Consequences of Microbial Pyrite Oxidation in Acid Sulfate Soils
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概要
- 論文の詳細を見る
Thai (Munoh and Kab Daeng), Japanese (Tomikura and Sagata) and Ghanaian (Ada) soils were analyzed for iron and sulfur bacteria to study their contribution to the formation of acidity in these soils. Acid sulfate potentiality was also tested for the soils (Sagata and Ada). High numbers of iron bacteria (> 10^6) and sulfur bacteria (> 10^5) were found in Tomikura and Kab Daeng soils, respectively. In addition to the high iron and sulfur bacterial numbers, these soils have high sulfate contents and high acidity (<pH 4). These properties qualify them as acid sulfate soils. In addition, Kab Daeng soil has high organic matter content and is regarded as a peat/acid sulfate soil. Munoh soil has also been classified as an acid sulfate soil since it also shows the presence of enough iron and sulfur bacteria coupled with low pH. Sagata soil has been classified as a typical potential acid sulfate soil because its pH drops sharply from 5.44 to 3.21 within 30 days of incubation. Ada soil is regarded as neither an acid sulfate soil nor a potential one, since it requires as long as 60 days for its pH to drop from 5.46 to 4.65.
- 日本微生物生態学会の論文
- 1993-05-31
著者
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Nonaka Masanori
The Graduate School of Science and Technology Faculty of Science, Niigata University
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Nonaka M
Niigata Univ. Niigata Jpn
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Nonaka Masanori
Faculty Of Agriculture Niigata University
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Kamura Takao
Faculty Of Agriculture Nagoya University
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SALLAH NICHOLAS
Faculty of Agriculture, Niigata University
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Sallah Nicholas
Faculty Of Agriculture Niigata University
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