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Long-term active restoration of extremely degraded alpine grassland accelerated turnover and increased stability of soil carbon

机译:长期积极恢复极低的高山草地加速周转,增加土壤碳的稳定性

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摘要

Soil nutrient contents and organic carbon (C) stability are key indicators for restoration of degraded grassland. However, the effects of long-term active restoration of extremely degraded grassland on soil parameters have been equivocal. The aims of this study were to evaluate the impact of active restoration of degraded alpine grassland on: (a) soil organic matter (SOM) mineralization; and (b) the importance of biotic factors for temperature sensitivity (Q(10)) of SOM mineralization. Soils were sampled from intact, degraded and restored alpine grasslands at altitudes ranging between 3,900 and 4,200 m on the Tibetan Plateau. The samples were incubated at 5, 15 and 25 degrees C, andQ(10)values of SOM mineralization were determined. Structural equation modeling was used to evaluate the importance of vegetation, soil physico-chemical properties and microbial parameters forQ(10)regulation. TheQ(10)of N mineralization was similar among intact, degraded and restored soils (0.84-1.24) and was higher in topsoil (1.09) than in subsoil (0.92). The best predictive factor of CO2-Q(10)for intact grassland was microbial biomass, for degraded grassland was basal microbial respiration, and for restored grassland was soil bulk density. Restoration by planting vegetation decreased theQ(10)of SOM mineralization as soil bulk density, the most important negative predictor, increased in restored grassland. TheQ(10)of SOM mineralization in topsoil was 14% higher than in subsoil because of higher microbial abundance and exo-enzyme activities. The NH(4)(+)content was greatest in intact soil, while NO(3)(-)content was greatest in degraded soil. The SOM mineralization rate decreased with grassland degradation and increased after long-term (>10 years) restoration. In conclusion, extremely degraded grassland needs proper long-term management in active restoration projects, especially for improvement of soil nutrients in a harsh environment.
机译:土壤养分含量和有机碳(C)稳定性是用于恢复退化草地的关键指标。然而,长期主动恢复极值恢复极值恢复在土壤参数上的土壤参数上具有等因素。本研究的目的是评估积极恢复降解的高山草地的影响:(a)土壤有机物(SOM)矿化; (b)SOM矿化温度敏感性(Q(10))的生物敏感性的重要性。在藏高高原的高度范围内,土壤从完整,降解和恢复的高山草原上取样,在藏高的高原上的3,900至4,200米之间。将样品在5,15和25℃温育,测定SOM矿化的Q(10)值。结构方程建模用于评估植被,土壤物理化学性质和微生物参数对Q(10)调节的重要性。 N矿化的Q(10)在完整性,降解和恢复的土壤中相似(0.84-1.24),表土较高(1.09),而不是在底土(0.92)。对于完整草地的CO2-Q(10)的最佳预测因素是微生物生物质,用于降解草地是基础微生物呼吸,而恢复的草原是土壤堆积密度。通过种植植被恢复降低SOM矿化作为土壤堆积密度,最重要的负面预测因子,在恢复的草地上增加。由于更高的微生物丰度和外酶活性,SOM矿化的SOM矿化的Q(10)矿化高出14%。在完整的土壤中,NH(4)(+)含量最大,而NO(3)( - )含量在降解的土壤中最大。 SOM矿化率随草地降解而降低,长期(> 10年)恢复后增加。总之,极其退化的草原需要适当的长期管理在积极恢复项目中,特别是改善恶劣环境中的土壤营养素。

著录项

  • 来源
    《Global change biology》 |2020年第12期|共12页
  • 作者单位

    Lanzhou Univ Sch Life Sci State Key Lab Grassland Agroecosyst Lanzhou 730000 Peoples R China;

    Lanzhou Univ Sch Life Sci State Key Lab Grassland Agroecosyst Lanzhou 730000 Peoples R China;

    Ben Gurion Univ Negev Blaustein Inst Desert Res Wyler Dept Dryland Agr Desert Anim Adaptat &

    Husb Beer Sheva Israel;

    Natl Agr Res Ctr Rangeland Res Inst Islamabad Pakistan;

    Univ Gottingen Dept Agr Soil Sci Dept Soil Sci Temperate Ecosyst Gottingen Germany;

    Lanzhou Univ Inst Innovat Ecol State Key Lab Grassland Agroecosyst Lanzhou Peoples R China;

    Chinese Acad Sci Northwest Inst Ecoenvironm &

    Resources Urat Desert Grassland Res Stn Lanzhou Peoples R China;

    Lanzhou Univ Sch Life Sci State Key Lab Grassland Agroecosyst Lanzhou 730000 Peoples R China;

    Lanzhou Univ Sch Life Sci State Key Lab Grassland Agroecosyst Lanzhou 730000 Peoples R China;

    Lanzhou Univ Sch Life Sci State Key Lab Grassland Agroecosyst Lanzhou 730000 Peoples R China;

    Lanzhou Univ Sch Life Sci State Key Lab Grassland Agroecosyst Lanzhou 730000 Peoples R China;

    Lanzhou Univ Sch Life Sci State Key Lab Grassland Agroecosyst Lanzhou 730000 Peoples R China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 物候学;生物科学;
  • 关键词

    active restoration; soil organic matter mineralization; soil warming; structural equation model; Tibetan grassland; topsoil and subsoil;

    机译:活跃恢复;土壤有机质矿化;土变暖;结构方程模型;藏草原;表土和底土;

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