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应用生态学报 ›› 2002, Vol. ›› Issue (9): 1104-1108.

• 研究论文 • 上一篇    下一篇

绿洲-荒漠交错带环境特征初步研究

贾宝全1, 慈龙骏1, 蔡体久2, 高志海3, 丁峰3   

  1. 1. 中国林业科学研究院林业研究所, 北京 100091;
    2. 北京林业大学, 北京 100083;
    3. 甘肃省治沙研究所, 武威 733000
  • 收稿日期:2001-06-11 修回日期:2001-10-21 出版日期:2002-09-15
  • 通讯作者: 贾宝全,男,1964年生,博士后,副研究员.主要从事干旱区绿洲景观生态及荒漠化研究工作,发表论文40余篇.Tel:010-62889679,E-mail:jiabq@rif.forestry.ac.cn
  • 基金资助:
    国家自然科学基金资助项目(39990490、40071004).

Preliminary research on environmental characteristics of oasis-desert ecotone

JIA Baoquan1, CI Longjun1, CAI Tijiu2, GAO Zhihai3, DING Feng3   

  1. 1. Institute of Forestry, Chinese Academy of Forestry, Beijing 100091;
    2. Beijing Forestry University, Beijing 100083;
    3. Gansu Desert Control Research Institute, Wuwei 733000
  • Received:2001-06-11 Revised:2001-10-21 Online:2002-09-15

摘要: 以甘肃省石羊河下游的民勤绿洲为例,对其绿洲外围与荒漠交错地带的植被和与植被关系密切的灌丛沙包特征进行了系统研究.结果表明,由于生态交错带边缘效应的存在,植被盖度的变化呈现绿洲附近与交错带外围靠近流沙的地方较低,而位于流沙和绿洲之间的部分相应较高.植被盖度较高的部位主要集中于自流动沙丘至绿洲外600m处,而非紧靠近绿洲.这与地下水自沙漠向绿洲方向运移有关.在绿洲外缘300~600m的范围内植被盖度出现下降,原因可能与绿洲荒漠交错带界外区的形成有关,说明研究区绿洲外0~600m范围即是该区域绿洲界外区的存在区域.灌丛沙包上的裸沙率以绿洲界外区为最大,大量沙包裸露,可致沙子的活动性增强,因此该地带是对绿洲土地造成沙质荒漠化的最大流沙来源.

关键词: 绿洲, 荒漠, 交错带, 植被, 沙丘密度, 裸沙率, 界外区

Abstract: Taking Minqin Oasis in the downstream of Shiyanghe Rivers as example,the shrub characteristics of sand dune,which was closely related to the vegetation of the interface between the outside of oasis and desert,was studied in this paper. The change of vegetation coverage and dune density indicated that the vegetation coverage in the ecotone was obviously higher than that in the outside of oasis and in drift desert. There existed an area outside oasis that was obviously affected by human activies and 0~600 m away from the outside of oasis. Meanwhile,the appearing position of area outside oasis was different in different place. The naked area ratio of dune in the area outside oasis was the biggest,so that the area outside oasis was the main resource of drift sand resulting in desertification of oasis. Over extracting ground water in oasis district resulted in a forming of dropping funnel of ground water there,and resulted in a fluid of ground water from desert to oasis. Ultimately,human activities aggravated those processes to some extent.

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