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黄强. 张应力放大系数矩阵—岩体无张力分析的捷径[J]. 岩土工程学报, 1986, 8(4): 19-24.
引用本文: 黄强. 张应力放大系数矩阵—岩体无张力分析的捷径[J]. 岩土工程学报, 1986, 8(4): 19-24.
Huang Qiang. A Coefficient Matrix of Amplifying Tensile Stresses ——A Shortcut for "No Tension" Analysis of Rock[J]. Chinese Journal of Geotechnical Engineering, 1986, 8(4): 19-24.
Citation: Huang Qiang. A Coefficient Matrix of Amplifying Tensile Stresses ——A Shortcut for "No Tension" Analysis of Rock[J]. Chinese Journal of Geotechnical Engineering, 1986, 8(4): 19-24.

张应力放大系数矩阵—岩体无张力分析的捷径

A Coefficient Matrix of Amplifying Tensile Stresses ——A Shortcut for "No Tension" Analysis of Rock

  • 摘要: 为模拟岩石的无张力性质,晋基维茨(Zienkiewicz)曾建议并且采用“应力转移法”进行无张力分析。任何应被减少的张应力经过一个迭代过程之后就可被近似地消除。迭代所进行的次数必须持续到张应力全部被消除(近似的)为止。 本文给出了一个仅需一次迭代就可消除(精确地)张应力的矩阵。将应减少的张应力乘以该矩阵之后仅需进行一次迭代就可达到“应力转移”的目的,大大加快了系统的收敛速度,节省了应用“应力转移法”进行无张力分析所耗费的大量计算机时。

     

    Abstract: Zienkiewicz et al., proposed and used the so-called stress trasfer (or relaxation) method to handle the no tension behavior of rock. Any tensile stresses to de induced are annihilated (approximately) by using an iterative procedure. The number of iteration increases till the zone is relieved (approxmately) of the tensile stresses.This paper gives a matrix, Dy means of which the exact solution of "no tension" analysis can be obtained. Multiplied by this matrix, the tensile stresses will be annihilated with only one iteration needed, It will save lots of computer hours in"no tension" analysis.

     

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