subject predicate object context
3917 Creator 9afccdbe975e25965953e777bb4d6a5f
3917 Creator a83b960ddf2843a8567430721dcd0f08
3917 Creator ext-c5ffe9f653998e566500b79f6dbf8603
3917 Date 2005
3917 Is Part Of repository
3917 Is Part Of p00948276
3917 abstract Wetlands are a potent source of the radiatively important gas methane (CH4). Recent findings have demonstrated that sulfate (SO4 2−) deposition via acid rain suppresses CH4 emissions by stimulating competitive exclusion of methanogens by sulfate-reducing microbial populations. Here we report data from a field experiment showing that a finite pulse of simulated acid rain SO4 2− deposition, as would be expected from a large Icelandic volcanic eruption, continues to suppress CH4 emissions from wetlands long after the pollution event has ceased. Our analysis of the stoichiometries suggests that 5 years is a minimum CH4 emission recovery period, with 10 years being a reasonable upper limit. Our findings highlight the long-term impact of acid rain on biospheric output of CH4 which, for discrete polluting events such as volcanic eruptions, outlives the relatively short-term SO4 2− aerosol radiative cooling effect.
3917 authorList authors
3917 issue L12804
3917 status peerReviewed
3917 volume 32
3917 type AcademicArticle
3917 type Article
3917 label Gauci, Vincent ; Dise, Nancy and Blake, Stephen (2005). Long-term suppression of wetland methane flux following a pulse of simulated acid rain. Geophysical Research Letters, 32(L12804)
3917 label Gauci, Vincent ; Dise, Nancy and Blake, Stephen (2005). Long-term suppression of wetland methane flux following a pulse of simulated acid rain. Geophysical Research Letters, 32(L12804)
3917 Title Long-term suppression of wetland methane flux following a pulse of simulated acid rain
3917 in dataset oro