地球科学进展 ›› 2002, Vol. 17 ›› Issue (2): 235 -240. doi: 10.11867/j.issn.1001-8166.2002.02.0235

中国典型地区土地利用变化对生态系统的影响机制 上一篇    下一篇

人类活动对北京东灵山山顶草甸植被的影响及草甸植被的保育对策
江源,赵海霞,刘肖骢,常玉涛   
  1. 北京师范大学资源科学研究所,北京师范大学中国生态资产评估研究中心,北京师范大学环境演变与自然灾害教育部重点实验室,北京 100875
  • 收稿日期:2001-12-07 修回日期:2001-12-28 出版日期:2002-12-20
  • 通讯作者: 江源(1960-),女,甘肃正宁人,副教授,博士,主要从事植被生态学、景观生态学以及城市生态环境研究.E-mail:jiangy@bnu.edu.cn E-mail:jiangy@bnu.edu.cn
  • 基金资助:

    国家自然科学基金重大项目“中国东部陆地农业生态系统与全球变化相互作用机理研究”(编号:39899374);国家自然科学基金项目“山地效应温度空间分异及其对植被景观作用机理的研究”(编号40071002)资助.

HUMAN IMPACT ON THE MEADOW VEGETATION IN DONGLING MOUNTAIN, BEIJING AND MEASURES FOR CONSERVATION OF THE MEADOW VEGETATION

JIANG Yuan, ZHAO Hai-xia, LIU Xiao-cong, CHANG Yu-tao   

  1. China Ecological Capital Assessment Research Center, Beijing Normal University;Key Laboratory of  Environmental Change and Natural Disaster, Ministry of Education, Beijing 100875,China
  • Received:2001-12-07 Revised:2001-12-28 Online:2002-12-20 Published:2002-04-01

通过对北京东灵山海拔 1500 m以上草甸植被资源的调查,共获得41个面积为 4 m×4 m的样方资料。将不同草甸群落按照人类活动的影响作用进行归类,并对各个草甸群落的生境和群落特征进行分析,结果表明:①东灵山山顶草甸植被以人类活动影响下形成的次生草甸群落为主,原生性草甸仅分布在海拔 2000 m以上的山顶及其邻近地段;②种类组成最丰富的草甸群落位于海拔1510~1900m的地段,这是自然条件和人类活动共同作用的结果;③旅游活动的影响已经使山顶原生性草甸受到威胁,局部地段草甸植被退化严重;④限制马匹活动,适时、适度提高缆车票价,在草甸分布地段部分拆除并制止新建饭店、旅馆,实行旅游功能分区规划和管理,有针对性地开展草甸承载力研究等,是现阶段草甸植被保育的重要措施。

The human impact on the mountain meadow vegetation growing 1 500 m above sea level in Dongling Mountain, Beijing, has been studied in this paper through the analyses to the field survey data collected from 41 quadrats (4 m×4 m each). The data were analyzed with respect to the ways and intensity of human impact, features of the meadow vegetation and characteristics of its habitats. The preliminary results are as follows: ①Most of the meadow communities in Dongling mountain are secondary vegetation under heavy human impacts. The primary meadow vegetation distributes only around the peak area of the mountain, higher than 2 000 m above sea level. ②The meadow communities with richer species composition are found at the places between 1 510~1 900 m above sea level, which is the direct results of natural environment deeply interfered by human activities. ③Development of tourism and sightseeing activities has exerted heavy impacts on the primary meadow vegetation around the peak area of the Mountain, which has led to the serious deterioration of the vegetation in some local areas. ④Regulations of restricting the tourism and sightseeing activities in meadow concentration areas, such as forbidding horse-riding on sensitive areas, raising the price of cable car in busy tourism seasons, removing excessive hotels, and diverging the tourists within the low elevation range, are effective measures to protect the meadow vegetation. Meanwhile, researching further into the environmental capacity of the meadow vegetation, enhancing the tourism planning and improving the functional tourism divisions accordingly are also conducive to the conservation of the meadow vegetation.

中图分类号: 

[1] Chen Lingzhi,Huang Jianhui. The Study of Forest Ecosystem Structure and Function in Warm-Temperate Zone[M].Beijing: Science Press,1997.1-87.[陈灵芝, 黄建辉. 暖温带森林生态系统结构与功能的研究 [M]. 北京: 科学出版社, 1997.1-87.]
[2] Li Jianguo, Chen Guohai, He Qingtang, et al. Quantitative analysis and evaluation of larix prince ruppercht's ecological adapation[J]. Acta Ecologica Sinica, 1996, 16(2): 180-186. [李建国, 陈国海, 贺庆棠,等. 华北落叶松生态适应性的定量分析与评价[J].生态学报, 1996, 16(2): 180-186.]
[3] Jiang Yuan. Research progress on biodiversity of agricultural ecosystem in the European countries[J]. Resources Science, 1999,21(5): 53-56.[江源. 欧洲农田生态系统物种多样性研究进展[J]. 资源科学, 1999, 21(5): 53-56.]
[4] Dierschke H. Pflanzensoziologie [M]. Stuttgart: Ulmer, 1994. 31-73.
[5] Jiang Y. Kleinraeumliche variation der vegetation und ihrer standortbedingungen im Pfannwadl und in Teilgebieten des Streitwaldes/Kraichgau[A]. Karlsruher Schriften zur Geographie und Geooekologie (Bd.5)[C]. Karlsruhe, 1995. 32-112. 
[6] He Shiyuan, Xing Qihua, Yin Zutang, et al.Flora of Beijing [M]. Beijing: Beijing Press, 1992.[贺士元, 邢其华,尹祖棠. 北京植物志 [M]. 北京: 北京出版社, 1992.]
[7] Sukopp H. Wandel von flora und vegetation in Mitteleuropa unter dem Einfluss des Menschen[A]. Berichte ueber Landwirtschaft[C]. Hamburg und Berlin: Paul Parey, 1972, Bd. 50: 112-130.

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