TY - JOUR
T1 - Grazing effects on the greenhouse gas balance of a temperate steppe ecosystem
AU - Schönbach, Philipp
AU - Wolf, Benjamin
AU - Dickhöfer, Uta
AU - Wiesmeier, Martin
AU - Chen, Weiwei
AU - Wan, Hongwei
AU - Gierus, Martin
AU - Butterbach-Bahl, Klaus
AU - Kögel-Knabner, Ingrid
AU - Susenbeth, Andreas
AU - Zheng, Xunhua
AU - Taube, Friedhelm
N1 - Funding Information:
Acknowledgments The authors would like to acknowledge the Deutsche Forschungsgemeinschaft (DFG) for funding the research group 536 MAGIM (Matter fluxes of grasslands in Inner Mongolia as influenced by stocking rate). We thank the reviewers of this paper for their helpful suggestions.
PY - 2012/7
Y1 - 2012/7
N2 - Although a significant fraction of the global soil-atmosphere exchange of greenhouse gases (GHGs) occurs in semi-arid zones little is known about the magnitude of fluxes in grazed steppe ecosystems and the interference with grazing intensity. In order to assess GHG burdens and to identify options of climate-optimized livestock farming, GHG emissions of sheep grazing in Inner Mongolia steppe were analyzed. Carbon sequestration and field-fluxes of methane (CH 4) and nitrous oxide (N 2O) were measured at a range of steppe sites differing in grazing intensity and management, i. e. ungrazed (UG), ungrazed with hay cutting (HC), lightly grazed (LG), moderately grazed (MG), and heavily grazed (HG). In addition, GHG emissions from enteric fermentation, manure management, and farming inputs (i. e. fossil fuels) were quantified for LG, MG, and HG. Monte Carlo simulation was used to estimate uncertainty. Sheep grazing changed the net GHG balance of the steppe from a significant sink at UG (-1476 ± 2481 kg CO 2eq ha -1 year -1) to a significant source at MG (2350 ± 1723 kg CO 2eq ha -1 year -1) and HG (3115 ± 2327 kg CO 2eq ha -1 year -1). In a similar way, the GHG intensity increased from 8.6 ± 79.2 kg CO 2eq kg -1 liveweight gain at LG up to 62.2 ± 45.8 and 62.6 ± 46.7 kg CO 2eq kg -1 liveweight gain at MG and HG, respectively. GHG balances were predominantly determined by CO 2 from changes in topsoil organic carbon. In grazing systems, CH 4 from enteric fermentation was the second most important component. The results suggest that sheep grazing under the current management changes this steppe ecosystem from a sink to a source of GHGs and that grazing exclusion holds large potential to restore soil organic carbon stocks and thus to sequester atmospheric CO 2. The balance between grazing intensity and grazing exclusion predominantly determines GHG balances of grass-based sheep farming in this region. Therefore, a high proportion of ungrazed land is most important for reducing GHG balances of sheep farms. This can be either achieved by high grazing intensity on the remaining grazed land or by confined hay feeding of sheep.
AB - Although a significant fraction of the global soil-atmosphere exchange of greenhouse gases (GHGs) occurs in semi-arid zones little is known about the magnitude of fluxes in grazed steppe ecosystems and the interference with grazing intensity. In order to assess GHG burdens and to identify options of climate-optimized livestock farming, GHG emissions of sheep grazing in Inner Mongolia steppe were analyzed. Carbon sequestration and field-fluxes of methane (CH 4) and nitrous oxide (N 2O) were measured at a range of steppe sites differing in grazing intensity and management, i. e. ungrazed (UG), ungrazed with hay cutting (HC), lightly grazed (LG), moderately grazed (MG), and heavily grazed (HG). In addition, GHG emissions from enteric fermentation, manure management, and farming inputs (i. e. fossil fuels) were quantified for LG, MG, and HG. Monte Carlo simulation was used to estimate uncertainty. Sheep grazing changed the net GHG balance of the steppe from a significant sink at UG (-1476 ± 2481 kg CO 2eq ha -1 year -1) to a significant source at MG (2350 ± 1723 kg CO 2eq ha -1 year -1) and HG (3115 ± 2327 kg CO 2eq ha -1 year -1). In a similar way, the GHG intensity increased from 8.6 ± 79.2 kg CO 2eq kg -1 liveweight gain at LG up to 62.2 ± 45.8 and 62.6 ± 46.7 kg CO 2eq kg -1 liveweight gain at MG and HG, respectively. GHG balances were predominantly determined by CO 2 from changes in topsoil organic carbon. In grazing systems, CH 4 from enteric fermentation was the second most important component. The results suggest that sheep grazing under the current management changes this steppe ecosystem from a sink to a source of GHGs and that grazing exclusion holds large potential to restore soil organic carbon stocks and thus to sequester atmospheric CO 2. The balance between grazing intensity and grazing exclusion predominantly determines GHG balances of grass-based sheep farming in this region. Therefore, a high proportion of ungrazed land is most important for reducing GHG balances of sheep farms. This can be either achieved by high grazing intensity on the remaining grazed land or by confined hay feeding of sheep.
KW - Carbon footprint
KW - Global warming potential
KW - Grazing intensity
KW - Greenhouse gas
KW - Life cycle assessment
KW - Sheep meat production
UR - http://www.scopus.com/inward/record.url?scp=84865481794&partnerID=8YFLogxK
U2 - 10.1007/s10705-012-9521-1
DO - 10.1007/s10705-012-9521-1
M3 - Article
AN - SCOPUS:84865481794
SN - 1385-1314
VL - 93
SP - 357
EP - 371
JO - Nutrient Cycling in Agroecosystems
JF - Nutrient Cycling in Agroecosystems
IS - 3
ER -