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用井下电缆测井仪采集核磁共振数据方法的出现引起实验室核磁共振测量方法的出现、实验室核磁共振装置最重要的特征是：把井下仪器测量的数据重现出来，提供一个将实验室直接测量的特性与井下仪器的响应进行联系的机会。实验对岩心和流体样品也是无损的，这一点允许核磁共振测量方法与任何一种用来获得岩石物理参数的传统方法相结合，如毛细管束缚水、渗透率和孔隙度。根据采集的这些岩召物理数据，建立适当的模型；并可直接用来解释井下的测量数据。
The emergence of methods of nuclear magnetic resonance (NMR) measurements using downhole cable tools for acquiring NMR data has led to the emergence of laboratory-based direct-to-home nuclear magnetic resonance (NMR) devices that reproduce the measured data from the downhole instrumentation The characteristics of the measurement relate to the downhole tool’s response. Experiments are also non-destructive to core and fluid samples, allowing NMR spectroscopy to be combined with any of the traditional methods for obtaining petrophysical parameters such as capillary bound water, permeability and porosity. Based on these acquired physical data collected, the appropriate model is established and can be used directly to interpret the downhole measurement data.