期刊
SOIL BIOLOGY & BIOCHEMISTRY
卷 40, 期 5, 页码 1149-1154出版社
PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.soilbio.2007.12.007
关键词
hydrogen consumption; tritium exchange; abiontic soil enzyme; kinetic parameter; pH optimum; temperature optimum
类别
Soils are the largest sink of atmospheric hydrogen contributing about 75% to the total budget. Atmospheric H, is assumed to be oxidized in soil by abiontic soil hydrogenases. Extraction of a forest soil with a slightly alkaline (pH 8.5) buffer containing polyethylene glycol (PEG), followed by filtration yielded a bacteria-free extract that oxidized H-2 at ambient concentrations (0.2-2.0 ppmv). Hydrogenase activity was assayed by gas chromatographic analysis of H-2 consumption and by conversion of H-3(2) to tritiated water. Only less than 2% of the original activity was recovered in the extract. Kinetic analysis nevertheless resulted in a biphasic kinetics exhibiting two K-m and V-max values that were similar to those detected in the original soil. In addition, activities of both original soil and soil extract showed similar optima at pH 4-6 and at 30 degrees C, indicating that representative fractions of soil hydrogenases were recovered in the extract. Precipitation with PEG or ultrafiltration allowed further purification of the activity, albeit only about 20% of that in the crude extract could be recovered in the precipitate or the fraction > 100 kDa. (C) 2007 Elsevier Ltd. All rights reserved.
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