S-35-sulphate reduction and transformation in peat

Citation
Sj. Chapman et Ms. Davidson, S-35-sulphate reduction and transformation in peat, SOIL BIOL B, 33(4-5), 2001, pp. 593-602
Citations number
39
Categorie Soggetti
Environment/Ecology
Journal title
SOIL BIOLOGY & BIOCHEMISTRY
ISSN journal
00380717 → ACNP
Volume
33
Issue
4-5
Year of publication
2001
Pages
593 - 602
Database
ISI
SICI code
0038-0717(200104)33:4-5<593:SRATIP>2.0.ZU;2-M
Abstract
The incorporation of S-35-labelled sulphate into reduced inorganic forms an d into organic S has been studied in pear samples from two contrasting site s, a deep blanket pear and a shallow hill blanket pest. During anaerobic in cubation, S-35 was rapidly incorporated into AVS (acid volatile sulphide), elemental S and Cr-reducible S but these pools showed evidence of rapid rec ycling, In the longer term, S-35 was found in the ester sulphate pool and i n a residual S pool, taken to be principally C-bonded organic S. Incorporat ion 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 s urface (0-10 cm) peat. Incorporation in the hill peat under aerobic incubat ion into either reduced inorganic or organic forms was very limited. Mean s ulphate 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 h ill peats, respectively. (C) 2001 Elsevier Science Ltd. All rights reserved .