一、前言 地下水的实际流动在平面上是不均匀的,它很容易集中在地下水易产生流动的部位,这一想法是符合实际的,而掌握被称为脉流或水囊等流动路线将成为解决现场各类问题的线索。作为获得地下水情报的手段,除有在地表通过地震法勘探或电测法勘探等调查地层结构或地下水蕴藏情况外,还有利用钻孔直接观测地下水流动方向或流速的方法。 地下水运动既是水体的运移,又是水体本身所具有的热运移。从这一点着手,通过观测浅层地温而获得地下水情报,这就是地温勘探法。以前此方法被用来寻找温泉泉 I. INTRODUCTION The actual flow of groundwater is uneven in the plane. It is easy to concentrate on the ground where the groundwater is likely to flow. This idea is realistic and the mastery of the flow path known as the pulse flow or the water sac will become Clues to solve all kinds of problems on site. As a means of obtaining groundwater information, there is a method of directly observing the groundwater flow direction or flow rate by drilling, in addition to surveying the stratum structure or groundwater reservoir by means of seismic surveys or electrical survey on the surface. Groundwater movement is not only the movement of water bodies, but also the water body itself has the heat transfer. From this point of view, groundwater information is obtained by observing the shallow ground temperature, which is the geothermal exploration method. This method was previously used to find hot springs