育良的英文

• ikuyoshi

• "育"英文翻译    give birth to
• "良"英文翻译    good people
• "李育良" 英文翻译 :    li yuliang
• "发育良好" 英文翻译 :    well developed; well nourished
• "发育良好的" 英文翻译 :    growthy; well-developed
• "选育良种" 英文翻译 :    breeding improved varieties; breeding improved variety; breeding variety
• "后肢发育良好" 英文翻译 :    let down well in the ham
• "选育良种小麦" 英文翻译 :    wheat variety development by selection
• "发育良好的节理" 英文翻译 :    well-developed joint
• "发育良好的劈理" 英文翻译 :    well-developed cleavage
• "发育良好的剖面" 英文翻译 :    well-developed profile
• "培育良好的环境" 英文翻译 :    foster a healthy environment
• "生长发育良好的" 英文翻译 :    thrifty
• "育良精机制作所" 英文翻译 :    ikure works co., ltd
• "猪后肢发育良好" 英文翻译 :    let down well in the ham
• "发育良好和营养良好的" 英文翻译 :    well developed
• "培育良好的网络环境" 英文翻译 :    to foster a good cyber environment
• "发育良好与营养良好的白种男人" 英文翻译 :    well-nourished white male well-developed
• "发育良好与营养良好的黑种男人" 英文翻译 :    well-nourished black male well-developed
• "育利" 英文翻译 :    ikutoshi
• "育林保水" 英文翻译 :    conserve water through afforestation
• "育里" 英文翻译 :    ikusato
• "育林基金" 英文翻译 :    woods-raising fund
• "育黎" 英文翻译 :    yuli
• "育林基金审计" 英文翻译 :    audit of woods-raising fund
• "育郎" 英文翻译 :    ikuo; ikuro

• Drbainstilling goodness developing virtue schools
  法界佛教总会育良小学培德中学
• Jiang ding - ding , li kai - duan and zhao yu - liang
  蒋定定李开端赵育良
• Peter wu is the volunteer teacher of the sunday buddhist class at gold sage monastery
  吴泊道，目前任教于金圣寺周日育良佛学班。
• Ding d . j . , cao z . l . et al . ( 1992 ) . " investigation on high - ductility rc shear walls . " studi e ricerche , 13 , politechnico di milano , italia
  谢育良,曹征良( 1990 ) . "钢筋混凝土简支梁考虑主压应力破坏的抗剪强度计算. "南京建筑工程学院学报,第14卷,第3期, 38 - 51页
• 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