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杉木人工林土壤微生物生物量碳氮特征及其与土壤养分的关系
引用本文:何友军,王清奎,汪思龙,于小军.杉木人工林土壤微生物生物量碳氮特征及其与土壤养分的关系[J].应用生态学报,2006,17(12):2292-2296.
作者姓名:何友军  王清奎  汪思龙  于小军
作者单位:1.中南林业科技大学, 长沙 410004;;2.湖南会同森林生态系统国家野外科学观测研究站, 湖南会同 418307;;3.湖南省林业厅, 长沙 410007
基金项目:中国科学院知识创新工程项目;国家自然科学基金
摘    要:研究了湖南会同红黄壤区杉木人工林和常绿阔叶林土壤微生物量和养分状况.结果表明,该区杉木人工林取代地带性常绿阔叶林和杉木连栽后,土壤微生物碳、氮和土壤养分含量下降,土壤严重退化.在0~10 cm土层内,常绿阔叶林土壤微生物碳和氮含量为800.5和84.5 mg·kg-1,分别是第1代杉木林的1.90和1.03倍、第2代杉木林的2.16和1.27倍;在10~20 cm土层内,常绿阔叶林土壤微生物碳和氮含量为475.4和63.3 mg·kg-1,分别是第1代杉木纯林的1.86、1.60倍和第2代杉木林的2.11和1.76倍.在0~10 cm 和10~20cm土层内,杉木人工林取代常绿阔叶林和杉木栽植代数增加后,土壤全氮、全钾、铵态氮和速效钾含量均明显降低,但差异并不显著.人工杉木林林分组成单一,其凋落物分解慢、归还养分数量少;炼山等造成的表土流失是杉木人工林土壤微生物量和养分库退化的重要原因.土壤微生物碳与土壤全氮、铵态氮、全钾和速效钾含量呈极显著的正相关,土壤微生物氮与土壤养分含量也达到极显著水平.

关 键 词:Cd吸收  Zn效率  基因型  大麦  Zn-Cd交互作用  
文章编号:1001-9332(2006)12-2292-05
收稿时间:2006-03-13
修稿时间:2006-10-10

Characteristics of soil microbial biomass carbon and nitrogen and their relationships with soil nutrients in Cunninghamia lanceolata plantations
HE Youjun,WANG Qingkui,WANG Silong,YU Xiaojun.Characteristics of soil microbial biomass carbon and nitrogen and their relationships with soil nutrients in Cunninghamia lanceolata plantations[J].Chinese Journal of Applied Ecology,2006,17(12):2292-2296.
Authors:HE Youjun  WANG Qingkui  WANG Silong  YU Xiaojun
Institution:1.Central South University of Forestry and Technology, Changsha 410004,China;2.Huitong National Research Station of Forest Ecosystem, Huitong 418307, Hunan, China;3.Forestry Department of Hunan Province, Changsha 410007, China ;
Abstract:The study on the soil microbial biomass and nutrient status under native broadleaved forest and Cunninghamia lanceolata plantations at the Huitong National Research Station of Forest Ecosystem showed that after the native broadleaved forest was replaced by mono-cultured C. lanceolata or C. lanceolata was planted continuously, soil microbial biomass and nutrient pool decreased greatly. In 0 - 10 cm soil layer, the concentrations of soil microbial carbon and nitrogen in broadleaved forest were 800.5 and 84.5 mg x kg(-1) , being 1.90 and 1.03 times as much as those in the first rotation of C. lanceolata plantation, and 2.16 and 1.27 times as much as those in the second rotation of the plantation, respectively, while in 10 - 20 cm soil layer, the microbial carbon and nitrogen in broad-leaved forest were 475.4 and 63.3 mg x kg(-1), being 1.86 and 1.60 times as much as those in the first rotation, and 2.11 and 1.76 times as much as those in the second rotation, respectively. Soil nutrient pools such as total nitrogen, total potassium, NH4(+) -N, and available potassium also declined after the C. lanceolata plantation replaced native broad-leaved forest, or C. lanceolata was planted continuously. Less litter and its slower decay rate in pure C. lanceolata plantation were the crucial factors leading to the decrease of soil microbial biomass and nutrient pool in this area, and human disturbance, especially slash-burning and site preparation, was the another factor leading to the decrease. There were significant positive correlations between soil microbial carbon and nitrogen and soil nutrients. To improve soil quality and maintain sustainable productivity, some measures including planting mixed conifer with hardwood, preserving residues after harvest, and adopting scientific site preparation should be taken.
Keywords:Cunninghamia lanceolata plantation  Evergreen broadleaved forest  Soil microbial biomass  Soil fertility  
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