汾河河岸带土壤硝化速率时空分布特征及其影响因子
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山西农业大学城乡建设学院


Spatiotemporal Distribution Characteristics of Soil Nitrification Rate and Influencing Factors in the Fen River Riparian Zone
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College of Urban and Rural Construction, Shanxi Agricultural University

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    摘要:

    水陆交错带是有效拦截径流氮污染物进入水体的最后屏障。硝化作用是土壤氮循环的一个关键过程,研究河岸水陆交错带土壤硝化速率时空分布特征及影响因素有助于了解河岸水陆交错带土壤脱氮作用。选取汾河太原段河岸水陆交错带作为研究对象,通过对距岸边不同距离、不同深度及不同季节的土壤样品进行硝化速率和理化指标的测定分析,揭示河岸水陆交错带土壤硝化速率和理化性质的时空分布特征,通过Spearman相关分析、RDA排序分析及结构方程模型进一步探讨影响土壤硝化速率的主要驱动因子。研究结果表明:(1)研究区水陆交错带土壤含水率、有机质、全氮、铵态氮和硝态氮随距岸边距离的增加而降低,而容重随距岸边距离的增加而增加;土壤含水率、电导率、有机质、全氮、铵态氮、硝态氮随土层深度的增加而降低;夏季土壤含水率、容重、有机质、全氮、硝态氮平均值均低于秋季,铵态氮则高于秋季;(2)土壤硝化速率随距岸边距离的增加呈先升高后降低的趋势,表层土壤硝化速率(20.43 mg·kg-1·d-1)高于底层(8.97 mg·kg-1·d-1);夏季和秋季土壤硝化速率的平均值分别为15.12 mg·kg-1·d-1、14.28 mg·kg-1·d-1;(3)土壤全氮是影响水陆交错带夏季土壤硝化速率的主要影响因子。土壤全氮是影响水陆交错带夏季土壤硝化速率的主要影响因素。综上,在河流氮污染严重的情况下,充分保护1 m以内的水陆交错带,有助于提高河岸带土壤拦截径流氮污染的能力,并为河岸带驳岸生态建设及保护和管理提供科学依据。

    Abstract:

    【Objective】The water-land ecotone is the last barrier to effectively intercept runoff nitrogen pollutants from entering the water body. Nitrification is a key process of soil nitrogen cycle, and studying the temporal and spatial distribution characteristics and influencing factors of soil nitrification rate in riparian water-land ecotone is helpful to understand soil denitrification in riparian water-land ecotone.【Method】In this study, the spatiotemporal distribution characteristics of soil nitrification rate and physicochemical properties in the riparian water-land ecotone of the Taiyuan section of the Fen River were studied by taking soil samples at different distances, depths and in seasons. By measuring and analyzing the nitrification rate and physicochemical indexes, the main driving factors affecting the soil nitrification rate in the riparian water-land ecotone were explored through Spearman correlation analysis, RDA ranking analysis, and structural equation model. 【Result】The results showed that: (1) The soil moisture content, organic matter, total nitrogen, ammonium nitrogen, and nitrate nitrogen in the water-land ecotone decreased as distance from the shore increased while the bulk density increased. Soil moisture content, electrical conductivity, organic matter, total nitrogen, ammonium nitrogen, and nitrate decreased with the increase in soil depth. Also, in summer, the average values of soil moisture content, bulk density, organic matter, total nitrogen, and nitrate were lower than those in autumn, while ammonium nitrogen was higher than that in autumn. (2) The soil nitrification rate increased first and then decreased with the increase in distance from the shore, and the nitrification rate of surface soil (20.43 mg·kg-1·d-1) was higher than that of the lower layer (8.97 mg·kg-1·d-1). In addition, the average soil nitrification rate in summer and autumn was 15.12 mg·kg-1·d-1 and 14.28 mg·kg-1·d-1, respectively. (3) Soil total nitrogen was the main influencing factor affecting the soil nitrification rate in summer in the water-land ecotone.【Conclusion】 In summary, the results of this study show that in the case of serious nitrogen pollution in river water, it is necessary to fully protect the water-land ecotone within 1 m of the waterbody, which will help improve the ability of riparian soil to intercept runoff nitrogen pollution, thereby protecting river water bodies. Thus, this study provides a scientific basis for the ecological construction, protection, and management of riparian ecotone.

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引用本文

迪娅妮,张以柯,张泽文,王春玲.汾河河岸带土壤硝化速率时空分布特征及其影响因子[J].土壤学报,,[待发表]
diyani, zhangyike, zhangzewen, wangchunling. Spatiotemporal Distribution Characteristics of Soil Nitrification Rate and Influencing Factors in the Fen River Riparian Zone[J]. Acta Pedologica Sinica,,[In Press]

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  • 收稿日期:2024-06-11
  • 最后修改日期:2025-02-13
  • 录用日期:2025-03-10
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