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Effects of lime applications to parts of an upland catchment on soil properties and the chemistry of drainage waters
Author(s) -
ADAMS W. A.,
EVANS G. M.
Publication year - 1989
Publication title -
journal of soil science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.244
H-Index - 111
eISSN - 1365-2389
pISSN - 0022-4588
DOI - 10.1111/j.1365-2389.1989.tb01300.x
Subject(s) - soil water , lime , drainage , drainage basin , soil ph , chemistry , leachate , environmental chemistry , soil acidification , soil science , environmental science , hydrology (agriculture) , geology , ecology , biology , paleontology , cartography , geography , geotechnical engineering
SUMMARY The liming of soils in the lower part of an upland catchment was found to have a major effect on both soil properties and the chemistry of drainage waters. Exchangeable Al was closely correlated with soil pH and showed a very steep rise from 2.6‐4.8 meq 1 −1 over the pH range 5.5‐4.5. As streams flowed from unimproved through improved land there was an increase in pH and the concentration of all major anions and basic cations. The greatest increase was in Ca (approximately 3.5‐fold). The concentrations of all dissolved Al species decreased, with inorganic monomeric Al falling to near zero. Leachates were examined from soils representative of the most acidic and the least acidic. Calcium concentrations differed by almost tenfold. Aluminium was present in leachates from the limed soil, but most was unreactive and none was inorganic monomeric. Most of the Al leached from the acid soil was monomeric. A model of soil acidification is proposed in which soil Ca is depleted at a rate of 8% of the exchangeable Ca per annum. The model predicts that liming a soil to neutrality would be likely to influence drainage water chemistry for 30‐40 years and that the most acidic soils of the catchment show no net loss of Ca to drainage.