Abstract
It has become increasingly well documented that human activities are enhancing the greenhouse effect and altering the global climate. Identifying strategies to mitigate atmospheric carbon dioxide emissions on the national level are therefore critical. Fossil fuel combustion is primarily responsible for the perturbation of the global carbon cycle, although the influence of humans extends far beyond the combustion of fossil fuels. Changes in land use arising from human activities contribute substantially to atmospheric carbon dioxide; however, land use changes can act as a carbon dioxide sink as well. A soil carbon model was built using STELLA to explore how soil organic carbon sequestration (SOC) varies over a range of values for key parameters and to estimate the amount of global soil carbon sequestration from livestock waste. To obtain soil carbon sequestration estimates, model simulations occurred for 11 different livestock types and with data for eight regions around the world. The model predicted that between 1980 and 1995, United States soils were responsible for the sequestration of 444–602 Tg C from livestock waste. Model simulations further predicted that during the same period, global soil carbon sequestration from livestock waste was 2,810–4,218 Tg C. Our estimates for global SOC sequestration are modest in proportion to other terrestrial carbon sinks (i.e. forest regrowth); however, livestock waste does represent a potential for long-term soil carbon gain. SOC generated from livestock waste is another example of how human activities and land use changes are altering soil processes around the world.
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Acknowledgements
The authors would like to thank Kent Keller and Andy Ford for their guidance and insightful comments on an earlier draft of this manuscript. This research was partially supported by a Lane Fellowship in Environmental Science and Regional Planning, Washington State University.
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Appendix A
Appendix A
Countries included in this study and considered climatic exceptions. Information on temperature and available moisture factors was obtained from Safley et al. (1992)
North America
Canadaa
United States
Western Europe
Austria
Belgium
Denmark
Finlanda
France
West Germany
Greece
Ireland
Italy
Netherlands
Norwaya
Portugal
Spain
Swedena
Switzerland
UK
East Europe
Albania
Bulgaria
Czechoslovakiaa
East Germany
Hungarya
Polanda
Romaniaa
Soviet Uniona
Yugoslavia
Oceania
Australiab
Fiji
New Caledonia
New Zealand
P. New Guinea
Vanuatu
Africa
Angola
Benin
Botswanab
Burkina Fasob
Burundi
Cameroon
Central African Republic
Chadb
Cote d’lvore
Ethiopiab
The Ghambia
Ghana
Guinea
Guinea-Bissau
Kenyab
Lesotho
Madagascar
Malawi
Malib
Mauritaniab
Mozambique
Namibiab
Nigerb
Nigeria
Rwanda
Senegal
Sierra Leone
Somaliab
South Africab
Swaziland
Tanzania
Togo
Uganda
Zaire
Zambia
Zimbabwe
Latin America
Argentina
Bolivia
Brazil
Chile
Columbia
Costa Rica
Cuba
Dominican Republic
Ecuador
El Salvador
Guatemala
Guyana
Haiti
Honduras
Jamaica
Mexico
Nicaragua
Panama
Paraguay
Peru
Puerto Rico
Uruguay
Venezuela
Near East & Mediterranean
Afghanistanb
Algeriab
Egyptb
Iranb
Iraqb
Israel
Jordanb
Kuwait
Libyab
Morocco
Omanb
Saudi Arabiab
Sudanb
Syriab
Tunisiab
Turkey
Yemen Arab Republicb
Asia & Far East
Bangladesh
Bhutan
Burma
China
India
Indonesia
Japan
Kampuchea
North Korea
South Korea
Laos
Malaysia
Mongoliab
Nepal
Pakistanb
Philippines
Sri Lanka
Thailand
Vietnam
a Countries considered climatic exceptions (cold)
b Countries considered climatic exceptions (arid/semiarid)
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Fellman, J.B., Franz, E.H., Crenshaw, C.L. et al. Global estimates of soil carbon sequestration via livestock waste: a STELLA simulation. Environ Dev Sustain 11, 871–885 (2009). https://doi.org/10.1007/s10668-008-9157-0
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DOI: https://doi.org/10.1007/s10668-008-9157-0