所计算的孔隙度与岩心分析孔隙度比较，雷莫方程的计算结果是令人满意的。

By comparison with the porosities from core analysis, the processed results with Raymer equation are satisfactory.

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岩石孔径越小，岩石孔隙内部磁场梯度越强，核磁共振测井计算的孔隙度明显偏低；

The more smaller pore size, the more stronger internal Magnetic field gradient. The nmr porosity is significantly lower.

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还利用建立的束缚水与孔隙度、渗透率之间的关系模型对束缚水饱和度进行了定量计算。

The saturation of the bound water was quantitatively concluded with the relational mode of the bound water's content, porosity and permeability.

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