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Published in Soil Sci Soc Am J 53:440-444 (1989)
© 1989 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Hydrogen Sulfide Production from Cysteine (Cystine) in Soil

M. J. Morra

Dep. of Plant, Soil, and Entomological Sciences, Univ. of Idaho, Moscow, ID 83843

W. A. Dick*

Dep. of Agronomy, Ohio State Univ. and Ohio Agric. Res. and Development Ctr. (OSU/OARDC), Wooster, OH 44691

* Corresponding author.

ABSTRACT

Hydrogen sulfide (H2S) production in aerobic soils amended with cysteine (cystine) is thought to result from cystathionase {gamma}-lyase (EC 4.4.1.1) activity. This enzyme yields thiocysteine (2-amino-2-carboxylethyl hydrodisulfide), which reacts spontaneously with free sulfhydryl groups to produce H2S. Hydrogen sulfide, however, may also be produced in soil as a result of sulfate reduction. This work was conducted to evaluate the physical and chemical parameters that affect H2S production in cystine-amended soil and to test the hypothesis that sulfate reduction is involved. Hydrogen sulfide, evolved from 4 g of soil placed in a 25-mL Erlenmeyer flask, was trapped in a center well containing pleated filter paper and 0.5 mL of 1 M zinc acetate. Three soils brought to a water potential of –0.033 MPa and incubated at 37 °C with 50 µmol L-cystine evolved 2.08 to 3.62 mg H2S-S kg–1 soil 24 h–1. Maximum rate of H2S evolution occurred at 57°C. Propargylglycine (12.5 mmol kg–1 soil), a specific inhibitor of cystathionine {gamma}-lyase, reduced H2S evolution by 90 to 98%. Incubating the soils under waterlogged conditions also reduced H2S evolution in two of the three soils studied, with no change observed in the third soil. Hydrogen sulfide evolution was not affected by the addition of 12.5 mmol kg–1 soil of sulfate or nitrate, thus providing additional evidence that sulfate reduction was not involved. The apparent Michaelis constant (Km) value for H2S production from cystine in soil was 2.3 mmol kg–1 soil. It is concluded that production of H2S in soil, which is a significant reaction of the S cycle, can occur as a result of the mineralization of cysteine (cystine) via participation of the enzyme cystathionine {gamma}-lyase.


NOTES

Journal Article no. 63-88. Salaries and research support provided by the Ohio Air Quality Development Authority (OSURF 714851) and by state and federal funds appropriated to OSU/OARDC.

Received for publication March 24, 1988.





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