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Spatio-temporal analysis of land use changes using remote sensing in Horqin sandy land, China

机译:中国距离Horqin Sandy Land的土地利用变化的时空分析

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Purpose The purpose of this paper is to analyze the characteristics of spatio-temporal dynamics and the evolution of land use change is essential for understanding and assessing the status and transition of ecosystems. Such analysis, when applied to Horqin sandy land, can also provide basic information for appropriate decision-making. Design/methodology/approach By integrating long time series Landsat imageries and geographic information system (GIS) technology, this paper explored the spatio-temporal dynamics and evolution-induced land use change of the largest sandy land in China from 1983 to 2016. Accurate and consistent land use information and land use change information was first extracted by using the maximum likelihood classifier and the post-classification change detection method, respectively. The spatio-temporal dynamics and evolution were then analyzed using three kinds of index models: the dynamic degree model to analyze the change of regional land resources, the dynamic change transfer matrix and flow direction rate to analyze the change direction, and the barycenter transfer model to analyze the spatial pattern of land use change. Findings The results indicated that land use in Horqin sandy land during the study period changed dramatically. Vegetation and sandy land showed fluctuating changes, cropland and construction land steadily increased, water body decreased continuously, and the spatial distribution patterns of land use were generally unbalanced. Vegetation, sandy land and cropland were transferred frequently. The amount of vegetation loss was the largest. Water body loss was 473.6 km(2), which accounted for 41.7 per cent of the total water body. The loss amount of construction land was only 1.0 km(2). Considerable differences were noted in the rate of gravity center migration among the land use types in different periods, and the overall rate of construction land migration was the smallest. Moreover, the gravity center migration rates of the w
机译:目的本文的目的是分析时空动力学的特点,土地利用变化的演变对于理解和评估生态系统的地位和转型至关重要。这种分析,当适用于Horqin Sandy Land时,还可以提供适当的决策的基本信息。本文通过整合长时间序列Landsat成像和地理信息系统(GIS)技术设计/方法/方法,从1983年到2016年,探讨了中国最大的沙地的时空动态和进化诱导的土地利用变化。准确和通过使用最大似然分类器和分类后变化检测方法,首先提取一致的土地利用信息和土地利用变更信息。然后使用三种指数模型分析时空动态和演化:动态度模型分析区域土地资源的变化,动态变化转移矩阵和流向率分析变化方向,以及重心转移模型分析土地利用变化的空间模式。调查结果表明,研究时期的Horqin Sandy Land的土地利用急剧变化。植被和砂土显示出变动变化,耕地和建筑陆地稳步增加,水体不断下降,土地使用的空间分布模式一般不平衡。经常转移植被,沙地和农作物。植被损失的数量最大。水体损失为473.6公里(2),占水体总体的41.7%。建筑用地的损失金额仅为1.0公里(2)。在不同时期的土地利用类型之间的重力中心迁移率达到了相当大的差异,建设土地迁移的总体速率最小。此外,W的重力中心迁移率

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