南京林业大学学报(自然科学版) ›› 2011, Vol. 35 ›› Issue (06): 44-48.doi: 10.3969/j.jssn.1000-2006.2011.06.009

• 研究论文 • 上一篇    下一篇

武夷山不同海拔植被带土壤微生物量磷的时空变异

王国兵1,金裕华1,王丰1,2,汪家社3,阮宏华1   

  1. 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,江苏南京210037;2.上海泽泉科技有限公司,上海200333;3.福建武夷山国家级自然保护区管理局,福建武夷山354315
  • 出版日期:2011-11-28 发布日期:2011-11-28
  • 基金资助:
    收稿日期:2011-06-15修回日期:2011-09-09基金项目:高等学校博士学科点专项科研基金(20103204120002);南京林业大学高学历人才基金(B2008-29)作者简介:王国兵(1979—),讲师,博士。Email: wangguobing81@yahoo.com.cn。

Temporal and spatial variations of soil microbial biomass P under different vegetations along an elevation gradients in Wuyi Mountains in southeast of China

WANG Guobing1,JIN Yuhua1,WANG Feng1,2,WANG Jiashe3,RUAN Honghua1   

  1. 1. Jiangsu Key Laboratory of Forestry Ecological Engineering, College of Forest Resources and Environment, Nanjing Forestry University, Nanjing 210037,China;2. Shanghai Zealquest Scientific Technology Co., Ltd., Shanghai 200333,China;3.The National Natu
  • Online:2011-11-28 Published:2011-11-28

摘要: 为了阐明我国中亚热带森林区土壤微生物量磷的时空变异特征及其主要影响因子,在福建省武夷山国家自然保护区选择了常绿阔叶林(EBF,海拔500 m)、针叶林(CF,海拔1 200 m)、亚高山矮林(SDF,海拔1 800 m)和高山草甸(AM,海拔2 100 m)共4种不同海拔植被类型作为实验样地进行了相关实验研究。结果表明:土壤微生物量磷含量随着海拔高度的增加显著增加,其中在0~10 cm的表层土壤中,EBF、CF、SDF和AM 4种植被类型土壤微生物量磷年均值分别为12.35、14.63、23.98和31.99 mg/kg,除EBF与CF两种植被类型之间土壤微生物量磷差异不显著外,其他不同海拔植被类型之间土壤微生物量磷含量均差异显著(p<0.05)。土壤微生物量磷含量在0~10 cm土壤表层最高,随着土壤深度的增加而逐渐减小。不同植被类型及不同土壤层次中土壤微生物量磷均具有明显的季节动态变化且变化规律一致,均表现为冬季最高,秋季次之,夏季最低。相关分析表明,在0~10 cm土层影响土壤微生物量磷沿海拔梯度空间变异的主要因子是土壤湿度和土壤有机质含量,而影响土壤微生物量磷季节性变异的主要因子是土壤湿度和土壤温度。

Abstract: To understand the temporal and spatial variation of soil microbial biomass P and its main controlling factors in subtropical forests regions in China, soil microbial biomass P and the associated factors were determined under different vegetations along an elevation gradients in the Wuyi Mountains National Nature Reserve, Fujian province, which were evergreen broadleaf forest (EBF, 500 m), coniferous forest (CF, 1 200 m), subalpine dwarf forest (SDF, 1 800 m) and alpine meadow (AM, 2 100 m) during April, 2006 to January, 2007. The results showed that: 1) Soil microbial biomass P content increased significantly with an increase altitude, which were 12.35 mg/kg, 14.63 mg/kg, 23.98 mg/kg and 31.99 mg/kg in 0—10 cm soil layer of EBF, CF, SDF and AM, respectively, soil microbial biomass P between different altitudes were significantly different except that no significant difference between EBF and CF (p <005); 2) Soil microbial biomass P was highest in top soil layer of 0—10 cm and decreased gradually with the increasing of soil depths; 3) there were consistent seasonal dynamics of soil microbial biomass P in four different ecosystems, which remained highest during winter, then tended to decrease during spring, and remained lowest during summer; 4) Correlation analysis of the data with 0—10 cm soil layer showed that soil moisture and soil organic matter content might be the main factors which controlling the spatial variations of soil microbial biomass P along the elevation gradients, and the seasonal variations of soil moisture and soil temperature mainly regulated the seasonal variations of soil microbial biomass P in subtropical forest regions of China.

中图分类号: