Abstract
The contribution of surface water and groundwater were studied in a small stream in the central part of Sweden using electrical conductivity of water as a tracer. The portion of deep groundwater increases in the downstream direction from approx. 5 % to 20 %.
Subject
Water Science and Technology
Cited by
9 articles.
订阅此论文施引文献
订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献