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哀牢山亚热带常绿阔叶林土壤温湿度对极端降雪的响应

汤显辉1,4,张一平1,2*,武传胜1,2,罗康1,2,梁乃申3   

  1. 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, 云南勐仑 666303;2中国科学院哀牢山亚热带森林生态系统研究站, 云南景东 676209; 3日本国立环境研究所, 筑波3058506;4中国科学院大学, 北京 100049)
  • 出版日期:2018-06-10 发布日期:2018-06-10

Responses of soil temperature and soil water content to extreme snow event in a subtropical evergreen broad-leaved forest in Ailao Mountains, Yunnan, Southwest China.

TANG Xian-hui1,4, ZHANG Yi-ping1,2*, WU Chuan-sheng1,2, LUO Kang1,2, LIANG Nai-shen3   

  1. (1Key Laboratory of Tropical Forest Ecology, Xishuangbanna Tropical Botanical Garden, Chinese Academy of Sciences, Menglun 666303, Yunnan, China; 2Ailaoshan Station for Subtropical Forest Ecosystem Studies, Chinese Academy of Sciences, Jingdong 676209, Yunnan, China; 3National Institute for Environmental Studies, Tsukuba 3058506, Japan; 4University of Chinese Academy of Sciences, Beijing 100049, China).
  • Online:2018-06-10 Published:2018-06-10

摘要: 利用2015年1月云南中部发生的极端降雪事件,对该事件前后哀牢山亚热带常绿阔叶林内外土壤温度和土壤含水量进行比较,探讨土壤温湿度对极端降雪事件的响应。结果表明:极端降雪事件导致森林林冠大面积受损,森林郁闭度减小,不仅使得林内土壤温度升高,而且改变了林内外土壤温度差值的年变化和日变化特征。极端降雪事件前,林内外不同深度温差年变化为单峰曲线,林内不同深度土壤最高温度相对于林外均发生滞后;发生极端降雪事件当年,林内10 cm土壤温度日较差增大,林内外不同深度温度差年变化为双峰曲线,林内表层土壤最高温度发生时间和林外不存在滞后,20 cm以下深层土壤仍然存在滞后;发生极端降雪事件后1年,林内外不同深度温度差值年变化回归为单峰曲线,林内除10 cm土壤外,更深层土壤最高温度回归到雪灾前相对于林外滞后的格局。极端降雪事件后林内不同深度土壤含水量均有所增加,其对林内表层土壤含水量的影响雨季大于干季。极端降雪事件导致的森林土壤温湿度的改变,很可能会增加土壤碳排放速率,最终削弱森林的碳汇能力。

关键词: 胞外酶, 同质园, 微生物生物量, 微生物代谢熵, 土壤固碳

Abstract: The frequency and intensity of extreme weather and the associated disturbances, such as extensive floods, droughts, and ice storms, have been increasing against the pronounced global warming. In recent years, southern China has suffered increasing frequency of severe ice storms. During early January 2015, a primary subtropical evergreen broadleaved forest in〖JP2〗 Southwest China experienced an extreme snow event that damaged the forest. Based on the automatically collected data from meteorological station, we analyzed the soil temperature and soil water content before and after this severe snow event. The results showed that extreme snow led to extensive canopy damage and formation of canopy gaps. There was obvious time lag in maximal soil temperature between the forest and the open areas at different depths. However, no palpable time lag was observed in 10 cm and 20 cm soil depths in the year when extreme snow occurred. Similarly, no time lag occurred in 10 cm soil one year after extreme snow event. Soil water content at different depths showed a peak in both the forest and open areas after extreme snow damage, and then soil moisture in the forest kept higher against normal years. The extreme snow damage had stronger influence on topsoil water content in rainy season than in dry season. The increases of soil temperature and soil water content caused by extreme snow event would accelerate soil respiration, which may reduce the strength of carbon sink in the forest.

Key words: microbial biomass, soil carbon sequestration, extracellular enzyme, common garden., microbial metabolic quotient