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在地下水资源计算和评价中,首先要划分含水岩组的富水性,确定水文地质参数。但所测泉流量并不完全是枯期流量,特别是在前人测流资料较多的地区,其测流时间又跨越了多个水文年。如何充分合理地利用这些测流资料,对含水岩组富水性的划分、地下水资源计算及评价都有重要意义。 对一个水文年不同季节偶测流量的处理,有关文献曾提出利用泉流量长期观测资料计算流量换算系数(本文称修
In the calculation and evaluation of groundwater resources, we must first divide the water-rich rock group aquifer, determine the hydrogeological parameters. However, the measured spring flow is not exactly the dry season flow, especially in the areas where the forerunner measured the flow data more, and the flow time spaned several hydrological years. How to make full and reasonable use of these hydrothermal data is of great importance to the division of water-rich reservoirs and the calculation and evaluation of groundwater resources. For a single year in different seasons measured hydrological flow measured, the literature has proposed the use of long-term spring flow data to calculate the flow rate conversion factor (referred to as repair