一、问题的提出在石油、采矿、环境、能源和岩溶水文地质研究中,经常遇到基岩断裂带、岩体接触带控制的廊道式含水带和含水层非均质性相差十分明显(如降落漏斗长、短轴之比为5～20倍或更大)的脉状体地区内冷水或热水水量如何评价的问题。由于用径向流公式常不适应,与实际情况差距较远,所以实践中评价脉状或似脉状含水系统的水量觉得十分棘手。如何解决这 First, the issue raised In the oil, mining, environment, energy and karst hydrogeology research, often encountered bedrock fracture zone, rock contact zone controlled corridor aquifer and aquifer heterogeneity is very different ( Such as long-term and long-term funnel, short axis ratio of 5 to 20 times or more) of the venous region of the cold water or hot water how to evaluate the issue. Due to the radial flow formula is often not suited, far from the actual situation, so in practice to evaluate veins or vein-like aquatic system of water is very tricky. How to solve this