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A critical examination of some common field tests to assess the acid‐sulphate condition in soils
Author(s) -
VegasVilarrúbia T.,
Baritto F.,
Meleán G.
Publication year - 2008
Publication title -
soil use and management
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.709
H-Index - 81
eISSN - 1475-2743
pISSN - 0266-0032
DOI - 10.1111/j.1475-2743.2007.00134.x
Subject(s) - pyrite , histosol , environmental chemistry , chemistry , soil water , hydrogen peroxide , organic matter , entisol , soil ph , inorganic chemistry , mineralogy , soil organic matter , soil science , environmental science , organic chemistry , soil biodiversity
Acid‐sulphate soils are of major environmental concern in many wetlands. Severe acidification episodes have occurred worldwide because of the oxidation of iron sulphides to sulphuric acid by human activities, and diverse techniques have been set up to determine the presence of acid‐sulphate soils. This paper evaluates the usefulness of four common easy‐to‐apply field survey tests for potential acid‐sulphate diagnosis in some Histosols and Entisols in wetlands: incomplete oxidation by fast air‐drying, incubation, fast oxidation with hydrogen peroxide, and the indirect determination of sulphide with lead acetate. Samples of 227 surface‐organic and underlying mineral soils of poorly drained Histosols and Entisols of the Orinoco river delta plain were tested. Results showed that for highly organic samples the interpretation of results obtained from the acid‐sulphate soil tests may be misleading, because they cannot be unambiguously related to the production of sulphuric acid derived from pyrite oxidation. Mineral samples yielded more reliable results. The incomplete oxidation by fast air‐drying test did not induce significant acidification either in organic or in mineral samples; the final pH values were dependent on the original pH values. The fast oxidation with hydrogen peroxide test was effective with mineral samples. During the incubation test, the slower rate of pH decrease and the final values obtained with the organic samples suggested retardation in the rate and amount of acid generation by pyrite oxidation because of the concurrent oxygen consumption by organic matter and bacterial activity. The indirect determination of sulphide with lead acetate yielded only qualitative results in organic samples, but worked well in mineral samples, indicating a higher content of pyrite intermediates. Effective estimation of the actual presence and potential for acidification of soil is important, in order to avoid excessive or inappropriate amelioration techniques to prevent acid production.