Differences in soil CO2 flux between different land use types in mid-subtropical China Export

@article{citeulike:3142294, abstract = {It is crucial to advance the understanding of the soil carbon dioxide (CO2) flux and environmental factors for a better comprehension of carbon dynamics in subtropical ecosystems. Red soil, one of the typical agricultural soils in subtropical China, plays important roles in the global carbon budget due to their large potential to sequester C and replenish atmospheric C through soil CO2 flux. We examined the relationship between soil CO2 flux and environmental determinants in four different land use types of subtropical red soil-paddy (P), orchard (O), woodland (W) and upland (U) using static closed chamber method. Objectives were to evaluate the relationship of soil temperature, water-filled pore space (WFPS), and dissolved organic carbon (DOC) with the soil CO2 flux. Soil CO2 fluxes were measured on each site about every 14 days between 09:00 and 11:00 a.m. during 14-July 2004 to 25-April 2007 at the experimental station of Heshengqiao at Xianning, Hubei, China. Soil CO2 fluxes revealed seasonal fluctuations, with the tendency that maximum values occurred in summer, minimum in winter and intermediate values in spring and autumn except for paddy soil when it was submerged. Further, significant differences in soil CO2 fluxes were observed among the four soils, following the order of P > O > U \~{} W. Average soil CO2 fluxes were estimated as 901 ± 114, 727 ± 55, 554 ± 22 and 533 ± 27 (±S.D.) g CO2 m-2 year-1 in paddy, orchard, upland and woodland soils, respectively. Variations in soil CO2 flux were related to soil temperature, WFPS, and dissolved organic carbon with a combined R2 of 0.49-0.75. Soil temperature was an important variable controlling 26-59\% of soil CO2 flux variability. The interaction of soil temperature and WFPS could explain 31-60\% of soil CO2 flux variations for all the land use types. We conclude that soil CO2 flux from red soil is under environmental controls, soil temperature being the main variable, which interact with WFPS and DOC to control the supply of readily mineralizable substrates.}, author = {Iqbal, Javed and Ronggui, Hu and Lijun, Du and Lan, Lu and Shan, Lin and Tao, Chen and Leilei, Ruan}, booktitle = {Special Section: Enzymes in the Environment, Enzymes in the Environment III}, citeulike-article-id = {3142294}, citeulike-linkout-0 = {http://dx.doi.org/10.1016/j.soilbio.2008.05.010}, citeulike-linkout-1 = {http://linkinghub.elsevier.com/retrieve/pii/S003807170800165X}, citeulike-linkout-2 = {http://www.sciencedirect.com/science/article/B6TC7-4SR0M1Y-4/2/6b17c98eeef7debcaf06576da34ccd9d}, doi = {10.1016/j.soilbio.2008.05.010}, journal = {Soil Biology and Biochemistry}, month = {September}, number = {9}, pages = {2324--2333}, posted-at = {2008-08-21 00:06:47}, priority = {2}, title = {Differences in soil CO2 flux between different land use types in mid-subtropical China}, url = {http://dx.doi.org/10.1016/j.soilbio.2008.05.010}, volume = {40}, year = {2008} }

TY - JOUR ID - citeulike:3142294 L3 - citeulike-article-id:3142294 N2 - It is crucial to advance the understanding of the soil carbon dioxide (CO2) flux and environmental factors for a better comprehension of carbon dynamics in subtropical ecosystems. Red soil, one of the typical agricultural soils in subtropical China, plays important roles in the global carbon budget due to their large potential to sequester C and replenish atmospheric C through soil CO2 flux. We examined the relationship between soil CO2 flux and environmental determinants in four different land use types of subtropical red soil-paddy (P), orchard (O), woodland (W) and upland (U) using static closed chamber method. Objectives were to evaluate the relationship of soil temperature, water-filled pore space (WFPS), and dissolved organic carbon (DOC) with the soil CO2 flux. Soil CO2 fluxes were measured on each site about every 14 days between 09:00 and 11:00 a.m. during 14-July 2004 to 25-April 2007 at the experimental station of Heshengqiao at Xianning, Hubei, China. Soil CO2 fluxes revealed seasonal fluctuations, with the tendency that maximum values occurred in summer, minimum in winter and intermediate values in spring and autumn except for paddy soil when it was submerged. Further, significant differences in soil CO2 fluxes were observed among the four soils, following the order of P > O > U ~ W. Average soil CO2 fluxes were estimated as 901 ± 114, 727 ± 55, 554 ± 22 and 533 ± 27 (±S.D.) g CO2 m-2 year-1 in paddy, orchard, upland and woodland soils, respectively. Variations in soil CO2 flux were related to soil temperature, WFPS, and dissolved organic carbon with a combined R2 of 0.49-0.75. Soil temperature was an important variable controlling 26-59% of soil CO2 flux variability. The interaction of soil temperature and WFPS could explain 31-60% of soil CO2 flux variations for all the land use types. We conclude that soil CO2 flux from red soil is under environmental controls, soil temperature being the main variable, which interact with WFPS and DOC to control the supply of readily mineralizable substrates. IS - 9 JF - Soil Biology and Biochemistry EP - 2333 TI - Differences in soil CO2 flux between different land use types in mid-subtropical China VL - 40 T2 - Special Section: Enzymes in the Environment, Enzymes in the Environment III SP - 2324 AU - Iqbal, Javed AU - Ronggui, Hu AU - Lijun, Du AU - Lan, Lu AU - Shan, Lin AU - Tao, Chen AU - Leilei, Ruan PY - 2008/09// UR - http://dx.doi.org/10.1016/j.soilbio.2008.05.010 ER -