非碳酸鹽 的英文怎麼說

中文拼音 [fēitànsuānyán]
非碳酸鹽 英文
noncarbonate
  • : Ⅰ名詞1 (錯誤) mistake; wrong; errors 2 (指非洲) short for africa 3 (姓氏) a surname Ⅱ動詞1 ...
  • : 名詞[化學] (非金屬元素) carbon (c)
  • : 酸構詞成分。
  • : 名詞1. (食鹽; 鹽類) salt 2. (姓氏) a surname
  • 碳酸鹽 : carbonas; carbonate
  • 碳酸 : carbonic acid碳酸氣 carbonic acid gas; 碳酸泉 [水文] carbonate spring; 碳酸泉水 apollinaris
  1. They do not have an illuvial horizon enriched with either silicate clay or with an amorphous mixture of aluminum and organic carbon

    沒有富含硅粘土或鋁有機晶質混合物的淀積層。
  2. Since 1980s, non - seismic geophysical instrumentation has achieved great progress in its acquisition accuracy, gathering styles and diversification of parameters, which provides new approaches for petroleum exploration in the newly developed area of western china and southern marine carbonate area, and also makes higher demands on data processing and inter pretation

    摘要20世紀80年代以來,地震地球物理勘探儀器有了長足的進步,採集精度的提高,採集手段與參數的多樣化,為我國西部新區和南方海相巖地區的油氣勘探提供了新的方法和途徑,同時對數據處理與解釋也提出了更高的要求。
  3. Could there exist another possibility for the south boundary of the system as follow : the rainfall infiltrates in the outcrop carbonate - mountain area of western, and moves towards south and deeper along carbonate rocks, then moves upper through the overlain tertiary system ( n ) with a thickness of 400m ( instead of running off to the springs and yellow river through a long approach of least hydraulic gradient ), and then mainly transforms into the horizontal drainage in the loess layer of quaternary, finally drains in lu - botan depres sion

    並且提出,關于對系統南界的認識,是否存在另一可能:即在西部巖裸露區大氣降水入滲后,沿巖向南向深部運動,然後,並在極小的水力坡度驅動下長距離地向東部黃河、泉群徑流排泄,而是通過上覆厚度約400m的第三系向上運動,繼而主要在第四系黃土層中轉為向南水平排泄到鹵泊灘。
  4. As a hard - core part of epikarst ecosystem, soil makes a hinge action in the karst process. it forms a leach layer between rainfalls and carbonate and gives a great much time and space in the karst process. soil co2, a very pivotal factor in the karst dynamic factors, makes an action of driving forces in karst dynamic system

    土壤作為表層帶巖溶生態系統的核心部分,在巖溶過程中起著樞紐作用,它的存在使得大氣降水與巖之間形成一個「過濾層」 ,賦予巖溶作用更廣闊的時間和空間,其中土壤co _ 2是個常關鍵的因子,它是巖溶作用的重要物質來源,在巖溶動力系統中起著驅動力作用。
  5. Divisional method and characteristic analysis of impermeable barrier layers in carbonate rock formation

    巖儲層中滲透性隔層的識別及分類評價
  6. The wumishan formation in yanling oilfield is a carbonate reservoir with percolation flow through dual media, and the reservoir heterogeneity is serious

    雁翎油田霧迷山組油藏為雙重滲流介質的巖油藏,裂縫、溶洞發育,儲層均質性嚴重。
  7. Apart from geochemists from western countries, which paid a particular attention on amorphous iron - manganese oxides extracted by enzyme or 0. 1 ~ 0. 25m nh2oh ? hc1, our results show that the extraction of metals adsorbed by clay and bound to the carbonate in soil is most useful to identify the concealed mineralizations in the semiarid and loess covered terrains, northern china

    但與國外重點關注晶質鐵錳氧化物如酶、羥氨提取結果不同,在我國北方半乾旱黃土覆蓋景觀區,粘土吸附和結合態金屬元素的提取為最有效的提取步驟。而游離態、有機結合態的提取效果則受景觀控制變化較大。
  8. Great burial - depth, low porosity, and strong heterogeneity are the basic characteristics of the ordovician carbonate reservoir in lunnan area of tarim basin

    超埋深、低基質孔和極強的均質性是塔里木盆地輪南奧陶系巖儲層的基本特點。
  9. For concrete structure in the practical engineering, the non - mechanics damages, such as alkali - aggregate reaction, sulfate attack, carbonization, steel rust, freeze and thaw, and so on, are unavoidable due to the exist of erosive media. the deterioration form of mono or multi - factor influences on the concrete property of construction and durability greatly, and shortens the service life of the concrete to a large extent. permeability of concrete is the most important factor for these non - mechanics damages, so the permeability test of concrete is the normal and required item to study the durability of concrete

    實際工程中的混凝土結構,因侵蝕性介質的存在而使力學破壞行為無處不在,這些力學破壞行為包括堿集料反應、硫侵蝕、化、鋼筋銹蝕、凍融等,單一的破壞形式或多形式的復合破壞作用對混凝土結構性能及耐久性能均有著較為嚴重的影響,在很大程度上縮短了建築物的服役年限,而這些力學破壞在很大程度上取決于其滲透性,所以測試混凝土滲透性能是研究判斷混凝土耐久性的常規必測項目。
  10. Must be softened and treated to make sure that is free from suspended solids and non - carbonate hardness, has a low carbonate hardness, is practically free from oil and dissolved oxygen and has a low dissolved silica content

    必須經過軟化和處理保證沒有懸浮固體和非碳酸鹽的硬度,有低硬度
  11. In view of the main feature of strong anisotropism of reservoir stratum of the paleozoic era carbonate rock in the middle part of ortos basin gas field, mainly by means of random analog formation, this paper makes a quantitative tranformation on the geological study on the area and the descriptive results of the gas pool, and finishes the whole geological model of underground carbonate rock in ortos basin, including the structure model / phy - sical model and fluid distribution model

    摘要針對鄂爾多斯盆地中部氣田下古巖儲層均質性強的主要矛盾,以隨機模擬建摸為主要方法,對該區地質研究和氣藏描述成果進行定量化轉變,形成了包括構造模型、物性模型和流體分佈模型的鄂爾多斯盆地下古巖整體地質模型。
  12. The most protruding question of carbonate reservoir are extremely strong unhomogeneity and dual porosity model characteristics

    巖油藏最突出的問題是極強的均質性和雙孔隙網路特徵。
  13. The waveform analytical method can he used to develop the geologic model for the carbonate reservoir in tahe field with heterogeneity and anisotropic property in its pore configuration, to research the omnidirectional feature and synthetic mechanism of seismic waveform, to gain the relations between carbonate reservoir characteristic by means of drilling and logging data, and finally to make a prediction of the growing degree of the reservoir

    摘要以塔河油田巖儲集層的孔隙空間結構所特有的均質性和各向異性為出發點建立地質模型,研究波形的全方位特徵及合成機理,依據鉆井、測井等資料,建立巖儲集層特徵與地震響應之間的對應關系,從而根據地震波的波形對儲集層的發育程度作出預測。
  14. Especially in carbonate formation, owing to its intricate interstice, the size, shape of cave, and the character of filling, it is almost impossible to get a all - around cognition. under the circumstance, comprehensively prediction by multi - subject method is the way to predict caves in carbonate formation

    尤其對巖儲層來說,由於孔隙空間常復雜,縫洞的大小、形狀、類型、充填物性質變化很大,用一種方法想全面了解巖的儲層發育情況幾乎是不可能的。
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