Rhizospheric methane oxidation determined via the methyl fluoride inhibition technique

Abstract

Methane oxidation rates in the rhizosphere of aquatic macrophytes were quantified by development of a technique employing a recently described inhibitor of methane oxidation, methyl fluoride. Unlike other inhibitors, methyl fluoride appears to be nontoxic to the plants, allowing them to act as natural conduits, transporting the inhibitor from the headspace to the rhizosphere. Increases in methane emissions were recorded after closed chamber methyl fluoride incubations, primarily in greenhouse (Pontederia cordata and Sagittaria landfolia) experiments with some preliminary outdoor and field (Oryza sativa and Typha latifolia) data. Comparison of emissions before and after incubation indicated oxidation of 23 to 90% of the methane produced (defined as CH4 emission in the absence of oxidation) in greenhouse studies and 10 to 47% in field and outdoor studies. A comparison of 1.5 and 3.0% methyl fluoride chamber headspace incubations as well as initial dose response data indicated that the lower concentration was sufficient to obtain inhibition of methane oxidation in the greenhouse studies without significantly affecting methanogenesis. Inhibition was possible with one 16‐ to 18‐hour incubation period. Methyl fluoride within the rhizosphere disappeared after approximately 1 week due to plant ventilation and possible bacterial uptake.