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甘家湖湿地边缘带土地荒漠化演变中土壤颗粒分形特征
引用本文:杨爱霞,李艳红,雷荣.甘家湖湿地边缘带土地荒漠化演变中土壤颗粒分形特征[J].干旱环境监测,2011,25(4):218-223.
作者姓名:杨爱霞  李艳红  雷荣
作者单位:新疆师范大学地理科学与旅游学院,新疆乌鲁木齐,830054
基金项目:新疆维吾尔自治区自然科学基金项目,新疆维吾尔自治区重点实验室“新疆干旱区湖泊环境与资源实验室”基金,新疆师范大学校级重点实验室“干旱区湖泊环境演变实验室”基金
摘    要:采用分形理论,研究了甘家湖湿地边缘带不同景观变化类型土壤颗粒体积分形维数的特征。结果表明,(1)从芦苇湿地边缘、胡杨林土、梭梭灌木林土、芦苇湿地、耕地周边、耕地到盐化草甸土的土壤粒径变化可以看出:湿地边缘带土壤荒漠化演变中砂粒含量在逐渐上升,粉粒、粘粒含量逐渐下降。这表明湿地边缘带人为的放牧、开垦、牛羊践踏对土壤产生了...

关 键 词:甘家湖湿地边缘带  土地荒漠化演变  土壤颗粒分形维数

The Soil Fractal Dimension Characteristics in Desertification Process on the Edge of Wetland in Ganjiahu
YANG Ai-xia,LI Yan-hong,LEI Rong.The Soil Fractal Dimension Characteristics in Desertification Process on the Edge of Wetland in Ganjiahu[J].Arid Environmental Monitoring,2011,25(4):218-223.
Authors:YANG Ai-xia  LI Yan-hong  LEI Rong
Institution:1.School of Geographic Science and Tourism,Xinjiang Normal University,Urumqi Xinjiang 830054,China;2.Xinjiang Laboratory of Lake Environment and Resources in Arid Zone,Urumqi Xinjiang 830054,China)
Abstract:This paper uses the fractal theory which has studied different types of the soil volume fractal dimension characteristics on the edge of wetland in Ganjiahu.The result indicates that:(1)The soil particle size is changing from the edge of reed wetland,Populus diversifolia forests soil,the ammodendron bush soil,the reed wetland,the cultivated land surrounding,cultivated land to the salt meadow soil.This shows that the sand content is rising gradually in the soil desertification process of the edge of wetland,while the silt clay content is decreasing gradually.The changing of the edge of reed wetland,Populus diversifolia soil,the ammodendron bush soil,the reed wetland,the cultivated land surrounding,cultivated land to the salt meadow soil shows that the sand content is raising gradually on the soil desertification of the edge of wetland,while the silt clay content is decreasing gradually.This indicates that the artificial grazing,cultivating,cattle and sheep trampling on the edge of wetland has had certain influence on the soil.This makes the fine soil materials occur coarse-grained evolution.(2)The volume fractal dimension's change reflects: the desertification degree is increasing with the soil fractal dimension decreasing on the edge of wetland in Ganjiahu.The desertification degree from high to low orderly is the edge of reed wetland,Populus diversifolia soil,the ammodendron bush soil,the reed wetland,the cultivated land surrounding,cultivated land to the salt meadow soil.The soil fractal dimension in vertical profile changes little on the cultivated land surrounding,cultivated land and the salt meadow soil,while the soil surface fractal dimension is greater than the middle and bottom on the edge of reed wetland,Populus diversifolia soil,the ammodendron bush soil,reed wetlands.This means grazing and cattle and sheep trampling accelerate the decomposition of soil which resulting in the surface soil clay content is larger than the middle and bottom.(3)There are different relativities between volume fractal dimension with the clay,silt and sand content.
Keywords:the edge of wetland in Ganjiahu  soil desertification process  soil fractal dimension
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