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A STUDY ON DESERTIFICATION OF WEST JILIN PROVINCE BASED ON REMOTE SENSING AND GIS TECHNIQUES

机译:基于遥感和GIS技术的西吉林省荒漠化研究

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"West Jilin Province" in this paper means Zhenlai, Baicheng, Taonan, Da'an, Tongyu, Fuyu,Songyuan, Qian'an, Changling, also includes Gongzhuling, Shuangliao, Lishu, Siping and Nong'an which have been suf-fered from desertification. In west Jilin Province there are three sand zones passing through, they are Xiang(Xianghai)-Wu(Ulan Tug) sand zone, Hai-Feng sand zone, and Tao'er River right bank sand zone. The desertification area of westJilin Province is 819 100 ha, making up 12. 5% of the total land area. Among desertification types, in Jilin Provincelight desertification is the major, then is medium dersertification, hevey desertification is the least. According to the compari-son of the interpretation results of the Landsat images of the 1980s and the 1990s by remote sensing and GIS techniques,it can be seen that the desertification area in west Jilin Province basically didn't change on the whole, only increased6130 ha, making up 0. 8% of the desertification area, change scale is less than 1%. Evidently, desertification is con-trolled mostly, but some areas are continuing deterioration. The desertification process of China can be divided into threetypes according to origin nature, they are sandy steppe desertification, fixed sand area(sand land) activation anddunes transfer invasion. Reasons of desertification of West Jilin Province are analyzed, they include natural factors (suchas material source factors, chimate factors) and artificial factors(such as destroying grass to reclaim, steppe decreasinggreatly, illegally feeling shelter forest stands, constructing reservoir to influence eco-environment etc. ) . Some sugges-tions are put forward as follows: establishing the social project for ecological reconstruction of degenerated land; intensify-ing planning and management of land use, reverting farmland into forestland or pasture in a planned way. The key desertifica-tion control is to depend mainly on policy and management, then control techniques.
机译:“西吉林省”在本文中,意味着镇利,白城,泰南,大安,通宇,福宇,松原,黔安,长岭,也包括公区,双辽,丽水,腹股沟和玉树,这一直含有suf-fered从荒漠化。在西吉林省有三个沙子横穿,它们是湘(仙曲)-WU(乌兰拖船)沙区,海峰沙区和陶河右岸沙子。韦斯林省荒漠化地区为819 100公顷,占陆地面积的5%。在荒漠化类型中,在吉林省省荒漠化是主要的,那么中等砍刀,赫维荒漠化是最少的。根据20世纪80年代Landsat图像和20世纪90年代的遥感和GIS技术的比较结果,可以看出,吉林省西荒漠化面积基本上没有改变,只有6130哈,占荒漠化面积的8%,变化规模小于1%。显然,荒漠化主要被摧毁,但部分地区正在继续恶化。中国的荒漠化进程可根据原产地分为划分的鹅卵石,它们是Sandy Steppe荒漠化,固定沙地面积(沙地)激活anddunes转移入侵。分析了西吉林省荒漠化的原因,包括自然因素(如诸如物质源极端因素,灵气因素)和人工因素(如摧毁草地以回收,草原减少,非法感受避难所森林,构建水库影响生态环境ETC。 ) 。一些建议如下所示:建立退变土地的生态重建社会项目;加强土地利用规划和管理,以计划的方式将耕地恢复到林地或牧场。关键的Deserfifica-Tion控制是主要依靠政策和管理,然后控制技术。

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