ISSN 1000-3665 CN 11-2202/P

    包气带反硝化强度空间分布规律的整合分析

    Meta-analysis of the spatial distribution of denitrification intensity in the vadose zone

    • 摘要: 依据1970~2017年间发表的3955篇包气带反硝化强度相关论文, 筛选出197组反硝化强度数据, 利用整合分析, 重点研究了包气带反硝化强度在典型生态类型(水平)和不同采样深度(垂向)的空间分布规律, 识别了包气带反硝化强度的主控因素并研究其函数关系。结果表明:水平空间上, 包气带表层0~0.5 m反硝化强度的分布特征显著, 由大到小排序为:森林(8.03±0.21 mg/(kg·d))、农田(3.54±0.08 mg/(kg·d))、草地(3.38±0.12 mg/(kg·d))、湿地(2.32±0.23 mg/(kg·d))、沙漠(2.15±0.56 mg/(kg·d))。垂向空间上(6 m内), 各生态类型反硝化强度随深度的增加均呈“S”型变化规律。不同生态类型和不同采样深度下包气带反硝化强度的主控因素存在一定差异, 主要为黏粒、有机质、全氮、硝态氮、有效磷, 并给出了包气带反硝化强度与主控因素的回归方程。

       

      Abstract: In this paper, the denitrification intensity data of 197 groups are screened out according to 3955 papers on the vadose zones published from 1970 to 2017. Based on the meta-analysis, the spatial distribution of denitrification intensity in typical ecological types (horizontal) and different sampling depths (vertical) is studied emphatically, the main factors of denitrification intensity in the vadose zone are analyzed and their function relations are studied. The regression function is used to obtain the denitrification intensity relation of the vadose zone. The results show that in the horizontal direction, the distribution characteristics of denitrification intensity of 0~0.5 m in the vadose zone are significant, which are sorted from big to small as follows: forest (8.03±0.21 mg/(kg·d)), farmland (3.54±0.08 mg/(kg·d)), grassland (3.38±0.12 mg/(kg·d)), wetland (2.32±0.23 mg/(kg·d)), and desert (2.15±0.56 mg/(kg·d)). In the vertical direction (within 6 m), the denitrification intensity of each ecological type is of the "S" type with the increasing depth. There are some differences in the main controlling factors of the denitrification intensity in the vadose zone under different ecological types and sampling depths, including clay, organic matter, total nitrogen, nitrate nitrogen and available phosphorus. The regression equation between the denitrification intensity and the main controlling factors in the vadose zone is given.

       

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