Fluid production from fractured rock masses readily induces fracture flow velocities of meters per second. Yet, most discrete fracture flow models treat flow as laminar creeping flow or account for inertia effects only by single-fracture constitutive relationships.

中文翻译：

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惯性力和离心力对天然裂缝网络中速率和流动模式的影响


裂隙岩体产生的流体很容易引起每秒数米的裂隙流速。然而，大多数离散裂缝流动模型将流动视为层流蠕变流动或仅通过单裂缝本构关系来解释惯性效应。