Sediment dynamics and implications for management: State of the science from long‐term research in the Chesapeake Bay watershed, USA

分水岭 沉积物 水文学(农业) 溪流 环境科学 河口 腐蚀 沉积预算 泥沙输移 切萨皮克湾 土地利用 水资源管理 地质学 生态学 海洋学 地貌学 生物 机器学习 计算机科学 计算机网络 岩土工程
作者
Gregory B. Noe,Matthew J. Cashman,Katie Skalak,Allen C. Gellis,Kristina G. Hopkins,Douglas Moyer,James S. Webber,A. Benthem,Kelly O. Maloney,John W. Brakebill,Andrew J. Sekellick,Mike Langland,Qian Zhang,Gary W. Shenk,Jeni Keisman,Cliff R. Hupp
出处
期刊:Wiley Interdisciplinary Reviews: Water [Wiley]
卷期号:7 (4) 被引量:93
标识
DOI:10.1002/wat2.1454
摘要

Abstract This review aims to synthesize the current knowledge of sediment dynamics using insights from long‐term research conducted in the watershed draining to the Chesapeake Bay, the largest estuary in the U.S., to inform management actions to restore the estuary and its watershed. The sediment dynamics of the Chesapeake are typical of many impaired watersheds and estuaries around the world, and this synthesis is intended to be relevant and transferable to other sediment‐impaired systems. The watershed's sediment sources, transport, delivery, and impacts are discussed with implications for effectively implementing best management practices (BMPs) to mitigate sediment issues. This synthesis revealed three key issues to consider when planning actions to reduce sediment loading: Scale, time, and land use. Geology and historical land use generated a template that current land use and climate, in addition to management, are acting upon to control sediment delivery. Important sediment sources in the Chesapeake include the Piedmont physiographic region, urban, and agricultural land use, and streambank erosion of headwater streams, whereas floodplain trapping is important along larger streams and rivers. Implementation of BMPs is widespread and is predicted to lead to decreased sediment loading; however, reworking of legacy sediment stored in stream valleys, with potentially long residence times in storage, can delay and complicate detection of the effects of BMPs on sediment loads. In conclusion, the improved understanding of sediment sources, storage areas, and transport lag times reviewed here can help target choices of BMP types and locations to better manage sediment problems—for both local streams and receiving waters. This article is categorized under: Science of Water > Water Quality Water and Life > Stresses and Pressures on Ecosystems Water and Life > Conservation, Management, and Awareness
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