气候变化领域集成服务门户(CCPortal): History and evolution of seepage meters for quantifying flow between groundwater and surface water: Part 1

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DOI	10.1016/j.earscirev.2020.103167
	History and evolution of seepage meters for quantifying flow between groundwater and surface water: Part 1 – Freshwater settings
	Rosenberry D.O.; Duque C.; Lee D.R.
发表日期	2020
ISSN	00128252
卷号	204
英文摘要	More than 75 years after its introduction, the seepage meter remains the only device for directly quantifying exchange across the sediment-water interface between groundwater and surface water. This device, first presented in the literature in the 1940s, has been in a state of near-constant improvement and design change, necessitating a review of the history and evolution of the device and a description of current best-measurement practices. Part 1 of this two-part review documents the evolution of seepage meters deployed in freshwater settings, including a listing of suggestions for best-measurement and deployment practices. Part 2 covers the same scope for seepage meters deployed in marine settings. Traditional seepage meters isolate a portion of the sediment bed; seepage commonly is determined by routing the volume of flow across that isolated interface to or from a submerged measurement bag over a known time interval. The time-integrated volume is then divided by the bed area covered by the meter to obtain a seepage flux expressed in distance per time. Both the instrument and the measurement are deceptively simple, leading some early users to question the viability of the measurement. Numerous sources of error have been identified and addressed over the decades, resulting in large improvements in measurement consistency and accuracy. Duration of each measurement depends on the seepage rate and can vary from minutes to days, leading to the erroneous and yet common assumption that seepage is relatively stable over time. Designs that replace the measurement bag with a flowmeter eliminate bag-related errors and provide much finer temporal resolution. Resulting data indicate seepage is highly variable in many settings and responds to numerous sub-daily processes, including evapotranspiration, rainfall, seiches and waves. Combining direct measurements from seepage meters with other measurements, such as vertical hydraulic gradients and vertical temperature profiles, provides far better understanding of the processes that control exchange between groundwater and surface water. © 2020
关键词	Groundwater-surface-water exchange Sediment-water interface Seepage Seepage meter
英文关键词	flow measurement; flow velocity; groundwater-surface water interaction; routing; sediment-water interface; seepage
语种	英语
来源期刊	Earth Science Reviews
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/203868
作者单位	U.S. Geological Survey, Lakewood, CO, United States; WATEC, Department of Geoscience, Aarhus University, Aarhus, Denmark; Canadian Nuclear Laboratories, Deep River, ON, Canada; Department of Earth and Environmental Sciences, University of WaterlooON, Canada
推荐引用方式 GB/T 7714	Rosenberry D.O.,Duque C.,Lee D.R.. History and evolution of seepage meters for quantifying flow between groundwater and surface water: Part 1 – Freshwater settings[J],2020,204.
APA	Rosenberry D.O.,Duque C.,&Lee D.R..(2020).History and evolution of seepage meters for quantifying flow between groundwater and surface water: Part 1 – Freshwater settings.Earth Science Reviews,204.
MLA	Rosenberry D.O.,et al."History and evolution of seepage meters for quantifying flow between groundwater and surface water: Part 1 – Freshwater settings".Earth Science Reviews 204(2020).