Hydrological Processes · 1999 · 257 citations · 40 references
AgricultureEarth SciencesHydrologySoil Carbon DynamicsSoil Organic MatterSoil-water RelationsCarbon CycleDissolved Organic Carbon DynamicsOrganic Matter AccumulationSoil Carbon ChemistrySoil-water BalanceDissolved Organic Carbon CompositionDissolved Organic Carbon CyclingDissolved Organic Carbon FateDissolved Organic Carbon TransportSoil Carbon PoolsSoil Dissolved Organic CarbonSoil Organic CarbonSoil Organic Carbon Pools
The relationship between stream water DOC concentrations and soil organic C pools was investigated at a range of spatial scales in subcatchments of the River Dee system in north-east Scotland. Catchment percentage peat cover and soil C pools, calculated using local, national and international soils databases, were related to mean DOC concentrations in streams draining small- (<5 km2), medium- (12–38 km2) and large-scale (56–150 km2) catchments. The results show that, whilst soil C pool is a good predictor of stream water DOC concentration at all three scales, the strongest relationships were found in the small-scale catchments. In addition, in both the small- and large-scale catchments, percentage peat cover was as a good predictor of stream water DOC concentration as catchment soil C pool. The data also showed that, for a given soil C pool, streams draining lowland (<700 m) catchments had higher DOC concentrations than those draining upland (>700 m) catchments, suggesting that disturbance and land use may have a small effect on DOC concentration. Our results therefore suggest that the relationship between stream water DOC concentration and catchment soil C pools exists at a range of spatial scales and this relationship appears to be sufficiently robust to be used to predict the effects of changes in catchment soil C storage on stream water DOC concentration. Copyright © 1999 John Wiley & Sons, Ltd.
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