Using lumped conceptual rainfall-runoff models to simulate daily isotope variability with fractionation in a nested mesoscale catchment

被引:37
作者
Birkel, Christian [1 ,2 ]
Tetzlaff, Doerthe [1 ]
Dunn, Sarah M. [2 ]
Soulsby, Chris [1 ]
机构
[1] Univ Aberdeen, No Rivers Inst, Sch Geosci, Aberdeen AB24 3UF, Scotland
[2] Macaulay Land Use Res Inst, Aberdeen AB15 8QH, Scotland
关键词
Stable isotopes; Conceptual models; Fractionation; Spatial scale; Hydrological processes; STORM RUNOFF; TRANSIT-TIME; WATER; UNCERTAINTY; TRANSPORT; FUTURE; DEUTERIUM; TRACERS; PRECIPITATION; GROUNDWATER;
D O I
10.1016/j.advwatres.2010.12.006
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
This paper presents 19 months of stable isotope (delta H-2 and delta O-18) data to enhance understanding of water and solute transport at two spatial scales (2.3 km(2) and 122 km(2)) in the agricultural Lunan catchment, Scotland. Daily precipitation and stream isotope data, weekly lake and spring isotope data and monthly groundwater isotope data revealed important insights into flow pathways and mixing of water at both scales. In particular, a deeper groundwater flow path significantly contributes to total streamflow (25-50%). Upstream lake isotope dynamics, susceptible to evaporative fractionation, also appeared to have an important influence on the downstream isotope composition. This unique tracer data set facilitated the conceptualization of a lumped catchment-scale flow-tracer model. The incorporation of hydrological, mixing and fractionation processes based on these data improved simulations of the stream delta H-2 isotope response at the catchment outlet from 0.37 to 0.56 for the Nash-Sutcliffe statistic. The stable isotope data successfully aided model conceptualization and calibration in the quest for a simple water and solute transport model with improved representation of process dynamics. (C) 2010 Elsevier Ltd. All rights reserved.
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页码:383 / 394
页数:12
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