First proposed in the late 1800s, the theory relies on a property of water not commonly associated with fluids: its tensile strength.
该理论于19世纪末首次提出，其依据是水的抗拉强度，而水的这种特性通常与流体无关。
The influence of viscosity change on fluid percolation and development response is revealed through core flow test with fluids of different viscosity.
通过不同粘度流体的岩心流动模拟实验，揭示粘度变化对流体渗流及开发效果的影响。
The influence of viscosity change on fluid percolation and development response is revealed through core flow test with fluids of different viscosity.
通过不同粘度流体的岩心流动模拟实验，揭示粘度变化对流体渗流及开发效果的影响。
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