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浅层土壤测温法是勘查地热资源的一种快速有效的方法,可用于普查和详查地热资源。地球内部热源的强度与分布,直接影响地表地温场的状态,因此,通过测量浅层土壤中的温度分布,与地质、物探方法配合解释,可以提供地热带的规模、热水通道位置等有重要价值的资料,并且有可能提供布置勘探钻孔的有利部位。由于测温是在浅层土壤中(1-2米)进
Shallow soil temperature measurement method is a rapid and effective method of geothermal exploration, which can be used for census and geothermal resources. The intensity and distribution of heat sources in the earth directly affect the state of surface geothermal field. Therefore, it is important to provide the scale of the tropics and the location of the hot water channel by measuring the temperature distribution in the shallow soil in cooperation with geological and geophysical methods Value information, and it is possible to provide advantageous locations for the placement of exploration bores. As the temperature is in the shallow soil (1-2 meters) into