介绍了以“压力—流量平衡法”为基础的模型求解方法和步骤。
The method and procedure of the model resolution is introduced based on " pressure-flow balance".
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.
按照等速采样的瞬时压力零点平衡法，结合现场应用实践，检验了采样装置的密封和传动机构性能。
The sealing and drive mechanism performance of the sampling device are examined in accordance with the transient pressure zero balance method and in combination with the field practice.
应用推荐