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典型草地土壤反硝化过程同位素分馏效应

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反硝化过程是生态系统气态氮损失的主要途径,然而其速率一直难以量化。15N同位素自然丰度法是量化陆地生态系统尺度反硝化速率的有效方法,但是该方法需要考虑反硝化过程中的氮氧同位素分馏效应。目前关于陆地土壤反硝化作用分馏系数的研究主要集中在森林和农田,对于草地土壤的研究十分有限。基于此,本研究以我国不同地区的4种典型草地土壤(大兴安岭、多伦、额尔古纳和刚察)为对象,通过室内厌氧培养实验测定土壤微生物群落反硝化作用的硝酸盐消耗速率,并借助瑞利分馏模型拟合出N和O同位素分馏效应(ε)及其比值(△δ180∶△δ15N)。结果显示,草地土壤15ε为21。6‰~32。0‰(27。1‰±2。1‰),18ε为10。4‰~15。7‰(12。9‰±1。1‰)。研究发现,不同环境之间15e存在一定差异,可能归因于不同类型土壤理化性质和反硝化微生物群落组成的差异。此外,不同研究所用计算方法的差异、底物硝酸盐浓度、硝酸盐异化还原反应以及开放环境中可能发生的硝化作用等都会在不同程度上影响15ε的计算。对于18ε来说,年均温和年均降水是影响18ε的重要因素。草地土壤△δ18O∶△δ15N比值为0。38~0。49(0。46±0。03),低于以往陆地和水体生态系统以及微生物纯培养的研究。亚硝酸盐的再氧化和与水之间的氧同位素交换可能是造成△δ18O∶△δ15N差异的重要原因。综上所述,不同草地生态系统土壤反硝化分馏效应存在一定差异,在定量评估陆地生态系统反硝化作用速率时需综合考虑气候类型和生态系统等变量。
Isotope fractionation effect in denitrification process of typical grassland soil
Denitrification process is the main pathway for gaseous nitrogen loss in ecosystems,but it is difficult to quantify the rate of denitrification.The 15N natural abundance method is proved to be effective for quantifying deni-trification rates at the ecosystem scale.However,this method requires an understanding of the nitrogen and oxygen isotope fractionation factors during denitrification.Currently,studies on the isotope fractionation factors during deni-trification mainly focused on forest and cropland soils,and only few studies have been conducted in grassland soils.Here,we determine microbial nitrate consumption rates of four typical grassland soils from different regions in China(Daxinganling,Duolun,Eerguna,and Gangcha)under anaerobic condition.The nitrogen and oxygen isotope effects(ε)and their ratios(△δ18O∶△δ15N)were then fitted using the Rayleigh fractionation model.Our results showed that the 15εof grassland soils ranged from 21.6‰ to 32.0‰(27.1‰±2.1‰),and the 18ε ranged from 10.4‰ to 15.7‰(12.9‰±1.1‰).There was a certain difference in 15ε among different soils,which could be at-tributed to the differences in physical and chemical properties of different soil types and composition of denitrifying microbial communities.In addition,different calculation methods,initial nitrate concentration,nitrate dissimilatory reduction reaction,and possible nitrification in open environments may also affect the calculation of 15 ε.Mean an-nual temperature and mean annual precipitation were important factors affecting 18ε value.The △δ18O∶△δ15N ratios of grassland soils ranged from 0.38 to 0.49(0.46±0.03),which were lower than previous studies on terrestrial and aquatic ecosystems and microbial pure cultures.The potential reason for the difference in △δ18O∶△δ15N might be the re-oxidation of nitrite and oxygen isotope exchange with water.In conclusion,there were certain differences in fractionation effects among different grassland ecosystems.Thus,variables such as climate and ecosystem type should be comprehensively considered in quantifying denitrification rates.

denitrificationstable isotope techniquegrasslandnitrogen and oxygen isotope fractionation effect△δ18O∶△δ15N

刘德泽、王盎、王莹莹、杨秀森、宿晨霞、宋琳琳、段伊行、于浩明、刘东、赵鹏武、李英华、方运霆

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东北大学资源与土木工程学院,沈阳 110819

森林生态与保育重点实验室(中国科学院),中国科学院沈阳应用生态研究所,沈阳 110016

辽宁清原森林生态系统国家野外科学观测研究站,沈阳 110016

辽宁省稳定同位素技术重点实验室,沈阳 110016

内蒙古农业大学林学院,呼和浩特 010019

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反硝化 稳定同位素技术 草地 氮氧同位素分馏效应 △818O∶△815N

2024

生态学杂志
中国生态学学会

生态学杂志

CSTPCD北大核心
影响因子:1.439
ISSN:1000-4890
年,卷(期):2024.43(9)