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地下水资源、顾名思义是指地下有多少水。过去在各部门自编的水文地质勘察规范中都把地下水资源叫做储量。地下水在天然和开采状态下都是运动的,故对于地下水的储量问题、从概念到计算都比静止的固体和流体矿产为复杂。旧规范都是根据苏联通用的分类分法,把地下水储量分为静储量(年最低水位以下的地下水体积)、动储量(含水层中通过某一断面的流量)、调节储量(年最高、最低水位间的水体积)和开采储量(经济、合理、水量水质有保证的开采量)四类。这种分类法自五十年代初期引进以来,经过我国多年的生产实践的
Groundwater resources, as the name suggests, refers to how much water there is in the ground. Groundwater resources were formerly called reserves in the self-compiled hydrogeological survey regulations of various departments. Groundwater is both sporty in both natural and mining conditions, and is therefore more complex than a stationary solid and fluid mineral, from concept to calculation, for groundwater reserves. The old norms are based on the general classification of the Soviet Union, the groundwater reserves are divided into static reserves (below the lowest water level in the groundwater volume), dynamic reserves (aquifers through a section of the flow), regulating reserves (the highest year, the lowest Water volume between the water level) and mining reserves (economic, reasonable, water quality guaranteed extraction) four categories. Since the introduction of this taxonomy in the early 1950s, after many years of production practice in our country,