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不同土地利用类型土壤温室气体排放对温湿度的响应

桑文秀 杨华蕾 唐剑武

桑文秀, 杨华蕾, 唐剑武. 不同土地利用类型土壤温室气体排放对温湿度的响应[J]. 华东师范大学学报(自然科学版), 2021, (4): 109-120. doi: 10.3969/j.issn.1000-5641.2021.04.013
引用本文: 桑文秀, 杨华蕾, 唐剑武. 不同土地利用类型土壤温室气体排放对温湿度的响应[J]. 华东师范大学学报(自然科学版), 2021, (4): 109-120. doi: 10.3969/j.issn.1000-5641.2021.04.013
SANG Wenxiu, YANG Hualei, TANG Jianwu. Response of soil greenhouse gas emissions to temperature and moisture across different land-use types[J]. Journal of East China Normal University (Natural Sciences), 2021, (4): 109-120. doi: 10.3969/j.issn.1000-5641.2021.04.013
Citation: SANG Wenxiu, YANG Hualei, TANG Jianwu. Response of soil greenhouse gas emissions to temperature and moisture across different land-use types[J]. Journal of East China Normal University (Natural Sciences), 2021, (4): 109-120. doi: 10.3969/j.issn.1000-5641.2021.04.013

不同土地利用类型土壤温室气体排放对温湿度的响应

doi: 10.3969/j.issn.1000-5641.2021.04.013
基金项目: 国家自然科学基金(41571130053)
详细信息
    通讯作者:

    唐剑武, 男, 教授, 博士生导师, 研究方向为全球变化生态学、碳氮循环. E-mail: jwtang@sklec.ecnu.edu.cn

  • 中图分类号: S154.1

Response of soil greenhouse gas emissions to temperature and moisture across different land-use types

  • 摘要: 针对我国南方红壤(江西鹰潭孙家坝小流域)4种不同土地利用类型, 在2019年6—10月开展了室内土壤温湿度控制实验, 采用温室气体分析仪(Picarro-G2508)结合静态箱法对土壤温室气体(CO2、CH4、N2O)排放通量进行同步实时监测, 以研究全球气候变化背景下不同土地利用类型土壤温室气体排放差异及其对温湿度的响应. 结果显示, 4种土地利用类型土壤的全球增温潜势(global warming potential, GWP)从高到低依次为稻田、橘园、林地、旱地, 表明稻田土壤温室气体排放对全球变暖贡献最大. 温控实验中, 土壤呼吸(CO2排放)与土壤温度呈显著正指数相关关系(p < 0.01), 且4种土地利用类型土壤呼吸的温度敏感系数Q10值分别为林地2.61、旱地2.51、橘园3.12、稻田3.17. 其中, 稻田土壤呼吸的温度敏感度最高, 表明稻田土壤具有较高的CO2排放潜力, 而CH4、N2O排放与土壤温度的相关性不显著. 湿度控制实验中, 土壤CO2排放随土壤湿度增加而先升高后降低, 并在土壤湿度20% GWC (gravity water content)时达到最大; 稻田土壤CH4排放与土壤湿度正相关(R2 = 0.8875), 但其他3种土地利用类型土壤CH4排放与土壤湿度不相关; 4种土地利用类型土壤N2O排放通量均随土壤湿度的增加呈先增后减趋势, 并在土壤湿度为25% GWC时达到峰值.
  • 图  1  研究区域采样图

    Fig.  1  Study area

    图  2  不同土地利用类型土壤温室气体排放对土壤温度的响应

    Fig.  2  Response of soil greenhouse gas emission flux to soil temperature across four different land-use types

    图  3  不同土地利用类型土壤温室气体排放对土壤湿度的响应

    Fig.  3  Response of soil greenhouse gases emission flux to soil moisture across four different land-use types

    图  4  不同土地利用类型土壤氧化还原电位与土壤湿度的关系

    Fig.  4  Relationship of soil oxidation-reduction potential and soil moisture across four different land-use types

    图  5  不同土地利用类型土壤GWP对土壤温度的响应

    Fig.  5  Response of soil GWP to soil temperature across four different land-use types

    图  6  不同土地利用类型土壤GWP对土壤湿度的响应

    Fig.  6  Response of soil GWP to soil moisture across four different land-use types

    表  1  土壤初始理化性质

    Tab.  1  Initial soil physicochemical properties of sample plots

    土地利用类型粘粒度/%土壤pH值有机碳/%总氮/%电导率/(S·m–1)土壤容重/ (g·cm–3)土壤湿度/%
    林地48.685 ± 1.1516.33 ± 0.03910.304 ± 0.8181.203 ± 0.1140.037 ± 0.0061.11 ± 0.04816.56 ± 2.06
    旱地33.065 ± 1.1176.83 ± 0.0366.286 ± 0.7010.842 ± 0.0560.033 ± 0.0051.06 ± 0.01913.47 ± 1.70
    橘园19.057 ± 1.0076.66 ± 0.0378.301 ± 0.6470.920 ± 0.1070.027 ± 0.0241.17 ± 0.04514.38 ± 1.26
    稻田14.279 ± 0.5095.50 ± 0.09123.457 ± 1.0200.685 ± 0.0872.335 ± 0.0861.02 ± 0.12925.60 ± 1.11
    注: 稻田土壤容重反映水稻收割后的水平.
    下载: 导出CSV

    表  2  4种土地利用类型土壤呼吸与温度的关系式

    Tab.  2  Equations for soil respiration and temperature across the four land-use types

    土地利用类型方程R2p
    林地y = 0.0230e0.0959x0.833p < 0.0001
    旱地y = 0.0179e0.0920x0.873p < 0.0001
    橘园y = 0.0153e0.1138x0.864p < 0.0001
    稻田y = 0.0221e0.1154x0.822p < 0.0001
    下载: 导出CSV
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