The release of dissolved organic carbon (DOC) into drainage waters was modelled using the hydrology of the Birkenes model of stream water chemistry and estimated parameters for the formation and decay of soluble organic matter in the soil. The model was first tested against soil water DOC concentrat
The relationship between dissolved organic carbon in stream water and soil organic carbon pools at different spatial scales
โ Scribed by J. A. Aitkenhead; D. Hope; M. F. Billett
- Publisher
- John Wiley and Sons
- Year
- 1999
- Tongue
- English
- Weight
- 298 KB
- Volume
- 13
- Category
- Article
- ISSN
- 0885-6087
No coin nor oath required. For personal study only.
โฆ Synopsis
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-(55 km 2 ), medium-(12ยฑ38 km 2 ) and large-scale (56ยฑ150 km 2 ) 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 (5700 m) catchments had higher DOC concentrations than those draining upland (4700 m) catchments, suggesting that disturbance and land use may have a small eect 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 suciently robust to be used to predict the eects of changes in catchment soil C storage on stream water DOC concentration.
๐ SIMILAR VOLUMES
## Abstract To detect the causal relationship between cave drip waters and stalagmite laminae, which have been used as a climate change proxy, three drip sites in Beijing Shihua Cave were monitored for discharge and dissolved organic carbon (DOC). Drip discharges and DOC were determined at 0 to 14โ