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应用生态学报 ›› 2017, Vol. 28 ›› Issue (8): 2431-2437.doi: 10.13287/j.1001-9332.201708.013

• 目次 • 上一篇    下一篇

喀斯特出露基岩生境两种典型乔木的树干液流特征

张慧玲1,2,3, 丁亚丽1,2,3, 陈洪松1,2, 王克林1,2, 聂云鹏1,2*   

  1. 1中国科学院亚热带农业生态研究所亚热带农业生态过程重点实验室, 长沙 410125
    2中国科学院环江喀斯特生态系统观测研究站, 广西环江547100
    3中国科学院大学, 北京 100049
  • 收稿日期:2016-12-22 发布日期:2017-08-18
  • 通讯作者: * E-mail: nyp@isa.ac.cn
  • 作者简介:张慧玲,女,1991年生,硕士研究生.主要从事生态水文学和稳定同位素生态学研究.E-mail:huiling2017@163.com
  • 基金资助:
    本文由国家重点研发计划项目(2016YFC0502400,2016YFC0502402)、国家自然科学基金项目(31570428)和中国科学院西部青年学者项目资助

Characteristics of sap flow of two typical trees in exposed bedrock habitat of Karst region, China

ZHANG Hui-ling1,2,3, DING Ya-li1,2,3, CHEN Hong-song1,2, WANG Ke-lin1,2, NIE Yun-peng1,2*   

  1. 1Key Laboratory of Agro-ecological Processes in Subtropical Region, Institute of Subtropical Agriculture, Chinese Academy of Sciences, Changsha 410125, China
    2 Huanjiang Observation and Research Station for Karst Ecosystems, Chinese Academy of Sciences, Huanjiang 547100, Guangxi, China
    3University of Chinese Academy of Sciences, Beijing 100049, China
  • Received:2016-12-22 Published:2017-08-18
  • Contact: * E-mail: nyp@isa.ac.cn
  • Supported by:
    This work was supported by the National Key Research and Development Program of China (2016YFC0502400, 2016YFC0502402), the National Natural Science Foundation of China (31570428), and the Young Scholars Program in Western China

摘要: 以西南喀斯特地区常见的出露基岩生境为研究对象,应用TDP热扩散探针技术,分析2种典型乔木菜豆树和圆叶乌桕的树干液流特征.结果表明: 2树种树干液流对干、湿季均有明显响应;同为落叶乔木,菜豆树(约1个月)无液流特征的时长远小于圆叶乌桕(约4个月);圆叶乌桕单位胸高断面积年总蒸腾耗水量高于菜豆树,生长季内(4—9月) 2树种单位胸高断面积耗水量分别约占全年的90%和66%;2树种液流密度与光合有效辐射、水汽压亏缺、温度均呈极显著正相关,与相对湿度呈极显著负相关;2树种生长季内液流密度、日蒸腾耗水不仅小于同处于亚热带季风区的非喀斯特地区,而且小于邻近的喀斯特地区,甚至低于降水稀少的干旱地区典型树种同一参数的值.喀斯特出露基岩生境2种典型植物的蒸腾耗水量因特殊的水分环境而受到限制,同为落叶乔木却对应着不同的水分利用策略.

Abstract: A unique but very common habitat, rocky outcrop in Karst region of southwest China was selected for this study. Sap flow patterns of two typical tree species (Radermachera sinica and Triadica rotundifolia) were analyzed by using the method of Granier’s thermal dissipation probe (TDP). The results showed that sap flow density of both species exhibited clear response to the wet and dry seasons. However, the absence of sap flow only last about 1 month for R. sinica but 4 months for T. rotundifolia, despite the same functional type of these two species. T. rotundifolia consumed relatively higher annual total amount of water per unit area at breast height than R. sinica. Moreover, water that was consumed during the growing season (from April to September) accounted for 90% and 66% of the annual total amount for T. rotundifolia and R. sinica, respectively. Sap flow densities of the two species were very significantly positively correlated with photosynthetically active radiation, water vapor pressure deficit, and temperature, while had very significant negative correlation with air relative humidity. Sap flow densities and daily water consumptions of two tree species were not only lower than the tree species distributed in the same climatic non-karst zone of the study area, but also lower than the main tree species in karst area nearby, and even lower than the typical species in dry area with extremely low precipitation. The above results suggested that water consumption of the two tree species were restricted by the specific water environment of rocky outcrop, and species of the same functional type exhibited different water use strategies.