土壤盐度和氮肥类型对氧化亚氮和氨通量的交互影响

IF 3.1 2区 农林科学 Q2 SOIL SCIENCE
Emrah Ramazanoglu , Vasan Almarie , Mehmet Hadi Suzer , Jun Shan , Zhijun Wei , Mehmet Ali Cullu , Roland Bol , Mehmet Senbayram
{"title":"土壤盐度和氮肥类型对氧化亚氮和氨通量的交互影响","authors":"Emrah Ramazanoglu ,&nbsp;Vasan Almarie ,&nbsp;Mehmet Hadi Suzer ,&nbsp;Jun Shan ,&nbsp;Zhijun Wei ,&nbsp;Mehmet Ali Cullu ,&nbsp;Roland Bol ,&nbsp;Mehmet Senbayram","doi":"10.1016/j.geodrs.2024.e00831","DOIUrl":null,"url":null,"abstract":"<div><p>Soil salinization, impaired by climate change and poor management practices, poses a global threat, particularly in arid and semi-arid regions, leading to significant land degradation. This study aims to investigate the effects of different nitrogen (N) fertilizer sources (urea, ammonium-sulfate, and biogas waste) on CO<sub>2</sub>, N<sub>2</sub>O, and NH<sub>3</sub> emissions and soil enzyme activities in two soil types varying in salinity level (non-saline: EC = 1.15 dS m<sup>−1</sup>, and saline: EC = 35.80 dS m<sup>−1</sup>) in a robotized continuous-flow soil incubation system. Our results showed a sharp increase in N<sub>2</sub>O and CO<sub>2</sub> emissions (up to 0.51 ± 0.02 g N<sub>2</sub>O-N ha<sup>−1</sup> day<sup>−1</sup>, 28.1 ± 3.9 kg CO<sub>2</sub>-C ha<sup>−1</sup> day<sup>−1</sup>) in non-saline soils following soil rewetting, attributed to bacterial denitrification. However, this pattern was not observed in saline soils, suggesting that salinity causes partial inhibition to the regeneration of soil organic matter mineralization and denitrification processes after rewetting. Although salinity did not alter the overall cumulative N<sub>2</sub>O losses in any fertilizer treatment, it significantly delayed the evolution of N<sub>2</sub>O peak during the incubation period. On the other hand, NH<sub>3</sub> volatilization was significantly higher in N-fertilized saline soils compared to non-saline soils (241% and 157% in ammonium-sulfate and biogas waste treatments, respectively), except for urea treatment, likely due to the decrease in nitrification rates. Furthermore, the study clearly showed lower soil enzyme activity levels for both nitrate reductase and urease activity. Interestingly, the lowest NH<sub>3</sub> emissions were measured in urea treatment in both soils. Overall, our findings highlight the complex interplay between soil salinity, nitrogen fertilizer sources, and microbial processes, significantly influencing gaseous nitrogen emissions and N cycling in agricultural soils. Identifying the specific fertilizer treatments that minimize or maximize gaseous nitrogen losses in varying soil salinity, may guide the selection of appropriate fertilization strategies for farmers and policymakers to mitigate environmental impacts of fertilizer use during agricultural production.</p></div>","PeriodicalId":56001,"journal":{"name":"Geoderma Regional","volume":"38 ","pages":"Article e00831"},"PeriodicalIF":3.1000,"publicationDate":"2024-07-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Interactive effects of soil salinity and nitrogen fertilizer types on nitrous oxide and ammonia fluxes\",\"authors\":\"Emrah Ramazanoglu ,&nbsp;Vasan Almarie ,&nbsp;Mehmet Hadi Suzer ,&nbsp;Jun Shan ,&nbsp;Zhijun Wei ,&nbsp;Mehmet Ali Cullu ,&nbsp;Roland Bol ,&nbsp;Mehmet Senbayram\",\"doi\":\"10.1016/j.geodrs.2024.e00831\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Soil salinization, impaired by climate change and poor management practices, poses a global threat, particularly in arid and semi-arid regions, leading to significant land degradation. This study aims to investigate the effects of different nitrogen (N) fertilizer sources (urea, ammonium-sulfate, and biogas waste) on CO<sub>2</sub>, N<sub>2</sub>O, and NH<sub>3</sub> emissions and soil enzyme activities in two soil types varying in salinity level (non-saline: EC = 1.15 dS m<sup>−1</sup>, and saline: EC = 35.80 dS m<sup>−1</sup>) in a robotized continuous-flow soil incubation system. Our results showed a sharp increase in N<sub>2</sub>O and CO<sub>2</sub> emissions (up to 0.51 ± 0.02 g N<sub>2</sub>O-N ha<sup>−1</sup> day<sup>−1</sup>, 28.1 ± 3.9 kg CO<sub>2</sub>-C ha<sup>−1</sup> day<sup>−1</sup>) in non-saline soils following soil rewetting, attributed to bacterial denitrification. However, this pattern was not observed in saline soils, suggesting that salinity causes partial inhibition to the regeneration of soil organic matter mineralization and denitrification processes after rewetting. Although salinity did not alter the overall cumulative N<sub>2</sub>O losses in any fertilizer treatment, it significantly delayed the evolution of N<sub>2</sub>O peak during the incubation period. On the other hand, NH<sub>3</sub> volatilization was significantly higher in N-fertilized saline soils compared to non-saline soils (241% and 157% in ammonium-sulfate and biogas waste treatments, respectively), except for urea treatment, likely due to the decrease in nitrification rates. Furthermore, the study clearly showed lower soil enzyme activity levels for both nitrate reductase and urease activity. Interestingly, the lowest NH<sub>3</sub> emissions were measured in urea treatment in both soils. Overall, our findings highlight the complex interplay between soil salinity, nitrogen fertilizer sources, and microbial processes, significantly influencing gaseous nitrogen emissions and N cycling in agricultural soils. Identifying the specific fertilizer treatments that minimize or maximize gaseous nitrogen losses in varying soil salinity, may guide the selection of appropriate fertilization strategies for farmers and policymakers to mitigate environmental impacts of fertilizer use during agricultural production.</p></div>\",\"PeriodicalId\":56001,\"journal\":{\"name\":\"Geoderma Regional\",\"volume\":\"38 \",\"pages\":\"Article e00831\"},\"PeriodicalIF\":3.1000,\"publicationDate\":\"2024-07-04\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Geoderma Regional\",\"FirstCategoryId\":\"97\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S2352009424000786\",\"RegionNum\":2,\"RegionCategory\":\"农林科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"SOIL SCIENCE\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geoderma Regional","FirstCategoryId":"97","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S2352009424000786","RegionNum":2,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"SOIL SCIENCE","Score":null,"Total":0}
引用次数: 0

摘要

土壤盐碱化受到气候变化和不良管理方法的影响,对全球构成威胁,尤其是在干旱和半干旱地区,导致严重的土地退化。本研究旨在通过机器人连续流土壤培养系统,研究不同氮(N)肥来源(尿素、硫酸铵和沼气废料)对两种不同盐碱度土壤(非盐碱地:EC = 1.15 dS m-1,盐碱地:EC = 35.80 dS m-1)中二氧化碳、一氧化二氮和氮氧化物排放以及土壤酶活性的影响。我们的研究结果表明,土壤复湿后,非盐碱地的 N2O 和 CO2 排放量急剧增加(高达 0.51 ± 0.02 g N2O-N ha-1 day-1,28.1 ± 3.9 kg CO2-C ha-1 day-1),这归因于细菌的反硝化作用。然而,在盐碱土中却观察不到这种模式,这表明盐分会部分抑制土壤有机物矿化再生和土壤复湿后的反硝化过程。虽然盐分没有改变任何肥料处理的总体累积一氧化二氮损失量,但却显著推迟了培育期一氧化二氮峰值的演变。另一方面,与非盐碱地相比,施过氮肥的盐碱地的 NH3 挥发率明显更高(硫酸铵处理和沼气废料处理分别为 241% 和 157%),尿素处理除外,这可能是由于硝化率降低所致。此外,研究清楚地表明,硝酸还原酶和脲酶的土壤酶活性水平都较低。有趣的是,在两种土壤中,尿素处理测得的 NH3 排放量最低。总之,我们的研究结果凸显了土壤盐度、氮肥来源和微生物过程之间复杂的相互作用,对农业土壤中的气态氮排放和氮循环产生了重大影响。确定在不同土壤盐度条件下能使气态氮损失最小或最大的特定肥料处理方法,可指导农民和决策者选择适当的施肥策略,以减轻农业生产过程中化肥使用对环境的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Interactive effects of soil salinity and nitrogen fertilizer types on nitrous oxide and ammonia fluxes

Soil salinization, impaired by climate change and poor management practices, poses a global threat, particularly in arid and semi-arid regions, leading to significant land degradation. This study aims to investigate the effects of different nitrogen (N) fertilizer sources (urea, ammonium-sulfate, and biogas waste) on CO2, N2O, and NH3 emissions and soil enzyme activities in two soil types varying in salinity level (non-saline: EC = 1.15 dS m−1, and saline: EC = 35.80 dS m−1) in a robotized continuous-flow soil incubation system. Our results showed a sharp increase in N2O and CO2 emissions (up to 0.51 ± 0.02 g N2O-N ha−1 day−1, 28.1 ± 3.9 kg CO2-C ha−1 day−1) in non-saline soils following soil rewetting, attributed to bacterial denitrification. However, this pattern was not observed in saline soils, suggesting that salinity causes partial inhibition to the regeneration of soil organic matter mineralization and denitrification processes after rewetting. Although salinity did not alter the overall cumulative N2O losses in any fertilizer treatment, it significantly delayed the evolution of N2O peak during the incubation period. On the other hand, NH3 volatilization was significantly higher in N-fertilized saline soils compared to non-saline soils (241% and 157% in ammonium-sulfate and biogas waste treatments, respectively), except for urea treatment, likely due to the decrease in nitrification rates. Furthermore, the study clearly showed lower soil enzyme activity levels for both nitrate reductase and urease activity. Interestingly, the lowest NH3 emissions were measured in urea treatment in both soils. Overall, our findings highlight the complex interplay between soil salinity, nitrogen fertilizer sources, and microbial processes, significantly influencing gaseous nitrogen emissions and N cycling in agricultural soils. Identifying the specific fertilizer treatments that minimize or maximize gaseous nitrogen losses in varying soil salinity, may guide the selection of appropriate fertilization strategies for farmers and policymakers to mitigate environmental impacts of fertilizer use during agricultural production.

求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
来源期刊
Geoderma Regional
Geoderma Regional Agricultural and Biological Sciences-Soil Science
CiteScore
6.10
自引率
7.30%
发文量
122
审稿时长
76 days
期刊介绍: Global issues require studies and solutions on national and regional levels. Geoderma Regional focuses on studies that increase understanding and advance our scientific knowledge of soils in all regions of the world. The journal embraces every aspect of soil science and welcomes reviews of regional progress.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信