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Effects of cultivation and abandonment on soil carbon content of subalpine meadows, northwest China

机译:种植和废弃对西北亚高山草甸土壤碳含量的影响

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摘要

Purpose Land use changes have a significant impact on soil carbon emission and sequestration worldwide. Accurate evaluation of the effect of land use change (cultivation and abandonment) on soil carbon content of subalpine meadows is required to monitor the soil carbon dynamics of rangeland ecosystems in China. Materials and methods Based on collection of soil cores and vegetation, investigations of four types of land use (undisturbed natural meadow, land cultivated for 20 years, land abandoned for 3 years following cultivation, and land abandoned for 10 years following cultivation) were undertaken in the headwater area of the Heihe River in northwest China. Three soil carbon fractions [soil organic carbon (SOC), light fraction organic carbon (LFOC), and microorganism biomass carbon (MBC)] were determined in the laboratory, and the relative abundances of LFOC/ SOC and MBC/SOC were calculated. Results and discussion Repeated cultivation by ploughing reduced the carbon content of the top soil layer, resulting in more uniform vertical distribution of soil organic matter. Ten years after cessation of cultivation, the organic carbon content within the top 10-cm soil layer (0-10 cm) had reached 90 % of the content in native meadows, equivalent to a mean annual sequestration rate of 1.73 tC ha~(-1). The rate of LFOC restoration was faster than that of SOC restoration. The variation in the ratio of MBC to SOC (0.91-1.07 %) was small. Conclusions The activity of cultivation reduced all indicators of soil carbon status, which were not completely restored to the level of natural meadow, even after abandonment of cultivation for 10 years. Nevertheless, abandonment of cultivation is a practical, even if long-term, means of improving carbon sequestration in subalpine meadow of China.
机译:目的土地用途的变化对全世界的土壤碳排放和封存产生重大影响。需要准确评估土地利用变化(耕种和废弃)对亚高山草甸土壤碳含量的影响,以监测中国牧场生态系统的土壤碳动态。材料和方法在收集土壤核心和植被的基础上,对四种土地利用类型(未受干扰的天然草地,耕种20年的土地,耕种后3年的土地和耕种后10年的土地)进行了调查。中国西北黑河的源头地区。在实验室中确定了三种土壤碳组分[土壤有机碳(SOC),轻质有机碳(LFOC)和微生物生物量碳(MBC)],并计算了LFOC / SOC和MBC / SOC的相对丰度。结果与讨论耕作的重复耕作减少了土壤表层的碳含量,从而使土壤有机质的垂直分布更加均匀。停止耕种十年后,最高10厘米土壤层(0-10厘米)内的有机碳含量已达到天然草地含量的90%,相当于每年平均固存率为1.73 tC ha〜(- 1)。 LFOC的恢复速率比SOC的恢复速率快。 MBC与SOC的比率(0.91-1.07%)的变化很小。结论耕作活动降低了土壤碳素状况的所有指标,即使放弃耕种10年也不能完全恢复到天然草甸的水平。然而,抛弃耕作是改善中国亚高山草甸碳固存的一种实用的方法,即使是长期的方法。

著录项

  • 来源
    《Journal of soil & sediments》 |2012年第6期|826-834|共9页
  • 作者单位

    International Centre for Tibetan Plateau Ecosystem Management, State Key Laboratory of Grassland Farming Systems, College of Pastoral Agriculture Science and Technology, Lanzhou University, No.768, Jiayuguan Western Road, Lanzhou City, Gansu Province 730020, People's Republic of China,Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, No. 18, Shuangqing Road, Haidian District, Beijing 100085, People's Republic of China;

    International Centre for Tibetan Plateau Ecosystem Management, State Key Laboratory of Grassland Farming Systems, College of Pastoral Agriculture Science and Technology, Lanzhou University, No.768, Jiayuguan Western Road, Lanzhou City, Gansu Province 730020, People's Republic of China;

    Institute of Arid Agroecology, School of Life Sciences, Lanzhou University, No. 222, Tianhsui Southern Road, Lanzhou City, Gansu Province 73000, People's Republic of China;

    International Centre for Tibetan Plateau Ecosystem Management, State Key Laboratory of Grassland Farming Systems, College of Pastoral Agriculture Science and Technology, Lanzhou University, No.768, Jiayuguan Western Road, Lanzhou City, Gansu Province 730020, People's Republic of China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Abandonment; Cultivation; Northwest China; Soil organic carbon; Subalpine meadow;

    机译:放弃;培养;中国西北;土壤有机碳;亚高山草甸;

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