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Altitudinal variations in soil carbon storage and distribution patterns in cold desert high altitude microclimate of India

机译:印度寒冷沙漠高海拔微气候中土壤碳储量和分布格局的垂直变化

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A study was conducted to assess the soil carbon distribution in cold desert high altitude region of Ladakh in India at different altitudes and their correlation patterns with the altitude. The role of carbon dynamics in the exchange of CO2?between the terrestrial biosphere and the atmosphere has important implications in this study of global climate change. The present study was done in Ladakh region of India from where soil samples were collected on the basis of different altitudes range and thereafter samples were analyzed for organic carbon and calcium carbonate content. Results of our study show that the soil organic carbon (SOC) content and storage increased significantly with the increase in the altitude where as when compared with the altitude of 10000 ft amsl, soil inorganic carbon (SIC content and its storage decreased significantly (P< 0.05) at an altitude of 11000 ft up to 12000 ft amsl. The SOC content and storage were observed positively (P<0.01) correlated with altitude, while soil inorganic carbon storage and contents were negatively (P<0.05) correlated with altitude. Hence, our study indicates that very harsh and unique climatic conditions in Ladakh influences storage and distribution pattern of soil carbon along the altitudes or elevation gradients. So investigations along altitude gradients is a useful approach to the study of environmental change and its effect on the soil processes, which can complement data obtained from controlled, large scale field studies as well as other practical and theoretical approaches to climate change research.
机译:进行了一项研究,以评估印度拉达克的寒冷沙漠高海拔地区不同海拔高度的土壤碳分布及其与海拔高度的相关关系。碳动力学在陆地生物圈与大气之间的CO 2交换中的作用对这项全球气候变化研究具有重要意义。本研究在印度拉达克地区进行,根据不同的海拔范围从该地区收集土壤样品,然后分析样品中的有机碳和碳酸钙含量。我们的研究结果表明,土壤有机碳(SOC)含量和存储量随着海拔的升高而显着增加,而与10000英尺海拔高度相比,土壤无机碳(SIC含量及其存储量则显着下降(P <在海拔11000英尺至海拔12000英尺之间,其SOC含量和存储量与海拔高度呈正相关(P <0.01),而土壤无机碳的存储量和含量与海拔高度呈负相关(P <0.05)。 ,我们的研究表明,拉达克非常恶劣和独特的气候条件会影响海拔或海拔梯度上土壤碳的存储和分布模式,因此,沿海拔梯度进行研究是研究环境变化及其对土壤过程影响的有用方法可以补充从受控的大规模实地研究以及其他有关气候变化研究的实践和理论方法中获得的数据rch。

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