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Journal of Geographical Sciences

, Volume 29, Issue 3, pp 377–388 | Cite as

Estimating spatial pattern of hyporheic water exchange in slack water pool

  • Jinxi SongEmail author
  • Dandong Cheng
  • Junlong Zhang
  • Yongqiang Zhang
  • Yongqing Long
  • Yan Zhang
  • Weibo Shen
Article
  • 2 Downloads

Abstract

Hyporheic zone (HZ) influences hydraulic and biogeochemical processes in and alongside streams, therefore, investigating the controlling geographic factors is beneficial for understanding the hydrological processes in HZ. Slack water pool (SWP) is an essential micro-topographic structure that has an impact on surface water and groundwater interactions in the HZ during and after high flows. However, only a few studies investigate HZ surface water and groundwater exchange in the SWP. This study used the thermal method to estimate the HZ water exchange in the SWP in a segment of the Weihe River in China during the winter season. The findings show that on the flow-direction parallel to the stream, river recharge dominates the HZ water exchange, while on the opposing flow-direction bank groundwater discharge dominates the water exchange. The water exchange in the opposing flow-direction bank is about 1.6 times of that in the flow-direction bank. The HZ water exchange is not only controlled by flow velocity but also the location and shape of the SWP. Great water exchange amount corresponds to the shape with more deformation. The maximum water exchange within the SWP is close to the river bank where the edge is relatively high. This study provides some guidelines for water resources management during flooding events.

Keywords

hyporheic water exchange thermal method discharge recharge surface water-groundwater interactions 

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Notes

Acknowledgements

We thank Guotao Zhang, Weiwei Jiang, Yuanyuan Wang, Ming Wen, Shaofeng Xu, and other members for assistance in fieldwork. In particular, we are grateful to the editor and two anonymous reviewers for providing numerous comments and suggestions, which helped improve this manuscript.

References

  1. Anibas C, Buis K, Verhoeven R et al., 2011. A simple thermal mapping method for seasonal spatial patterns of groundwater-surface water interaction. Journal of Hydrology, 397(1): 93–104.CrossRefGoogle Scholar
  2. Anibas C, Fleckenstein J H, Volze N et al., 2009. Transient or steady-state? Using vertical temperature profiles to quantify groundwater-surface water exchange. Hydrological Processes, 23(15): 2165–2177.CrossRefGoogle Scholar
  3. Baxter C, Hauer F R, Woessner W W, 2003. Measuring groundwater-stream water exchange: New techniques for installing minipiezometers and estimating hydraulic conductivity. Transactions of the American Fisheries Society, 132(3): 493–502.CrossRefGoogle Scholar
  4. Bellin A, Tonina D, Marzadri A, 2015. Breakthrough curve moments scaling in hyporheic exchange. Water Resources Research, 51(2): 1112–1126.CrossRefGoogle Scholar
  5. Boano F, Camporeale C, Revelli R et al., 2006. Sinuosity-driven hyporheic exchange in meandering rivers. Geophysical Research Letters, 33(18): L18406.CrossRefGoogle Scholar
  6. Boano F, Revelli R, Ridolfi L, 2008. Reduction of the hyporheic zone volume due to the stream-aquifer interaction. Geophysical Research Letters, 35(9): L09401.CrossRefGoogle Scholar
  7. Boano F, Revelli R, Ridolfi L, 2010. Effect of streamflow stochasticity on bedform-driven hyporheic exchange. Advances in Water Resources, 33(11): 1367–1374.CrossRefGoogle Scholar
  8. Boulton A J, Datry T, Kasahara T et al., 2010. Ecology and management of the hyporheic zone: Stream-groundwater interactions of running waters and their floodplains. Journal of the North American Benthological Society, 29(1): 26–40.CrossRefGoogle Scholar
  9. Cardenas M B, Wilson J, Zlotnik V A, 2004. Impact of heterogeneity, bed forms, and stream curvature on subchannel hyporheic exchange. Water Resources Research, 40(8): W08307.CrossRefGoogle Scholar
  10. Caruso A, Ridolfi L, Boano F, 2016. Impact of watershed topography on hyporheic exchange. Advances in Water Resources, 94: 400–411.CrossRefGoogle Scholar
  11. Chen X, Dong W, Ou G et al., 2013. Gaining and losing stream reaches have opposite hydraulic conductivity distribution patterns. Hydrology and Earth System Sciences, 17(7): 2569–2579.CrossRefGoogle Scholar
  12. Chen X B, Cardenas M B, Chen L, 2015. Three-dimensional versus two-dimensional bed form-induced hyporheic exchange. Water Resources Research, 51(4): 2923–2936.CrossRefGoogle Scholar
  13. Cheng D H, Chen X H, Huo A D et al., 2013. Influence of bedding orientation on the anisotropy of hydraulic conductivity in a well-sorted fluvial sediment. International Journal of Sediment Research, 28(1): 118–125.CrossRefGoogle Scholar
  14. Conant B, 2004. Delineating and quantifying ground water discharge zones using streambed temperatures. Groundwater, 42(2): 243–257.CrossRefGoogle Scholar
  15. Conant Jr B, Cherry J A, Gillham R W, 2004. A PCE groundwater plume discharging to a river: Influence of the streambed and near-river zone on contaminant distributions. Journal of Contaminant Hydrology, 73(1): 249–279.CrossRefGoogle Scholar
  16. Darracq A, Destouni G, Persson K et al., 2009. Quantification of advective solute travel times and mass transport through hydrological catchments. Environmental Fluid Mechanics, 10(1/2): 103–120.Google Scholar
  17. Doble R, Brunner P, McCallum J et al., 2012. An analysis of river bank slope and unsaturated flow effects on bank storage. Groundwater, 50(1): 77–86.CrossRefGoogle Scholar
  18. Dochartaigh B, MacDonald A, Archer N et al., 2012. Groundwater-surface water interaction in an upland hillslope- floodplain environment, Eddleston, Scotland, BHS 11th National Symposium, Hydrology for a Changing World, Dundee, Scotland, pp. 2012.Google Scholar
  19. Dudley-Southern M, Binley A, 2015. Temporal responses of groundwater-surface water exchange to successive storm events. Water Resources Research, 51(2): 1112–1126.CrossRefGoogle Scholar
  20. Dunster K, 2011. Dictionary of Natural Resource Management. UBC Press.Google Scholar
  21. Fischer H, Kloep F, Wilzcek S et al., 2005. A river's liver-microbial processes within the hyporheic zone of a large lowland river. Biogeochemistry, 76(2): 349–371.CrossRefGoogle Scholar
  22. Fox A, Boano F, Arnon S, 2014. Impact of losing and gaining streamflow conditions on hyporheic exchange fluxes induced by dune-shaped bed forms. Water Resources Research, 50(3): 1895–1907.CrossRefGoogle Scholar
  23. Frei S, Lischeid G, Fleckenstein J H, 2010. Effects of micro-topography on surface-subsurface exchange and runoff generation in a virtual riparian wetland: A modeling study. Advances in Water Resources, 33(11): 1388–1401.CrossRefGoogle Scholar
  24. Gerecht K E, Cardenas M B, Guswa A J et al., 2011. Dynamics of hyporheic flow and heat transport across a bed-to-bank continuum in a large regulated river. Water Resources Research, 47: W03524.CrossRefGoogle Scholar
  25. Gualtieri C, Filizola Jr N, Oliveira M et al., 2017. A field study of the confluence between Negro and Solimões rivers. Part 1: Hydrodynamics and sediment transport. Comptes Rendus Geoscience, 350(1/2): 31–42.Google Scholar
  26. Ianniruberto M, Trevethan M, Pinheiro A et al., 2017. A field study of the confluence between Negro and Solimões rivers. Part 2: Bed morphology and stratigraphy. Comptes Rendus Geoscience, 350(1/2): 43–54.Google Scholar
  27. Irvine D J, Lautz L K, Briggs M A et al., 2015. Experimental evaluation of the applicability of phase, amplitude, and combined methods to determine water flux and thermal diffusivity from temperature time series using VFLUX 2. Journal of Hydrology, 531: 728–737.CrossRefGoogle Scholar
  28. Isiorho S A, Meyer J H, 1999. The effects of bag type and meter size on seepage meter measurements. Groundwater, 37(3): 411–413.CrossRefGoogle Scholar
  29. Jiang W, Song J, Zhang J et al., 2015. Spatial variability of streambed vertical hydraulic conductivity and its relation to distinctive stream morphologies in the Beiluo River, Shaanxi Province, China. Hydrogeology Journal, 23(7): 1617–1626.CrossRefGoogle Scholar
  30. Josset L, Ginsbourger D, Lunati I, 2015. Functional error modeling for uncertainty quantification in hydrogeology. Water Resources Research, 51(2): 1050–1068.CrossRefGoogle Scholar
  31. Kalbus E, Reinstorf F, Schirmer M, 2006. Measuring methods for groundwater-surface water interactions: A review. Hydrology and Earth System Sciences, 10(6): 873–887.CrossRefGoogle Scholar
  32. Kasahara T, Wondzell S M, 2003. Geomorphic controls on hyporheic exchange flow in mountain streams. Water Resources Research, 39(1): SBH 3-1-SBH 3–14.Google Scholar
  33. Koch J, Nowak W, 2015. Predicting DNAPL mass discharge and contaminated site longevity probabilities: Conceptual model and high-resolution stochastic simulation. Water Resources Research, 51: 806–831.CrossRefGoogle Scholar
  34. Korbel K L, Hose G C, 2015. Habitat, water quality, seasonality, or site? Identifying environmental correlates of the distribution of groundwater biota. Freshwater Science, 34(1): 329–343.CrossRefGoogle Scholar
  35. Kuhlman KL, Malama B, Heath J E, 2015. Multiporosity flow in fractured low-permeability rocks. Water Resources Research, 51(2): 848–860.Google Scholar
  36. Kumar K N, Entekhabi D, Molini A, 2015. Hydrological extremes in hyperarid regions: A diagnostic characterization of intense precipitation over the Central Arabian Peninsula. Journal of Geophysical Research: Atmospheres, 120: 1637–1650.Google Scholar
  37. Larkin R G, Sharp J M, 1992. On the relationship between river-basin geomorphology, aquifer hydraulics, and ground-water flow direction in alluvial aquifers. Geological Society of America Bulletin, 104(12): 1608–1620.CrossRefGoogle Scholar
  38. Lautz L K, Siegel D I, 2006. Modeling surface and ground water mixing in the hyporheic zone using MODFLOW and MT3D. Advances in Water Resources, 29(11): 1618–1633.CrossRefGoogle Scholar
  39. Li Q, Song J X, Wei A et al., 2013. Changes in major factors affecting the ecosystem health of the Weihe River in Shaanxi Province, China. Frontiers of Environmental Science & Engineering, 7(6): 875–885.CrossRefGoogle Scholar
  40. Malard F, Tockner K, Dole-Olivier M J et al., 2002. A landscape perspective of surface-subsurface hydrological exchanges in river corridors. Freshwater Biology, 47(4): 621–640.CrossRefGoogle Scholar
  41. Malcolm I A, Soulsby C, Youngson A F, 2006. High-frequency logging technologies reveal state-dependent hyporheic process dynamics: Implications for hydroecological studies. Hydrological Processes, 20(3): 615–622.CrossRefGoogle Scholar
  42. Marzadri A, Tonina D, McKean J A et al., 2014. Multi-scale streambed topographic and discharge effects on hyporheic exchange at the stream network scale in confined streams. Journal of Hydrology, 519: 1997–2011.CrossRefGoogle Scholar
  43. Mendoza-Lera C, Datry T, 2017. Relating hydraulic conductivity and hyporheic zone biogeochemical processing to conserve and restore river ecosystem services. Science of the Total Environment, 579: 1815–1821.CrossRefGoogle Scholar
  44. Min L L, Yu J J, Liu C M et al., 2013. The spatial variability of streambed vertical hydraulic conductivity in an intermittent river, northwestern China. Environmental Earth Sciences, 69(3): 873–883.CrossRefGoogle Scholar
  45. Naiman R J, Latterell J J, 2005. Principles for linking fish habitat to fisheries management and conservation. Journal of Fish Biology, 67: 166–185.CrossRefGoogle Scholar
  46. Nazemi A, Wheater H S, 2014. How can the uncertainty in the natural inflow regime propagate into the assessment of water resource systems? Advances in Water Resources, 63: 131–142.Google Scholar
  47. Peralta-Maraver I, Reiss J, Robertson A L, 2018. Interplay of hydrology, community ecology and pollutant attenuation in the hyporheic zone. Science of the Total Environment, 610/611: 267–275.CrossRefGoogle Scholar
  48. Pozdniakov S P, Wang P, Lekhov M V, 2016. A semi-analytical generalized Hvorslev formula for estimating riverbed hydraulic conductivity with an open-ended standpipe permeameter. Journal of Hydrology, 540: 736–743.CrossRefGoogle Scholar
  49. Prancevic J P, Lamb M P, 2015. Particle friction angles in steep mountain channels. Journal of Geophysical Research: Earth Surface, 120(2): 242–259.Google Scholar
  50. Ramirez J A, Baird A J, Coulthard T J et al., 2015. Testing a simple model of gas bubble dynamics in porous media. Water Resources Research, 51(2): 1036–1049.CrossRefGoogle Scholar
  51. Rau G C, Andersen M S, McCallum A M et al., 2014. Heat as a tracer to quantify water flow in near-surface sediments. Earth-Science Reviews, 129: 40–58.CrossRefGoogle Scholar
  52. Rivett M O, Buss S R, Morgan P et al., 2008. Nitrate attenuation in groundwater: A review of biogeochemical controlling processes. Water Research, 42(16): 4215–4232.CrossRefGoogle Scholar
  53. Sapriza-Azuri G, Jódar J, Navarro V et al., 2015. Impacts of rainfall spatial variability on hydrogeological response. Water Resources Research, 51(2): 1112–1126.CrossRefGoogle Scholar
  54. Schmeeckle M W, Nelson J M, Shreve R L, 2007. Forces on stationary particles in near-bed turbulent flows. Journal of Geophysical Research, 112(F2): F02003.CrossRefGoogle Scholar
  55. Schmidt C, Conant Jr B, Bayer-Raich M et al., 2007. Evaluation and field-scale application of an analytical method to quantify groundwater discharge using mapped streambed temperatures. Journal of Hydrology, 347(3): 292–307.CrossRefGoogle Scholar
  56. Somogyvári M, Bayer P, Brauchler R, 2016. Travel-time-based thermal tracer tomography. Hydrology and Earth System Sciences, 20(5): 1885–1901.CrossRefGoogle Scholar
  57. Song J X, Zhang G T, Wang W Z et al., 2017. Variability in the vertical hyporheic water exchange effected by hydraulic conductivity and river morphology at a natural confluent meander bend. Hydrological Processes, 31(19): 3407–3420.CrossRefGoogle Scholar
  58. Stegen J C, Johnson T, Fredrickson J K et al., 2018. Influences of organic carbon speciation on hyporheic corridor biogeochemistry and microbial ecology. Nat. Commun., 9(1): 585.CrossRefGoogle Scholar
  59. Storey R G, Howard K W F, Williams D D, 2003. Factors controlling riffle-scale hyporheic exchange flows and their seasonal changes in a gaining stream: A three-dimensional groundwater flow model. Water Resources Research, 39(2): 1034.CrossRefGoogle Scholar
  60. Stubbington R, 2012. The hyporheic zone as an invertebrate refuge: A review of variability in space, time, taxa and behaviour. Marine and Freshwater Research, 63(4): 293–311.CrossRefGoogle Scholar
  61. Suzuki S, 1960. Percolation measurements based on heat flow through soil with special reference to paddy fields. Journal of Geophysical Research, 65(9): 2883–2885.CrossRefGoogle Scholar
  62. Tonina D, Buffington J M, 2007. Hyporheic exchange in gravel bed rivers with pool-riffle morphology: Laboratory experiments and three-dimensional modeling. Water Resources Research, 43(1): W01421.CrossRefGoogle Scholar
  63. Trauth N, Fleckenstein J H, 2017. Single discharge events increase reactive efficiency of the hyporheic zone. Water Resources Research, 53(1): 779–798.CrossRefGoogle Scholar
  64. Vogt T, Schirmer M, Cirpka O A, 2012. Investigating riparian groundwater flow close to a losing river using diurnal temperature oscillations at high vertical resolution. Hydrology and Earth System Sciences, 16(2): 473–487.CrossRefGoogle Scholar
  65. Wang P, Pozdniakov S P, Vasilevskiy P Y, 2017. Estimating groundwater-ephemeral stream exchange in hyper-arid environments: Field experiments and numerical simulations. Journal of Hydrology, 555: 68–79.CrossRefGoogle Scholar
  66. Wang W Z, Song J X, Zhang G T et al., 2018. The influence of hyporheic upwelling fluxes on inorganic nitrogen concentrations in the pore water of the Weihe River. Ecological Engineering, 112: 105–115.CrossRefGoogle Scholar
  67. Westhoff M C, Gooseff M N, Bogaard T A et al., 2011. Quantifying hyporheic exchange at high spatial resolution using natural temperature variations along a first-order stream. Water Resources Research, 47(10): W10508.CrossRefGoogle Scholar
  68. Wroblicky G J, Campana M E, Valett H M et al., 1998. Seasonal variation in surface-subsurface water exchange and lateral hyporheic area of two stream-aquifer systems. Water Resources Research, 34(3): 317–328.CrossRefGoogle Scholar
  69. Zhang G T, Song J X, Wen M et al., 2017. Effect of bank curvatures on hyporheic water exchange at meter scale. Hydrology Research, 48(2): 355–369.CrossRefGoogle Scholar

Copyright information

© Science in China Press and Springer-Verlag GmbH Germany, part of Springer Nature 2019

Authors and Affiliations

  • Jinxi Song
    • 1
    • 2
    Email author
  • Dandong Cheng
    • 1
    • 3
  • Junlong Zhang
    • 2
    • 4
  • Yongqiang Zhang
    • 5
  • Yongqing Long
    • 2
  • Yan Zhang
    • 2
  • Weibo Shen
    • 1
  1. 1.State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water ConservationCAS & MWRYangling, ShaanxiChina
  2. 2.Shaanxi Key Laboratory of Earth Surface System and Environmental Carrying Capacity, College of Urban and Environmental SciencesNorthwest UniversityXi’anChina
  3. 3.University of Chinese Academy of SciencesBeijingChina
  4. 4.College of Geography and EnvironmentShandong Normal UniversityJinanChina
  5. 5.CSIRO Land and WaterCanberraAustralia

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