GREENHOUSE GAS FLUXES IN TROPICAL AND TEMPERATE AGRICULTURE : THE NEED FOR A FULL-COST ACCOUNTING OF GLOBAL WARMING POTENTIALS

Agriculture’s contribution to radiative forcing is principally through its historical release of carbon in soil and vegetation to the atmosphere and through its contemporary release of nitrous oxide (N2O) and methane (CH4). The sequestration of soil carbon in soils now depleted in soil organic matter is a well-known strategy for mitigating the buildup of CO2 in the atmosphere. Less well-recognized are other mitigation potentials. A full-cost accounting of the effects of agriculture on greenhouse gas emissions is necessary to quantify the relative importance of all mitigation options. Such an analysis shows nitrogen fertilizer, agricultural liming, fuel use, N2O emissions, and CH4 fluxes to have additional significant potential for mitigation. By evaluating all sources in terms of their global warming potential it becomes possible to directly evaluate greenhouse policy options for agriculture. A comparison of temperate and tropical systems illustrates some of these options.

[1]  G. Robertson,et al.  THE FUNCTIONAL SIGNIFICANCE OF DENITRIFIER COMMUNITY COMPOSITION IN A TERRESTRIAL ECOSYSTEM , 2000 .

[2]  G. Robertson,et al.  Soil CO2, N2O, and CH4 Exchange , 1999 .

[3]  C. E. Evans,et al.  Nitrogen and carbon changes in great plains soils as influenced by cropping and soil treatments , 1957 .

[4]  William H. Schlesinger,et al.  Carbon Sequestration in Soils , 1999, Science.

[5]  Arvin R. Mosier,et al.  Mitigating Agricultural Emissions of Methane , 1998 .

[6]  W. Chern,et al.  The Irrigation Demand for Electricity , 1982 .

[7]  G. Robertson Nitrification in forested ecosystems , 1982 .

[8]  Rattan Lal,et al.  Cropland to Sequester Carbon and Mitigate the Greenhouse Effect , 1998 .

[9]  G. Robertson,et al.  Greenhouse gases in intensive agriculture: contributions of individual gases to the radiative forcing of the atmosphere , 2000, Science.

[10]  R. Izaurralde,et al.  Carbon Cost of Applying Nitrogen Fertilizer , 2000, Science.

[11]  R. Lal Soil Management and Greenhouse Effect , 1995 .

[12]  T. Parkin,et al.  Direct measurement of oxygen profiles and denitrification rates in soil aggregates , 1985 .

[13]  R. Lal,et al.  Scientific challenges in developing a plan to predict and verify carbon storage in Canadian prairie soils. , 1998 .

[14]  W. V. Lierop Soil pH and lime requirement determination. , 1990 .

[15]  G. Robertson,et al.  Nitrification and denitrification in humid tropical ecosystems: potential controls on nitrogen retention , 1989 .

[16]  M. Keller,et al.  Soil‐atmosphere exchange of nitrous oxide, nitric oxide, and methane under secondary succession of pasture to forest in the Atlantic lowlands of Costa Rica , 1994 .

[17]  D. R. Nielsen,et al.  The Mineralogy, Chemistry, and Physics of Tropical Soils With Variable Charge Clays , 1983 .

[18]  G. Robertson,et al.  Decomposition and Soil Organic Matter Dynamics , 2000 .

[19]  Arvin R. Mosier,et al.  Assessing and Mitigating N2O Emissions from Agricultural Soils , 1998 .

[20]  Paul J. Crutzen,et al.  An inverse modeling approach to investigate the global atmospheric methane cycle , 1997 .

[21]  K. Bronson,et al.  Automated Chamber Measurements of Methane and Nitrous Oxide Flux in a Flooded Rice Soil: I. Residue, Nitrogen, and Water Management , 1997 .

[22]  R. Buresh,et al.  Direct Measurement of Dinitrogen and Nitrous Oxide Flux in Flooded Rice Fields , 1988 .

[23]  G. Robertson,et al.  Nutrient mobility in variable- and permanent-charge soils , 1988 .

[24]  Keith Paustian,et al.  Management Controls on Soil Carbon , 2019, Soil Organic Matter in Temperate Agroecosystems.

[25]  Keith A. Smith,et al.  Oxidation of atmospheric methane in Northern European soils, comparison with other ecosystems, and uncertainties in the global terrestrial sink , 2000 .