Underground Sound: Application of Seismic Waves

Underground Sound: Application of Seismic Waves
复制标题

DOI:
10.1029/eo065i025p00403-01
复制
发表时间:
1984-06
期刊:
Eos, Transactions American Geophysical Union
影响因子:
--
通讯作者:
T. Morgan
T. Morgan
中科院分区:
其他
文献类型:
--
作者:
T. Morgan

文献摘要

被引文献

相似文献

J.E.正如引言中所述,白色关注的是自然和人工产生的地震波,它们穿过的岩石的性质,以及用于产生和检测它们的方法。他讨论了地球材料的模型,其中包括孔隙度,分层,旅行方向,损失机制和一些其他现象的影响。虽然重点肯定是钻孔方法,但也注意到地面问题,引用的许多数据实例都是地面记录。第一章简要介绍了傅里叶变换和卷积等数学工具。在大多数情况下,他声明的目的是避免使用向量运算符和张量符号,尽管缺乏这些方法可能会导致一些读者难以将特定关系与其他来源的一般陈述联系起来。他坚定不移地坚持这一目标,但书中仍然充满了令人印象深刻的数学。下面的第二章是对平面波和平面边界的一般讨论。这一部分涵盖了大多数读者都非常熟悉的基础知识。
J.E. White concerns himself, as stated in the Introduction, with naturally and artificially generated seismic waves, the properties of the rock they travel through, and the methods used to generate and detect them. He discusses these in terms of models of earth materials which can include the effects of porosity, layering, direction of travel, loss mechanisms, and a number of other phenomena. Although the emphasis is definitely on borehole methods, attention is given to surface problems, and many of the data examples cited are surface recordings. Some needed mathematical tools, such as Fourier transforms and convolution, are briefly introduced in chapter 1. For the most part, his stated aim is to avoid the use of vector operators and tensor notation, although the lack of these methods may cause some readers to have difficulty connecting specific relations with general presentations from other sources. He steadfastly sticks to this goal, but the book is still laden with imposing math. Following in chapter 2 is a general discussion of plane waves and plane boundaries. This section covers the groundwork with which most readers will be very familiar.