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哀牢山亚热带常绿阔叶林地温特征及变化趋势

游广永 张一平 刘玉洪 巩合德 罗有勇

北京林业大学学报2011,Vol.33Issue(2):53-58,6.
北京林业大学学报2011,Vol.33Issue(2):53-58,6.

哀牢山亚热带常绿阔叶林地温特征及变化趋势

Characteristics and trend of soil temperature in subtropical evergreen broad-leaved forests in Mt. Ailaoshan.

游广永 1张一平 2刘玉洪 1巩合德 3罗有勇4

作者信息

  • 1. 中国科学院热带森林生态学重点实验室,西双版纳热带植物园
  • 2. 中国科学院研究生院
  • 3. 中国科学院哀牢山亚热带森林生态系统研究站
  • 4. 云南哀牢山森林生态系统国家野外科学观测研究站
  • 折叠

摘要

Abstract

Soil temperature is an important factor affecting plant growth and soil respiration. We analyzed the long-term data of soil temperature in the open areas and interior forests observed at the Ailaoshan Station for Subtropical Forest Ecosystem Study(ASSFE). Compared with open areas, interior forests had a lower mean soil temperature( by 2. 4 ℃ ), a lower mean maximum soil temperature( by 13.4 ℃ ) and a higher minimum soil temperature (by 3.4 ℃ ), which implies a strong canopy shading effect on soil temperature. The difference between soil temperature inside forests and in open areas was higher in dry seasons than in wet seasons. Soil temperature increased with a stronger trend in dry seasons than in wet seasons. Soil temperature of interior forests had a stronger rising trend(0.017 ℃/year) than in open areas(0. 010 ℃/year). In conclusion, soil temperature is generally rising, while the difference of soil temperature and air temperature is decreasing, and so is the soil temperature difference between open areas and interior forests. Consequently, the distribution elevation of subtropical montane evergreen broad-leaved forest will be driven upward by the trend of warming, and carbon balance and soil respiration will be inevitably disturbed as a result of rising soil temperatures.

关键词

哀牢山/亚热带山地常绿阔叶林/地温/趋势

Key words

Ailaoshan/ subtropical montane evergreen broad-leaved forest/ soil temperature/ trend

分类

农业科技

引用本文复制引用

游广永,张一平,刘玉洪,巩合德,罗有勇..哀牢山亚热带常绿阔叶林地温特征及变化趋势[J].北京林业大学学报,2011,33(2):53-58,6.

基金项目

中国科学院知识创新工程重要方向项目(KZCX2-YW-Q1-05-04). (KZCX2-YW-Q1-05-04)

北京林业大学学报

OA北大核心CSCDCSTPCD

1000-1522

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