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讨论了上地幔各向异性介质中的潮汐运动方程，根据Deiewonski提供的地球模型参数，利用经典的Runge－Kutta数值积分方法，计算了固体潮勒夫数和负荷勒夫数．结果表明，考虑上地幔介质各向异性与否对固体潮勒夫数的影响较小（约为0．06％），而对负荷勒夫数的影响较大（2．5％），进一步说明了中低阶负荷勒大数对上地慢介质特性的敏感性．
The tidal equations of motion in the upper mantle anisotropic media are discussed. Based on the model parameters provided by Deiewonski, the classical Runge-Kutta numerical integration method is used to calculate the solid and dynamic Leuven numbers. The results show that considering the anisotropy of the medium in the upper mantle, the effect on solid Bollwoud's number is small (about 0.06%), while the effect on load Lough's number is greater (2.5%), which further explains Sensitivity of medium and low-order load Lehrs to slow medium characteristics.