、沉降中心向南北兩側展開的古地理格局:中晚侏羅世時期,裂谷帶內由深濁積巖、放射蟲硅質巖和淺碳酸巖、碎屑巖巖片及基性超基性巖等組成;裂谷帶兩側由濱淺海相碎屑巖和碳酸巖組成。
  14. Tufa form when underwater springs rich in calcium meet lake water rich in carbonates, forming calcium carbonate, or limestone

    由於地下富含鈣,而又富含碳酸,於是兩者接觸便產生出碳酸鈣,即石灰石。
  15. Study of clay minerals and trace metals composition of suspensions in water column of vanda lake in antarctica

    南極洲萬達的懸浮物中的粘土礦物和痕量金屬組成的研究
  16. Ice cores contain evidence that sudden cold periods occurred after the north atlantic became less salty, perhaps because freshwater lakes burst through the walls of glaciers and found their way to the sea

    冰心內的證據顯示,北大西洋度降低后驟冷時期才開始,這或許是由於淡沖破冰河築成的屏障流入海中所致。
  17. Places of interest : plover cove, panorama of pat sin leng and ma on shan

    半島上設有觀景臺,遊人可遠眺船灣淡、八仙嶺、田仔和馬鞍山的景色。
  18. 6 avoid swimming in fresh water. salt water is usually safer

    6不要在淡中游泳,鹽水湖海通常比較安全。
  19. Compared with the distributions of cyanophyta in other three salt lakes of china, cyanophyta distributions in polyhalinous waters is more similar than those in freshwaters

    與國內其它3個藻類的分佈相比較,藍藻在混體比淡體具有更高的相似性。
  20. Located in front of dajhong templ, sihcaohu is a saline water lake that formed after the flood of taijiang in 1823 daoguang 3rd year, cing dynasty. it has a broad surface and uneven shores. people can reach anping from the lake

    位於大眾廟前,是道光三年(西元1823年)臺江大風雨所形成的鹽水湖面壯闊,岸曲折,循著路可直達安平。
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