Surface water-groundwater interaction at restored streams and associated reference reaches

被引:35
作者
Daniluk, Timothy L. [1 ]
Lautz, Laura K. [1 ]
Gordon, Ryan P. [1 ]
Endreny, Theodore A. [2 ]
机构
[1] Syracuse Univ, Dept Earth Sci, Heroy Geol Lab 204, Syracuse, NY 13224 USA
[2] SUNY Syracuse, ESF, Dept Environm Resources Engn, Syracuse, NY USA
基金
美国国家科学基金会;
关键词
stream restoration; hyporheic; surface water-groundwater interaction; cross-vane; natural channel design; HYPORHEIC EXCHANGE FLOWS; SOUTHERN ONTARIO; ZONE CHEMISTRY; RESTORATION; CHANNEL; RIVER; DESIGN; TEMPERATURE; CLASSIFICATION; ECOLOGY;
D O I
10.1002/hyp.9501
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Stream restoration goals include improving habitat and water quality through reconstruction of morphological features found at analogous, pristine stream reaches. Enhancing hyporheic exchange may facilitate achieving these goals. Although hyporheic exchange at restoration sites has been explored in a few previous studies, comparative studies of restored versus reference or control streams are largely absent. We hypothesized that restoration cross-vanes enhance hyporheic exchange, resulting in biogeochemical alteration of stream water chemistry in the streambed. Two streams restored using cross-vanes to control erosion and improve habitat were compared with their associated reference reaches, which provided the basis for the restoration design. Thirteen temperature profile rods with vertically stacked sensors were installed at each site for 2weeks. Heat tracing was used to quantify vertical flux in the streambed from the diurnal temperature fluctuations in the subsurface. Stream water and bed pore waters from mini-piezometers were analysed for ion and nutrient chemistry. In general, mean vertical flux rates through the streambed were small throughout reference sites (-0.3 to 0.3m/day) and at most locations at restored sites. Immediately adjacent to cross-vanes, vertical flux rates were larger (up to 3.5m/day). Geochemistry of pore waters shows distinct differences in the sources for the reference and restored sites. Strong downwelling zones adjacent to cross-vanes showed high dissolved oxygen (10.75mg/l) and geochemistry in the streambed similar to surface water. Reference sites had lower dissolved oxygen in the streambed (0.66-5.14mg/l), and geochemical patterns suggest a mixture of discharging groundwater and surface water in the hyporheic zone. Restored sites also clearly show sulfate and nitrate reduction occurring in the streambed, which is not observed at the reference sites. The stream restoration sites studied here enhance rapid hyporheic exchange, but upwelling of groundwater has a stronger influence on streambed geochemistry at reference sites. Copyright (c) 2012 John Wiley & Sons, Ltd.
引用
收藏
页码:3730 / 3746
页数:17
相关论文
共 50 条
[41]   Conceptual models for surface water and groundwater interactions at pond and plug restored meadows [J].
Rodriguez, K. ;
Swanson, S. ;
McMahon, A. .
JOURNAL OF SOIL AND WATER CONSERVATION, 2017, 72 (04) :382-394
[42]   Evaluation of surface water-groundwater interaction using environmental isotopes (D, 18O and 222Rn) in Chongli Area, China [J].
Du, Shanghai ;
Deng, Zhiqun ;
Liu, Yingjie ;
Zhang, Lijie ;
Xu, Hang ;
Yang, He .
JOURNAL OF RADIOANALYTICAL AND NUCLEAR CHEMISTRY, 2019, 321 (01) :303-311
[43]   Water transfer imposes hydrochemical impacts on groundwater by altering the interaction of groundwater and surface water [J].
Yuan, Ruiqiang ;
Wang, Meng ;
Wang, Shiqin ;
Song, Xianfang .
JOURNAL OF HYDROLOGY, 2020, 583
[44]   Multiobjective Optimization for Water Resource Management in Low-Flow Areas Based on a Coupled Surface Water-Groundwater Model [J].
Zeinali, Masoomeh ;
Azari, Arash ;
Heidari, Mohammad Mehdi .
JOURNAL OF WATER RESOURCES PLANNING AND MANAGEMENT, 2020, 146 (05)
[45]   Surface water-groundwater interactions in catchment scale water resources assessments-understanding and hypothesis testing with a hydrological model [J].
Tanner, J. L. ;
Hughes, D. A. .
HYDROLOGICAL SCIENCES JOURNAL-JOURNAL DES SCIENCES HYDROLOGIQUES, 2015, 60 (11) :1880-1895
[46]   Near-stream soil water-groundwater coupling in the headwaters of the Afon Hafren, Wales: Implications for surface water quality [J].
Haria, Atul H. ;
Shand, Paul .
JOURNAL OF HYDROLOGY, 2006, 331 (3-4) :567-579
[47]   Data-driven and numerical simulation coupling to quantify the impact of ecological water replenishment on surface water-groundwater interactions [J].
Lyu, Kewei ;
Dong, Yihan ;
Lyu, Wensheng ;
Zhou, Yan ;
Wang, Sufen ;
Wang, Zhaomeng ;
Cui, Weizhe ;
Zhang, Yaobin ;
Zhang, Qiulan ;
Cui, Yali .
JOURNAL OF HYDROLOGY, 2025, 649
[48]   Wetlands as integral parts of surface water-groundwater interactions in the Athabasca Oil Sands Area: Review and synthesis [J].
Volik, Olena ;
Petrone, Richard ;
Price, Jonathan .
ENVIRONMENTAL REVIEWS, 2024, 32 (02) :145-172
[49]   Assessment of ensemble data assimilation based heat tracer method for estimating surface water-groundwater interaction at seasonal timescale under complex field conditions [J].
Zhai, Xuchen ;
Chen, Kewei ;
Liang, Xiuyu ;
Wang, Guoliang ;
Zhao, Xin ;
Guo, Zhilin ;
Zhou, Renjie ;
Ding, Chen ;
Liu, Cancan ;
Zheng, Chunmiao .
JOURNAL OF HYDROLOGY, 2025, 649
[50]   Evolution of plume geometry, dilution and reactive mixing in porous media under highly transient flow fields at the surface water-groundwater interface [J].
Hazas, Monica Basilio ;
Ziliotto, Francesca ;
Lee, Jonghyun ;
Rolle, Massimo ;
Chiogna, Gabriele .
JOURNAL OF CONTAMINANT HYDROLOGY, 2023, 258