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Article: Importance of biophysical effects on climate warming mitigation potential of biofuel crops over the conterminous United States
Title | Importance of biophysical effects on climate warming mitigation potential of biofuel crops over the conterminous United States |
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Authors | |
Keywords | agricultural management biofuel crops biophysical effect carbon sequestration community land model marginal land |
Issue Date | 2017 |
Citation | GCB Bioenergy, 2017, v. 9, n. 3, p. 577-590 How to Cite? |
Abstract | Current quantification of climate warming mitigation potential (CWMP) of biomass-derived energy has focused primarily on its biogeochemical effects. This study used site-level observations of carbon, water, and energy fluxes of biofuel crops to parameterize and evaluate the community land model (CLM) and estimate CO2 fluxes, surface energy balance, soil carbon dynamics of corn (Zea mays), switchgrass (Panicum virgatum), and miscanthus (Miscanthus × giganteus) ecosystems across the conterminous United States considering different agricultural management practices and land-use scenarios. We find that neglecting biophysical effects underestimates the CWMP of transitioning from croplands and marginal lands to energy crops. Biogeochemical effects alone result in changes in carbon storage of −1.9, 49.1, and 69.3 g C m−2 y−1 compared to 20.5, 78.5, and 96.2 g C m−2 y−1 when considering both biophysical and biogeochemical effects for corn, switchgrass, and miscanthus, respectively. The biophysical contribution to CWMP is dominated by changes in latent heat fluxes. Using the model to optimize growth conditions through fertilization and irrigation increases the CWMP further to 79.6, 98.3, and 118.8 g C m−2 y−1, respectively, representing the upper threshold for CWMP. Results also show that the CWMP over marginal lands is lower than that over croplands. This study highlights that neglecting the biophysical effects of altered surface energy and water balance underestimates the CWMP of transitioning to bioenergy crops at regional scales. |
Persistent Identifier | http://hdl.handle.net/10722/326099 |
ISSN | 2023 Impact Factor: 5.9 2023 SCImago Journal Rankings: 1.414 |
ISI Accession Number ID |
DC Field | Value | Language |
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dc.contributor.author | Zhu, Peng | - |
dc.contributor.author | Zhuang, Qianlai | - |
dc.contributor.author | Eva, Joo | - |
dc.contributor.author | Bernacchi, Carl | - |
dc.date.accessioned | 2023-03-09T09:58:01Z | - |
dc.date.available | 2023-03-09T09:58:01Z | - |
dc.date.issued | 2017 | - |
dc.identifier.citation | GCB Bioenergy, 2017, v. 9, n. 3, p. 577-590 | - |
dc.identifier.issn | 1757-1693 | - |
dc.identifier.uri | http://hdl.handle.net/10722/326099 | - |
dc.description.abstract | Current quantification of climate warming mitigation potential (CWMP) of biomass-derived energy has focused primarily on its biogeochemical effects. This study used site-level observations of carbon, water, and energy fluxes of biofuel crops to parameterize and evaluate the community land model (CLM) and estimate CO2 fluxes, surface energy balance, soil carbon dynamics of corn (Zea mays), switchgrass (Panicum virgatum), and miscanthus (Miscanthus × giganteus) ecosystems across the conterminous United States considering different agricultural management practices and land-use scenarios. We find that neglecting biophysical effects underestimates the CWMP of transitioning from croplands and marginal lands to energy crops. Biogeochemical effects alone result in changes in carbon storage of −1.9, 49.1, and 69.3 g C m−2 y−1 compared to 20.5, 78.5, and 96.2 g C m−2 y−1 when considering both biophysical and biogeochemical effects for corn, switchgrass, and miscanthus, respectively. The biophysical contribution to CWMP is dominated by changes in latent heat fluxes. Using the model to optimize growth conditions through fertilization and irrigation increases the CWMP further to 79.6, 98.3, and 118.8 g C m−2 y−1, respectively, representing the upper threshold for CWMP. Results also show that the CWMP over marginal lands is lower than that over croplands. This study highlights that neglecting the biophysical effects of altered surface energy and water balance underestimates the CWMP of transitioning to bioenergy crops at regional scales. | - |
dc.language | eng | - |
dc.relation.ispartof | GCB Bioenergy | - |
dc.subject | agricultural management | - |
dc.subject | biofuel crops | - |
dc.subject | biophysical effect | - |
dc.subject | carbon sequestration | - |
dc.subject | community land model | - |
dc.subject | marginal land | - |
dc.title | Importance of biophysical effects on climate warming mitigation potential of biofuel crops over the conterminous United States | - |
dc.type | Article | - |
dc.description.nature | link_to_subscribed_fulltext | - |
dc.identifier.doi | 10.1111/gcbb.12370 | - |
dc.identifier.scopus | eid_2-s2.0-84978805823 | - |
dc.identifier.volume | 9 | - |
dc.identifier.issue | 3 | - |
dc.identifier.spage | 577 | - |
dc.identifier.epage | 590 | - |
dc.identifier.eissn | 1757-1707 | - |
dc.identifier.isi | WOS:000402740900007 | - |