自然资源学报 ›› 2008, Vol. 23 ›› Issue (2): 237-244.doi: 10.11849/zrzyxb.2008.02.008

• 资源生态 • 上一篇    下一篇

呼伦贝尔沙质草原风蚀坑积沙区的植被分带性

张萍, 哈斯, 王帅, 张素红   

  1. 北京师范大学 资源学院, 地表过程与资源生态国家重点实验室, 北京 100875
  • 收稿日期:2007-06-19 修回日期:2007-09-12 出版日期:2008-03-25 发布日期:2008-03-25
  • 作者简介:张萍(1981- ),女,宁夏盐池人,硕士生,主要从事干旱区地貌与植被生态学研究。
  • 基金资助:

    国家自然科学基金(40471013)资助。

Zonation of Vegetation on Depositional Area of Blowout in Hulun Buir Gassland

ZHANG Ping, HASI Eerdun, WANG Shuai, ZHANG Su-hong   

  1. College of Resources Science & Technology,State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal University, Beijing 100875, China
  • Received:2007-06-19 Revised:2007-09-12 Online:2008-03-25 Published:2008-03-25

摘要: 呼伦贝尔沙质草原现代风蚀坑主要包括平缓草地的简单风蚀坑、复合风蚀坑和固定沙丘的简单风蚀坑3种类型。坑后积沙区植被出现明显的分带性,且随风蚀坑及其下风侧积沙体的形态、尺度而发生变化。在平缓草地简单风蚀坑下风侧积沙体平面形态呈顺风向的舌状,由坑口至原生草地,随积沙厚度顺风向减小,依次出现沙蓬、冰草和百里香3个植被带;平缓草地复合风蚀坑后缘形成具有滑落面的大型流动沙丘,在沙丘背风侧顺风向依次出现舌状裸沙带、舌状拂子茅带及两侧的冰草带;固定沙丘风蚀坑坑后积沙呈裸沙形式穿越沙丘原有的山刺玫和小叶锦鸡儿两个灌木带,并在裸沙带外围形成舌状拂子茅带。风蚀坑下风侧积沙区植被的分带性反映了草地植被对风沙活动的响应,即随着坑后积沙体的扩大,草地植被由原生向沙生逆向演替。

关键词: 风蚀坑, 积沙区形态, 植被分带性, 呼伦贝尔草原

Abstract: Three types of modern blowouts including simple blowout,compound blowout on level grassland and simple blowout on stabilized dune are identified in sandy grassland of Hulun Buir.We investigate the morphology and vegetation distribution of sand deposit of blowouts and the results indicate that the distribution of plant species has a characteristic of zonation and species vary with the morphology and scales of sand deposit.The projected configuration of sand deposit of individual blowout on level grassland is tongue-shaped.From the edge of blowout to primary grassland there are three regular crescent-shaped plant zonations that were sequentially dominated by the species of Agriophyllum pungens,Agropyron cristatum and Thymus mongolicu with sand transport direction.The depositional area of combined blowout are dismembered by the dune with slip-face,bare tongue-shaped sandy zonation,crescent-shaped plant zonation of Calamagrostis epigejos following wind and stripped zonation dominated by Agropyron cristatum which are distributed in the two-sides of the two zonations on level grassland.On stabilized dune the bare depositional area of blowout that is tongued-shaped passes through the zonations of Rosa davurica and Caragana microphylla that grew on dune before the appearance of blowout and extends to primary grassland.The leeward of bare depositional area is occupied by crescent-shaped zonation of Calamagrostis epigejos.Analyzing the factor of vegetation zonation,we found there is a cubic equation correlation between Shannon-Wiener index and burial depth of sand,which suggests that the depth of deposition may be the major factor in zonation.These results demonstrate that the vegetation zonation is induced by sand-wind activity on sandy grassland.With the expanse of temporal and spatial scales of sand deposit of blowout,the primary grassland vegetation will degrade to sand vegetation in converse succession.

Key words: blowout, depositional area, vegetation zonation, Hulun Buir Grassland

中图分类号: 

  • Q948.15