The Experts below are selected from a list of 234 Experts worldwide ranked by ideXlab platform

S J Deverel - One of the best experts on this subject based on the ideXlab platform.

  • Methyl halide and chloroform emissions from a subsiding sacramento san joaquin delta island converted to rice fields
    Atmospheric Environment, 2011
    Co-Authors: M A H Khan, Robert C. Rhew, M Whelan, K Zhou, S J Deverel
    Abstract:

    Net fluxes of Methyl Halides and chloroform were measured from recently converted rice fields on Twitchell Island, California, using field- and laboratory-based incubations. A stable isotope tracer method was used to demonstrate that the net emissions of CH3Cl and CH3Br during the growing season were predominantly the result of large gross production rates, with gross consumption rates being relatively minor. In agreement with prior studies, the production rates for Methyl Halides differed significantly at different rice plant growth phases. The Twitchell Island rice field, however, had production rates of CH3Cl during the growth phases that were higher than rates reported at commercial rice fields, presumably because of higher soil chloride concentrations. Laboratory soil incubations showed that the non-flooded rice field soils acted as a small net sink for CH3Cl and as small net sources for CH3Br, CH3I and CHCl3. Despite the higher CH3Cl emissions during the growing season, the overall emissions of halomethanes from the conversion of all potential islands in the San Joaquin Delta to rice paddies is predicted to be an insignificant source of halomethanes.

  • Methyl halide and chloroform emissions from a subsiding Sacramento–San Joaquin Delta island converted to rice fields
    Atmospheric Environment, 2011
    Co-Authors: M A H Khan, Robert C. Rhew, M Whelan, K Zhou, S J Deverel
    Abstract:

    Net fluxes of Methyl Halides and chloroform were measured from recently converted rice fields on Twitchell Island, California, using field- and laboratory-based incubations. A stable isotope tracer method was used to demonstrate that the net emissions of CH3Cl and CH3Br during the growing season were predominantly the result of large gross production rates, with gross consumption rates being relatively minor. In agreement with prior studies, the production rates for Methyl Halides differed significantly at different rice plant growth phases. The Twitchell Island rice field, however, had production rates of CH3Cl during the growth phases that were higher than rates reported at commercial rice fields, presumably because of higher soil chloride concentrations. Laboratory soil incubations showed that the non-flooded rice field soils acted as a small net sink for CH3Cl and as small net sources for CH3Br, CH3I and CHCl3. Despite the higher CH3Cl emissions during the growing season, the overall emissions of halomethanes from the conversion of all potential islands in the San Joaquin Delta to rice paddies is predicted to be an insignificant source of halomethanes.

Robert C. Rhew - One of the best experts on this subject based on the ideXlab platform.

  • Methyl halide and chloroform emissions from a subsiding sacramento san joaquin delta island converted to rice fields
    Atmospheric Environment, 2011
    Co-Authors: M A H Khan, Robert C. Rhew, M Whelan, K Zhou, S J Deverel
    Abstract:

    Net fluxes of Methyl Halides and chloroform were measured from recently converted rice fields on Twitchell Island, California, using field- and laboratory-based incubations. A stable isotope tracer method was used to demonstrate that the net emissions of CH3Cl and CH3Br during the growing season were predominantly the result of large gross production rates, with gross consumption rates being relatively minor. In agreement with prior studies, the production rates for Methyl Halides differed significantly at different rice plant growth phases. The Twitchell Island rice field, however, had production rates of CH3Cl during the growth phases that were higher than rates reported at commercial rice fields, presumably because of higher soil chloride concentrations. Laboratory soil incubations showed that the non-flooded rice field soils acted as a small net sink for CH3Cl and as small net sources for CH3Br, CH3I and CHCl3. Despite the higher CH3Cl emissions during the growing season, the overall emissions of halomethanes from the conversion of all potential islands in the San Joaquin Delta to rice paddies is predicted to be an insignificant source of halomethanes.

  • Methyl halide and chloroform emissions from a subsiding Sacramento–San Joaquin Delta island converted to rice fields
    Atmospheric Environment, 2011
    Co-Authors: M A H Khan, Robert C. Rhew, M Whelan, K Zhou, S J Deverel
    Abstract:

    Net fluxes of Methyl Halides and chloroform were measured from recently converted rice fields on Twitchell Island, California, using field- and laboratory-based incubations. A stable isotope tracer method was used to demonstrate that the net emissions of CH3Cl and CH3Br during the growing season were predominantly the result of large gross production rates, with gross consumption rates being relatively minor. In agreement with prior studies, the production rates for Methyl Halides differed significantly at different rice plant growth phases. The Twitchell Island rice field, however, had production rates of CH3Cl during the growth phases that were higher than rates reported at commercial rice fields, presumably because of higher soil chloride concentrations. Laboratory soil incubations showed that the non-flooded rice field soils acted as a small net sink for CH3Cl and as small net sources for CH3Br, CH3I and CHCl3. Despite the higher CH3Cl emissions during the growing season, the overall emissions of halomethanes from the conversion of all potential islands in the San Joaquin Delta to rice paddies is predicted to be an insignificant source of halomethanes.

  • gross production exceeds gross consumption of Methyl Halides in northern california salt marshes
    Geophysical Research Letters, 2010
    Co-Authors: Robert C. Rhew, Olivier Mazeas
    Abstract:

    [1] Coastal salt marshes are sources of CH3Br and CH3Cl to the atmosphere, but the wide range of reported emission rates illustrates the need to understand better the factors controlling net fluxes. Here we demonstrate the use of a stable isotope tracer method to separately evaluate gross production and consumption fluxes to determine their relative roles in the overall net flux. At two salt marshes in northern California, gross production exceeds gross consumption at all measured sites, leading to a large net source overall. Emission rates are within the range observed at other temperate salt marshes. By evaluating the consumption component separately, we explain how a typical salt marsh source might convert into a temporary net sink by exposing the ecosystem to uncharacteristically high concentrations of Methyl Halides. This circumstance may account for the reported net uptake of Methyl chloride during the growing season at a coastal salt marsh in China.

  • Genetic control of Methyl halide production in Arabidopsis.
    Current biology : CB, 2003
    Co-Authors: Robert C. Rhew, Eric S Saltzman, Lars Østergaard, Martin F. Yanofsky
    Abstract:

    Methyl chloride (CH(3)Cl) and Methyl bromide (CH(3)Br) are the primary carriers of natural chlorine and bromine, respectively, to the stratosphere, where they catalyze the destruction of ozone, whereas Methyl iodide (CH(3)I) influences aerosol formation and ozone loss in the boundary layer. CH(3)Br is also an agricultural pesticide whose use is regulated by international agreement. Despite the economic and environmental importance of these Methyl Halides, their natural sources and biological production mechanisms are poorly understood. Besides CH(3)Br fumigation, important sources include oceans, biomass burning, tropical plants, salt marshes, and certain crops and fungi. Here, we demonstrate that the model plant Arabidopsis thaliana produces and emits Methyl Halides and that the enzyme primarily responsible for the production is encoded by the HARMLESS TO OZONE LAYER (HOL) gene. The encoded protein belongs to a group of Methyltransferases capable of catalyzing the S-adenosyl-L-methionine (SAM)-dependent Methylation of chloride (Cl(-)), bromide (Br(-)), and iodide (I(-)) to produce Methyl Halides. In mutant plants with the HOL gene disrupted, Methyl halide production is largely eliminated. A phylogenetic analysis with the HOL gene suggests that the ability to produce Methyl Halides is widespread among vascular plants. This approach provides a genetic basis for understanding and predicting patterns of Methyl halide production by plants.

M A H Khan - One of the best experts on this subject based on the ideXlab platform.

  • Methyl halide and chloroform emissions from a subsiding sacramento san joaquin delta island converted to rice fields
    Atmospheric Environment, 2011
    Co-Authors: M A H Khan, Robert C. Rhew, M Whelan, K Zhou, S J Deverel
    Abstract:

    Net fluxes of Methyl Halides and chloroform were measured from recently converted rice fields on Twitchell Island, California, using field- and laboratory-based incubations. A stable isotope tracer method was used to demonstrate that the net emissions of CH3Cl and CH3Br during the growing season were predominantly the result of large gross production rates, with gross consumption rates being relatively minor. In agreement with prior studies, the production rates for Methyl Halides differed significantly at different rice plant growth phases. The Twitchell Island rice field, however, had production rates of CH3Cl during the growth phases that were higher than rates reported at commercial rice fields, presumably because of higher soil chloride concentrations. Laboratory soil incubations showed that the non-flooded rice field soils acted as a small net sink for CH3Cl and as small net sources for CH3Br, CH3I and CHCl3. Despite the higher CH3Cl emissions during the growing season, the overall emissions of halomethanes from the conversion of all potential islands in the San Joaquin Delta to rice paddies is predicted to be an insignificant source of halomethanes.

  • Methyl halide and chloroform emissions from a subsiding Sacramento–San Joaquin Delta island converted to rice fields
    Atmospheric Environment, 2011
    Co-Authors: M A H Khan, Robert C. Rhew, M Whelan, K Zhou, S J Deverel
    Abstract:

    Net fluxes of Methyl Halides and chloroform were measured from recently converted rice fields on Twitchell Island, California, using field- and laboratory-based incubations. A stable isotope tracer method was used to demonstrate that the net emissions of CH3Cl and CH3Br during the growing season were predominantly the result of large gross production rates, with gross consumption rates being relatively minor. In agreement with prior studies, the production rates for Methyl Halides differed significantly at different rice plant growth phases. The Twitchell Island rice field, however, had production rates of CH3Cl during the growth phases that were higher than rates reported at commercial rice fields, presumably because of higher soil chloride concentrations. Laboratory soil incubations showed that the non-flooded rice field soils acted as a small net sink for CH3Cl and as small net sources for CH3Br, CH3I and CHCl3. Despite the higher CH3Cl emissions during the growing season, the overall emissions of halomethanes from the conversion of all potential islands in the San Joaquin Delta to rice paddies is predicted to be an insignificant source of halomethanes.

Lester Andrews - One of the best experts on this subject based on the ideXlab platform.

M Whelan - One of the best experts on this subject based on the ideXlab platform.

  • Methyl halide and chloroform emissions from a subsiding sacramento san joaquin delta island converted to rice fields
    Atmospheric Environment, 2011
    Co-Authors: M A H Khan, Robert C. Rhew, M Whelan, K Zhou, S J Deverel
    Abstract:

    Net fluxes of Methyl Halides and chloroform were measured from recently converted rice fields on Twitchell Island, California, using field- and laboratory-based incubations. A stable isotope tracer method was used to demonstrate that the net emissions of CH3Cl and CH3Br during the growing season were predominantly the result of large gross production rates, with gross consumption rates being relatively minor. In agreement with prior studies, the production rates for Methyl Halides differed significantly at different rice plant growth phases. The Twitchell Island rice field, however, had production rates of CH3Cl during the growth phases that were higher than rates reported at commercial rice fields, presumably because of higher soil chloride concentrations. Laboratory soil incubations showed that the non-flooded rice field soils acted as a small net sink for CH3Cl and as small net sources for CH3Br, CH3I and CHCl3. Despite the higher CH3Cl emissions during the growing season, the overall emissions of halomethanes from the conversion of all potential islands in the San Joaquin Delta to rice paddies is predicted to be an insignificant source of halomethanes.

  • Methyl halide and chloroform emissions from a subsiding Sacramento–San Joaquin Delta island converted to rice fields
    Atmospheric Environment, 2011
    Co-Authors: M A H Khan, Robert C. Rhew, M Whelan, K Zhou, S J Deverel
    Abstract:

    Net fluxes of Methyl Halides and chloroform were measured from recently converted rice fields on Twitchell Island, California, using field- and laboratory-based incubations. A stable isotope tracer method was used to demonstrate that the net emissions of CH3Cl and CH3Br during the growing season were predominantly the result of large gross production rates, with gross consumption rates being relatively minor. In agreement with prior studies, the production rates for Methyl Halides differed significantly at different rice plant growth phases. The Twitchell Island rice field, however, had production rates of CH3Cl during the growth phases that were higher than rates reported at commercial rice fields, presumably because of higher soil chloride concentrations. Laboratory soil incubations showed that the non-flooded rice field soils acted as a small net sink for CH3Cl and as small net sources for CH3Br, CH3I and CHCl3. Despite the higher CH3Cl emissions during the growing season, the overall emissions of halomethanes from the conversion of all potential islands in the San Joaquin Delta to rice paddies is predicted to be an insignificant source of halomethanes.