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DOI10.5194/hess-23-5199-2019
Spatial and temporal variation in river corridor exchange across a 5th-order mountain stream network
Ward A.S.; Wondzell S.M.; Schmadel N.M.; Herzog S.; Zarnetske J.P.; Baranov V.; Blaen P.J.; Brekenfeld N.; Chu R.; Derelle R.; Drummond J.; Fleckenstein J.H.; Garayburu-Caruso V.; Graham E.; Hannah D.; Harman C.J.; Hixson J.; Knapp J.L.A.; Krause S.; Kurz M.J.; Lewandowski J.; Li A.; Martí E.; Miller M.; Milner A.M.; Neil K.; Orsini L.; Packman A.I.; Plont S.; Renteria L.; Roche K.; Royer T.; Segura C.; Stegen J.; Toyoda J.; Wells J.; Wisnoski N.I.
发表日期2019
ISSN1027-5606
起始页码5199
结束页码5225
卷号23期号:12
英文摘要Although most field and modeling studies of river corridor exchange have been conducted at scales ranging from tens to hundreds of meters, results of these studies are used to predict their ecological and hydrological influences at the scale of river networks. Further complicating prediction, exchanges are expected to vary with hydrologic forcing and the local geomorphic setting. While we desire predictive power, we lack a complete spatiotemporal relationship relating discharge to the variation in geologic setting and hydrologic forcing that is expected across a river basin. Indeed, the conceptual model ofWondzell (2011) predicts systematic variation in river corridor exchange as a function of (1) variation in baseflow over time at a fixed location, (2) variation in discharge with location in the river network, and (3) local geomorphic setting. To test this conceptual model we conducted more than 60 solute tracer studies including a synoptic campaign in the 5th-order river network of the H. J. Andrews Experimental Forest (Oregon, USA) and replicate-intime experiments in four watersheds. We interpret the data using a series of metrics describing river corridor exchange and solute transport, testing for consistent direction and magnitude of relationships relating these metrics to discharge and local geomorphic setting. We confirmed systematic decrease in river corridor exchange space through the river networks, from headwaters to the larger main stem. However, we did not find systematic variation with changes in discharge through time or with local geomorphic setting. While interpretation of our results is complicated by problems with the analytical methods, the results are sufficiently robust for us to conclude that space-for-time and time-for-space substitutions are not appropriate in our study system. Finally, we suggest two strategies that will improve the interpretability of tracer test results and help the hyporheic community develop robust datasets that will enable comparisons across multiple sites and/or discharge conditions. © Author(s) 2019.
语种英语
scopus关键词Solute transport; Watersheds; Analytical method; Discharge conditions; Field and model studies; Geologic settings; Predictive power; Spatial and temporal variation; Spatio-temporal relationships; Systematic variation; Rivers; baseflow; hyporheic zone; mountain stream; river discharge; solute; spatial variation; temporal variation; tracer; water exchange; Oregon; United States
来源期刊Hydrology and Earth System Sciences
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/159538
作者单位Ward, A.S., O'Neill School of Public and Environmental Affairs, Indiana University, Bloomington, IN, United States; Wondzell, S.M., USDA Forest Service, Pacific Northwest Research Station, Corvallis, OR, United States; Schmadel, N.M., O'Neill School of Public and Environmental Affairs, Indiana University, Bloomington, IN, United States, USGS Earth Surface Processes Division, U.S. Geological Survey, Reston, VA, United States; Herzog, S., O'Neill School of Public and Environmental Affairs, Indiana University, Bloomington, IN, United States; Zarnetske, J.P., Department of Earth and Environmental Sciences, Michigan State University, East Lansing, MI, United States; Baranov, V., LMU Munich Biocenter, Department of Biology II, Großhaderner Str. 2, Planegg-Martinsried, 82152, Germany, Department of River Ecology and Conservation, Senckenberg Research Institute and Natural History Museum, Gelnhausen, 63571, Germany; Blaen, P.J., School of Geography, Earth and Environmental Sciences, University of Birmingham, Edgb...
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Ward A.S.,Wondzell S.M.,Schmadel N.M.,et al. Spatial and temporal variation in river corridor exchange across a 5th-order mountain stream network[J],2019,23(12).
APA Ward A.S..,Wondzell S.M..,Schmadel N.M..,Herzog S..,Zarnetske J.P..,...&Wisnoski N.I..(2019).Spatial and temporal variation in river corridor exchange across a 5th-order mountain stream network.Hydrology and Earth System Sciences,23(12).
MLA Ward A.S.,et al."Spatial and temporal variation in river corridor exchange across a 5th-order mountain stream network".Hydrology and Earth System Sciences 23.12(2019).
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