2026年10月18日 星期日
宁夏第三排水沟岸边带植物根系土壤脱氮差异及影响因子分析
Analyses on the nitrogen removal differences and the influencing factors of soils around riparian plant roots in the Third Drainage Ditch in Ningxia
2026年 第35卷 第5期 页码[63-73]    下载全文[3.2MB]  

摘要

为探究宁夏第三排水沟岸边带典型植物根系土壤脱氮贡献差异及影响因子,以第三排水沟岸边带的芦苇〔Phragmites australis (Cav.) Trin. ex Steud.〕、地肤〔Bassia scoparia (Linn.) A. J. Scott〕和马蔺(Iris lactea Pall.)为研究对象,采用15N同位素示踪法,分析植物根系土壤的反硝化和厌氧氨氧化速率、脱氮贡献及相关影响因子。结果表明:芦苇根系土壤的NH+4-N含量、NO-3-N含量、NO-2-N含量、总有机碳含量、总氮含量和C/N比均显著(P<0.05)高于马蔺和地肤根系土壤,地肤根系土壤的pH值和电导率显著高于芦苇和马蔺根系土壤;3种植物根系土壤反硝化菌的丰富度和多样性均高于厌氧氨氧化菌。芦苇、马蔺、地肤根系土壤的反硝化速率分别为2.397、2.137和1.479 μmol·kg-1·h-1,厌氧氨氧化速率分别为0.650、0.479和0.405 μmol·kg-1·h-1,三者根系土壤的反硝化脱氮贡献率(78.52%~81.70%)均大于厌氧氨氧化(18.30%~21.48%)。土壤反硝化速率和厌氧氨氧化速率与NH+4-N含量、NO-3-N含量、总有机碳含量和含水量呈显著或极显著(P<0.01)正相关,而与pH值和电导率呈显著或极显著负相关。反硝化菌优势属金黄杆形菌属(Luteitalea)、亚硝化球菌属(Nitrososphaera)、盖亚菌属(Gaiella)和红长命菌属(Rubrivivax)及厌氧氨氧化菌属Candidatus Brocadia和Candidatus Jettenia的相对丰度与对应的脱氮速率呈显著或极显著正相关。反硝化功能基因nirS和厌氧氨氧化功能基因AMX16S的丰度分别与对应的脱氮速率呈显著正相关。综上所述,反硝化是植物根系土壤主要脱氮途径,芦苇根系土壤脱氮速率最高,土壤理化性质、细菌群落及其功能基因共同调控土壤的脱氮过程。

Abstract

To investigate the differences in nitrogen removal contribution and the influencing factors of soils around typical plant roots in the riparian zone of the Third Drainage Ditch in Ningxia, Phragmites australis (Cav.) Trin. ex Steud., Bassia scoparia (Linn.) A. J. Scott, and Iris lactea Pall. in the riparian zone of the Third Drainage Ditch were taken as research materials, the denitrification and anaerobic ammonium oxidation rates, nitrogen removal contributions, and related influencing factors of soils around plant roots were analyzed by using the 15N isotope tracer method. The results show that the NH+4-N content, NO-3-N content, NO-2-N content, total organic corbon content, total nitrogen content, and C/N ratio of soils around P. australis roots are significantly (P<0.05) higher than those of soils around I. lactea and B. scoparia roots, while the pH value and electrical conductivity of soils around B. scoparia roots are significantly higher than those of soils around P. australis and I. lactea roots; the richness and diversity of denitrification bacteria in soils around the three plant roots are higher than those of anaerobic ammonium oxidation bacteria. The denitrification rates of soils around P. australis, I. lactea, and B. scoparia roots are 2.397, 2.137, and 1.479 μmol·kg-1·h-1, respectively, the anaerobic ammonium oxidation rates are 0.650, 0.479, and 0.405 μmol·kg-1·h-1, respectively, and the denitrification nitrogen removal contribution rates (78.52%-81.70%) of soils around the three plant roots are all greater than those of anaerobic ammonium oxidation (18.30%-21.48%). Soil denitrification rate and anaerobic ammonium oxidation rate show significant or extremely significant (P<0.01) positive correlations with NH+4-N content, NO-3-N content, total organic carbon content, and water content, while showing significant or extremely significant negative correlations with pH value and electrical conductivity. The relative abundances of dominant genera of denitrification bacteria Luteitalea, Nitrososphaera, Gaiella, and Rubrivivax, and anaerobic ammonium oxidation bacterial genera Candidatus Brocadia and Candidatus Jettenia show significant or extremely significant positive correlations with the corresponding nitrogen removal rates. The abundance of the denitrification functional gene nirS and the anaerobic ammonium oxidation functional gene AMX16S show significant positive correlations with the corresponding nitrogen removal rates. In conclusion, denitrification is the main nitrogen removal pathway in soils around plant roots, with soils around P. australis roots having the highest nitrogen removal rate, and soil physical and chemical properties, microbial communities, and their functional genes jointly regulate the soil nitrogen removal process.

 

 

关键词根系土壤; 反硝化速率; 厌氧氨氧化速率; 土壤理化性质; 细菌群落; 第三排水沟
Key wordssoil around roots; denitrification rate; anaerobic ammonium oxidation rate; soil physical and chemical properties; bacterial community; Third Drainage Ditch
作者杜晓蕊, 郑兰香, 祁若曈, 孙华琳
所在单位宁夏大学生态环境学院, 宁夏 银川 750021
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基金项目国家自然科学基金项目(42267011); 宁夏自然科学基金项目(2026AAC030138)