利用平衡深度法研究了鄂尔多斯盆地中生代地层的流体剩余压力分布特征。
The distribution of fluid residual pressure of Mesozoic strata in Ordos basin is studied based on the equilibrium depth method.
周期性脉冲式注水可以在地层中造成不稳定压力状态,在薄含水层中造成剩余压力。
Cyclic pulse injection may cause the transient pressure regime in the reservoir and remaining pressure in a thin aquifer.
对于装有剩余压力阀门的气瓶,如果瓶内剩余压力是正压,把它抽真空到150 mbar以下就可以了;
For cylinders equipped with residual (positive) pressure valves, one evacuation under vacuum at 150 millibar is sufficient if the pressure is positive.
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