摘要
本文通过金岭铁矿地层渗透性与埋深关系的研究,提出了形成“双层水位”的力学条件——交点Da的成因,对解释“双层水位”理论具有重要意义。
This paper first studies the relation between the permeability and the strata depth. It presents the mechanical conditions to form the “double layer water level”——genesis of the intersecting point Da. This is of significant importance to the theory explaining the 'double layer water level'.
出处
《勘察科学技术》
1991年第5期39-41,共3页
Site Investigation Science and Technology
