Stream–Groundwater Interactions
Stream–Groundwater Interactions
复制标题
溪流-地下水相互作用
DOI：
10.1016/b978-0-444-53199-5.00115-9
复制
发表时间：
2011
影响因子：
2.8
通讯作者：
K. Bencala
中科院分区：
文献类型：
--
作者：
K. Bencala
溪流及其周围的集水区在一系列物理尺度上交换水和溶质。与河流的交换可能会延伸到河床的间隙区、潜流区、河岸区或集水区的地下水流系统。即使在较小的尺度上，交换显着影响溶质运移，养分循环和水生生态系统。近几十年来，河流-地下水相互作用的溶质运移方面得到了相当大的关注。河流-地下水的相互作用现在被认为是在河流恢复和鱼类生境等环境问题中需要考虑的实际问题。在本章中，重点是介绍（1）河流和地下水之间的水文相互作用的广度和（2）解释这些相互作用的重要性，以了解流化学和生态。
Streams and their surrounding catchments exchange water and solutes on a range of physical scales. Exchange with the stream may extend into the interstitial areas of the streambed, the hyporheic zone, the riparian area, or the catchment's groundwater flow system. Even at the smaller scales, the exchanges significantly influence solute transport, nutrient cycling, and the aquatic ecosystem. Over the recent decades, considerable attention has been given to the solute transport aspects of stream–groundwater interactions. Stream–groundwater interactions are now being recognized as practical matters to be considered in environmental issues, such as stream restoration and fish habitat. In this chapter, the emphasis is on introducing (1) the breadth of hydrologic interactions between streams and groundwater and (2) the importance of interpreting these interactions to understanding stream chemistry and ecology.
影响因子：
3.2
作者：
Hannah, David M.;Malcolm, Iain A.;Bradley, Chris
通讯作者：
Bradley, Chris