Soil characteristics and landcover relationships on soil hydraulic conductivity at a hillslope scale: A view towards local flood management

JOURNAL OF HYDROLOGY

卷:497

Article

Archer, N. A. L.^1,2  Bonell, M.¹  Coles, N.³  MacDonald, A. M.²  Auton, C. A.²  Stevenson, R.¹ 

[1] Univ Dundee, IHP HELP Ctr Water Law Policy & Sci, Auspices UNESCO, Dundee DD1 4HN, Scotland

[2] British Geol Survey, Edinburgh EH9 3LA, Midlothian, Scotland

[3] Univ Western Australia, Ctr Ecohydrol, Nedlands, WA 6009, Australia

关键词: Soil hydraulic conductivity;    Overland flow;    Infiltration;    Flood management;    Landcover;   

DOI  :  10.1016/j.jhydrol.2013.05.043

来源: Elsevier

【 摘 要 】

There are surprisingly few studies in humid temperate forests which provide reliable evidence that soil permeability is enhanced under forests. This work addresses this research gap through a detailed investigation of permeability on a hillslope in the Eddleston Catchment, Scottish Borders UK, to evaluate the impact of land cover, superficial geology and soil types on permeability using measurements of field saturated hydraulic conductivity (K-fs) supported by detailed topsoil profile descriptions and counting of roots with diameters >2 mm. K-fs was measured at depth 0.04-0.15 m using a constant head well permeameter across four paired landcover sites of adjacent tree and intensely grazed grassland. The measured tree types were: 500-year-old mixed woodland; 180-year-old mixed woodland; 45-year-old Pinus sylvestris plantation; and 180-year-old Salix caprea woodland. The respective paired grids of trees and grassland were compared on similar soil texture and topography. This study highlights the significant impact of broadleaf woodland at a hillslope scale on K-fs in comparison to grassland areas: median K-fs values under 180-year-old S. caprea woodland (8 mm h(-1)), 180-year-old mixed woodland (119 mm h(-1)) and 500-year-old broadleaf woodland (174 mm h(-1)) were found to be respectively 8, 6 and 5 times higher than neighbouring grazed grassland areas on the same superficial geology. Further statistical analysis indicates that such K-fs enhancement is associated with the presence of coarse roots (>2 mm diameter) creating conduits for preferential flow and a deeper organic layer in the topsoil profile under woodlands. By contrast the P. sylvestris forest had only slightly higher (42 mm h(-1)), but not statistically different K-fs values, when compared to adjacent pasture (35 mm h(-1)). In the grassland areas, in the absence of course roots, the superficial geology was dominant in accounting for differences in 4, with the alluvium floodplain having a significantly lower median K-fs (1 mm h(-1)) than surrounding hillslope sites, which had a range of median K-fs from 21 to 39 mm h(-1). The data were used to infer areas of runoff generation by comparing K-fs values with modelled 15 min maximum intensity duration rainfall with a 1 in 10 year return period. Infiltration prevailed in the 180- and 500-year-old mixed and broadleaf woodland, whereas some grassland areas and the floodplain were inferred to generate overland flow. The significantly higher K-fs under broadleaf mature forests suggests that planting broadleaf woodlands on hillslopes in clusters or as shelterbelts within grasslands would provide areas of increased capacity for rainfall infiltration and arrest runoff generation during flood-producing storm events. (C) 2013 Elsevier B.V. All rights reserved.

【 授权许可】

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