Simulating the spatio-temporal dynamics of soil erosion, deposition, and yield using a coupled sediment dynamics and 3D distributed hydrologic model

被引:28
作者
Zi, Tan [1 ]
Kumar, Mukesh [1 ,2 ]
Kiely, Gerard [3 ]
Lewis, Ciaran [3 ]
Albertson, John [1 ,4 ]
机构
[1] Duke Univ, Dept Civil & Environm Engn, Durham, NC 27706 USA
[2] Duke Univ, Nicholas Sch Environm, Durham, NC 27706 USA
[3] Univ Coll Cork, Ctr Hydrol Micrometeorol & Climate Change, Dept Civil & Environm Engn, Cork, Ireland
[4] Cornell Univ, Sch Civil & Environm Engn, Ithaca, NY 14853 USA
基金
美国国家科学基金会;
关键词
Distributed hydrologic model; Soil erosion; Sediment spatio-temporal dynamics; Coupled modeling; Sediment transport model; GEOtop model; OVERLAND-FLOW GENERATION; RUNOFF GENERATION; HYDRAULIC CONDUCTIVITY; PHOSPHORUS EXPORT; BLANKET PEATLAND; MOISTURE; SCALE; CATCHMENT; SURFACE; WATER;
D O I
10.1016/j.envsoft.2016.06.004
中图分类号
TP39 [计算机的应用];
学科分类号
081203 ; 0835 ;
摘要
Since soil erosion is driven by overland flow, it is fair to expect heterogeneity in erosion and deposition in both space and time. In this study, we develop and evaluate an open-source, spatially-explicit, sediment erosion, deposition and transport module for the distributed hydrological model, GEOtop. The model was applied in Dripsey catchment in Ireland, where it captured the total discharge volume and suspended sediment yield (SSY) with a relative bias of -1.2% and -22.4%, respectively. Simulation results suggest that daily SSY per unit rainfall amount was larger when the top soil was near saturation. Simulated erosion and deposition areas, which varied markedly between events, were also found to be directly influenced by spatial patterns of soil saturation. The distinct influence of soil saturation on erosion, deposition and SSY underscores the role of coupled surface-subsurface hydrologic interactions and a need to represent them in models for capturing fine resolution sediment dynamics. (C) 2016 Elsevier Ltd. All rights reserved.
引用
收藏
页码:310 / 325
页数:16
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