4.7 Article

35S-sulphate reduction and transformation in peat

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SOIL BIOLOGY & BIOCHEMISTRY
卷 33, 期 4-5, 页码 593-602

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PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/S0038-0717(00)00201-7

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organic S; peat; S cycle; sulphate reduction; sulphide

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The incorporation of S-35-labelled sulphate into reduced inorganic forms and into organic S has been studied in pear samples from two contrasting sites, a deep blanket pear and a shallow hill blanket pest. During anaerobic incubation, S-35 was rapidly incorporated into AVS (acid volatile sulphide), elemental S and Cr-reducible S but these pools showed evidence of rapid recycling, In the longer term, S-35 was found in the ester sulphate pool and in a residual S pool, taken to be principally C-bonded organic S. Incorporation was more rapid in the deep pear than in the hill peat, in peat from wet areas more than dry areas and in subsurface (10-20 cm) peat more than in surface (0-10 cm) peat. Incorporation in the hill peat under aerobic incubation into either reduced inorganic or organic forms was very limited. Mean sulphate reduction rates at the temperature of incubation (26 degreesC) were estimated to be in the range 60-12,000 mug S kg(-1) wet weight peat d(-1) while mean turnover times of reduced S were 17 and 550 d for the deep and hill peats, respectively. (C) 2001 Elsevier Science Ltd. All rights reserved.

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