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武夷山不同海拔植被土壤微生物量N时空变异

王国兵 王丰 金裕华 汪家社 阮宏华

生态学杂志2011,Vol.30Issue(4):784-789,6.
生态学杂志2011,Vol.30Issue(4):784-789,6.

武夷山不同海拔植被土壤微生物量N时空变异

Spatiotemporal variation of soil microbial biomass N under different vegetations along an altitude gradient in Wuyi Mountains of Southeast China

王国兵 1王丰 1金裕华 2汪家社 1阮宏华3

作者信息

  • 1. 南京林业大学森林资源与环境学院江苏省林业生态工程重点实验室,南京210037
  • 2. 上海泽泉科技有限公司,上海200333
  • 3. 福建省武夷山国家级自然保护区管理局,福建武夷山354315
  • 折叠

摘要

Abstract

In order to understand the spatiotemporal variation of soil microbial biomass N and its main controlling factors in subtropical forest regions in China, 0-10, 10-25 , and 25 -40 cm soil samples were collected from the evergreen broadleaf forest ( EBF, 500 m a, s. l. ) , coniferous forest ( CF, 1200 m a. s. l. ) , subalpine dwarf forest ( DF, 1800 m a. s. l. ) , and alpine meadow ( AM, 2100 m a. s. l. ) along an altitude gradient in the Wuyi Mountains National Nature Reserve, Fujian Province from April 2006 to January 2007. With increasing altitude, the soil microbial biomass N increased significantly, being 106. 7, 140. 8, 254. 9 and 355. 8 mg · kg-1 in 0-10 cm soil layer under EBF, CF, SDF, and AM, respectively, and there was a significant difference (P<0. 05 ) among different altitudes. Soil microbial biomass N was the highest in 0-10 cm layer, and decreased gradually with soil depth. In the four ecosystems, there was a consistent seasonal variation of soil microbial biomass N, i. e. , the highest in winter, tended to decrease in spring, and the lowest in summer. Correlation analysis showed that in 0-10 cm soil layer, the main factors controlling the spatial variation of soil microbial biomass N along the altitude gradient were soil moisture, organic matter, and total N, while the main factors regulating the temporal variation of soil microbial biomass N were soil moisture and temperature.

关键词

武夷山/土壤微生物量N/时空变异

分类

农业科技

引用本文复制引用

王国兵,王丰,金裕华,汪家社,阮宏华..武夷山不同海拔植被土壤微生物量N时空变异[J].生态学杂志,2011,30(4):784-789,6.

基金项目

国家自然科学基金项目(30670313)和南京林业大学高学历人才基金项目(163010063)资助. (30670313)

生态学杂志

OA北大核心CSCDCSTPCD

1000-4890

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