1998
DOI: 10.1016/s0304-3770(98)00071-0
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Growth and root oxygen release by Typha latifolia and its effects on sediment methanogenesis

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Cited by 116 publications
(54 citation statements)
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References 31 publications
(44 reference statements)
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“…Collectively, these data suggest that Peltandra was a weak source of both electron donor and acceptor compounds to the soil compared to the other species. This observation and the fact that CH 4 production was not correlated to plant production within any of the four species (only across species) suggests there are species-specific exceptions to the widely-held view that CH 4 emissions (and by implication CH 4 production) increase with plant production (Whiting and Chanton,1993;Jespersen et al,1998;Updegraff et al, 2001;Vann and Megonigal, 2003;Kankaala et al, 2005).…”
Section: Discussionmentioning
confidence: 91%
“…Collectively, these data suggest that Peltandra was a weak source of both electron donor and acceptor compounds to the soil compared to the other species. This observation and the fact that CH 4 production was not correlated to plant production within any of the four species (only across species) suggests there are species-specific exceptions to the widely-held view that CH 4 emissions (and by implication CH 4 production) increase with plant production (Whiting and Chanton,1993;Jespersen et al,1998;Updegraff et al, 2001;Vann and Megonigal, 2003;Kankaala et al, 2005).…”
Section: Discussionmentioning
confidence: 91%
“…Many studies have investigated oxygen transport from aquatic plants into wetlands (e.g. MOORHEAD and REDDY, 1988, JACKSON and ARMSTRONG 1999, JESPERSEN et al, 1998. CALLAWAY and KING (1996) found Typha raised soil oxygen in wetlands by 2-4 mg l -1 at 11-12°C, compared to the near anoxic conditions without it.…”
Section: Discussionmentioning
confidence: 99%
“…The water supply from the constant head tanks entered the drainage layer of the buckets, and although the redox potentials were not significantly higher in the vegetated inundated sediments, the rates of methanogenesis were significantly lower there compared to the unvegetated sediment. The high oxygen demand of the sediments could mask the effect of oxidants from supply of water and root oxygen release, so that a significant reduction in methanogenesis rates could be observed without any significant increase in measured redox potentials (Jespersen et al, 1998).…”
Section: Discussionmentioning
confidence: 99%