首页|秸秆及其生物质炭输入对毛竹林土壤氨氧化微生物与氮循环相关酶活性的影响

秸秆及其生物质炭输入对毛竹林土壤氨氧化微生物与氮循环相关酶活性的影响

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[目的]探讨不同外源碳(玉米Zea mays秸秆及其生物质炭)输入对亚热带毛竹Phvllostachys edulis林土壤氨氧化微生物和氮循环相关酶活性的影响,以揭示其对土壤硝化作用的生物学机制。[方法]以亚热带毛竹林为研究对象,设置3个处理:对照(不施用)、施用玉米秸秆(5 t·hm-2)和施用玉米秸秆生物质炭(5 t·hm-2),进行为期1a的野外试验。于试验的第3个月和第12个月采集土壤样品,利用荧光定量聚合酶链式反应(qPCR)及高通量测序技术分析不同处理下毛竹林土壤氨氧化微生物群落结构特征、酶活性与总硝化速率的变化规律。[结果]与对照相比,秸秆及其生物质炭处理显著改变了土壤氨氧化细菌(AOB)丰度和群落结构(P<0。05),而对氨氧化古菌(AOA)丰度和群落结构无显著影响;秸秆处理显著提高土壤氨氧化细菌丰度及其优势菌属亚硝化螺菌属Nitrosospira的相对丰度、蛋白酶活性和脲酶活性以及总硝化速率,而生物质炭处理则使其显著降低(P<0。05)。相关性分析表明:氨氧化细菌丰度及其优势菌属亚硝化螺菌属的相对丰度、蛋白酶活性和脲酶活性与铵态氮(NH4+-N)、硝态氮(NO3--N)、水溶性有机氮(WSON)和土壤总硝化速率呈正相关(P<0。05)。冗余分析表明:土壤NH4+-N、NO3--N、微生物生物量氮(MBN)和水溶性有机氮质量分数对氨氧化细菌群落结构存在显著影响(P<0。05)。[结论]秸秆生物质炭输入通过降低土壤NH4+-N、NO3--N和水溶性有机氮质量分数,从而降低土壤氨氧化细菌丰度及其优势菌相对丰度,削弱氮循环相关酶活性,进而抑制土壤硝化作用。与秸秆直接输入相比,秸秆生物质炭有利于减少毛竹林土壤氧化亚氮气体排放以及土壤氮素损失。图6表1参57
Effects of straw and its biochar application on soil ammonia-oxidizing microorganisms and N cycling related enzyme activities in a Phyllostachys edulis forest
[Objective]The objective is to investigate the effects of different exogenous carbon application(Zea mays straw and its biochar)on soil ammonia-oxidizing microorganisms and N cycling related enzyme activities in a subtropical Phyllostachys edulis forest,so as to reveal the biological mechanism of soil nitrification.[Method]A 1-year field experiment was conducted in a typical subtropical Ph.edulis forest.Three treatments were set up:control(no application),straw(5 t·hm-2)and biochar(5 t·hm-2).Soil samples were collected at the 3rd and 12th month of the treatment.Quantitative PCR and high-throughput sequencing techniques were used to analyze the changes in soil ammonia-oxidizing microbial community structure characteristics,enzyme activities and gross nitrification rate under different treatments.[Result]Straw and its biochar treatment significantly changed the abundance and community structure of ammonia oxidizing bacteria(AOB)in soil(P<0.05),but had no significant effect on the abundance and community structure of ammonia oxidizing archaea(AOA).Compared with the control,straw treatment significantly increased the abundance of AOB and the relative abundance of Nitrosospira,the activities of soil protease and urease,and the gross nitrification rate of soil(P<0.05),while biochar treatment had the opposite effect.Correlation analysis showed that AOB abundance and the relative abundance of its dominant genus Nitrosospira,protease and urease activity were positively correlated with the content of NH4-N,NO3-N and water-soluble organic nitrogen(WSON),and the soil gross nitrification rate.Redundancy analysis revealed that the contents of NH4+-N,NO3--N,microbial biomass nitrogen(MBN)and WSON had a significant impact on the community structure of AOB(P<0.05).[Conclusion]The application of straw biochar reduces the contents of soil NH4_-N,NO3--N and WSON,as well as soil AOB abundance and relative abundance of dominant genera,weakens N cycling related enzyme activity,and inhibits soil nitrification.Compared with direct application of straw,straw biochar is beneficial for reducing soil N2O emission and soil nitrogen loss in a Ph.edulis forest.[Ch,6 fig.1 tab.57 ref.]

biocharPhyllostachys edulis forest soilammonia oxidizing microorganismssoil enzyme activitynitrification

潘丽霞、姜振辉、张雯怡、周家树、刘娟、蔡延江、李永夫

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浙江农林大学省部共建亚热带森林培育国家重点实验室,浙江杭州 311300

浙江农林大学浙江省森林生态系统碳循环与固碳减排重点实验室,浙江杭州 311300

生物质炭 毛竹林土壤 氨氧化微生物 土壤酶活性 硝化作用

国家自然科学基金资助项目国家重点研发计划项目

322718452022YFE0127800

2024

浙江农林大学学报
浙江农林大学

浙江农林大学学报

CSTPCD北大核心
影响因子:0.929
ISSN:2095-0756
年,卷(期):2024.41(1)
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