Hyporheic Exchange under the Influence of Clay Lens

ZHUANG Wei, LU Cheng-peng, ZHU Xuan-yu, LI Hui-min, WANG Su-wan

Journal of Changjiang River Scientific Research Institute ›› 2019, Vol. 36 ›› Issue (8) : 49-54.

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Journal of Changjiang River Scientific Research Institute ›› 2019, Vol. 36 ›› Issue (8) : 49-54. DOI: 10.11988/ckyyb.20170634
WATER RESOURCES AND ENVIRONMENT

Hyporheic Exchange under the Influence of Clay Lens

  • ZHUANG Wei1, LU Cheng-peng2, ZHU Xuan-yu2, LI Hui-min2, WANG Su-wan2
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Abstract

Hyporheic exchange is one of the important physical processes that affect the flow conditions of river-groundwater belt, the water environment restoration, and the ecological balance. However, the mechanism of the influence of clay lens on subsurface flow in riverbed has not been well revealed. In this study,the hyporheic exchange under the influence of clay lens is investigated by means of physical modeling with appropriate dimensions with reference to actual geological conditions.Under controlled water head and discharge, the hyporheic exchange is simulated in the presence of varied sizes of clay lens at different depths, and the groundwater flow field in the hyporheic zone is rendered according to the measured pressure data. For each simulation case, the gradient of flow field is calculated using the contours drawn at the same distance from the clay lens in four directions. The velocity field near the lens can then be obtained, and is further transformed to flow field in line with Darcy’s law. The study reveals that hyporheic discharge decreases with the increase of the size and depth of single clay lens.As the water head difference between the upper and lower surface water increases, the flow velocity increases at the upstream face of clay lens with an attenuating growth rate, but reduces at the back side of the lens with an aggravating reduction rate. In addition, a method for studying small scale subsurface flow exchange processes is also provided.

Key words

clay lens / physical model / hyporheic exchange / Darcy’s law / velocity of flow

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ZHUANG Wei, LU Cheng-peng, ZHU Xuan-yu, LI Hui-min, WANG Su-wan. Hyporheic Exchange under the Influence of Clay Lens[J]. Journal of Changjiang River Scientific Research Institute. 2019, 36(8): 49-54 https://doi.org/10.11988/ckyyb.20170634

References

[1] HANCOCK P,BOULTON A,HUMPHREYS W.Aquifers and Hydraulic Zones:Towards an Ecological Understanding of Groundwater. Hydrogeology Journal, 2005,13(1):98-111.
[2] 吴健,黄沈发,唐 浩,等,河流潜流带的生态系统健康研究进展.水资源保护,2006,22(5):5-8.
[3] BOULTON A.Stream Ecology and Surface Hyporheric Exchange:Implications, Techniques and Limitations. Australian Journal of Marine and Fresh Water Research,1993,44(4):553-564.
[4] MIALL A D. The Geology of Fluvial Deposits: Sedimentary Facies, Basin Analysis, and Petroleum Geology. Berlin: Springer, 1996.
[5] LAUTZ L K, KRANES N T, SIEGEL D I. Heat Tracing of Heterogeneous Hyporheic Exchange Adjacent to In-stream Geomorphic Features. Hydrological Processes, 2010,24(21):3074-3086.
[6] BRIGGS M A, LAUTZ L K, HARE D K, et al. Relating Hyporheic Fluxes, Residence Times, and Redox-sensitive Biogeochemical Processes Upstream of Beaver Dams. Freshwater Science, 2013, 32(2): 622-641.
[7] GORDON R P, LAUTZ L K, DANILUK T L. Spatial Patterns of Hyporheic Exchange and Biogeochemical Cycling around Cross-vane Restoration Structures: Implications for Stream Restoration Design. Water Resources Research, 2013, 49(4): 2040-2055.
[8] 鲁程鹏, 束龙仓, 陈洵洪. 河床地形影响潜流交换作用的数值分析 . 水科学进展, 2012,23(6): 789-795.
[9] BELLIN A, TONINA D, MARZADRI A,et al.Scaling in Hyporheic Exchange. Water Resources Research, 2015, 51(2): 1353-1358.
[10] ENDRENY T, LAUTZ L, SIEGEL D. Hyporheic Flow Path Response to Hydraulic Jumps at River Steps: Hydrostatic Model Simulations. Water Resources Research, 2011, 47: W02518.
[11] 鲁程鹏, 张 颖, 朱静思, 等. 基于热追踪方法的河流横断面潜流交换时空非均质特征研究 . 第四纪研究, 2014,34(5): 1094-1105.
[12] KARWAN D L, SAIERS J E. Hyporheic Exchange and Streambed Filtration of Suspended Particles. Water Resources Research, 2012, 48: W01519.
[13] SALEHIN M, PACKMAN A I, PARADIS M. Hyporheic Exchange with Heterogeneous Streambeds: Laboratory Experiments and Modeling. Water Resources Research, 2004, 40(11): W11504.
[14] 霍思远,靳孟贵,梁 杏. 包气带弱渗透性黏土透镜体对降雨入渗补给影响的数值模拟. 吉林大学学报(地球科学版), 2013,43(5):1579-1587.
[15] ANIBAS C, BUIS K, VERHOEVEN R, et al. A Simple Thermal Mapping Method for Seasonal Spatial Patterns of Groundwater-Surface Water Interaction. Journal of Hydrology, 2011, 397(1/2): 93-104.
[16] 杨国强, 苏小四, 王 璜, 等. 热量示踪在潜流带水动力交换量计算中的应用 . raybet体育在线 院报, 2014, 31(10): 124-127,133.
[17] 李佳选, 王元元, 宋进喜, 等. 北洛河潜流带水交换研究 . 水土保持学报, 2015,29(2): 310-313.
[18] SINGHA K, PIDLISECKY A, DAY-LEWIS F D, et al. Electrical Characterization of Non-Fickian Transport in Groundwater and Hyporheic Systems . Water Resources Research, 2008, 44: W00d07.
[19] WARD A S, GOOSEFF M N, SINGHA K. Imaging Hyporheic Zone Solute Transport Using Electrical Resistivity. Hydrological Processes, 2010, 24(7): 948-953.
[20] COSCIA I, LINDE N, GREENHALGH S, et al. Estimating TravelTimes and Groundwater Flow Patterns Using 3D Time-lapse Crosshole ERT Imaging of Electrical Resistivity Fluctuations Induced by Infiltrating River Water. Geophysics, 2012, 77(4): 239-250.
[21] ANGERMANN L, KRAUSE S, LEWANDOWSKI J. Application of Heat Pulse Injections for Investigating Shallow Hyporheic Flow in a Lowland River. Water Resources Research, 2012, 48:W00p02.
[22] CARDIFF M,BARRASH W,KITANITIS P K,et al.A Potential-based Inversion of Unconfined Steady-state Hydraulic Tomography. Groundwater,2009,47:259-270.
[23] WONDZELL S M, LANIER J, HAGGERTY R. Evaluation of Alternative Groundwater Flow Models for Simulating Hyporheic Exchange in a Small Mountain Stream. Journal of Hydrology, 2009, 364(1/2): 142-151.
[24] BROOKFIELD A E, SUDICKY E A. Implications of Hyporheic Flow on Temperature-based Estimates of Groundwater/Surface Water Interactions. Journal of Hydrologic Engineering, 2013, 18(10): 1250-1261.
[25] LINDGREN G A, DESTOUNI G, MILLER A V. Solute Transport Through the Integrated Groundwater-Stream System of a Catchment. Water Resources Research, 2004, 40(3): W03511.
[26] FISHER S G, WEITER J R. Flowpaths as Integrators of Heterogeneity in Streams and Landscapes∥LOVETT G M, TURNER M G, JONES C G, et al.Ecosystem Function in Heterogeneous Landscapes. New York: Springer, 2005.
[27] WINTER T. Relation of Streams, Lakes, and Wetlands to Groundwater Flow Systems. Hydrogeology Journal, 1999,7(1):28-45.
[28] CHEN C, ZENG L. Using the Level Set Method to Study the Effects of Heterogeneity and Anisotropy on Hyporheic Exchange. Water Resources Research, 2015, 51(5): 3617-3634.
[29] GOMEZ-VELEZ J D, KRAUSE S, WILSON J L. Effect of Low-permeability Layers on Spatial Patterns of Hyporheic Exchange and Groundwater Upwelling. Water Resources Research, 2014, 50(6): 5196-5215.
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