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随着科学技术的不断发展,地球科学已经从单一的学科转向不同学科相互交融渗透的综合化、整体化的学科。同时,地球科学还与水文科学、工程科学等其他学科不断交叉,衍生出新的地球探测方法。其中,地球物理水文物探方法就是一种最为著名和常用的方法。本文就将简述地球物理水文物探方法在测定地下水流速、流向中的具体应用。
With the continuous development of science and technology, earth science has shifted from a single discipline to a comprehensive and integrated discipline in which different disciplines blend with each other. At the same time, Earth Science has also continuously crossed with other disciplines such as Hydrology and Engineering Science, which have led to new Earth exploration methods. Among them, the geophysical hydrological exploration method is one of the most famous and commonly used method. This article will briefly describe the application of geophysical hydrological geophysical prospecting methods in the determination of groundwater velocity and direction.