Sediment sources in the Upper Severn catchment: a fingerprinting approach

被引:67
作者
Collins, A. L. [1 ]
Walling, D. E. [1 ]
Leeks, G. J. L. [2 ]
机构
[1] Univ Exeter, Dept Geog, Exeter EX4 4RJ, Devon, England
[2] Inst Hydrol, Wallingford OX10 8BB, Oxon, England
基金
英国自然环境研究理事会;
关键词
D O I
10.5194/hess-1-509-1997
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Suspended sediment sources in the Upper Severn catchment are quantified using a composite fingerprinting technique combining statistically-verified signatures with a multivariate mixing model. Composite fingerprints are developed from a suite of diagnostic properties comprising trace metal (Fe, Mn, Al), heavy metal (Cu, Zn, Pb, Cr, Co, Ni), base cation (Na, Mg, Ca, K), organic (C, N), radiometric (Cs-137, Pb-210), and other (total P) determinands. A numerical mixing model, to compare the fingerprints of contemporary catchment source materials with those of fluvial suspended sediment in transit and those of recent overbank floodplain deposits, provides a means of quantifying present and past sediment sources respectively. Sources are classified in terms of eroding surface soils under different land uses and channel banks. Eroding surface soils are the most important source of the contemporary suspended sediment loads sampled at the Institute of Hydrology flow gauging stations at Plynlimon and at Abermule. The erosion of forest soils, associated with the autumn and winter commercial activities of the Forestry Commission, is particularly evident. Reconstruction of sediment provenance over the recent past using a sediment core from the active river floodplain at Abermule, in conjunction with a Cs-137 chronology, demonstrates the significance of recent phases of afforestation and deforestation for accelerated catchment soil erosion.
引用
收藏
页码:509 / 521
页数:13
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