1) hole gas(liquid) pressure
孔隙气(液)体压力
2) pore air pressure
孔隙气压力
1.
Based on the results of tests,the regulations of pore water pressure and pore air pressure as well as suction are described in tension staterespectively,furthermore,conclusions in this paper can be referenced for the research of tensile strength and ultimate strain.
本文用直接试验方法,对粘性土进行了非饱和三轴拉伸和单轴拉伸试验,根据试验资料就粘性土在受拉状态下孔隙水压力、孔隙气压力以及吸力的变化特性进行了阐述,以供对抗拉强度和极限应变的深入研究之用。
2.
The pore air pressure and pore water pressure can be calculated regarding the pore air pressure and pore water pressure as independent variables.
将孔隙气压力和孔隙水压力作为独立变量,推导了孔隙气压和孔隙水压计算表达式。
3) pore fluid pressure
孔隙流体压力
1.
In this paper the authors discuss the relationship between the pore fluid pressure and the fluid expulsion under the compaction, and suggests that the abnormal pore fluid pressure results from the increase of the capilary force due to the change of permeability and that a dynimic balance is maintained between them during the pregnancy of the fluid pressure.
本文讨论了在压实作用下孔隙流体压力的形成以及与流体排驱的关系,指出异常孔隙流体压力是因岩石渗透率变化引起毛细管力增加而产生的,且二者之间在流体压力孕育过程中一直维持一个动态平衡状态。
4) high pore fluid pressure
高孔隙流体压力
1.
It is a quite universal phenomenon that abnormal high pore fluid pressure (overpressure) occurs in oil gas-bearing basins, overpressure is one of the major earth kinetic reasons of the reservoir formation which is a kind of highly complicated self-organizing phenomenon.
含油气盆地中发现异常高孔隙流体压力(超压)是一个相当普遍的现象，它可能是油气藏形成即一种高度复杂的自组织现象的主要地球动力学原因之一。
5) pore liquid pressure
孔隙液压
1.
The pore liquid pressure supporting load is reduced and the load is moved to the solid structure.
定量给出了饱和岩石内孔隙液压的前期变化过程、岩石结构受力过程以及饱和体体积弹模的变化过程,并通过试验验证了这一现象的变化过程的合理性,展示了岩石由于结构浸水、胶质软化而在后期刚度下降。
6) pore gas pressure
孔隙气压
1.
Finite element analyses of influence of pore gas pressure on coupled thermo-fluid-mechanical processes in geological disposal of nuclear waste
孔隙气压对核废物地质处置热-流-固耦合影响的有限元分析
补充资料：气压梯度力
| 气压梯度力 pressure gradient force 在大气中由于气压在空间的分布不均匀，而作用于气块上的力。对单位质量的气块而言，气压梯度力的方向与等压面垂直，且从高气压指向低气压；它的大小与气压梯度的数值成正比，与空气密度成反比。水平方向上的气压梯度力在水平面上垂直于等压线，且由高气压指向低气压。在地面天气图上，经常存在一些高、低气压中心。通常在高气压区内，气块所受的水平气压梯度力垂直于等压线且由高气压中心指向外；而在低气压区内，气块所受的水平气压梯度力垂直于等压线且指向低气压中心。由于在大气中气压随高度的增加而减少，因此通常铅直方向上的气压梯度力与重力的方向相反。 |
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条