Using long-term data sets to understand transit times in contrasting headwater catchments

被引:120
作者
Hrachowitz, M. [1 ]
Soulsby, C. [1 ]
Tetzlaff, D. [1 ]
Dawson, J. J. C. [1 ]
Dunn, S. M. [2 ]
Malcolm, I. A. [3 ]
机构
[1] Univ Aberdeen, Sch Geosci, Aberdeen AB24 3UF, Scotland
[2] Macaulay Land Use Res Inst, Aberdeen AB15 8QH, Scotland
[3] FRS Freshwater Lab, Pitlochry PH16 5LB, Perth, Scotland
关键词
Runoff processes; Transit times; Tracers; Chloride; Spectral analysis; 1/f; WATER RESIDENCE TIMES; STABLE-ISOTOPE TRACERS; SMALL UPLAND CATCHMENT; HYDROGRAPH SEPARATION; HYDROLOGICAL PATHWAYS; STREAM WATER; CONTAMINANT TRANSPORT; ENVIRONMENTAL-CHANGE; MESOSCALE CATCHMENT; RUNOFF PROCESSES;
D O I
10.1016/j.jhydrol.2009.01.001
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Long-term tracer data collected over an 8 year period were analyzed to explore the transit times of two small (similar to 1 km(2)), contrasting headwater catchments in the uplands of Scotland. At Loch Ard, the catchment was characterized by low permeability gleyed soils overlying metamorphic geology. At Sourhope, more freely draining podzolic soils were dominant, which mantled fractured and faulted volcanic rocks. Hydrometric data and chemically-based hydrograph separations indicated that Loch Ard was a flashy catchment dominated by runoff processes in the upper soil horizons. In contrast, around 77% of annual flow at Sourhope was sustained by well-buffered groundwater sources. Weekly Cl- time series in precipitation and stream flow revealed similar variability in inputs at both sites, but much greater damping in outputs at Sourhope. Despite this, both catchments filtered white noise frequencies in precipitation inputs into I If outputs. These input-output relationships were modeled with a range of transit time distributions (TTD). At the responsive Loch Ard catchment, mean transit times (MTT) for the study period were estimated at 135-202 days. Models based on a gamma distribution or two parallel linear reservoirs were best able to capture the short- and long-term fluctuations in stream water in response to input variations. At Sourhope, the highly damped tracer signal in stream waters was poorly captured by all the TTDs used. Resulting MTT estimates of 1830-1970 days are based on weak model fits and poorly identifiable parameter sets, indicating that natural tracers such as Cl- are inadequate for catchments where MTTs are greater than a few years. At both sites, estimates of MTT using moving windows over the 8 year data sets revealed sensitivity to precipitation amounts and the length of monitoring period. It is concluded that time series of around 4 years are required to adequately constrain MTT estimates. (C) 2009 Elsevier B.V. All rights reserved.
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页码:237 / 248
页数:12
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