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营林用火对针叶林地土壤化学性质的影响研究
引用本文:熊建平,熊建红,郑育桃,罗嘉东,肖金香.营林用火对针叶林地土壤化学性质的影响研究[J].江西林业科技,2014(4):8-14.
作者姓名:熊建平  熊建红  郑育桃  罗嘉东  肖金香
作者单位:江西省森林公安局直属三分局;江西农业大学林学院;丰城市第一中学;江西省林业科学院;中国林业科学研究院亚热带林业实验中心;
基金项目:江西省科技厅项目(20122BBG70164)
摘    要:营林用火对维护林地土壤生态平衡和林地养分管理有重要指导意义。在针叶林地每两个月燃烧一次,每次用火时间30 min、60 min、90 min、120 min和CK 5个处理,3次重复。1 a后统一采样,采样深度设置0-5 cm、5-10 cm、10-20 cm 3个层次。结果表明:用火1年后,1土壤pH值变化不大,土壤有机质含量、土壤速效氮、土壤速效磷和土壤速效钾均有不同程度的增加。最大增幅分别为:燃烧30 min,5-10 cm土壤有机质含量增加50.2%,0-5 cm土壤速效氮增加34.9%,5-10 cm速效磷增加53.3%,10-20 cm土壤速效钾增加57.2%。2用火1 a后,燃烧60 min,0-5 cm有机质含量加39.4%,10-20 cm土壤速效氮增加20.6%,5-10 cm土壤速效磷增加38.2%,0-5 cm土壤速效钾增加51.5%。3燃烧90 min,0-5 cm土壤有机质含量增加38.5%,土壤速效氮变化不大,5-10 cm土壤速效磷增加38.4%,5-10 cm土壤速效钾增加51.7%。4燃烧120 min,10-20 cm土壤有机质含量增加38.5%,0-5 cm有效氮增加23.2%,5-10 cm的土壤速效磷增加42.9%,5-10 cm速效钾增加51.7%。土壤化学成分与用火时间没有关系,与燃烧时间长度关系很大。

关 键 词:营林用火  针叶林  土壤化学性质  江西

Effect of Use of Fire in Silviculture on Soil Chemical Properties of Needle Leaf Forest Land
Institution:XIONG Jian-ping, XIONG Jian-hong, ZHENG Yu-tao, LUO Jia-dong, XIAO Jin-xiang (1. Third-branch of Jiangxi Forest Public Security Bureau, Fenyi Jiangxi 336600, China; 2. College of Forestry, JAU, Nanehang Jiangxi 330045, China; 3. The First High School of Fengcheng City, Fengcheng Jiangxi 331100, China; 4. Jiangxi Academy of Forestry, Nanchang Jiangxi 330013, China; 5. Subtropical Forestry Experimental Center, Chinese Academy of Forestry.,Fenyi Jiangxi 336600, China)
Abstract:Prescribed burning has important guiding significance for maintain the ecological balance and nutrient management of forest land. There was once prescribed burning every two months in plot. The burning time was set to 30 min, 60 min, 90 min, 120 min and CK 5 treatments, repeated three times each burning. And a year later, unified sampling. The sampling depth is set to 0-5 cm, 5-10 cm, 10-20 cm three levels. A year later, the results were as follows: (1) the soil pH did not change significantly, but organic matter, available N, available P and available K in soil increase to different levels. In processing of 30 min combustion, organic matter in depth between 5 cm to 10 cm increases 50.2%, available N in depth between 0 cm to 5 cm increases 34.9%, available P in depth between 5 cm to 10 cm increases 53.3% and available K in depth between 10 cm to 20 cm 57.2%. (2) A year later, with fire burn 60 min, the content of organic matter increased 39.4%between 0 cm to 5 cm, the content of soil available N increased 20.6%between 10 cm to 20 cm, the content of soil available P increased 38.2% between 5 cm to 10 cm, the content of soil available K increased 51.5% between 0 cm to 5 cm. (3) In processing of 90 min combustion, the content of organic matter increased 38.5% between 0 cm to 5 cm, and there is little change of soil available nitrogen, the content of soil available P increased 38.4% between 5 cm to 10 cm, the content of rapidly-available K increased 51.7%between 5 cm to 10 cm. (4) By burnning 120 min, the content of organic matter content increased 38.5% between 10 cm to 20 cm, the content of soil available N increased 23.2% between 0 cm to 5 cm, the content of soil available P increased 42.9% between 5 cm to 10 cm, the content of rapidly-available K increased 51.7%between 5 cm to 10 cm. Soil chemical composition has nothing to do with fire time, but has a relationship with the length of burning time.
Keywords:use of fire in silviculture  coniferous forests  soil chemistry properties  Jiangxi
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