Hydrologic connectivity as a framework for understanding biogeochemical flux through watersheds and along fluvial networks

被引:226
作者
Covino, Tim [1 ]
机构
[1] Colorado State Univ, Dept Ecosyst Sci & Sustainabil, Ft Collins, CO 80523 USA
关键词
Hydrologic connectivity; Nutrient transport; Hyporheic exchange; Stream-groundwater interactions; River-floodplain interactions; DISSOLVED ORGANIC-CARBON; HYPORHEIC ZONE; HEADWATER CATCHMENTS; PHOSPHORUS DYNAMICS; SUBSURFACE EXCHANGE; NUTRIENT LIMITATION; TRANSIENT STORAGE; RUNOFF GENERATION; RIVER CONTINUUM; MATTER DYNAMICS;
D O I
10.1016/j.geomorph.2016.09.030
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Hydrologic connections can link hillslopes to channel networks, streams to lakes, subsurface to surface, land to atmosphere, terrestrial to aquatic, and upstream to downstream. These connections can develop across vertical, lateral, and longitudinal dimensions and span spatial and temporal scales. Each of these dimensions and scales are interconnected, creating a mosaic of nested hydrologic connections and associated processes. In turn, these interacting and nested processes influence the transport, cycling, and transformation of organic material and inorganic nutrients through watersheds and along fluvial networks. Although hydrologic connections span dimensions and spatiotemporal scales, relationships between connectivity and carbon and nutrient dynamics are rarely evaluated within this framework The purpose of this paper is to provide a cross-disciplinary view of hydrologic connectivity highlighting the various forms of hydrologic connectivity that control fluxes of organic material and nutrients and to help stimulate integration across scales and dimensions, and collaboration among disciplines. (C) 2016 Elsevier B.V. All rights reserved.
引用
收藏
页码:133 / 144
页数:12
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