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纸质出版日期:2009,
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李爱华,刘沛清,许唯临.复杂裂隙网络内冲击射流脉动压力传播过程数值研究[J].工程科学与技术,2009,41(5):36-41.
Numerical Study of Fluctuating Pressure Propagation Within Complicated Fracture Network Due to Impinging Jet[J]. Advanced Engineering Sciences, 2009,41(5):36-41.
中文摘要: 引入高坝下游基岩复杂裂隙网络结构,对裂隙网络内冲击射流脉动压力的传播过程和机理展开数值研究。应用蒙特卡洛方法,建立河床岩体仿真裂隙网络内脉动压力的瞬变流传播模型。数值模拟得出各裂隙线元内的瞬时脉动压力时间过程,以及脉动压力强度的空间分布云图。结论认为:点脉动压力的瞬时分布是各裂隙线元内的压力波传播、反射并叠加的结果,具有显著地各向异性特性。脉动强度基本服从正态分布。频谱分析得出点脉动压力不仅和岩体控制体外部施加的干扰脉动有关,而且和与此点相衔接的线元、以及通过其他线元与此点相贯通的线元的几何、物理特性有关。
Abstract:The complicated fracture structure of bed rock was introduced to study the process and mechanism of propagation of fluctuating pressure due to jet impingement downstream of high dams. Applying the Monte Carlo method
the transient model of fluctuating pressure propagation within an imitated rock fracture network was established. The transient time process of pressure fluctuation within each fissure and the special distribution of the intensity of pressure fluctuation were obtained by numerical simulation. It was concluded that the transient distribution of the fluctuating pressure of any node
with typically anisotropy
was the result of the propagating
reflecting and interating of pressure waves within fissure cells. The fluctuating intensity obeyed on the normal distribution. Through the spectrum analyzing
it was verified that the fluctuating pressure of any node not only lied on the pressure forced outside to the control volume
but also were determined by the geometric and physical characters of the fissure cells which are joined with the node or reached it through other cells.
脉动压力蒙塔卡洛方法裂隙网络瞬变流模型
fluctuating pressureMonte Carlo methodfracture networkmodel of transient flow
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