断裂(地质)
半径
缩放比例
机械
长度刻度
相似解
幂律
比例(比率)
流体压力
标度律
数学
材料科学
地质学
物理
几何学
岩土工程
计算机科学
计算机安全
统计
边界层
量子力学
作者
Andrew P. Bunger,Emmanuel Detournay
出处
期刊:Journal of Engineering Mechanics-asce
[American Society of Civil Engineers]
日期:2007-04-18
卷期号:133 (5): 534-540
被引量:72
标识
DOI:10.1061/(asce)0733-9399(2007)133:5(534)
摘要
The small-time asymptotic solution for a penny-shaped fluid-driven fracture is obtained semianalytically. Scaling considerations indicate that the portion of the fracture that is filled with fluid increases with time according to a power law. The problem is shown to be self-similar at the length scale of the small fluid-filled region and to depend on only the mean fluid pressure at the length scale of the fracture. This similarity solution is unusual as the two length scales of the problem—the radius of the fracture and the radius of the fluid front—evolve according to two different power laws of time.
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