separating fluid 中文意思是什麼
separating fluid
解釋
分重液體- fluid : n 流體，液。 body fluid 體液。 cooling fluid 冷卻液。adj 1 流動的；流體的；液體的。2 容易[可]變動...
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According to separating touch of fluid potential field in f, y oil layer, eight oil or gas accumulation systems are divided in f, y oil layer, they are daqing - zhaoyuan oil or gas accumulation system, longhupao - taikang oil or gas accumulation system, heiyupao - yian oil or gas accumulation system, haerbin - shuangcheng oil or gas accumulation system, zhaodong - mingshui oil or gas accumulation system and hailun oil or gas accumulation system
根據扶、楊油層流體勢場分隔槽，將松遼盆地北部扶、楊油層劃分出八個含油氣系統，即即大慶?肇源含油氣系統、龍虎泡?太康含油氣系統、英臺?大安含油氣系統、朝陽溝?肇東含油氣系統、齊齊哈爾?依安含油氣系統、肇東?明水含油氣系統、哈爾濱?雙城含油氣系統、海倫含油氣系統。 -
3. algebraically explicit analytical solutions of two - buoyancy natural convection in porous media applying the approach of separating variables with addition, the thesis derives three sets of simple and clear algebraically explicit analytical equations describing the natural convection in porous media with both temperature and concentration gradients. besides the theoretical meaning, they are more valuable for be the benchmark solutions to check and improve the computational fluid dynamics and computational heat and mass transfer
三、多孔介質中溫度與濃度梯度耦合自然對流基本方程的代數顯式解析解本論文對王補宣院士等給出的反映多孔介質中溫度與濃度耦合自然對流的五元非線性聯立偏微分方程，利用加法分離變量法，導出了三套比較簡明的代數顯式解析解。 -
5, south region oil has the feature of " three high and one low ", the stratum water is type nahco3, and plane distribution is affected by gravity differentiation and faults, which caused each fluid block separating into individual
5 、南區原油具有「三高一低」的特徵，地層水為n司hco3型，平面分佈主要受重力分異作用以及斷層的影響，導致各斷塊流體自成體系。 -
The zijinshan fluid system and the gonglang fluid system were driven by the stress of extrusion nappe onto the basin and the thermal driving force of magmatism. when the fluids cycling in the basin encountered the boundary of reduction - oxidation or underwent fluid mixing, phase separating and fluid boiling caused by fault - induced pressure reducing, the physical chemistry condition abruptly changed and mineralization then took place
在盆地兩側擠壓推覆構造應力及巖漿作用熱力驅動下，紫金山背斜和公郎弧兩大流體系統的流體在盆地中運動，當遇到氧化還原界面或遭受流體混合、相分離及斷裂導致的減壓沸騰時，因物理化學條件發生重大變化而導致成礦作用的發生。
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