机构地区:[1]中国林业科学研究院热带林业研究所,广州510520 [2]广东新丰云髻山省级自然保护区管理处,新丰511100
出 处:《生态学报》2024年第3期1092-1103,共12页Acta Ecologica Sinica
基 金:国家重点研发计划项目(2022YFF1303003-06);中央级公益性科研院所基本科研业务费专项资金(CAFYBB2021SY004);广东省科技厅林业生态监测网络平台建设(2022CG646);广东珠江三角洲森林生态系统国家定位观测研究站(0144135)。
摘 要:土壤微生物是土壤有机质和养分循环的主要驱动者,研究土壤微生物生物量碳氮变化、稳态特征及其对环境因子内在的长期响应机理具有重要意义。以南亚热带常绿阔叶林土壤为对象,对土壤微生物生物量碳和氮(MBC和MBN)、土壤有机碳(SOC)、总氮(TN)、总磷(TP)、可溶性碳(ROC)、速效氮(AN)、pH、土壤温度(ST)和土壤含水量(SWC)进行连续10年监测;应用方差分析、相关性和回归分析及稳态分析等探究MBC和MBN的年际变化和稳态特征及主要影响因素。研究结果表明:(1)旱季MBC和MBN含量分别在171.32—358.45和25.90—54.08 mg/kg区间波动,雨季分别在394.01—507.97和68.40—88.05 mg/kg区间波动;旱、雨季的MBC含量年际间变化显著(P<0.05),但MBN含量仅在旱季变化显著(P<0.05)。雨季MBC和MBN含量均显著高于旱季(P<0.01),且雨季的MBC和MBN含量是旱季的2倍以上。(2)旱、雨季的MBC与MBN之间均呈显著正相关(P<0.05)。在旱季,MBC和MBN均与ROC和AN含量显著正相关(P<0.05),此外,MBN含量也与TP(P<0.05)和SOC(P<0.01)显著正相关。在雨季,仅SOC与MBN呈显著正相关(P<0.05)。(3)在旱季,MBC含量变化主要受ROC(P<0.05)和AN(P<0.001)影响,MBN则受AN控制(P<0.05)。在雨季,AN(P<0.05)主导了MBC的变化,TP(P<0.05)和SOC(P<0.05)是MBN变异的主导因子。AN(P<0.001)和SOC(P<0.001)是旱、雨季土壤MBC和MBN变化的主导因子。(4)土壤MBC和MBC/MBN稳态指数在年际间均为绝对稳态型(P>0.05);雨季的MBN(P=0.685)为绝对稳态型,但旱季为非稳态(P<0.01,H>1)。雨季微生物熵显著高于旱季(P<0.01),表明土壤有机质质量及养分利用效率更高。综上,MBC和MBN含量受季节更替显著影响,且主要受土壤SOC和AN的影响;受旱季水分限制,MBN的稳态更差。Soil microbes are the primary drivers of soil organic matter and nutrient cycling.It is critical to study carbon and nitrogen variations in soil microbial biomass,as well as their steady-state properties and inherent long-term response mechanisms to environmental variables.Soil microbial biomass carbon and nitrogen(MBC and MBN),organic carbon,total nitrogen,total phosphorus,readily oxidizable carbon(ROC),available nitrogen,pH,temperature,and water content have been continuously monitored in a subtropical evergreen broad-leaved forest soil for 10 years in this study.The ANOVA,correlation and regression analysis,and steady-state analysis were employed to investigate the interannual variations and steady-state characteristics of MBC and MBN and the main factors influencing them.The results demonstrated that(1)the MBC and MBN contents varied between 171.32 to 358.45 mg/kg and 25.90 to 54.08 mg/kg in the dry season and from 394.01 to 507.97 mg/kg and 68.40 to 88.05 mg/kg in the rainy season,respectively.Significant inter-annual variation of MBC content in both dry and rainy seasons was detected(P<0.05).Whereas,the content of MBN only changed significantly between years in the dry season(P<0.05).The MBC and MBN contents in the rainy season were significantly higher than those in the dry season(P<0.01)and it′s twice as high in the dry season than in the rainy season.(2)There was a significantly positive correlation between MBC and MBN in both dry and rainy seasons(P<0.05).Both MBC and MBN were positively correlated with ROC and AN in the dry season.Meanwhile,MBN was significantly positively correlated with TP(P<0.05)and SOC(P<0.01).In the rainy season,only MBN was significantly positively correlated with SOC(P<0.05).(3)In the dry season,the variety of the MBC content was mainly influenced by ROC(P<0.05)and AN(P<0.001),whereas MBN variation was primarily influenced by AN(P<0.05).AN(P<0.05)dominated the variation of MBC in the rainy season,while TP(P<0.05)and SOC(P<0.05)were the dominant factors of MBN variation.Taken t
关 键 词:常绿阔叶林 土壤微生物生物量碳氮 年际动态特征 环境因子
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