Sources of fine sediment stored in agricultural lowland streams, Midwest, USA

被引:32
作者
Lamba, Jasmeet [1 ,2 ]
Thompson, A. M. [1 ]
Karthikeyan, K. G. [1 ]
Fitzpatrick, Faith A. [3 ]
机构
[1] Univ Wisconsin, Dept Biol Syst Engn, Madison, WI 53706 USA
[2] USDA ARS, Pasture Syst & Watershed Management Res Unit, University Pk, PA 16802 USA
[3] US Geol Survey, Middleton, WI 53562 USA
关键词
Sediment sources; Stream bed sediment; Sediment tracers; Land use; Stream bank erosion; Sediment fingerprinting; EFFECTS ASSESSMENT PROJECT; SUSPENDED-SEDIMENT; RIVER-BASINS; CATCHMENT; UK; PHOSPHORUS; MANAGEMENT; VALLEY; ALLUVIATION; WATERSHEDS;
D O I
10.1016/j.geomorph.2015.02.001
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Agricultural activities can accelerate the offsite transport of productive soil from fields leading to stream water quality degradation. Identification of the nature and relative contribution of different sources to fine-grained sediment (e.g., silts, clays) in streams is important to effectively focus agricultural best management practices in watersheds. Sediment fingerprinting techniques through the use of geochemical tracers are commonly used to differentiate relative contribution from various sources. Research was conducted in lowland streams in the Pleasant Valley watershed in South Central Wisconsin (USA) to identify provenance of fine-grained sediment deposits and evaluate the impact of land use on relative contributions from the following potential sources: cropland, pasture, woodland, and eroding stream banks. Results show that both agriculture (croplands and pastures) and eroding stream banks are primary sources to fine sediment deposits on the stream bed with contributions ranging from 19 to 100% and 0 to 81%, respectively. The increase in area under agricultural land use within a subwatershed results in greater contribution from agriculture (R-2 = 0.846, p = 0.0034). Relative contributions from eroding stream banks increased with increasing area under grasslands and woodlands within a subwatershed (R-2 = 0.814, p = 0.0055). Subwatersheds with greater mass of fine sediment deposited on the stream bed per unit area should be prioritized for best management practices. The conservation practices should be targeted to stream banks or croplands depending on the dominant source of fine sediment within a subwatershed. Site specific changes in relative contributions from different sources to fine-grained sediment in this watershed highlights the complexities involved in sediment transport dynamics. The nested sampling sites helped determine that sediment dynamics at the subwatershed scale need to be considered for application of targeted conservation techniques. (C) 2015 Elsevier B.V. All rights reserved.
引用
收藏
页码:44 / 53
页数:10
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