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Carbonate rock dissolution rates in different landuses and their carbon sink effect 被引量:33

Carbonate rock dissolution rates in different landuses and their carbon sink effect
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摘要 Research on karst processes is important for the determination of their carbon sink potential,as is research into terrestrial ecosystems in karst areas.Solutional denudation rates of soils from three karst spring watersheds supporting different land uses were studied.Solution rates showed a distinct pattern based on land use,with a generally higher rate being recorded in forest use soil.The mean values for tablet dissolution from the cultivated land,shrublands,secondary forest,grassland and primary forest were 4.02,7.0,40.0,20.0,63.5 t km-2 a-1 respectively.Changes in vegetation patterns could improve the size of karst carbon sinks;for example,in this study the carbon sink was 3 times higher in primary forest than in secondary forest soil and 9 times higher than under shrubland,equating to an increase from 5.71-7.02 to 24.86-26.17 t km-2 a-1 from cultivated land or shrub to secondary forest and to primary forest,respectively. Research on karst processes is important for the determination of their carbon sink potential, as is research into terrestrial ecosystems in karst areas. Solutional denudation rates of soils from three karst spring watersheds supporting different land uses were studied. Solution rates showed a distinct pattern based on land use, with a generally higher rate being recorded in forest use soil. The mean values for tablet dissolution from the cultivated land, shrublands, secondary forest, grassland and primary forest were 4.02, 7.0, 40.0, 20.0, 63.5 t km^-2 a^-1 respectively. Changes in vegetation patterns could improve the size of karst carbon sinks; for example, in this study the carbon sink was 3 times higher in primary forest than in secondary forest soil and 9 times higher than under shrubland, equating to an increase from 5.71-7.02 to 24.86-26.17 t km^-2 a^-1 from cultivated land or shrub to secondary forest and to primary forest, respectively.
作者 ZHANG Cheng
出处 《Chinese Science Bulletin》 SCIE EI CAS 2011年第35期3759-3765,共7页
基金 supported by the National Natural Science Foundation of China (40772164) the Special Fund for Public Benefit Scientific Research of Ministry of Land and Resources of China (201111022) the China Geological Survey Project (1212010911062 and water-2010030701)
关键词 碳酸盐岩 土地用途 溶出率 陆地生态系统 岩溶地区 原始森林 次生林 剥蚀速率 carbonate rock, dissolution rate, land-use change, carbon sink, southern China
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