地震学报
地震學報
지진학보
ACTA SEISMOLOGICA SINICA
2009年
4期
377-384
,共8页
广义反射-透射系数%无量纲%频散%瑞利波
廣義反射-透射繫數%無量綱%頻散%瑞利波
엄의반사-투사계수%무량강%빈산%서리파
generalized reflection-transmission coefficient%dimensionless%dis-persion%Rayleigh wave
水平层状介质中瑞利波频散曲线的计算一直是受关注的问题.陈晓非提出的广义反射-透射系数方法虽然具备很好的精确性和稳定性,但是算法中起决定作用的矩阵E存在有量纲元素,并且不同元素之间的数量级差异很大.本文作者通过把广义反射-透射系数算法无量纲化,得到了简洁的瑞利波频散函数的公式体系.分别计算了改进后算法和原算法中矩阵E的最大模元素与最小模元素的比值ε,发现前者的矩阵E中最大模元素与最小模元素最多只相差1个数量级,而后者的矩阵E中最大模元素与最小模元素之间最大达11个数量级的差异,尽管后者可以通过选取变量的单位减小ε的值,但新算法精度更高,从而完善了利用广义反射-透射系数方法求解瑞利波频散曲线问题的理论和算法.
水平層狀介質中瑞利波頻散麯線的計算一直是受關註的問題.陳曉非提齣的廣義反射-透射繫數方法雖然具備很好的精確性和穩定性,但是算法中起決定作用的矩陣E存在有量綱元素,併且不同元素之間的數量級差異很大.本文作者通過把廣義反射-透射繫數算法無量綱化,得到瞭簡潔的瑞利波頻散函數的公式體繫.分彆計算瞭改進後算法和原算法中矩陣E的最大模元素與最小模元素的比值ε,髮現前者的矩陣E中最大模元素與最小模元素最多隻相差1箇數量級,而後者的矩陣E中最大模元素與最小模元素之間最大達11箇數量級的差異,儘管後者可以通過選取變量的單位減小ε的值,但新算法精度更高,從而完善瞭利用廣義反射-透射繫數方法求解瑞利波頻散麯線問題的理論和算法.
수평층상개질중서리파빈산곡선적계산일직시수관주적문제.진효비제출적엄의반사-투사계수방법수연구비흔호적정학성화은정성,단시산법중기결정작용적구진E존재유량강원소,병차불동원소지간적수량급차이흔대.본문작자통과파엄의반사-투사계수산법무량강화,득도료간길적서리파빈산함수적공식체계.분별계산료개진후산법화원산법중구진E적최대모원소여최소모원소적비치ε,발현전자적구진E중최대모원소여최소모원소최다지상차1개수량급,이후자적구진E중최대모원소여최소모원소지간최대체11개수량급적차이,진관후자가이통과선취변량적단위감소ε적치,단신산법정도경고,종이완선료이용엄의반사-투사계수방법구해서리파빈산곡선문제적이론화산법.
The calculation of dispersion curves of Rayleigh wave in horizontal multilayered medium has been a concerned subject. Chen's generalized reflec-tion-transmission coefficient method has good accuracy and stability, but in the calculation of matrix E, which plays a decisive role in the algorithm, has dimen-sional elements, and the different elements have an order of magnitude differ-ence. By making the generalized reflection-transmission coefficient calculation dimensionless, we obtained a more concise formula system for computing the dispersion function of Rayleigh wave. We calculated the ratio ε of the largest el-ement over the smallest in the matrix E using the improved and the original al-gorithm, respectively. We found that in the improved algorithm the elements of matrix E have at most one order of magnitude difference, while in the original algorithm the difference reaches to eleven orders. This indicates that the im-proved approach has higher accuracy. It is expected that the improved general-ized reflection-transmission coefficient method is more applicable to the compu-tation of Rayleigh wave dispersion.