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Soil redox and pH effects on methane production in a flooded rice soil

Journal Article · · Soil Science Society of America Journal; (United States)
; ;  [1];  [2]
  1. Louisiana State Univ., Baton Rouge (United States)
  2. Ghent Univ. (Belgium)
Methane formation in soil is a microbiological process controlled by many factors. Of them soil redox potential (Eh) and soil pH are considered critical controls. A laboratory incubation experiment was conducted to study the critical initiation soil Eh, the optimum soil pH, and the interaction of Eh and pH on CH[sub 4] production. The critical soil Eh for initiation of CH[sub 4] production observed was approximately from [minus]150 to [minus]160 mV. Between [minus]230 and [minus]150 mV, the relationship of CH[sub 4] production and soil Eh appeared to be negatively exponential (Y = a10[sup [minus]bx], where Y is the CH[sub 4] production rate, [mu]g g[sup [minus]1] d[sup [minus]1]: x the soil Eh, mV; and a and b are constants). The optimum pH of CH[sub 4] production was near neutrality. A small decrease in pH resulting from the introduction of acidic materials significantly decreased CH[sub 4] production. A slight increase in soil pH (about 0.2 unit higher than the natural soil suspension pH), however, resulted in an enhancement of CH[sub 4] production by 11 to 20% and 24 to 25% at controlled Eh of [minus]250 and [minus]200 mV, respectively. Results suggest that a decrease in CH[sub 4] emissions could be obtained by a small reduction in soil pH in Crowley soil (fine, montmorillonitic, thermic Typic Albaqualf). 19 refs., 3 figs., 3 tabs.
OSTI ID:
6225730
Journal Information:
Soil Science Society of America Journal; (United States), Journal Name: Soil Science Society of America Journal; (United States) Vol. 57:2; ISSN 0361-5995; ISSN SSSJD4
Country of Publication:
United States
Language:
English