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中国沙漠 ›› 2005, Vol. 25 ›› Issue (4): 511-518.

• 研究论文 • 上一篇    下一篇

青海贵南草原沙漠化影响因子的贡献率

张春来1, 董光荣2, 邹学勇1, 程宏1, 杨硕1   

  1. 1. 北京师范大学中国沙漠研究中心, 教育部环境演变与自然灾害重点实验室, 北京 100875;
    2. 中国科学院寒区旱区环境与工程研究所, 甘肃兰州 730000
  • 收稿日期:2004-03-15 修回日期:2004-05-09 出版日期:2005-08-20 发布日期:2005-08-20
  • 作者简介:张春来(1972-),男(汉族),宁夏海原人,副教授,从事沙漠化与风沙工程研究。E-mail:clzhang@ires.cn
  • 基金资助:
    国家自然科学基金(40301025);北京市科技新星计划共同资助

Contributing Ratios of Several Factors to the Steppe Desertification in Guinan, Qinhai Province

ZHANG Chun-lai1, DONG Guang-rong2, ZOU Xue-yong1, CHEN Hong1, YANG Shuo1   

  1. 1. China Center of Desert Research at Beijing Normal University;Key Laboratory of Environmental Change and Natural Disaster of the Ministry of Education of China, Beijing Normal University, Beijing 100875, China;
    2. Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China
  • Received:2004-03-15 Revised:2004-05-09 Online:2005-08-20 Published:2005-08-20

摘要: 影响因子贡献率是目前沙漠化研究的焦点之一,诸因子对沙漠化发展的贡献和对沙漠化现状的贡献是这一科学问题的两个方面。利用风洞模拟实验和137Cs示踪技术,建立了青海贵南现代草原沙漠化多因子方程,分别区分了该区风速变化、植被变化、牲畜践踏(滥牧)、樵采破坏(滥樵)和草地开垦(滥垦)等五个主要影响因子对沙漠化现状及其发展的贡献率。结果表明,牲畜践踏、樵采活动和草地开垦对沙漠化发展的贡献率分别为54.78%、4.66%和40.56%,人类不合理经济活动是近40a来沙漠化发展的根本原因。平均侵蚀风速变化很小,对沙漠化发展的贡献率为零。植被盖度的变化对沙漠化发展具有显著的贡献,但在近几十年来气候变化尚不足于对植被盖度造成明显影响的前提下,对沙漠化的影响作用被进一步归结为人文因子的贡献。沙漠化现状是在自然沙漠化过程的基础上人类不合理经济活动进一步叠加的结果,自然因子和人文因子对当前沙漠化现状的贡献率分别为27.8%和72.2%,人文因子中牲畜践踏、樵采活动和草地开垦对沙漠化现状的贡献率分别为39.55%、3.37%和29.28%。沙漠化影响因子的贡献率因时、因地而异。

关键词: 沙漠化, 土壤风蚀, 影响因子, 贡献率

Abstract: Contributing ratio of desertification factors is an important issue in the field of desertification study. The ratios to the development of desertification and to the status of desertification are two sides of the scientific issue. Making use of wind tunnel test and 137Cs technique, a multi-factor function of modern desertification in steppe area of Guinan County is constructed, in which change of wind speed, vegetation cover, livestock trampling, woodcutting, and grassland cultivation are involved. The results show that contributing ratios of livestock trampling, woodcutting and grassland cultivation to the development of desertification are 54.78%, 4.66%, and 0.56% respectively. That is to say, human unreasonable activities are conclusive cause of the development of desertification since 1960s. Change of average wind speed is very small, hence it has little contribution to the development of desertification. Change of vegetation cover is very important to the development of desertification. Since climatic change had no obvious affects on vegetation cover and humane activities directly led to the decrease of vegetation cover in the latest several years, contribution of vegetation cover's change to the development of desertification is ascribed to humane factors. The status of desertification is a result of climatic change and human unreasonable activities. Climatic change-induced natural desertification is the background, human activities accelerating the process. Contributing ratios of natural and humane factors to the status of desertification are 27.8% and 72.2% respectively. The contributing ratio of each factor changes with time and site.

Key words: desertification, soil wind erosion, desertification factor, contributing ratio

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