The change of Zoige Plateau mire as the result of the human activities is discussed in this paper,by way of the comparative analysis the mire vegetation,mire soil(infusible N,P,K in Chuolajiang lakeshore(CLJL) mire soil without disturbance plot is higher than its in ninth road group(1) which is low degree disturbed or its in ninth road group(2) which is high degree disturbed.But the solubility N,P,K(namely quick result N,P,K) is in the adverse,its conttent in the disturb mire pasture soil is higher than its in the original mire.Tht analysis of mire hydro chemistry,mire microclimate shows made known that the region environment have distinctly changed in the recent years,resnlting in the pasture degeneration,wild animal decrease,mouse harm increase,part of the land is sandy and salt.This paper analyzed the cause of the above problem and puts forward some preventing countermeasures.
ZHAO Kui-yi, HE Chi-quan
. Influence of Human Activities on the Mire in Zoige Plateau and Countermeasure[J]. SCIENTIA GEOGRAPHICA SINICA, 2000
, 20(5)
: 444
-449
.
DOI: 10.13249/j.cnki.sgs.2000.05.444
[1] 赵魁义.西藏高原沼泽植被的基本特征[J],地理科学.1992,2(1):18~23.
[2] 柴岫,等.若尔盖高原沼泽[M]北京:科学出版社,1965.58~60.
[3] 中国科学院长春地理研究所沼泽研究室.三江平原沼泽[C].北京:科学出版社,1983.79~84.
[4] 杨福明,等.龙日坝泥炭沼泽改良途径的试验研究[J].四川草原,1984,1:7~12.
[5] 赵佐成,等.若尔盖辖曼一阿西高原沼泽自然保护区沼泽植物特征[J].武汉植物学研究.1984,5(3):121~124.
[6] 孙广友,等.若尔盖高原沼泽生态环境及其合理开发的研究[A].中国科学院长春地理研究所(编著).中国沼泽研究[C].北京:科学出版社,1988.78~82.
[7] 柴岫(主编).泥炭地学[C].北京:地质出版社,1990.97~99.
[8] 孙广友,张文芬.若尔盖高原黄河古河道及其古地理意义[A].中国科学院长春地理研究所(编著).中国沼泽研究[C].北京:科学出版社,1988.87~90.
[9] 马学慧,牛焕光.中国的沼泽[M],北京:科学出版社,1991.48~52
[10] 赵佐成,等.中国红原泥炭沼泽植物区系研究[J].武汉植物学研究,1995,13(1):118~123.