首页|期刊导航|生态学报|氮负荷增强对冬季闽江河口芦苇湿地土壤N2O产生过程的影响

氮负荷增强对冬季闽江河口芦苇湿地土壤N2O产生过程的影响OA北大核心

Effects of enhanced nitrogen load on N2 O production in Phragmites australis marsh soil of the Minjiang River estuary in winter

中文摘要英文摘要

选择闽江河口典型芦苇(Phragmites australis)湿地为研究对象,基于野外氮负荷增强模拟试验(NN,无氮负荷处理,0 g N m-2 a-1;NL,低氮负荷处理,12.5 g N m-2 a-1;NM,中氮负荷处理,25.0 g N m-2 a-1;NH,高氮负荷处理,75.0 g N m-2 a-1),通过获取不同年份冬季各氮负荷样地土壤开展室内培养实验,对比研究了氮负荷持续 9 个月(2021 年 12 月,WT9)和 21 个月(2022 年12 月,WT21)后湿地土壤的N2O产生过程.结果表明,氮负荷增强条件下湿地土壤不同过程的N2O产生量发生了明显改变,不同年份土壤的N2O总产生量均在NM处理下最高.异养反硝化作用对不同年份土壤的N2O产生均存在较大的削弱作用,但其N2O产生量整体随氮负荷时间的延长而增加;不同氮负荷处理下的非生物作用均是N2O产生的重要过程,但其N2O产生量在较短时期(WT9)随氮负荷水平的升高呈降低变化,而在较长时期(WT21)则呈增加趋势.不同氮负荷处理下非生物过程对N2O产生的较大贡献主要与该区土壤铁锰、硫化物等含量丰富以及氮负荷增强条件下土壤酸碱状况(pH)的改变有关.氮负荷水平与温度对不同年份冬季土壤的N2O产生过程均存在不同程度的交互影响,不同处理下的N2O产生在 WT9 时期的较低温度下(5.5-11.5℃)以非生物作用为主,在WT21 时期以硝化作用和非生物作用为主;而在较高温度下(17.5℃),不同年份冬季土壤的N2O产生均以非生物作用和硝化细菌反硝化作用为主.研究发现,氮负荷增强改变了不同年份冬季土壤N2O产生的生物和非生物贡献模式,其主要通过改变土壤养分状况来影响N2O产生的生物或非生物过程.在闽江河口湿地冬季低温并叠加氮负荷增强条件下,其对土壤N2O产生的综合影响表现为抵消效应,而这有助于降低该区冬季的N2O排放量.

The typical Phragmites australis marsh in the Minjiang estuary was selected as the study object and a field N load experiment was conducted,which included four N load levels(NN,no N treatment,0 g N m-2 a-1;NL,low N treatment,12.5 g N m-2 a-1;NM,medium N treatment,25 g N m-2 a-1;and NH,high N treatment,75 g N m-2 a-1).The marsh soils were sampled in different N load treatments after 9(December 2021,WT9)and 21 months(December 2022,WT21)of N import and the N2 O production processes of different marsh soils were comparatively assessed through incubation experiments.Results showed that,with increased N loads,the sources of N2 O production varied significantly,with the NM treatment showing the highest total N2 O emissions during both the WT9 and WT21 periods.While the heterotrophic denitrification process significantly reduced N2 O emissions in the soils during the WT9 and WT21 periods,N2 O emissions generally rose with extended N loading durations.Under different N load treatments,the N2 O productions of marsh soils were primarily due to the non-biological process,but its N2 O production generally decreased with increasing N load levels in a short-term period(WT9)and increased in a long-term period(WT21).The higher contributions of non-biological process to N2 O production in different N load treatments mainly depended on the abundant iron(Fe),manganese(Mn)and sulfides in soils and the great alteration of soil pH under enhanced N load conditions.The interactions between N load levels and temperature showed different influences on N2 O production processes in soils of WT9 and WT21 periods.At lower temperature(5.5-11.5℃),the N2 O productions in soils of different N load treatments at WT9 period were mainly dependent on non-biological process,while those at WT21 period were predominated by nitrification and non-biological processes.However,at higher temperatures(17.5℃),the N2 O productions in soils of WT9 and WT21 periods were predominantly governed by non-biological process and nitrifier denitrification process.This study found that enhanced N load altered the original contribution patterns of biological and non-biological processes to soil N2 O production at WT9 and WT21 periods,which mainly influenced the biological or non-biological processes of N2 O production by altering soil nutrient status.Under low temperature and N load conditions in winter in the Minjiang estuary marsh,the interactions between temperature and N enrichment showed an offset effect on soil N2 O production,which was favorable for reducing the N2 O emissions in winter.

廖宇晨;孙志高;方冠荣;宋振阳;贺攀霏;姚钦予

福建师范大学福建省亚热带资源与环境重点实验室,福州 350117||福建师范大学湿润亚热带生态地理过程教育部重点实验室,福州 350117福建师范大学福建省亚热带资源与环境重点实验室,福州 350117||福建师范大学湿润亚热带生态地理过程教育部重点实验室,福州 350117福建师范大学福建省亚热带资源与环境重点实验室,福州 350117||福建师范大学湿润亚热带生态地理过程教育部重点实验室,福州 350117福建师范大学福建省亚热带资源与环境重点实验室,福州 350117||福建师范大学湿润亚热带生态地理过程教育部重点实验室,福州 350117福建师范大学福建省亚热带资源与环境重点实验室,福州 350117||福建师范大学湿润亚热带生态地理过程教育部重点实验室,福州 350117福建师范大学福建省亚热带资源与环境重点实验室,福州 350117||福建师范大学湿润亚热带生态地理过程教育部重点实验室,福州 350117

氧化亚氮氮负荷处理非生物过程冬季闽江河口

nitrous oxidenitrogen load treatmentnon-biological processwinterMinjiang estuary

《生态学报》 2025 (6)

2655-2668,14

福建省自然科学基金重点项目(2023J02012)国家自然科学基金面上项目(42371105,41971128)福建省"闽江学者奖励计划"项目

10.20103/j.stxb.202406151388

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