王莹莹;王英杰;张桐艳;张生瑞;方雷;

• 1:中国科学院地理科学与资源研究所资源与环境信息系统国家重点实验室
• 2:中国科学院大学

摘要(Abstract)：

针对平原区县级地名密度演变、重心时空演变及语义演变特征问题,该文以东北平原、华北平原、长江中下游平原为例,利用GIS、核密度估计方法对其进行直观地展示与分析。结果表明:隋代至今,县级地名密度与地名重心均不同,平原区一直是地名密度较高的区域,地名重心呈现出先南移后北移的特征;县级地名的数量随时间变迁及政权更迭表现出波动变化,总体趋势是随时间推进数量逐渐增多,且地名密度基本高于全国平均水平,华北平原、长江中下游平原地名密度是全国均值的3倍以上;三大平原因山、水得名的县级地名数量均占总数的30%以上,因社会人文因素得名的比重呈上升趋势;东北平原县级地名形成时间比较集中,华北平原和长江中下游平原则较为分散。

关键词(KeyWords)： 县级政区地名;时空演变;语义演变;平原区

Abstract:

Keywords:

基金项目(Foundation): 民政部第二次全国地名普查项目(Y55L0500AJ)

作者(Authors): 王莹莹;王英杰;张桐艳;张生瑞;方雷;

DOI: 10.16251/j.cnki.1009-2307.2019.11.011

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