Indirect Impacts of Land Use Change on Soil Organic Carbon Change in China
Received date: 2005-12-20
Revised date: 2006-01-11
Online published: 2006-02-15
Soil organic carbon (SOC) storage and its change trend in China is important to the global carbon cycles under the background of global warming. Land use change has both direct and indirect influences on SOC storage. On the one hand, the land use change directly modifies the original ecosystem type and then makes the net primary productivity and soil carbon input change, which directly impacts SOC storage. On the other hand, land use change modifies some physical or chemical properties of soil and thus potentially impacts the value of temperature sensitivity of soil heterogeneous respiration (Q10). Under the situation of global warming, the changed Q10 will modify the feedback intensity of soil respiration and then indirectly impacts the soil organic carbon storage. In this study, a regional process-based carbon cycle model (CASA model) was used to estimate the Q10 values for the different land use types. Basing on the differences of Q10 among land use types, the indirect impacts of land use change on soil organic carbon storage was assessed. The results showed that the land use changes from grassland or forest to cropland will increase the value of Q10. Furthermore, the human activities, such as utilizing of irrigation and nitrogenous fertilizer will also increase the values of Q10. So, the land use change and human activities will potentially increase soil carbon releasing under the situation of global warming and then will indirectly impact soil organic carbon storage.
Key words: Soil respiration; Temperature sensitivity; Q10; CASA model; China.
Zhou Tao,Shi Peijun . Indirect Impacts of Land Use Change on Soil Organic Carbon Change in China[J]. Advances in Earth Science, 2006 , 21(2) : 138 -143 . DOI: 10.11867/j.issn.1001-8166.2006.02.0138
[1] Houghton J T, et al, eds. In Climate Change 2001: The Science of Climate Change[M]. New York: Cambridge University Press, 2001.
[2] IGBP Terrestrial Carbon Working Group. The terrestrial carbon cycle: Implications for the Kyoto protocol[J]. Science, 1998, 280:1 393-1 394.
[3] Piao S, Fang J, Zhou L, et al. Changes in vegetation net primary productivity from 1982 to 1999 in China[J]. Global Biogeochemical Cycles, 2005, 19:GB2027, doi:10.1029/2004GB002274.
[4] Zhou Tao, Shi Peijun, Wang Shaoqiang. Impacts of climate change and human activities on soil carbon storage in China[J]. Acta Geographica Sinica, 2003, 58(5): 727-734.[周涛,史培军,王绍强. 气候变化及人类活动对中国土壤有机碳储量的影响[J]. 地理学报,2003, 58(5): 727-734.]
[5] Zhou Tao, Shi Peijun, Sun Rui, et al. The impacts of climate change on net ecosystem production in China[J]. Acta Geographica Sinica, 2004, 59(3): 357-365.[周涛,史培军,孙睿,等. 气候变化对净生态系统生产力的影响[J].地理学报, 2004, 59(3): 357-365.]
[6] Luo Y, Wan S, Hui D, et al. Acclimatization of soil respiration to warming in a tall grass prairie[J]. Nature,2001, 413:622-625.
[7] Reichstein M, Rey A, Freibauer A, et al. Modeling temporal and large-scale spatial variability of soil respiration from soil water availability, temperature and vegetation productivity indices[J]. Global Biogeochemical Cycles, 2003, 17(4): 1104, doi:10.1029/2003GB002035.
[8] Kirschbaum M U F. Will changes in soil organic carbon act as a positive or negative feedback on global warming?[J]. Biogeochemistry, 2000, 48:21-51.
[9] Raich J W, Tufekcioglu A. Vegetation and soil respiration: Correlations and controls[J]. Biogeochemistry,2000, 48: 71-90.
[10] Lloyd J, Taylor J A. On the temperature dependence of soil respiration[J]. Function of Ecology, 1994, 8:315-323.
[11] Kirschbaum M U F. The temperature dependence of soil organic matter decomposition, and the effect of global warming on soil organic C storage[J]. Soilogical Biolistry Biochemistry,1995, 27:753-760.
[12] Davidson E A, Belk E, Boone R D. Soil water content and temperature as independent or confound factors controlling soil respiration in a temperate mixed hardwood forest[J]. Global Change Biology,1998, 4(2):217-227.
[13] Liu X, Wan S, Su B, et al. Responses of soil CO2 efflux to water manipulation in a tallgrass prairie ecosystem[J]. Plant and Soil,2002, 240:213-223.
[14] Reichstein M, Tenhunen J D, Ourcival J M, et al. Ecosystem respiration in two Mediterranean evergreen Holm oak forests: Drought effects and decomposition dynamics[J]. Function of Ecology, 2002, 16:27-39.
[15] Hui D, Luo Y. Evaluation of soil CO2 production and transport in duke forest using a process-based modeling approach[J]. Global Biogeochemical Cycles, 2004,18:GB4029,doi:10.1029/ 2004GB002297.
[16] Taylor B R, Parkinson D, Parsons W F J. Nitrogen and lignin content as predictors of litter decay rates: A microcosm test[J]. Ecology,1989, 70:97-104.
[17] Liski J, Ilvesniemi H, Mäkelä A, et al. CO2 emissions from soil in response to climatic warming are overestimated-The decomposition of old soil organic matter is tolerant of temperature[J]. AMBIO,1999, 28:171-174.
[18] Wan S Q, Luo Y Q. Substrate regulation of soil respiration in a tallgrass prairie: Results of a clipping and shading experiment[J]. Global Biogeochemical Cycles,2003, 17(2):Art. No. 1054.
[19] Fang Jingyun, Liu Shaohui, Zhao Kun. Factors affecting soil respiration in reference with temperature's role in the global scale[J]. Chinese Geographical Science,1998, 8(3): 246-255.
[20] Thompson M V, Randerson J T, Malmstrom C M, et al. Change in net primary production and heterotrophic respiration: How much is necessary to sustain the terrestrial carbon sink?[J]. Global Biogeochemical Cycles,1996, 10(4):711-726.
[21] Schimel D S, Braswell B H, Holland E A, et al. Climatic, edaphic, and biotic controls over storage and turnover of carbon in soils[J]. Global Biogeochemical Cycles,1994, 8(3): 279-293.
[22] Potter C S, Randerson J T, Field C B, et al. Terrestrial ecosystem production: A process model based on global satellite and surface data[J]. Global Biogeochemical Cycles,1993, 7(4):811-841.
[23] Field C B, Randerson J T, Malmstrom C M. Global net primary production: Combining ecology and remote sensing[J]. Remote Sensing of Environment,1995, 51: 74-88.
[24] GSDP: the global soil data products[EB/OL]. Oak Ridge, Tenn: International Geosphere-Biosphere Programme-Data and Information Services,2000[2004-03-16].http∥www.daac.ornl.gov.
[25] Qi Y, Xu M, Wu J. Temperature sensitivity of soil respiration and its effects on ecosystem carbon budget: Nonlinearity begets surprises[J]. Ecological Modelling,2002, 153: 131-142.
[26] Yuste J C, Janssens I A, Carrara A, et al. Interactive effects of temperature and precipitation on soil respiration in a temperate maritime pine forest[J]. Tree Physiology,2003, 23:1 263-1 270.
[27] Dörr H, Münnich K O. Annual variation in soil respiration in selected areas of the temperate zone[J]. Tellus,1987, 9B:114-121.
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