Dissolved organic carbon(DOC) is an important component of the terrestrial carbon cycle.However,the sources and controlling factors of DOC in soils remain uncertain.In this study,the effects of nitrogen(N) amendment a...Dissolved organic carbon(DOC) is an important component of the terrestrial carbon cycle.However,the sources and controlling factors of DOC in soils remain uncertain.In this study,the effects of nitrogen(N) amendment and crop growth on DOC in soil solution were examined at a maize-wheat rotated field located in the central Sichuan Basin in southwestern China.Nitrogen treatments in this study included 150 kg N ha-1 season-1,200 kg N ha-1 season-1 and the control without any fertilizer application.During the whole experimental period,we observed significant decreases(p<0.05) in DOC concentrations in the sampled soil solutions associated with increase in N inputs at the bare soil plots,but no change in DOC at the plots with crop growth.The estimated average contributions of plantderived DOC were 16%,24% and 32% of total DOC in the summer maize season and 21%,32% and 38% in the winter wheat season along with the gradient of N fertilizer application rates.The results implied thatthe crop growth could play a key role in the soil DOC production,and the N input enhanced DOC production by increasing crop growth.The relationship between the DOC concentrations and the crop root biomass was statistically significant for both the maize and winter wheat seasons.Our observations indicated that crop growth exerted greater influence on the seasonal variability of DOC concentration in soil solutions at the experimental site,which overwhelmed the effect of soil native organic matter decomposition on DOC concentrations in soil solutions.展开更多
Soil organic carbon is of great importance to terrestrial ecosystems.Studies on the amount and spatial distribution of soil organic carbon stock in various types of soil can help to better understand the role of soil ...Soil organic carbon is of great importance to terrestrial ecosystems.Studies on the amount and spatial distribution of soil organic carbon stock in various types of soil can help to better understand the role of soil in the global carbon cycle and provide a scientific basis for the assessment of the magnitude of carbon stored in a given area.Here we present estimates of soil organic carbon stock in soils in the upper reaches of the Yangtze River based on soil types as defined by Chinese Soil Taxonomy and recently compiled into a digital soil database.The results showed that the total soil organic carbon stock of the upper Yangtze River to a depth of 100 cm was 1.452×1013kg.The highest soil organic carbon stock was found in felty soils(2.419×1012kg),followed by dark brown soils(1.269×1012kg),and dark felty soils(1.139×1012kg).Chernozems and irrigation silting soils showed the lowest soil organic carbon stock,mainly due to the small total area of such soils.The soil organic carbon density of these major soil types ranged from 5.6 to 26.1 kg m-2.The average soil organic carbon density of the upper reaches of the Yangtze River was 16.4 kg m-2,which was higher than that of the national average.Soil organic carbon density indicated a distinct decreasing trend from west to east,which corresponds to the pattern of increasing temperature from cold to subtropical.展开更多
基金the Natural Science Foundation of China (Grant No.41371302)Innovative Team Program of Chinese Academy of Sciences (Grant No.KZZDEW-TZ-06)the West Light Foundation of the Chinese Academy of Sciences
文摘Dissolved organic carbon(DOC) is an important component of the terrestrial carbon cycle.However,the sources and controlling factors of DOC in soils remain uncertain.In this study,the effects of nitrogen(N) amendment and crop growth on DOC in soil solution were examined at a maize-wheat rotated field located in the central Sichuan Basin in southwestern China.Nitrogen treatments in this study included 150 kg N ha-1 season-1,200 kg N ha-1 season-1 and the control without any fertilizer application.During the whole experimental period,we observed significant decreases(p<0.05) in DOC concentrations in the sampled soil solutions associated with increase in N inputs at the bare soil plots,but no change in DOC at the plots with crop growth.The estimated average contributions of plantderived DOC were 16%,24% and 32% of total DOC in the summer maize season and 21%,32% and 38% in the winter wheat season along with the gradient of N fertilizer application rates.The results implied thatthe crop growth could play a key role in the soil DOC production,and the N input enhanced DOC production by increasing crop growth.The relationship between the DOC concentrations and the crop root biomass was statistically significant for both the maize and winter wheat seasons.Our observations indicated that crop growth exerted greater influence on the seasonal variability of DOC concentration in soil solutions at the experimental site,which overwhelmed the effect of soil native organic matter decomposition on DOC concentrations in soil solutions.
基金funded by Special Program of Strategic Science and Technology of Chinese Academy of Sciences (Grant No. XDA05050506)State Key and Basic Research Development Planning (Grant No. 2012CB417101)+1 种基金Project of Natural Science Foundation of China (Grant No. 40901134)West Light Foundation of Chinese Academy of Sciences
文摘Soil organic carbon is of great importance to terrestrial ecosystems.Studies on the amount and spatial distribution of soil organic carbon stock in various types of soil can help to better understand the role of soil in the global carbon cycle and provide a scientific basis for the assessment of the magnitude of carbon stored in a given area.Here we present estimates of soil organic carbon stock in soils in the upper reaches of the Yangtze River based on soil types as defined by Chinese Soil Taxonomy and recently compiled into a digital soil database.The results showed that the total soil organic carbon stock of the upper Yangtze River to a depth of 100 cm was 1.452×1013kg.The highest soil organic carbon stock was found in felty soils(2.419×1012kg),followed by dark brown soils(1.269×1012kg),and dark felty soils(1.139×1012kg).Chernozems and irrigation silting soils showed the lowest soil organic carbon stock,mainly due to the small total area of such soils.The soil organic carbon density of these major soil types ranged from 5.6 to 26.1 kg m-2.The average soil organic carbon density of the upper reaches of the Yangtze River was 16.4 kg m-2,which was higher than that of the national average.Soil organic carbon density indicated a distinct decreasing trend from west to east,which corresponds to the pattern of increasing temperature from cold to subtropical.