The effect of soil acidification on atmospheric methane uptake by a Maine forest soil(1).

Abstract:

:Soil from the zone of maximal methanotrophic activity (approximately 5-8 cm depth) in a mixed coniferous-hardwood forest consumed atmospheric methane over a wide pH range (3.5-7.5) with a broad optimum between 4.8 and 6.0. Methane uptake at native soil pH values (4.4-4.8) was only slightly less rapid than rates at optimal pH values. Addition of mineral acids to intact soil cores in pulsed applications decreased atmospheric methane consumption. The extent of inhibition varied with the type, concentration and volume of acid added: nitric acid was more inhibitory than sulfuric acid at an equivalent soil pH, and methane uptake decreased with increasing volumes and concentrations of added acid. Although ammonium chloride at 1 µmol g fresh weight (gfw) soil(-1) inhibited methane uptake, the extent of inhibition did not vary significantly with decreasing soil pH below values of 4.4.

journal_name

FEMS Microbiol Ecol

authors

Benstead J,King GM

doi

10.1111/j.1574-6941.2001.tb00771.x

subject

Has Abstract

pub_date

2001-01-01 00:00:00

pages

207-212

issue

3

eissn

0168-6496

issn

1574-6941

pii

S0168649600000969

journal_volume

34

pub_type

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