An empirical map of critical loads of acidity for soils in Great Britain
Identifieur interne : 001730 ( Main/Exploration ); précédent : 001729; suivant : 001731An empirical map of critical loads of acidity for soils in Great Britain
Auteurs : M. Hornung [Royaume-Uni] ; K. R. Bull [Royaume-Uni] ; M. Cresser [Royaume-Uni] ; J. Hall [Royaume-Uni] ; S. J. Langan [Royaume-Uni] ; P. Loveland [Royaume-Uni] ; C. Smith [Royaume-Uni, Nouvelle-Zélande]Source :
- Environmental Pollution [ 0269-7491 ] ; 1995.
Abstract
The method used to produce a critical load map of acidity for soils in Great Britain is described. Critical loads were assigned to the dominant soil in each 1 km grid square of the UK national grid. Mineral soils were assigned a critical load based on mineralogy and chemistry, using approaches appropriate to UK conditions. Critical loads for peat soils are based primarily on a maximum acceptable reduction of peat pH, and results from laboratory equilibration studies. The map shows that soils with small critical loads (<0.5 kmolc ha−1 year−1) i.e. highly sensitive to acidic deposition, dominate in the north and west of Britain; the south and east are dominated by soils with large critical loads, with small areas of more sensitive soils associated with sandy soil-forming materials. A modified critical load map illustrates the potential impact of agricultural liming on soil critical loads.
Url:
DOI: 10.1016/0269-7491(95)00026-N
Affiliations:
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<front><div type="abstract" xml:lang="en">The method used to produce a critical load map of acidity for soils in Great Britain is described. Critical loads were assigned to the dominant soil in each 1 km grid square of the UK national grid. Mineral soils were assigned a critical load based on mineralogy and chemistry, using approaches appropriate to UK conditions. Critical loads for peat soils are based primarily on a maximum acceptable reduction of peat pH, and results from laboratory equilibration studies. The map shows that soils with small critical loads (<0.5 kmolc ha−1 year−1) i.e. highly sensitive to acidic deposition, dominate in the north and west of Britain; the south and east are dominated by soils with large critical loads, with small areas of more sensitive soils associated with sandy soil-forming materials. A modified critical load map illustrates the potential impact of agricultural liming on soil critical loads.</div>
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