磷的供应和空间分布决定了微生物对碳氮添加的响应

IF 6.6 1区 农林科学 Q1 SOIL SCIENCE
Sara L. Bauke , Ye Wang , Steffen A. Schweizer , Carmen Hoeschen , Jan Wolff , Sabine J. Seidel , Christian von Sperber , Wulf Amelung
{"title":"磷的供应和空间分布决定了微生物对碳氮添加的响应","authors":"Sara L. Bauke ,&nbsp;Ye Wang ,&nbsp;Steffen A. Schweizer ,&nbsp;Carmen Hoeschen ,&nbsp;Jan Wolff ,&nbsp;Sabine J. Seidel ,&nbsp;Christian von Sperber ,&nbsp;Wulf Amelung","doi":"10.1016/j.geoderma.2025.117493","DOIUrl":null,"url":null,"abstract":"<div><div>Phosphorus (P) supply can limit microbial activity especially under conditions of high carbon (C) and nitrogen (N) supply, but this observation is mostly based on analyses of topsoil bulk samples, while processes in the subsoil or at the microscale remain largely unexplored. Here, we collected topsoil (0–30 cm) and subsoil (&gt;30 cm) samples from two temperate forest and two arable sites (Cambisols and Luvisols with pH 4.2 to 7.0 and C content of 2 to 113 g kg<sup>−1</sup>), to provide a set of model soil samples with varying P content and varying contributions of organic and mineral P forms. We conducted an incubation experiment at 20 °C for 16 weeks with addition of either glucose (C treatment), ammonium nitrate (N treatment), both glucose and ammonium nitrate (CN treatment), or without additions (control). In a separate incubation of topsoil samples with CN addition and <sup>18</sup>O labeled water, we analyzed microsite enrichment with <sup>18</sup>O as an indicator of microbial activity using nanoscale secondary ion mass spectrometry (NanoSIMS). Soil respiration rates were significantly increased after C and CN addition but not after N addition, and organic P mineralization by acid phosphatase was also enhanced with CN addition. However, the response in respiration rates after CN addition in topsoil samples decreased with increasing soil C:P ratio, while acid phosphatase activity increased, indicating increasing P limitation and mineralization of organic P in samples with low P supply (wide C:P ratio). In the subsoil samples, the response in microbial and enzymatic activity was weaker, but showed a similar trend as in topsoils. NanoSIMS analyses indicated <sup>18</sup>O enrichment especially in P-rich microsites of soils with low P content and in co-location with patches dominated by organic matter. We conclude that also at the microsite level, under conditions of high C and N supply, microbial activity is controlled by the inherent supply of P in both arable and forest soils studied here.</div></div>","PeriodicalId":12511,"journal":{"name":"Geoderma","volume":"461 ","pages":"Article 117493"},"PeriodicalIF":6.6000,"publicationDate":"2025-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Phosphorus supply and spatial distribution determine the microbial response to carbon and nitrogen addition\",\"authors\":\"Sara L. Bauke ,&nbsp;Ye Wang ,&nbsp;Steffen A. Schweizer ,&nbsp;Carmen Hoeschen ,&nbsp;Jan Wolff ,&nbsp;Sabine J. Seidel ,&nbsp;Christian von Sperber ,&nbsp;Wulf Amelung\",\"doi\":\"10.1016/j.geoderma.2025.117493\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Phosphorus (P) supply can limit microbial activity especially under conditions of high carbon (C) and nitrogen (N) supply, but this observation is mostly based on analyses of topsoil bulk samples, while processes in the subsoil or at the microscale remain largely unexplored. Here, we collected topsoil (0–30 cm) and subsoil (&gt;30 cm) samples from two temperate forest and two arable sites (Cambisols and Luvisols with pH 4.2 to 7.0 and C content of 2 to 113 g kg<sup>−1</sup>), to provide a set of model soil samples with varying P content and varying contributions of organic and mineral P forms. We conducted an incubation experiment at 20 °C for 16 weeks with addition of either glucose (C treatment), ammonium nitrate (N treatment), both glucose and ammonium nitrate (CN treatment), or without additions (control). In a separate incubation of topsoil samples with CN addition and <sup>18</sup>O labeled water, we analyzed microsite enrichment with <sup>18</sup>O as an indicator of microbial activity using nanoscale secondary ion mass spectrometry (NanoSIMS). Soil respiration rates were significantly increased after C and CN addition but not after N addition, and organic P mineralization by acid phosphatase was also enhanced with CN addition. However, the response in respiration rates after CN addition in topsoil samples decreased with increasing soil C:P ratio, while acid phosphatase activity increased, indicating increasing P limitation and mineralization of organic P in samples with low P supply (wide C:P ratio). In the subsoil samples, the response in microbial and enzymatic activity was weaker, but showed a similar trend as in topsoils. NanoSIMS analyses indicated <sup>18</sup>O enrichment especially in P-rich microsites of soils with low P content and in co-location with patches dominated by organic matter. We conclude that also at the microsite level, under conditions of high C and N supply, microbial activity is controlled by the inherent supply of P in both arable and forest soils studied here.</div></div>\",\"PeriodicalId\":12511,\"journal\":{\"name\":\"Geoderma\",\"volume\":\"461 \",\"pages\":\"Article 117493\"},\"PeriodicalIF\":6.6000,\"publicationDate\":\"2025-09-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Geoderma\",\"FirstCategoryId\":\"97\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0016706125003349\",\"RegionNum\":1,\"RegionCategory\":\"农林科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"SOIL SCIENCE\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geoderma","FirstCategoryId":"97","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0016706125003349","RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"SOIL SCIENCE","Score":null,"Total":0}
引用次数: 0

摘要

磷(P)供应可以限制微生物活动,特别是在高碳(C)和高氮(N)供应的条件下,但这一观察主要基于对表土散装样品的分析,而底土或微观尺度的过程在很大程度上尚未探索。在这里,我们收集了两个温带森林和两个耕地的表层土壤(0-30 cm)和底土(>30 cm)样品(Cambisols和Luvisols, pH为4.2至7.0,C含量为2至113 g kg - 1),以提供一组具有不同P含量和不同贡献的有机和矿物P形式的模型土壤样品。我们在20℃下进行了16周的孵育实验,分别添加葡萄糖(C处理)、硝酸铵(N处理)、葡萄糖和硝酸铵(CN处理),或不添加任何添加剂(对照)。在添加CN和18O标记水的表土样品的单独孵育中,我们使用纳米二级离子质谱(NanoSIMS)分析了18O作为微生物活性指标的微位点富集情况。添加C和CN显著提高了土壤呼吸速率,但添加N后没有显著提高;添加CN也促进了酸性磷酸酶对有机磷的矿化作用。表层土壤添加CN后呼吸速率的响应随土壤C:P比的增加而降低,酸性磷酸酶活性增加,表明低磷供应(宽C:P比)样品的磷限制和有机磷矿化程度增加。在底土样品中,微生物和酶活性的响应较弱,但表现出与表土相似的趋势。NanoSIMS分析表明,18O在富磷土壤中富集,特别是在低磷土壤和与有机质为主的斑块共存的土壤中。结果表明,在高碳、高氮供给条件下,土壤微生物活性受土壤磷的内在供给控制。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Phosphorus supply and spatial distribution determine the microbial response to carbon and nitrogen addition
Phosphorus (P) supply can limit microbial activity especially under conditions of high carbon (C) and nitrogen (N) supply, but this observation is mostly based on analyses of topsoil bulk samples, while processes in the subsoil or at the microscale remain largely unexplored. Here, we collected topsoil (0–30 cm) and subsoil (>30 cm) samples from two temperate forest and two arable sites (Cambisols and Luvisols with pH 4.2 to 7.0 and C content of 2 to 113 g kg−1), to provide a set of model soil samples with varying P content and varying contributions of organic and mineral P forms. We conducted an incubation experiment at 20 °C for 16 weeks with addition of either glucose (C treatment), ammonium nitrate (N treatment), both glucose and ammonium nitrate (CN treatment), or without additions (control). In a separate incubation of topsoil samples with CN addition and 18O labeled water, we analyzed microsite enrichment with 18O as an indicator of microbial activity using nanoscale secondary ion mass spectrometry (NanoSIMS). Soil respiration rates were significantly increased after C and CN addition but not after N addition, and organic P mineralization by acid phosphatase was also enhanced with CN addition. However, the response in respiration rates after CN addition in topsoil samples decreased with increasing soil C:P ratio, while acid phosphatase activity increased, indicating increasing P limitation and mineralization of organic P in samples with low P supply (wide C:P ratio). In the subsoil samples, the response in microbial and enzymatic activity was weaker, but showed a similar trend as in topsoils. NanoSIMS analyses indicated 18O enrichment especially in P-rich microsites of soils with low P content and in co-location with patches dominated by organic matter. We conclude that also at the microsite level, under conditions of high C and N supply, microbial activity is controlled by the inherent supply of P in both arable and forest soils studied here.
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
Geoderma 农林科学-土壤科学
CiteScore
11.80
自引率
6.60%
发文量
597
审稿时长
58 days
期刊介绍: Geoderma - the global journal of soil science - welcomes authors, readers and soil research from all parts of the world, encourages worldwide soil studies, and embraces all aspects of soil science and its associated pedagogy. The journal particularly welcomes interdisciplinary work focusing on dynamic soil processes and functions across space and time.
×
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:604180095
Book学术官方微信