脱水作用的英文

• anhydration
• deaquation
• dehydrating
• dehydration
• dehydrolysis
• dewatering
• water deprivation

• "脱水"英文翻译    deprivation of body fluids; ...
• "作用"英文翻译    act on; affect
• "电脱水作用" 英文翻译 :    electric dehydration
• "催化脱水作用" 英文翻译 :    catakytic dehydration; catalytic dehydration
• "前进脱水作用" 英文翻译 :    progressive dehydration
• "芳化成环脱水作用" 英文翻译 :    aromatic cyclodehydration
• "水作用" 英文翻译 :    gleization
• "冰水作用" 英文翻译 :    glaciofluvial activity
• "冰水作用的" 英文翻译 :    fluvioglacial; glacioaqueous; glaciofluvial
• "充水作用" 英文翻译 :    recharge
• "抽水作用" 英文翻译 :    pumping action
• "动水作用力" 英文翻译 :    dynamic water pressure
• "河水作用" 英文翻译 :    fluviation
• "回水作用" 英文翻译 :    backwater effect
• "减水作用" 英文翻译 :    slush
• "泌水作用" 英文翻译 :    exudation
• "潜水作用" 英文翻译 :    gleization
• "浅水作用" 英文翻译 :    shoaling
• "亲水作用" 英文翻译 :    hydrophilic interaction
• "去水作用" 英文翻译 :    dehydration
• "渗水作用" 英文翻译 :    influent action
• "疏水作用" 英文翻译 :    hydrophobic effect; hydrophobic interaction; lyophobic interaction
• "吐水作用" 英文翻译 :    guttation
• "吸水作用" 英文翻译 :    water sorption
• "滞水作用" 英文翻译 :    meromixis

• Test method for dehydration of oil - type preservatives
  油质防腐剂脱水作用测试方法
• Under freezing conditions , n . commune suffered cellular dehydration due to ice formation outside the cell
  此外，通过核磁共振技术发现在冻结条件下，细胞外结冰导致了细胞内脱水，但脱水作用并不彻底。
• Abstract : yanchang series is a typical low permeability reservoir , and its favourable sandstone reservoir is delta facies . heavy compaction , cementation and heterogeneity exist in it . according to the analysis of the main control factors of forming the secondary pore , it is held that the secondary pore in longdong area is controlled by both favorable facies belt and abnormal formation pressure . it is also held that the formation of the abnormal formation pressure is due to the dewatering of the clay mineral during diagenesis because the dewatering time is identical with the decarboxylation time of organism . organic acid and co2 are driven to adjacent favorable reservoirs under the abnormal formation pressure , and a lot of secondary pore is produced in the runners . from the present exploration result , it is useful to predicting the development of secondary pore to study the distribution of abnormal formation pressure
  文摘:陕甘宁盆地三叠系延长统是国内外典型的低渗特低渗油田，储集层主要为三角洲砂体，压实作用和胶结作用强烈，储层非均质性非常严重，因此预测次生孔隙发育带是寻找油气聚集带的关键.通过对陕甘宁盆地陇东地区延长统次生孔隙形成的主控因素分析，认为陕甘宁盆地延长统次生孔隙的形成除了受沉积有利相带控制外，还与地层异常压力的作用密切相关.研究认为陇东地区异常压力的形成机理主要由于成岩过程中粘土矿物脱水作用.粘土矿物大量脱水时间正好与有机质脱羧期相一致，从而在异常压力作用下将生油岩中的大量有机酸及co2带到与之相邻的储集层中，并沿着有利储集相带运移，在酸性水经过的地方形成大量的次生孔隙，为后期油气运聚提供有利通道及宿住空间，从现今的勘探结果来看，通过研究地层异常压力纵横向分布特征，并结合有利相带研究预测次生孔隙育良带是行之有效的方法
• Yanchang series is a typical low permeability reservoir , and its favourable sandstone reservoir is delta facies . heavy compaction , cementation and heterogeneity exist in it . according to the analysis of the main control factors of forming the secondary pore , it is held that the secondary pore in longdong area is controlled by both favorable facies belt and abnormal formation pressure . it is also held that the formation of the abnormal formation pressure is due to the dewatering of the clay mineral during diagenesis because the dewatering time is identical with the decarboxylation time of organism . organic acid and co2 are driven to adjacent favorable reservoirs under the abnormal formation pressure , and a lot of secondary pore is produced in the runners . from the present exploration result , it is useful to predicting the development of secondary pore to study the distribution of abnormal formation pressure
  陕甘宁盆地三叠系延长统是国内外典型的低渗特低渗油田，储集层主要为三角洲砂体，压实作用和胶结作用强烈，储层非均质性非常严重，因此预测次生孔隙发育带是寻找油气聚集带的关键.通过对陕甘宁盆地陇东地区延长统次生孔隙形成的主控因素分析，认为陕甘宁盆地延长统次生孔隙的形成除了受沉积有利相带控制外，还与地层异常压力的作用密切相关.研究认为陇东地区异常压力的形成机理主要由于成岩过程中粘土矿物脱水作用.粘土矿物大量脱水时间正好与有机质脱羧期相一致，从而在异常压力作用下将生油岩中的大量有机酸及co2带到与之相邻的储集层中，并沿着有利储集相带运移，在酸性水经过的地方形成大量的次生孔隙，为后期油气运聚提供有利通道及宿住空间，从现今的勘探结果来看，通过研究地层异常压力纵横向分布特征，并结合有利相带研究预测次生孔隙育良带是行之有效的方法