Comparative study on active soil organic matter in Chinese fir plantation and native broad-leaved forest in subtropical China

被引:21
作者
Wang Qing-kui
Wang Si-long
Deng Shi-jian
机构
[1] Chinese Academy of Sciences,Institute of Applied Ecology
[2] Graduate School of Academy of Sciences,undefined
关键词
Active soil organic matter; Chinese fir plantation; Native broad-leaved forest; Soil nutrient elements; S714.5; S791.27; A;
D O I
10.1007/BF02856848
中图分类号
学科分类号
摘要
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.
引用
收藏
页码:23 / 26
页数:3
相关论文
共 55 条
[11]  
Diaz-Ravina M.(1998)Management-induced change in labile soil organic matter under continuous corn in eastern Canadian soils [J] Biol. Fertil. Soils. 26 88-94
[12]  
Acea M.J.(1999)Distribution, decomposition and nutrient return of the fine root in pure Acta Ecologica Sinia 19 342-346
[13]  
Carballas T.(1997) and the mixed plantations [J] Acta Ecologica Sinia 17 176-183
[14]  
Gregorich E.G.(2000)Effect of different ground clearing on Chinese fir plantatin ecosystems [J] J. Moun. Sci. 18 237-243
[15]  
Carter M.R.(1989)Effects of site preparations on ecosystem of Chinese fir plantations [J] Nature. 338 499-500
[16]  
Angers D.A.(1992)Microbial biomass acts as a source of plant nutrients in dry tropical forest and savanna [J] Aust. J. Soil Reas. 30 195-207
[17]  
Haynes R.J.(2002)Rate of microbial biomass carbon to soil organic carbon as a sensitive indicator of changes in soil organic matter [J] Forest Ecology and Management 159 3-14
[18]  
Haynes R.J.(1987)Factors controlling soil carbon and nitrogen stores in pure stands of Norway spruce ( Soil Biol. Biochem. 19 703-707
[19]  
Francis G.S.(1994)) and mixed species stands in Austria [J] Soil Sci. Soc. Am. J. 58 1130-1139
[20]  
Hu C.B.(2000)An extraction method for measuring microbial biomass C [J] Chinese Journal of Applied Ecology 11 185-190