Hillslope hydrologic connectivity controls riparian groundwater turnover: Implications of catchment structure for riparian buffering and stream water sources

[1] Hydrologic connectivity between catchment upland and near stream areas is essential for the transmission of water, solutes, and nutrients to streams. However, our current understanding of the role of riparian zones in mediating landscape hydrologic connectivity and the catchment scale export of water and solutes is limited. We tested the relationship between the duration of hillslope-riparian-stream (HRS) hydrologic connectivity and the rate and degree of riparian shallow groundwater turnover along four HRS well transects within a set of nested mountain catchments (Tenderfoot Creek Experimental Forest, MT). Transect HRS water table connectivity ranged from 9 to 123 days during the annual snowmelt hydrograph. Hillslope water was always characterized by low specific conductance (∼27 μS cm−1). In transects with transient hillslope water tables, riparian groundwater specific conductance was elevated during base flow conditions (∼127 μS cm−1) but shifted toward hillslope signatures once a HRS groundwater connection was established. The degree of riparian groundwater turnover was proportional to the duration of HRS connectivity and inversely related to the riparian: hillslope area ratios (buffer ratio; r2 = 0.95). We applied this relationship to the stream network in seven subcatchments within the Tenderfoot Creek Experimental Forest and compared their turnover distributions to source water contributions measured at each catchment outlet. The amount of riparian groundwater exiting each of the seven catchments was linearly related (r2 = 0.92) to their median riparian turnover time. Our observations suggest that the size and spatial arrangement of hillslope and riparian zones along a stream network and the timing and duration of groundwater connectivity between them is a first-order control on the magnitude and timing of water and solutes observed at the catchment outlet.

[1]  D. Dewalle,et al.  Three-component tracer model for stormflow on a small Appalachian forested catchment , 1988 .

[2]  Peter S. Murdoch,et al.  Effect of groundwater springs on NO3− concentrations during summer in Catskill Mountain streams , 1998 .

[3]  Tim Burt,et al.  Temporal and spatial patterns of nitrate losses from an agricultural catchment , 1987 .

[4]  R. O'Neill,et al.  Flow variability and hillslope hydrology , 1982 .

[5]  Malcolm G. Anderson,et al.  Automatic monitoring of soil moisture conditions in a hillslope spur and hollow , 1977 .

[6]  G. Hornberger,et al.  Modeling catchment‐scale mixing in the near‐stream zone—Implications for chemical and isotopic hydrograph separation , 2003 .

[7]  Tim Burt,et al.  Topographic controls of soil moisture distributions , 1985 .

[8]  Doerthe Tetzlaff,et al.  How does landscape structure influence catchment transit time across different geomorphic provinces? , 2009 .

[9]  Jeffrey J. McDonnell,et al.  Role of discrete landscape units in controlling catchment dissolved organic carbon dynamics , 2003 .

[10]  T. Burt,et al.  Denitrification in riparian buffer zones : the role of floodplain hydrology , 1999 .

[11]  D. Genereux,et al.  Quantifying uncertainty in tracer‐based hydrograph separations , 1998 .

[12]  M. Sivapalan Process complexity at hillslope scale, process simplicity at the watershed scale: is there a connection? , 2003 .

[13]  Michael N. Gooseff,et al.  Channel water balance and exchange with subsurface flow along a mountain headwater stream in Montana, United States , 2009 .

[14]  David M. Hannah,et al.  Using tracers to upscale flow path understanding in mesoscale mountainous catchments: two examples from Scotland , 2004 .

[15]  R. Lowrance Groundwater nitrate and denitrification in a coastal plain riparian forest , 1992 .

[16]  J. McDonnell,et al.  Quantifying contributions to storm runoff through end‐member mixing analysis and hydrologic measurements at the Panola Mountain Research Watershed (Georgia, USA) , 2001 .

[17]  R. D. Black,et al.  Partial Area Contributions to Storm Runoff in a Small New England Watershed , 1970 .

[18]  Tim Covino,et al.  Stream gains and losses across a mountain‐to‐valley transition: Impacts on watershed hydrology and stream water chemistry , 2007 .

[19]  Günter Blöschl,et al.  Preferred states in spatial soil moisture patterns: Local and nonlocal controls , 1997 .

[20]  George M. Hornberger,et al.  Modeling transport of dissolved silica in a forested headwater catchment: Implications for defining the hydrochemical response of observed flow pathways , 2001 .

[21]  Y. Kodama,et al.  Stream temperature, specific conductance and runoff process in mountain watersheds , 1999 .

[22]  Jeffrey Shaman,et al.  Are big basins just the sum of small catchments? , 2004 .

[23]  Brian L. McGlynn,et al.  Distributed assessment of contributing area and riparian buffering along stream networks , 2003 .

[24]  Alan R. Hill,et al.  Groundwater phosphate dynamics in a river riparian zone: effects of hydrologic flowpaths, lithology and redox chemistry , 2001 .

[25]  J. McDonnell,et al.  Riparian zone flowpath dynamics during snowmelt in a small headwater catchment , 1999 .

[26]  K. Beven,et al.  The hydrological response of headwater and sideslope areas / La réponse hydrologique des zones de cours supérieurs et des zones de pente latérale , 1978 .

[27]  Alan R. Hill,et al.  Landscape controls on nitrate removal in stream riparian zones , 2004 .

[28]  Separation of a snowmelt hydrograph by stream conductance , 1986 .

[29]  L. Band,et al.  Export of nitrogen from catchments within a temperate forest: Evidence for a unifying mechanism regulated by variable source area dynamics , 1998 .

[30]  P. Vidon,et al.  Upland Controls on the Hydrological Functioning of Riparian Zones in Glacial Till Valleys of the Midwest 1 , 2007 .

[31]  Irena F. Creed,et al.  A framework for broad‐scale classification of hydrologic response units on the Boreal Plain: is topography the last thing to consider? , 2005 .

[32]  Jeffrey J. McDonnell,et al.  Scale effects on headwater catchment runoff timing, flow sources, and groundwater‐streamflow relations , 2004 .

[33]  Jeffrey J. McDonnell,et al.  Linking the hydrologic and biogeochemical controls of nitrogen transport in near-stream zones of temperate-forested catchments: a review , 1997 .

[34]  A. Butturini,et al.  Water table fluctuations in the riparian zone: comparative results from a pan-European experiment , 2002 .

[35]  Phillip E. Farnes,et al.  Comparisons of hydrology, geology, and physical characteristics between Tenderfoot Creek Experimental Forest (east side) Montana, and Coram Experimental Forest (west side) Montana , 1995 .

[36]  K. Bencala,et al.  Response characteristics of DOC flushing in an alpine catchment , 1997 .

[37]  Doerthe Tetzlaff,et al.  Runoff processes, stream water residence times and controlling landscape characteristics in a mesoscale catchment: An initial evaluation , 2006 .

[38]  J. Sharp,et al.  On the relationship between river-basin geomorphology, aquifer hydraulics, and ground-water flow direction in alluvial aquifers , 1992 .

[39]  J. Seibert,et al.  A new triangular multiple flow direction algorithm for computing upslope areas from gridded digital elevation models , 2007 .

[40]  Shoji Noguchi,et al.  Stormflow generation in steep forested headwaters: a linked hydrogeomorphic paradigm , 2000 .

[41]  Jeffrey J. McDonnell,et al.  Effect of Catchment‐Scale Subsurface Mixing on Stream Isotopic Response , 1991 .

[42]  James M. Buttle,et al.  Hydrologic coupling of slopes, riparian zones and streams: an example from the Canadian Shield , 2004 .

[43]  Mark Ross,et al.  Calibration of Base Flow Separation Methods with Streamflow Conductivity , 2007, Ground water.

[44]  M. Sivapalan,et al.  Hydrological connectivity of upland-riparian zones in agricultural catchments: Implications for runoff generation and nitrate transport , 2006 .

[45]  Malcolm G. Anderson,et al.  The role of topography in controlling throughflow generation , 1978 .

[46]  J. Welker,et al.  The role of topography on catchment‐scale water residence time , 2005 .

[47]  D. Correll,et al.  Nutrient dynamics in an agricultural watershed: Observations on the role of a riparian forest , 1984 .

[48]  Yuichi Onda,et al.  Are headwaters just the sum of hillslopes? , 2005 .

[49]  W. Schlesinger Biogeochemistry: An Analysis of Global Change , 1991 .

[50]  Jeffrey J. McDonnell,et al.  Quantifying the relative contributions of riparian and hillslope zones to catchment runoff , 2003 .

[51]  H. Laudon,et al.  Hydrograph separation using stable isotopes, silica and electrical conductivity: an alpine example , 1997 .

[52]  B. McGlynn,et al.  Variable flushing mechanisms and landscape structure control stream DOC export during snowmelt in a set of nested catchments , 2010 .

[53]  D. Weyman,et al.  THROUGHFLOW ON HILLSLOPES AND ITS RELATION TO THE STREAM HYDROGRAPH , 1970 .

[54]  Michael N. Gooseff,et al.  Hydrologic connectivity between landscapes and streams: Transferring reach‐ and plot‐scale understanding to the catchment scale , 2009 .

[55]  P. Vidon,et al.  Frontiers in riparian zone research in the 21st century , 2008 .

[56]  A. Hill 3 – Stream Chemistry and Riparian Zones , 2000 .

[57]  D. Wolock,et al.  Effects of basin size on low‐flow stream chemistry and subsurface contact time in the Neversink River watershed, New York , 1997 .

[58]  M. Brinson Changes in the functioning of wetlands along environmental gradients , 1993, Wetlands.

[59]  Laura R. Skubal,et al.  Integrated Environmental Modeling: Pollutant Transport, Fate, and Risk in the Environment , 2005 .

[60]  Daniel Caissie,et al.  Variation in stream water chemistry and hydrograph separation in a small drainage basin , 1996 .

[61]  Alan R. Hill,et al.  Nitrate Removal in Stream Riparian Zones , 1996 .

[62]  Mitchell W. Reynolds,et al.  Geology of Tenderfoot Creek Experimental Forest Little Belt Mountains, Meagher County, Montana , 1975 .

[63]  Patrick J. Mulholland,et al.  Regulation of nutrient concentrations in a temperate forest stream: Roles of upland, riparian, and instream processes , 1992 .

[64]  J. McDonnell,et al.  Topographic controls on the chemistry of subsurface stormflow , 2001 .

[65]  Keith Beven,et al.  Riparian control of stream-water chemistry: Implications for hydrochemical basin models , 1998 .

[66]  Brian L. McGlynn,et al.  Calculating terrain indices along streams: A new method for separating stream sides , 2010 .

[67]  Alan R. Hill,et al.  Denitrification and patterns of electron donors and acceptors in eight riparian zones with contrasting hydrogeology , 2004 .

[68]  A. Hill,et al.  Influence of stream bank seepage during low‐flow conditions on riparian zone hydrology , 2006 .