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亚热带地区杉木人工林和阔叶林土壤活性有机质研究(英文)
引用本文:王清奎,汪思龙,邓仕坚.亚热带地区杉木人工林和阔叶林土壤活性有机质研究(英文)[J].林业研究,2005,16(1):23-26.
作者姓名:王清奎  汪思龙  邓仕坚
作者单位:中国科学院沈阳应用生态研究所,中国科学院沈阳应用生态研究所,中国科学院沈阳应用生态研究所 沈阳 110016,中国科学院研究生院,北京 100039,中国,沈阳 110016,中国,沈阳 110016,中国
基金项目:This research was supported by Chinese Academy of Sci-ence Program (NO.KZCX3-SW-418) and the National Natural Science Foun-dation of China (NO.30270268 and 30470303).
摘    要:土壤活性有机质对土壤养分如氮、磷、硫的生物化学循环具有作用,其含量和质量影响土壤的初级生产力。本试验在中国科学院会同森林生态实验站通过对第一代、第二代杉木纯林和地带性阔叶林土壤活性有机质组分的对比研究,发现杉木纯林土壤活性有机质的含量低于地带性阔叶林。第一代杉木纯林易氧化有机碳、微生物生物量碳、水溶性有机碳和水溶性碳水化合物的含量分别比第二代杉木纯林高35.9%、13.7%、87.8%和50.9%,比地带性阔叶林的低15.8%、47.3%、38.1%和30.2%。在调查的三种林地内,土壤微生物生物量碳和水溶性有机碳含量下降幅度较大,其次为水溶性碳水化合物,而易氧化有机碳的变化最小。同时,杉木纯林土壤养分等理化性质也比地带性阔叶林低。这表明在杉木纯林取代地带性阔叶林以及杉木纯林连栽后林地的土壤肥力降低。图3 表2参26。

关 键 词:土壤活性有机质  杉木人工林  地带性阔叶林  土壤养分
收稿时间:15 November 2004

Comparative study on active soil organic matter in Chinese fir plantation and native broad-leaved forest in subtropical China
Wang Qing-kui,Wang Si-long,Deng Shi-jian.Comparative study on active soil organic matter in Chinese fir plantation and native broad-leaved forest in subtropical China[J].Journal of Forestry Research,2005,16(1):23-26.
Authors:Wang Qing-kui  Wang Si-long  Deng Shi-jian
Institution:(1) Institute of Applied Ecology, Chinese Academy of Sciences, 110016 Shenyang, P.R. China;(2) Graduate School of Academy of Sciences, 100039 Beijing, P.R. China
Abstract:Active soil organic matter (ASOM) has a main effect on biochemical cycles of soil nutrient elements such as N, P and S, and the quality and quantity of ASOM reflect soil primary productivity. The changes of ASOM fractions and soil nutrients in the first rotation site and the second rotation site of Chinese fir plantation and the native broad-leaved forest were investigated and analyzed by soil sampling at the Huitong Experimental Station of Forestry Ecology (at latitude 26°48′N and longitude 109°30′E under a subtropical climate conditions), Chinese Academy of Sciences in March, 2004. The results showed that values of ASOM fractions for the Chinese fir plantations were lower than those for the broad-leaved forest. The contents of easily oxidisable carbon (EOC), microbial biomass carbon (MBC), water soluble carbohydrate (WSC) and water-soluble organic carbon (WSOC) for the first rotation of Chinese fir plantation were 35.9%, 13.7%, 87.8% and 50.9% higher than those for the second rotation of Chinese fir plantation, and were 15.8%, 47.3%, 38.1% and 30.2% separately lower than those for the broad-leaved forest. For the three investigated forest sites, the contents of MBC and WSOC had a larger decrease, followed by WSC, and the change of EOC was least. Moreover, soil physico-chemistry properties such as soil nutrients in Chinese fir plantation were lower than those in broad-leaved forest. It suggested that soil fertility declined after Chinese fir plantation replaced native broad-leaved forest through continuous artificial plantation. Foundation item: This research was supported by Chinese Academy of Science Program (NO.KZCX3-SW-418) and the National Natural Science Foundation of China (NO.30270268 and 30470303). Biography: WANG Qing-kui (1977-), male, Ph. D. candidate in Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, P.R. China. Responsible editor: Zhu Hong
Keywords:Active soil organic matter  Chinese fir plantation  Native broad-leaved forest  Soil nutrient elements
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