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1 水文物探回顾用于固体矿产物探方法始于19世纪末至20世纪初。20世纪40年代,前苏联等国开始用电阻率法找水,50年代发现含水体的弱激发极化效应,美国、前苏联等国作了一些理论研究和野外试验,但实际应用发展缓慢。我国的物探工作始于20世纪30年代,至40年代末仅有丁毅、顾功叙、王子昌等少数科学家,做了较小规模的试验性研究工作。50年代以后,我国的物探工作得到了迅猛发展,水文物探亦同时起步。60年代末进行了激发极化法找水野外试验研究,
A survey of hydrological relics Geophysical prospecting methods for solid minerals began in the late 19th century to early 20th century. In the 1940s, the former Soviet Union and other countries began to find water using the resistivity method. In the 1950s, the weak-excitation polarization effect of aquifer was discovered. Some theoretical and field experiments were conducted in the United States and the former Soviet Union, but the practical application has been slow. Geophysical work in our country began in the 1930s. Only a few scientists, such as Ding Yi, Gu Gongxu and Wang Zichang, made a small-scale experimental research work by the late 1940s. Since the 1950s, the geophysical work in our country has witnessed rapid development, and hydrological geophysical exploration has started at the same time. In the late 1960s, field experiments were conducted to find out the water by using the induced polarization method.