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裘布依稳定流理论在水文地质上仍广泛使用,故探讨裘式与客观水文地质条件间的相互关系具有明显的实用意义。钻孔的单位涌水量q与含水层的导水系数T,二者在理论上虽然是两个不同的概念,但实践中的大量资料证明它们有明显的相关性(线性相关)。本文通过东北、内蒙地区的193个单孔(完整井)抽水试验资料,探讨在裘布依稳定流条件下建立潜水含水层和承压含水层的导水系数T与钻孔单位涌水量q之间的相关关系。
Qiu Buyi steady flow theory is still widely used in hydrogeology, so to explore the relationship between the Qur’an and the objective hydrogeological conditions has obvious practical significance. There are two different concepts in theory, but a large amount of data in practice proves that they have obvious correlation (linear correlation). In this paper, 193 single well (intact) pumping test data from northeastern and Inner Mongolia were used to investigate the relationship between the water transfer coefficient T and the water inflow q of submerged aquifers and confined aquifers under the condition of Qiubu constant flow The relationship between.