• 中国中文核心期刊
  • 中国科学引文数据库(CSCD)核心库来源期刊
  • 中国科技论文统计源期刊(CJCR)
  • 第二届国家期刊奖提名奖

Citation:

Spatial and Temporal Variations of Water Poten tia l of theMa in Tree Spec iesfor Vegeta tion Restora tion in the Dry-hot Va lleys of the Jin sha River

  • Received Date: 2006-08-02
  • The spatial and temporal variations of water potential of 18 tree species for vegetation restoration in thedry-hot valleys of the J insha riverwere systematically analyzed on typ ical sunny day of different seasons in 2005 and2006, some main conclusionswere gotten as follows: (1) The daily water potentials within leaves of the main treespecies in the dry-hot valleys of the Jinsha river all obviously p resented a figure of single2peak in different seasons,the most peak values of dailywater potentials of the leaves appeared at 14: 00; (2) The water potentialwithin leavesof the main tree species in the valleys was deep ly affected by the change of seasons, the characteristic seasonalchange ofwater potentialwithin leaves for all the tree species studied was that the water potential inMarch was bigger than water potential inMay and water potential inMaywas smaller than water potential in October; the dry andhot inMay p romoted the diversity ofwater potential, and the relief of dry and hot stress after rainy season decreasedthe diversity; the diurnal variation of water potentialwithin leaves of the tree species inMay was relatively stable.(3) The water potential within leaves had the negative, positive and negative linear correlation with temperature, humidity and light intensity. (4)Different tree specieswere differently affected by altitude, the change of environmental factors and phenology caused by changeable altitude could affect the diurnal and seasonal variation of waterpotentials of some tree species; the lower location of slope was beneficial to keep ingwater potential at a relative highlevel; the order of leaf water potential of Azad irachta indica in three mixed stands from high to low was Azad irachtaindica & Acacia auric, Azadirach ta indica & Leucaena leucojpha la, and Azadirachta indica & Sctdeichera oleosa,which was closely related to the supp ressed condition of Azadirachta ind ica, the extremely dry and hot environmentcould decrease the affection of differentmixed stands on p lant leafwater potential; the water stress caused by the extreme drought inMay could be relieved by irrigation.
  • 加载中
  • [1] 张荣祖. 横断山区干旱河谷[M]. 北京:科学出版社, 1996

    [2] 吴征镒. 云南植被[M]. 北京:科学出版社, 1987: 503~509

    [3] 刘刚才,刘淑珍. 金沙江干热河谷区土地荒漠化程度的土壤评判指标确定[J]. 土壤学报, 1999, 36 (4) : 559~563

    [4] 周蛟,马焕成,胥辉. 元谋干热河谷引种造林试验及树种选择研究[J]. 西南林学院学报, 2000, 20 (2) : 78~84

    [5] 张信宝,杨忠,张建平,等. 元谋干热河谷坡地岩土类型与植被恢复分区[J]. 林业科学, 2003, 39 (4) : 16~22

    [6] 杨再强,谢以萍. 金沙江干热河谷生态问题与退耕还林技术模式的研究[J]. 四川林勘设计, 2003 (4) : 28~29

    [7] 李昆,张春华,崔永忠,等. 金沙江干热河谷区退耕还林适宜造林树种筛选研究[J]. 林业科学研究, 2004, 17 (5) : 555~563

    [8] 袁远亮,孙辉. 金沙江干热河谷区黑荆树引种研究[J]. 中国生态农业学报, 2002, 10 (4) : 99~100

    [9] 高洁. 干热河谷主要造林树种光合作用光抑制的防御机制[J].应用与环境生物学报, 2004, 10 (3) : 286~291

    [10] 张建国,李吉跃,沈国舫. 树木耐旱特性及其机理研究[M]. 北京:中国林业出版社, 2000

    [11] 汤章城. 植物对水分胁迫的反应和适应:植物对干旱的反应和适应[J]. 植物生理学通讯, 1983, 7 (4) : 1~7

    [12] 赵平. 退化生态系统植被恢复的生理生态学研究进展[J]. 应用生态学报, 2003, 14 (11) : 2031~2036

    [13]

    TurnerN C. Drought resistance and adap tation to water deficits incrop p lants[A]. In: Harry M. Stress Physiology in Crop Plants[C]. New York: JohnWiley and Sons, 1979: 343~372
    [14] 郭连生,田有亮. 9种针阔叶幼树的蒸腾速率、叶水势与环境因子关系的研究[J]. 生态学报, 1992, 12 (1) : 47~52

    [15] 沈允钢,施教耐,许大全. 动态光合作用[M]. 北京:科学出版社, 1985

  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Article views(3429) PDF downloads(1113) Cited by()

Proportional views

Spatial and Temporal Variations of Water Poten tia l of theMa in Tree Spec iesfor Vegeta tion Restora tion in the Dry-hot Va lleys of the Jin sha River

  • 1. Research Institute of Forestry, CAF

Abstract: The spatial and temporal variations of water potential of 18 tree species for vegetation restoration in thedry-hot valleys of the J insha riverwere systematically analyzed on typ ical sunny day of different seasons in 2005 and2006, some main conclusionswere gotten as follows: (1) The daily water potentials within leaves of the main treespecies in the dry-hot valleys of the Jinsha river all obviously p resented a figure of single2peak in different seasons,the most peak values of dailywater potentials of the leaves appeared at 14: 00; (2) The water potentialwithin leavesof the main tree species in the valleys was deep ly affected by the change of seasons, the characteristic seasonalchange ofwater potentialwithin leaves for all the tree species studied was that the water potential inMarch was bigger than water potential inMay and water potential inMaywas smaller than water potential in October; the dry andhot inMay p romoted the diversity ofwater potential, and the relief of dry and hot stress after rainy season decreasedthe diversity; the diurnal variation of water potentialwithin leaves of the tree species inMay was relatively stable.(3) The water potential within leaves had the negative, positive and negative linear correlation with temperature, humidity and light intensity. (4)Different tree specieswere differently affected by altitude, the change of environmental factors and phenology caused by changeable altitude could affect the diurnal and seasonal variation of waterpotentials of some tree species; the lower location of slope was beneficial to keep ingwater potential at a relative highlevel; the order of leaf water potential of Azad irachta indica in three mixed stands from high to low was Azad irachtaindica & Acacia auric, Azadirach ta indica & Leucaena leucojpha la, and Azadirachta indica & Sctdeichera oleosa,which was closely related to the supp ressed condition of Azadirachta ind ica, the extremely dry and hot environmentcould decrease the affection of differentmixed stands on p lant leafwater potential; the water stress caused by the extreme drought inMay could be relieved by irrigation.

Reference (15)

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return