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    放牧对荒漠草原土壤呼吸速率及养分特征的影响

    The effects of grazing on Soil Respiration Rate and Nutrient Characteristics in desert steppes

    • 摘要: 土壤呼吸是表征土壤有机碳周转速率、养分供给潜力及微生物群落活性的核心指标,在维持生态系 统碳平衡中具有关键作用,放牧对土壤呼吸的影响研究存在显著的区域性差异。本研究以宁夏荒漠草原油 蒿(Artemisia ordosica)群落为对象,设置无牧(NG)、轻度放牧(LG)和重度放牧(HG)三种强度,连 续监测生长季土壤呼吸速率及其水热环境,系统分析了放牧对土壤呼吸的作用及影响机制。结果表明: (1)放牧改变了土壤水热环境,土壤温度在生长季呈先升后降趋势,湿度变化趋势与之相反,LG和HG 土壤温度分别较NG提高6.83 %和13.06 %,而湿度则分别提高1.90 %和3.80 %;(2)放牧增加了群落 多样性指数,随放牧强度增加植被盖度、高度和地上生物量显著降低;(3)放牧显著提高了土壤pH、全 磷、碱解氮和容重,而HG处理下土壤速效磷和速效钾较NG分别显著降低43.44 %和37.34 %;(4)土 壤呼吸在生长季呈先升后降动态,初期和末期随放牧强度增加而升高,旺期则相反,且随放牧强度增加年 累积量显著下降,LG和HG分别较NG减少5.18 %和7.37 %;(5)Mantel - test 分析表明土壤呼吸并非 单一因子驱动,受多种因子综合调控。本研究揭示放牧通过改变土壤水热过程和养分格局,间接调控土壤 呼吸及碳循环过程,可为荒漠草原恢复与可持续管理策略制定提供科学依据。

       

      Abstract: Backguound Soil respiration is a core indicator reflecting soil organic carbon turnover rate, nutrient supply potential, and microbial community activity, and it plays a crucial role in maintaining ecosystem carbon balance. However, the effects of grazing on soil respiration show pronounced regional variation. Methods In this study, we examined an Artemisia ordosica community in the desert steppe of Ningxia and established three grazing treatments—no grazing (NG), light grazing (LG), and heavy grazing (HG)—to systematically analyze the impacts of grazing on soil respiration and its underlying mechanisms.. Results (1) Grazing altered the soil hydrothermal environment. Soil temperature exhibited a unimodal pattern during the growing season, while soil moisture showed the opposite trend. Compared with NG, soil temperature under LG and HG increased by 6.83% and 13.06%, respectively, whereas soil moisture increased by 1.90% and 3.80%. (2) Grazing increased community diversity index, while vegetation cover, height, and aboveground biomass declined significantly with increasing grazing intensity; (3) Grazing significantly increased soil pH, total phosphorus, alkali-hydrolyzable nitrogen, and bulk density, while significantly reduced available phosphorus and available potassium, with HG showing decreases of 43.44% and 37.34% relative to NG. (4) Soil respiration displayed a unimodal seasonal pattern, increasing with grazing intensity during the early and late growing season but showing the opposite trend during the peak season. Annual cumulative soil respiration decreased significantly with grazing intensity, with LG and HG 5.18% and 7.37% lower than NG; (5) Mantel test analysis revealed that soil respiration was not driven by a single factor but jointly regulated by multiple variables. Conclusion This study demonstrates that grazing regulates soil respiration and carbon cycling processes indirectly by modifying soil hydrothermal dynamics and nutrient patterns, which can provide a scientific basis for desert steppe restoration and sustainable grassland management.

       

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