Collaborative Research: Groundwater transit time distributions: bridging the gap between advanced tracer techniques and numerical modeling
合作研究:地下水渡越时间分布:弥合先进示踪技术和数值模拟之间的差距
基本信息
- 批准号:1744721
- 负责人:
- 金额:$ 23.95万
- 依托单位:
- 依托单位国家:美国
- 项目类别:Continuing Grant
- 财政年份:2018
- 资助国家:美国
- 起止时间:2018-06-01 至 2023-05-31
- 项目状态:已结题
- 来源:
- 关键词:
项目摘要
The transit time of groundwater from recharge to discharge into streams is an important control on how quickly contaminants are flushed out of aquifers and into streams. Field studies and groundwater models both indicate that groundwater with a range of transit times contributes to streamflow at any given time. However, field studies suggest the relative contribution of young groundwater (i.e., groundwater with short transit times) to streams is substantially less than calculated in modeling studies. This discrepancy in the groundwater transit time distribution (TTD) leads to a very different understanding of streamflow sources, fundamentally different predictions of the future impact of groundwater discharge on stream water quality, and potentially different perspectives on the design and assessment of efforts to manage non-point-source contamination in aquifers. This project will conduct field measurements and groundwater modeling to investigate differences in groundwater TTDs, and to determine and understand the processes that drive TTD at a range of spatial scales. Results of the project will assist water resources managers, regulators, and consultants to better understand and manage both water quantity and quality. Information will be disseminated through Cooperative Extension programs.The overall goals of this project are to (1) evaluate why there is a discrepancy between TTDs derived from groundwater measurements (field sampling of age-dating tracers) and groundwater models, (2) investigate how these processes may be better understood by using both field measurements and models in nested watersheds at a range of scales (14-3900 km2 in this project) and (3) determine the processes that control the shape of the groundwater TTDs,. This project will be conducted in a watershed overlying the High Plains aquifer in the Nebraska Sandhills, where groundwater accounts for approximately 90% of the annual stream discharge. The TTDs will be determined using age-dating tracers for both young and old groundwater (3H/3He, SF6, 14C, 4He). Groundwater age information will be coupled with discharge measurements in streams and groundwater discharge measurement from tube seepage meters in streambeds. The tracer-based TTDs will be compared to groundwater TTDs derived from particle tracking simulations in a numerical groundwater model (MODFLOW), at both the reach and watershed scale. The model will be used as a tool to investigate differences that arise between tracer- and model-based TTDs. For example, the project will investigate the variation in groundwater recharge relative to the stream channel, and if a higher resolution and more accurate representation of recharge in the model leads to better agreement between field- and model-based TTDs. The model will also be re-calibrated using groundwater age data to evaluate how TTDs compare to field-based estimates after refinement and recalibration. Information will be disseminated through Cooperative Extension programs, including interactive online training materials at www.nebraskawatershedscience.org.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.
地下水从补给到排入溪流的过渡时间是控制污染物从含水层排入溪流的速度的重要因素。实地研究和地下水模型都表明,在任何给定的时间,地下水与过境时间的范围内有助于径流。然而,实地研究表明,年轻地下水的相对贡献(即,短时间的地下水)到溪流的流量大大低于模拟研究中的计算值。这种差异在地下水过境时间分布(TTD)导致一个非常不同的理解径流源,根本不同的预测未来的影响地下水排放对河流水质,并可能不同的角度设计和评估的努力,以管理非点源污染的含水层。该项目将进行实地测量和地下水建模,以调查地下水TTD的差异,并确定和理解在一系列空间尺度上驱动TTD的过程。该项目的成果将有助于水资源管理者、监管者和顾问更好地了解和管理水量和水质。信息将通过合作推广计划传播。本项目的总体目标是:(1)评估地下水测量得出的TTD之间存在差异的原因(年龄测定示踪剂的现场取样)和地下水模型,(2)调查如何通过在一系列尺度上使用嵌套流域中的实地测量和模型来更好地理解这些过程(14-3900 km 2在这个项目中)和(3)确定控制地下水TTD形状的过程。该项目将在内布拉斯加州沙丘高地平原含水层上的分水岭进行,地下水约占年径流量的90%。将使用年龄测定示踪剂(3 H/3 He、SF6、14 C、4 He)测定新老地下水的TTD。地下水年龄信息将与溪流中的流量测量和河床中的管式渗透计的地下水流量测量相结合。基于示踪剂的TTD将进行比较,地下水TTD来自粒子跟踪模拟的数值地下水模型(MODFLOW),在达到和流域尺度。该模型将被用作一种工具,以调查示踪剂和基于模型的TTD之间出现的差异。例如,该项目将调查地下水补给相对于河道的变化,以及模型中更高的分辨率和更准确的补给表示是否会导致基于实地和模型的TTD之间更好的一致性。该模型还将使用地下水年龄数据重新校准,以评估TTD如何与改进和重新校准后的实地估计进行比较。 信息将通过合作推广计划传播,包括www.nebraskawatershedscience.org上的互动式在线培训材料。该奖项反映了NSF的法定使命,并被认为值得通过使用基金会的知识价值和更广泛的影响审查标准进行评估来支持。
项目成果
期刊论文数量(5)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
An Automated Seepage Meter for Streams and Lakes
溪流和湖泊的自动渗流计
- DOI:10.1029/2019wr026983
- 发表时间:2020
- 期刊:
- 影响因子:5.4
- 作者:Solomon, D. Kip;Humphrey, Eric;Gilmore, Troy E.;Genereux, David P.;Zlotnik, Vitaly
- 通讯作者:Zlotnik, Vitaly
Modeling groundwater transit time distributions and means across a Nebraska watershed: effects of heterogeneity in the aquifer, riverbed, and recharge parameters
- DOI:10.1016/j.jhydrol.2022.128891
- 发表时间:2022-12
- 期刊:
- 影响因子:6.4
- 作者:Can Zeyrek;A. Mittelstet;T. Gilmore;V. Zlotnik;D. Kip Solomon;D. Genereux;Eric Humphrey;Nawaraj Shrestha
- 通讯作者:Can Zeyrek;A. Mittelstet;T. Gilmore;V. Zlotnik;D. Kip Solomon;D. Genereux;Eric Humphrey;Nawaraj Shrestha
Using Automated Seepage Meters to Quantify the Spatial Variability and Net Flux of Groundwater to a Stream
使用自动渗流计量化地下水流向河流的空间变化和净通量
- DOI:10.1029/2021wr030711
- 发表时间:2022
- 期刊:
- 影响因子:5.4
- 作者:Humphrey, C. Eric;Solomon, D. Kip;Genereux, David P.;Gilmore, Troy E.;Mittelstet, Aaron R.;Zlotnik, Vitaly A.;Zeyrek, Caner;Jensen, Craig R.;MacNamara, Markus R.
- 通讯作者:MacNamara, Markus R.
Estimating groundwater mean transit time from SF6 in stream water: field example and planning metrics for a reach mass-balance approach
估算溪流水中 SF6 的地下水平均传输时间:达到质量平衡方法的现场示例和规划指标
- DOI:10.1007/s10040-021-02435-8
- 发表时间:2022
- 期刊:
- 影响因子:2.8
- 作者:Jensen, Craig R.;Genereux, David P.;Gilmore, Troy E.;Solomon, D. Kip;Mittelstet, Aaron R.;Humphrey, C. Eric;MacNamara, Markus R.;Zeyrek, Caner;Zlotnik, Vitaly A.
- 通讯作者:Zlotnik, Vitaly A.
Modified Tracer Gas Injection for Measuring Stream Gas Exchange Velocity in the Presence of Significant Temperature Variation
改进的示踪气体注入,用于在存在显着温度变化的情况下测量流气体交换速度
- DOI:10.1029/2023wr034495
- 发表时间:2023
- 期刊:
- 影响因子:5.4
- 作者:Jensen, Craig R.;Genereux, David P.;Gilmore, Troy E.;Solomon, D. Kip
- 通讯作者:Solomon, D. Kip
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D. Kip Solomon其他文献
Deep desert aquifers as an archive for Mid- to Late Pleistocene hydroclimate: An example from the southeastern Mediterranean
作为中晚更新世水文气候档案的深层沙漠含水层:来自地中海东南部的一个例子
- DOI:
10.1016/j.scitotenv.2024.175737 - 发表时间:
2024-11-15 - 期刊:
- 影响因子:8.000
- 作者:
Roi Ram;Eilon M. Adar;Yoseph Yechieli;Reika Yokochi;Werner Aeschbach;Moshe Armon;D. Kip Solomon;Roland Purtschert;Alan M. Seltzer;Kerstin L. Urbach;Michael Bishof;Peter Mueller;Jake C. Zappala;Wei Jiang;Zheng-Tian Lu;Itay J. Reznik - 通讯作者:
Itay J. Reznik
Groundwater dominates snowmelt runoff and controls streamflow efficiency in the western United States
在美国西部,地下水主导着融雪径流并控制着河流流量效率。
- DOI:
10.1038/s43247-025-02303-3 - 发表时间:
2025-05-03 - 期刊:
- 影响因子:8.900
- 作者:
Paul D. Brooks;D. Kip Solomon;Stephanie Kampf;Sara Warix;Carleton Bern;David Barnard;Holly R. Barnard;Gregory T. Carling;Rosemary W. H. Carroll;Jon Chorover;Adrian Harpold;Kathleen Lohse;Fabiola Meza;Jennifer McIntosh;Bethany Neilson;Megan Sears;Margaret Wolf - 通讯作者:
Margaret Wolf
Quantifying stream-loss recovery in a spring using dual-tracer injections in the Snake Creek drainage, Great Basin National Park, Nevada, USA
- DOI:
10.1007/s10040-023-02619-4 - 发表时间:
2023-03-17 - 期刊:
- 影响因子:2.300
- 作者:
C. Eric Humphrey;Philip M. Gardner;Lawrence E. Spangler;Nora C. Nelson;Laura Toran;D. Kip Solomon - 通讯作者:
D. Kip Solomon
Large-scale paleo water-table rise in a deep desert aquifer recorded by dissolved noble gases
溶解的稀有气体记录了沙漠深处含水层的大规模古地下水位上升
- DOI:
- 发表时间:
2022 - 期刊:
- 影响因子:6.4
- 作者:
Roi Ram;D. Kip Solomon;R. Yokochi;A. Burg;R. Purtschert;A. Seltzer;Y. Yechieli;J. Zappala;Zheng‐Tian Lu;Wei Jiang;P. Mueller;E. Adar - 通讯作者:
E. Adar
Excess air during aquifer storage and recovery in an arid basin (Las Vegas Valley, USA)
- DOI:
10.1007/s10040-010-0659-0 - 发表时间:
2010-10-12 - 期刊:
- 影响因子:2.300
- 作者:
D. Kip Solomon;Erin Cole;Joseph F. Leising - 通讯作者:
Joseph F. Leising
D. Kip Solomon的其他文献
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{{ truncateString('D. Kip Solomon', 18)}}的其他基金
Collaborative Research: Evaluating how the sampling integration scale affects field estimates of groundwater transit time and nitrogen fluxes
合作研究:评估采样积分规模如何影响地下水传输时间和氮通量的现场估计
- 批准号:
1045134 - 财政年份:2011
- 资助金额:
$ 23.95万 - 项目类别:
Continuing Grant
Exchange-Corrected CFC Dating of Stream Flow
交换校正的溪流 CFC 测年
- 批准号:
0309212 - 财政年份:2003
- 资助金额:
$ 23.95万 - 项目类别:
Continuing Grant
COLLABORATIVE RESEARCH: Radiogenic Helium as a Chronologic Tracer for Younger Groundwater
合作研究:放射性氦作为较年轻地下水的年代示踪剂
- 批准号:
9628627 - 财政年份:1996
- 资助金额:
$ 23.95万 - 项目类别:
Continuing Grant
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