Knowledge Resource Center for Ecological Environment in Arid Area
基于数字成像技术的风蚀地表颗粒空间异质性 | |
其他题名 | Spatial Heterogenity of Soil Particles on Wind Erosion Surface Based on Digital Imaging Technology |
蒙仲举1; 王猛1; 王淮亮2; 高永1![]() | |
来源期刊 | 干旱区研究
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ISSN | 1001-4675 |
出版年 | 2016 |
卷号 | 33期号:6页码:1270-1277 |
中文摘要 | 通过对吉兰泰盐湖上风向的戈壁、灌木林地表层颗粒空间格局特点及其空间分布特征的研究,揭示该地区的风沙运动规律,对加强相关地区的植被类型及其空间配置格局的防沙效应研究具有重要意义。以乌兰布和沙漠西南边缘的吉兰泰盐湖为试验区,以试验区内戈壁、灌木林地表层颗粒为研究对象,利用样方法和数字图像处理技术,获取地表层不同土壤风蚀颗粒的百分含量,采用经典描述性统计及地统计学方法,分析不同抗风蚀能力颗粒百分含量的小尺度空间特征。结果表明: ① 2个样地颗粒越小,空间分布的变异性越大,峰度越尖锐。②裸露戈壁样地内3种风蚀颗粒含量的半方差函数模型均为线性模型,模型决定系数均在0.8以上,分布形态为随机分布,空间相关性中等;灌丛林地内3种风蚀颗粒的分布特征比较复杂,< 0.42 mm颗粒的随机因素引起的空间变异大。 ③由于灌丛对样地内不同风蚀颗粒分布的影响,导致灌丛林地及其周边> 0.84 mm的不可蚀颗粒呈聚集分布,空间分布比较强烈。 |
英文摘要 | It is of great importance in reinforcing the study on the vegetation types and the spatial distribution of vegetation against wind-blown sand to research the spatial pattern and distribution of surface soil particles on the Gobi desert and under the shrubbery in the upwind place of Jilantai Salt Lake and to reveal the movement of windblown sand. In this study,the Jilantai Salt Lake in the south margin of the Ulanbuh Desert was selected as the study area to research the soil particles in the Gobi desert and under the shrubbery using the quadrat sampling method and digital image processing technique,the percentages of different wind erosional particles were derived using the classical descriptive statistics and the statistical method,and the spatial distribution of percentage composition of soil particles with different capabilities of anti-wind erosion was analyzed. Results are as follows: ① Because of the long-term wind erosion,the surface soil particles were coarse,and the smaller the soil particles were,the higher the variability of spatial distribution and the sharper the kurtosis would be; ② Semivariance of soil particles with different diameters (< 0.42 mm,0.42 - 0.84 mm and > 0.84 mm) in the Gebi desert could be fitted with linear model very well,and grazing was also an important cause of leading to the spatial heterogeneity. Semi-variance model coefficient of < 0.42 mm soil particles under shrubbery was low,and the spatial heterogeneity was mainly caused by random factors (such as the shrub distribution); ③ Because of the effect of shrubs on sand flow structure,there was an aggregated distribution of > 0.84 mm soil particles,but a random distribution of < 0.42 mm erodible soil particles. In contrast,the spatial distribution of soil particles under shrubbery was much more complex. |
中文关键词 | 风蚀 ; 土壤颗粒 ; 数字图像技术 ; 空间异质性 ; 吉兰泰盐湖 |
英文关键词 | wind erosion soil particle digital image technology spatial heterogeneity Jilantai Salt Lake |
语种 | 中文 |
国家 | 中国 |
收录类别 | CSCD |
WOS类目 | AGRICULTURE MULTIDISCIPLINARY |
WOS研究方向 | Agriculture |
CSCD记录号 | CSCD:5859955 |
来源机构 | 内蒙古农业大学 |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/234337 |
作者单位 | 1.内蒙古农业大学沙漠治理学院, 呼和浩特, 内蒙古 010018, 中国; 2.河北省水利技术试验推广中心, 石家庄, 河北 050061, 中国; 3.内蒙古气象局,气象科学研究所, 呼和浩特, 内蒙古 010051, 中国 |
推荐引用方式 GB/T 7714 | 蒙仲举,王猛,王淮亮,等. 基于数字成像技术的风蚀地表颗粒空间异质性[J]. 内蒙古农业大学,2016,33(6):1270-1277. |
APA | 蒙仲举,王猛,王淮亮,高永,汪季,&任晓萌.(2016).基于数字成像技术的风蚀地表颗粒空间异质性.干旱区研究,33(6),1270-1277. |
MLA | 蒙仲举,et al."基于数字成像技术的风蚀地表颗粒空间异质性".干旱区研究 33.6(2016):1270-1277. |
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