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火烧对河北平泉油松林土壤微生物量的影响
引用本文:李伟克,刘晓东,牛树奎,李炳怡,刘冠宏,褚艳琴.火烧对河北平泉油松林土壤微生物量的影响[J].北京林业大学学报,2017,39(10):70-77.
作者姓名:李伟克  刘晓东  牛树奎  李炳怡  刘冠宏  褚艳琴
作者单位:北京林业大学林学院
基金项目:国家重点研发计划项目,国家自然科学基金项目
摘    要:以河北平泉油松林近期(火后半年)火烧迹地为研究对象,根据树干熏黑高度和树木死亡率情况,划分不同火烧强度(轻度、中度、重度),并以邻近未火烧区设置对照样地,采用氯仿熏蒸浸提法测定各研究区土壤微生物量碳、氮(Cmic、Nmic),分析不同强度火烧对其土壤微生物量碳、氮(Cmic、Nmic)的影响。结果表明:不同强度火烧后土壤Cmic、Nmic含量均呈下降的趋势,不同土层间土壤Cmic、Nmic含量随土层深度增加而逐渐减小,土壤Cmic变化在34~205 mg/kg之间,土壤Nmic变化在7~40 mg/kg之间;土壤微生物量碳氮比(Cmic/Nmic)整体处于5~6之间。双因素方差分析表明:火烧强度、土层深度及二者的交互作用对土壤有机碳(SOC)、全氮(TN)、铵态氮(NH4+-N)、硝态氮(NO3--N)均有显著影响(P < 0.05),对于土壤pH值,仅火烧强度对其影响显著(P < 0.05);同时,火烧强度、土层深度及二者的交互作用对土壤Cmic和Nmic的影响均达到极显著水平(P < 0.01)。土壤养分(SOC、TN、NH4+-N和NO3--N)主要集中在表层(0~10 cm),重度火烧后土壤养分含量显著减少,同时,土壤pH显著升高。相关分析结果表明:土壤有机碳、全氮对土壤Cmic、Nmic有极显著影响(P < 0.01),土壤Cmic、Nmic含量与土壤有机碳、全氮均呈正相关。主成分分析进一步表明土壤有机碳、全氮是影响土壤Cmic、Nmic的主要因素。 

关 键 词:林火    火烧强度    土壤理化性质    土壤微生物量
收稿时间:2016-12-29

Impact of fire on soil microbial biomass of Pinus tabuliformis forest in Pingquan County,Hebei of northern China
LI Wei-ke,LIU Xiao-dong,NIU Shu-kui,LI Bing-yi,LIU Guan-hong,CHU Yan-qin.Impact of fire on soil microbial biomass of Pinus tabuliformis forest in Pingquan County,Hebei of northern China[J].Journal of Beijing Forestry University,2017,39(10):70-77.
Authors:LI Wei-ke  LIU Xiao-dong  NIU Shu-kui  LI Bing-yi  LIU Guan-hong  CHU Yan-qin
Institution:College of Forestry, Beijing Forestry University, Beijing, 100083, P. R. China
Abstract:In the burned area of Pinus tabuliformis forest in Pingquan County, Hebei of northern China, we measured soil microbial biomass carbon (Cmic), nitrogen (Nmic) of different fire intensity regions with a fumigation-extraction method after burned half a year. The study area was classified into different levels according to the smoked height and tree mortality: high-severity sites, middle-severity sites, low-severity sites and nearby unaffected sites. The purpose of our research was to explore the effects of different severity fire on Cmic and Nmic . The results showed that both Cmic and Nmic decreased after different intensity burning and gradually declined with the soil depth. Cmic ranged from 34-205 mg/kg;Nmic ranged from 7-40 mg/kg;Cmic/Nmic was wholly at 5-6. Two-way ANOVA showed that fire severity, soil layer and the interaction of the two factors had significant effects on soil organic carbon ( SOC) , soil total nitrogen ( TN) , NH4+-N, NO3--N ( P <0. 05 ) . However, soil pH was only positively correlated with fire severity ( P <0. 05 ) . Meanwhile, fire severity, soil layer and the interaction of the two factors had significant effects on Cmic and Nmic(P<0. 01). Soil nutrients were distributed mainly in the 0-10 cm layer and dropped sharply after the high-severity fire. Besides, soil pH increased significantly after the high-severity fire. The correlation analysis result showed that SOC and TN influenced the Cmicand Nmic extremely significantly (P<0. 01).The soil microbial biomass was positively correlated with SOC and TN. Principal component analysis further prove that SOC and TN are the main factors affecting Cmic and Nmic .
Keywords:forest fire  fire intensity  soil physiochemical characteristics  soil microbial biomass
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