The second kind of model is complete coupling one and this model includes the coupling temperature field equation, fluid coupling seepage model equation, rock coupling deformation equation.
第二类模型为完全耦合模型，包括耦合温度场方程、流体耦合渗流方程和岩石耦合变形方程。
This means that the material balances around the stages are actually differential equations and each equation includes holdup as a variable.
这就意味着，在某一个阶段的前后物料平衡函数实际上是一个微分方程，而每一个方程都以一个停滞为变量。
This means that the material balances around the stages are actually differential equations and each equation includes holdup as a variable.
这就意味着，在某一个阶段的前后物料平衡函数实际上是一个微分方程，而每一个方程都以一个停滞为变量。
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