{"title":"盐渍化农业沟渠中硝酸盐的来源和转化途径:沿不同盐度梯度的生物地球化学响应","authors":"Shenhao Qu, Dongli She, Yongchun Pan, Alimu Abulaiti, Peng Chen, Zhenqi Shi, Lei Hu, Yongqiu Xia","doi":"10.1007/s10533-026-01318-y","DOIUrl":null,"url":null,"abstract":"<div><p>Agricultural nitrate pollution, largely associated with high-intensity fertilizer application and untreated or insufficiently treated waste inputs, has become a major driver of water quality degradation worldwide. Agricultural ditches, as key recipients of surface runoff and lateral seepage, function as both transport conduits and biogeochemical hotspots for nitrogen transformation. In salt-affected ditches, high nitrogen inputs and salinity can interact to enhance nitrate accumulation and mobility, thereby increasing the potential for downstream transport. To bridge this knowledge gap, we investigated two representative saline agricultural ditches located in northwestern China, a region characterized by an arid climate and saline–alkaline soils. We employed stable isotope analysis (δ<sup>15</sup>N-NO<sub>3</sub><sup>–</sup> and δ<sup>18</sup>O-NO<sub>3</sub><sup>–</sup>) combined with a Bayesian stable isotope mixing model (MixSIAR) to identify nitrate sources and transformation pathways. Results showed that manure and sewage (M&S) and chemical fertilizer (CF) were the dominant contributors, accounting for 42.6% and 42.1%, respectively, in the first ditch and 43.8% and 36.0% in the fifth ditch. Soil nitrogen (SN) contributed relatively less (15.3% and 20.2%, respectively). The results of both nitrate isotope analysis and chloride ion tracing revealed that the nitrate in the ditches originated primarily from agricultural activities and anthropogenic discharge. Interestingly, the nitrate transformation pathways differed notably between the two ditches, which is primarily driven by variations in nitrogen substrate availability and salinity levels. Hydrochemical and isotopic patterns suggest reduced nitrate removal potential under higher salinity, consistent with constraints on microbial nitrate reduction. These findings highlight the pivotal role of salinity in influencing nitrogen cycling and underscore the need for integrated management strategies that simultaneously address nutrient inputs and control salinity. Effective mitigation measures should prioritize seasonal fertilizer management and manure handling improvement, especially during winter irrigation periods when residual nutrients are mobilized. In addition, adaptive drainage strategies are needed to maintain nitrate removal efficiency under increasing salinity stress. This study provides isotope-based constraints to support science-based policymaking and adaptive water governance under salinization pressure.</p></div>","PeriodicalId":8901,"journal":{"name":"Biogeochemistry","volume":"169 2","pages":""},"PeriodicalIF":3.7000,"publicationDate":"2026-03-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://link.springer.com/content/pdf/10.1007/s10533-026-01318-y.pdf","citationCount":"0","resultStr":"{\"title\":\"Nitrate sources and transformation pathways in salt-affected agricultural ditches: biogeochemical responses along contrasting salinity gradients\",\"authors\":\"Shenhao Qu, Dongli She, Yongchun Pan, Alimu Abulaiti, Peng Chen, Zhenqi Shi, Lei Hu, Yongqiu Xia\",\"doi\":\"10.1007/s10533-026-01318-y\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Agricultural nitrate pollution, largely associated with high-intensity fertilizer application and untreated or insufficiently treated waste inputs, has become a major driver of water quality degradation worldwide. Agricultural ditches, as key recipients of surface runoff and lateral seepage, function as both transport conduits and biogeochemical hotspots for nitrogen transformation. In salt-affected ditches, high nitrogen inputs and salinity can interact to enhance nitrate accumulation and mobility, thereby increasing the potential for downstream transport. To bridge this knowledge gap, we investigated two representative saline agricultural ditches located in northwestern China, a region characterized by an arid climate and saline–alkaline soils. We employed stable isotope analysis (δ<sup>15</sup>N-NO<sub>3</sub><sup>–</sup> and δ<sup>18</sup>O-NO<sub>3</sub><sup>–</sup>) combined with a Bayesian stable isotope mixing model (MixSIAR) to identify nitrate sources and transformation pathways. Results showed that manure and sewage (M&S) and chemical fertilizer (CF) were the dominant contributors, accounting for 42.6% and 42.1%, respectively, in the first ditch and 43.8% and 36.0% in the fifth ditch. Soil nitrogen (SN) contributed relatively less (15.3% and 20.2%, respectively). The results of both nitrate isotope analysis and chloride ion tracing revealed that the nitrate in the ditches originated primarily from agricultural activities and anthropogenic discharge. Interestingly, the nitrate transformation pathways differed notably between the two ditches, which is primarily driven by variations in nitrogen substrate availability and salinity levels. Hydrochemical and isotopic patterns suggest reduced nitrate removal potential under higher salinity, consistent with constraints on microbial nitrate reduction. These findings highlight the pivotal role of salinity in influencing nitrogen cycling and underscore the need for integrated management strategies that simultaneously address nutrient inputs and control salinity. Effective mitigation measures should prioritize seasonal fertilizer management and manure handling improvement, especially during winter irrigation periods when residual nutrients are mobilized. In addition, adaptive drainage strategies are needed to maintain nitrate removal efficiency under increasing salinity stress. This study provides isotope-based constraints to support science-based policymaking and adaptive water governance under salinization pressure.</p></div>\",\"PeriodicalId\":8901,\"journal\":{\"name\":\"Biogeochemistry\",\"volume\":\"169 2\",\"pages\":\"\"},\"PeriodicalIF\":3.7000,\"publicationDate\":\"2026-03-09\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://link.springer.com/content/pdf/10.1007/s10533-026-01318-y.pdf\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Biogeochemistry\",\"FirstCategoryId\":\"93\",\"ListUrlMain\":\"https://link.springer.com/article/10.1007/s10533-026-01318-y\",\"RegionNum\":3,\"RegionCategory\":\"环境科学与生态学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"2026/3/30 0:00:00\",\"PubModel\":\"Epub\",\"JCR\":\"Q2\",\"JCRName\":\"ENVIRONMENTAL SCIENCES\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Biogeochemistry","FirstCategoryId":"93","ListUrlMain":"https://link.springer.com/article/10.1007/s10533-026-01318-y","RegionNum":3,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"2026/3/30 0:00:00","PubModel":"Epub","JCR":"Q2","JCRName":"ENVIRONMENTAL SCIENCES","Score":null,"Total":0}
Nitrate sources and transformation pathways in salt-affected agricultural ditches: biogeochemical responses along contrasting salinity gradients
Agricultural nitrate pollution, largely associated with high-intensity fertilizer application and untreated or insufficiently treated waste inputs, has become a major driver of water quality degradation worldwide. Agricultural ditches, as key recipients of surface runoff and lateral seepage, function as both transport conduits and biogeochemical hotspots for nitrogen transformation. In salt-affected ditches, high nitrogen inputs and salinity can interact to enhance nitrate accumulation and mobility, thereby increasing the potential for downstream transport. To bridge this knowledge gap, we investigated two representative saline agricultural ditches located in northwestern China, a region characterized by an arid climate and saline–alkaline soils. We employed stable isotope analysis (δ15N-NO3– and δ18O-NO3–) combined with a Bayesian stable isotope mixing model (MixSIAR) to identify nitrate sources and transformation pathways. Results showed that manure and sewage (M&S) and chemical fertilizer (CF) were the dominant contributors, accounting for 42.6% and 42.1%, respectively, in the first ditch and 43.8% and 36.0% in the fifth ditch. Soil nitrogen (SN) contributed relatively less (15.3% and 20.2%, respectively). The results of both nitrate isotope analysis and chloride ion tracing revealed that the nitrate in the ditches originated primarily from agricultural activities and anthropogenic discharge. Interestingly, the nitrate transformation pathways differed notably between the two ditches, which is primarily driven by variations in nitrogen substrate availability and salinity levels. Hydrochemical and isotopic patterns suggest reduced nitrate removal potential under higher salinity, consistent with constraints on microbial nitrate reduction. These findings highlight the pivotal role of salinity in influencing nitrogen cycling and underscore the need for integrated management strategies that simultaneously address nutrient inputs and control salinity. Effective mitigation measures should prioritize seasonal fertilizer management and manure handling improvement, especially during winter irrigation periods when residual nutrients are mobilized. In addition, adaptive drainage strategies are needed to maintain nitrate removal efficiency under increasing salinity stress. This study provides isotope-based constraints to support science-based policymaking and adaptive water governance under salinization pressure.
期刊介绍:
Biogeochemistry publishes original and synthetic papers dealing with biotic controls on the chemistry of the environment, or with the geochemical control of the structure and function of ecosystems. Cycles are considered, either of individual elements or of specific classes of natural or anthropogenic compounds in ecosystems. Particular emphasis is given to coupled interactions of element cycles. The journal spans from the molecular to global scales to elucidate the mechanisms driving patterns in biogeochemical cycles through space and time. Studies on both natural and artificial ecosystems are published when they contribute to a general understanding of biogeochemistry.