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Soil Organic Carbon Stock and Distribution in Cultivated Land Converted to Grassland in a Subtropical Region of China

机译:亚热带地区退耕还林地土壤有机碳储量与分布

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摘要

Land-use change from one type to another affects soil carbon (C) stocks which is associated with fluxes of CO_2 to the atmosphere. The 10-years converted land selected from previously cultivated land in hilly areas of Sichuan, China was studied to understand the effects of land-use conversion on soil organic casrbon (SOC) sequestration under landscape position influences in a subtropical region of China. The SOC concentrations of the surface soil were greater (P < 0.001) for converted soils than those for cultivated soils but lower (P < 0.001) than those for original uncultivated soils. The SOC inventories (1.90-1.95 kg m~(-2)) in the 0-15 cm surface soils were similar among upper, middle, and lower slope positions on the converted land, while the SOC inventories (1.41-1.65 kg m~(-2)) in this soil layer tended to increase from upper to lower slope positions on the cultivated slope. On the whole, SOC inventories in this soil layer significantly increased following the conversion from cultivated land to grassland (P < 0.001). In the upper slope positions, converted soils (especially in 0-5 cm surface soil) exhibited a higher C/N ratio than cultivated soils (P = 0.012), implying that strong SOC sequestration characteristics exist in upper slope areas where severe soil erosion occurred before land conversion. It is suggested that landscape position impacts on the SOC spatial distribution become insignificant after the conversion of cultivated land to grassland, which is conducive to the immobilization of organic C. We speculate that the conversion of cultivated land to grassland would markedly increase SOC stocks in soil and would especially improve the potential for SOC sequestration in the surface soil over a moderate period of time (10 years).
机译:从一种类型到另一种类型的土地利用变化会影响土壤碳(C)储量,这与CO_2向大气的通量有关。从中国四川亚山丘陵地区以前耕种的土​​地中选择了十年的转化土地进行了研究,以了解在中国亚热带地区景观位置影响下土地利用转化对土壤有机碳(SOC)固存的影响。转化土壤的表层土壤SOC浓度高于耕作土壤(P <0.001),但低于原始未耕种土壤的SOC浓度(P <0.001)。转换土地上上,中,下坡位在0-15 cm表层土壤中的SOC清单(1.90-1.95 kg m〜(-2))相似,而SOC清单(1.41-1.65 kg m〜(-2))相似。 (-2))在耕作坡度上,该土壤层有从上到下坡位置增加的趋势。总体而言,从耕地转为草地后,该土壤层的SOC清单显着增加(P <0.001)。在上坡位置,转化土壤(尤其是0-5 cm表层土壤)的C / N比高于耕作土壤(P = 0.012),这表明在发生严重土壤侵蚀的上坡地区存在强大的SOC固存特性。土地转换之前。耕地转为草地后,景观位置对土壤有机碳空间分布的影响不显着,这有利于有机碳的固定化。我们推测耕地转为草地会明显增加土壤有机碳的储量。并会在一定的时间段(10年)内提高SOC在表层土壤中的固存潜力。

著录项

  • 来源
    《Environmental Management》 |2014年第2期|274-283|共10页
  • 作者单位

    Key Laboratory of Mountain Surface Processes and Ecological Regulation, CAS, Chengdu 610041, People's Republic of China,Institute of Mountain Hazards and Environment, Chinese Academy of Sciences and Ministry of Water Conservancy, P O Box 417, Chengdu 610041, People's Republic of China;

    Key Laboratory of Mountain Surface Processes and Ecological Regulation, CAS, Chengdu 610041, People's Republic of China,Institute of Mountain Hazards and Environment, Chinese Academy of Sciences and Ministry of Water Conservancy, P O Box 417, Chengdu 610041, People's Republic of China;

    Key Laboratory of Mountain Surface Processes and Ecological Regulation, CAS, Chengdu 610041, People's Republic of China,Institute of Mountain Hazards and Environment, Chinese Academy of Sciences and Ministry of Water Conservancy, P O Box 417, Chengdu 610041, People's Republic of China;

    Key Laboratory of Mountain Surface Processes and Ecological Regulation, CAS, Chengdu 610041, People's Republic of China,Institute of Mountain Hazards and Environment, Chinese Academy of Sciences and Ministry of Water Conservancy, P O Box 417, Chengdu 610041, People's Republic of China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Soil organic carbon; Cultivated soil; Land conversion; Landscape position; Soil erosion; Sloping field;

    机译:土壤有机碳;耕地土地流转;景观位置;水土流失;坡地;

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