最后探讨了非均匀性的度量方法。
Finally, the measurement method of nonuniformity is discussed.
试验结果满足实时性和非均匀性的要求，对环境的适应性较强。
The test result shows that the method can meet the real-time and nonuniform requirements and has a good adaptability to environment.
我们利用这些高精度的走时数据研究了地幔体波的走时残差的范围及地幔非均匀性的强度。
These mantle body wave data are used to investigate the range of variations in the travel time residuals which indicate the degree of mantle heterogeneity.
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