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media pore
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  “media pore”译为未确定词的双语例句
     In basic media, pore size gradually increases withpH value. At pH value of 12, the primary pore size concentrates on 2. 1 nm.
     在碱性介质中蒙脱土孔径逐渐增大,pH=12时主孔径集中在2.1nm处。
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  相似匹配句对
     Media
     媒体
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     Media
     媒介
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     Application on pore network model of porous media
     多孔介质孔隙网络模型的应用现状
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     THE EFFECT OF STRESS IN POROUS MEDIA ON PORE PRESSURE
     多孔介质应力对孔隙压力影响的研究
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     e. pore model.
     它最终表现为储层现今的孔隙几何学特征─—孔隙模型。
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  media pore
The results suggest that media pore size and porosity play a significant role in the performance of upflow APBRs.
      


The estimation of gas hydrate sediment velocity is an important component of the seismic methods and technical research on hydrate. There are three kinds of micromodel for hydrate in media pore: suspending, grain contact and cementation. With experimental models, several methods of velocity estimation are studied. The applicability and condition of application of those methods, especially the Time average Equation, Wood Equation, Lee Weight Equation and equivalent media are emphasized. The results...

The estimation of gas hydrate sediment velocity is an important component of the seismic methods and technical research on hydrate. There are three kinds of micromodel for hydrate in media pore: suspending, grain contact and cementation. With experimental models, several methods of velocity estimation are studied. The applicability and condition of application of those methods, especially the Time average Equation, Wood Equation, Lee Weight Equation and equivalent media are emphasized. The results demonstrate that there is a condition of application for every method, and the most applicable methods for suspending model, grain contact model and cementation model are Wood Equation, Lee Weight Equation and Time average Equation, respectively. Lee Weight Equation is more applicable by reasonably adjusting the weight factor.

天然气水合物沉积介质速度的估算是水合物人工地震探测理论方法和技术研究的组成部分。文中针对水合物在介质孔隙中悬浮、颗粒接触和胶结 3种微观模式 ,对前人估算其速度的多种方法进行了分析研究 ,结合试算模型 ,重点考查时间平均方程、伍德方程、李权重方程和等效介质等方法估算速度的适用性和使用条件。研究结果表明 ,每种方法都有其适用和不适用 (或不太适用 )的条件 ,水合物悬浮模式、颗粒接触模式和胶结模式 ,最为适宜使用的速度估算方法分别是伍德方程、权重方程和时间平均方程。权重方程在合理调整权重参数时有较宽的适用性。

The Sudeerte buried-hills are very important reservoirs in the Hailaer Basin.The best reservoirs are generally developed on top of the Triassic metamorphosed silici-clastic rocks called Budate Group and with a thickness from several tens to over 100 meters.The so-called bi-media pore spaces composed of pore and fractures are the prevailing reservoir types with mean porosity of 5.0% and permeability of 0.03×10-3μm2.Two genetic types of the buried-hills can be recognized,faulted block and weathered...

The Sudeerte buried-hills are very important reservoirs in the Hailaer Basin.The best reservoirs are generally developed on top of the Triassic metamorphosed silici-clastic rocks called Budate Group and with a thickness from several tens to over 100 meters.The so-called bi-media pore spaces composed of pore and fractures are the prevailing reservoir types with mean porosity of 5.0% and permeability of 0.03×10-3μm2.Two genetic types of the buried-hills can be recognized,faulted block and weathered peleo-uplift.With southwards subduction of the Mongolia-Okhotsk plate north of the studied area during Triassic to early Cretaceous,the Hailaer Basin suffered uplifting and weathering,secondary burying and block faulting,volcanism and fluid alteration,which constructed the buried-hill reservoirs there.

布达特群古潜山油气藏是海拉尔盆地苏德尔特地区的主要油气藏类型,发育于三叠系浅变质的砂、泥岩地层顶部,储层有效厚度由几十米到100余m。储集空间类型属于孔隙-裂缝双孔介质储层,平均孔隙度5.0%,平均渗透率0.03×10-3μm2。按成因本区古潜山可分为断块型和古隆起剥蚀型。印支期区域挤压隆升、印支期燕山早期长期暴露剥蚀、燕山期差异块断是本区古潜山形成的动因;风化作用、流体活动和构造破裂作用是储集空间形成的主控因素。

 
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