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(C_(mic)、N_(mic)),分析不同强度火烧对其土壤微生物量碳、氮(C_(mic)、N_(mic))的影响。结果表明:不同强度火烧后土壤C_(mic)、N_(mic)含量均呈下降的趋势,不同土层间土壤C_(mic)、N_(mic)含量随土层深度增加而逐渐减小,土壤C_(mic)变化在34~205 mg/kg之间,土壤N_(mic)变化在7~40 mg/kg之间;土壤微生物量碳氮比(C_(mic)/N_(mic))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(NH+4-N)、硝态氮(NO-3-N)均有显著影响(P<0.05),对于土壤p H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C_(mic)和N_(mic)的影响均达到极显著水平(P<0.01)。土壤养分(SOC、TN、NH+4-N和NO-3-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p H显著升高。相关分析结果表明:土壤有机碳、全氮对土壤C_(mic)、N_(mic)有极显著影响(P<0.01),土壤C_(mic)、N_(mic)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C_(mic)、N_(mic)的主要因素。
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 Cmicand Nmic. The results showed that both Cmicand Nmicdecreased after different intensity burning and gradually declined with the soil depth. Cmicranged from 34-205 mg/kg; Nmicranged from 7-40 mg/kg; Cmic/Nmicwas 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 Cmicand 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 Nmicextremely 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 Cmicand Nmic.
出处
《北京林业大学学报》
CAS
CSCD
北大核心
2017年第10期70-77,共8页
Journal of Beijing Forestry University
基金
国家重点研发计划项目(2017YFD060010006)
国家自然科学基金项目(31270696)
关键词
林火
火烧强度
土壤理化性质
土壤微生物量
forest fire
fire intensity
soil physiochemical characteristics
soil microbial biomass