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鄱阳湖地区国土资源数据库系统的研究
作者: 金志农  来源:国土与自然资源研究 年份:1990 文献类型 :期刊 关键词: 信息  数据库  国土资源 
描述:采用dBASE—Ⅱ数据库方法,贮存了鄱阳湖地区25个县相关地区国土资源方面548个属性10余万个数据,并且实现了数据的增加、删除、修改、检索、查询和统计等数据管理功能。采用AutoCAD软件包和汉字菜单、数字化仪,制取了二十幅专业地图;通过接口程序,连接 AutoCAD 和数据库文件,可以输出任意数据库文件数值型数据的统计地图,并可进行统计地图的条件查询。建立了包括水位——湖面积——湖容积关系模型、灰色预测模型和多变量统计模型的模型库。成功地实现了 dBASE、BASICA和AutoCAD之间的数据传递。
全文:采用dBASE—Ⅱ数据库方法,贮存了鄱阳湖地区25个县相关地区国土资源方面548个属性10余万个数据,并且实现了数据的增加、删除、修改、检索、查询和统计等数据管理功能。采用AutoCAD软件包和汉字菜单、数字化仪,制取了二十幅专业地图;通过接口程序,连接 AutoCAD 和数据库文件,可以输出任意数据库文件数值型数据的统计地图,并可进行统计地图的条件查询。建立了包括水位——湖面积——湖容积关系模型、灰色预测模型和多变量统计模型的模型库。成功地实现了 dBASE、BASICA和AutoCAD之间的数据传递。
鄱阳湖面积容积量算及误差分析
作者: 李树明 蒋建平 方波  来源:人民长江 年份:2002 文献类型 :期刊 关键词: 光电测积法  使用方法  鄱阳湖  操作步骤  误差分析 
描述:介绍光电测积法在鄱阳湖面积容积计算中的应用 ,该方法是利用计算机根据编制的程序在AutoCAD环境下对照扫描校正的地形栅格图用短线段来替代等高线的曲线段 ,使其描绘的短线段能真实地反映曲线的变化 ,再利用短线段的坐标进行面积容积量算。具体地阐述此方法的操作步骤及使用方法 ,并从多个方面分析产生误差的原因及影响程度 ,从而说明光电测积法应用于白纸测图的面积容积计算的优越性及可行性
全文:介绍光电测积法在鄱阳湖面积容积计算中的应用 ,该方法是利用计算机根据编制的程序在AutoCAD环境下对照扫描校正的地形栅格图用短线段来替代等高线的曲线段 ,使其描绘的短线段能真实地反映曲线的变化 ,再利用短线段的坐标进行面积容积量算。具体地阐述此方法的操作步骤及使用方法 ,并从多个方面分析产生误差的原因及影响程度 ,从而说明光电测积法应用于白纸测图的面积容积计算的优越性及可行性
鄱阳湖非平稳水位波动及其与长江的交互作用关系
作者: 戴雪 万荣荣 杨桂山  来源:地理学报(英文版) 年份:2015 文献类型 :期刊 关键词: Yangtze  earlier  seasonal  intensified  downstream  lacustrine  river  representative  flood  dominate 
描述:Seasonal water-level fluctuations(WLF) play a dominate role in lacustrine ecosystems. River-lake interaction is a direct factor in changes of seasonal lake WLF, especially for those lakes naturally connected to upstream and downstream rivers. During the past decade, the modification of WLF in the Poyang Lake(the largest freshwater lake in China) has caused intensified flood and irrigation crises, reduced water availability, compromised water quality and extensive degradation of the lake ecosystem. There has been a conjecture as to whether the modification was caused by its interactions with Yangtze River. In this study, we investigated the variations of seasonal WLF in China’s Poyang Lake by comparing the water levels during the four distinct seasons(the dry season, the rising season, the flood season, and the retreating season) before and after 2003 when the Three Gorge Dam operated. The Water Surface Slope(WSS) was used as a representative parameter to measure the changes in river-lake interaction and its impacts on seasonal WLF. The results showed that the magnitude of seasonal WLF has changed considerably since 2003; the seasonal WLF of the Poyang Lake have been significantly altered by the fact that the water levels both rise and retreat earlier in the season and lowered water levels in general. The fluctuations of river-lake interactions, in particular the changes during the retreating season, are mainly responsible for these variations in magnitude of seasonal WLF. This study demonstrates that WSS is a representative parameter to denote river-lake interactions, and the results indicate that more emphasis should be placed on the decrease of the Poyang Lake caused by the lowered water levels of the Yangtze River, especially in the retreating season.
全文:Seasonal water-level fluctuations(WLF) play a dominate role in lacustrine ecosystems. River-lake interaction is a direct factor in changes of seasonal lake WLF, especially for those lakes naturally connected to upstream and downstream rivers. During the past decade, the modification of WLF in the Poyang Lake(the largest freshwater lake in China) has caused intensified flood and irrigation crises, reduced water availability, compromised water quality and extensive degradation of the lake ecosystem. There has been a conjecture as to whether the modification was caused by its interactions with Yangtze River. In this study, we investigated the variations of seasonal WLF in China’s Poyang Lake by comparing the water levels during the four distinct seasons(the dry season, the rising season, the flood season, and the retreating season) before and after 2003 when the Three Gorge Dam operated. The Water Surface Slope(WSS) was used as a representative parameter to measure the changes in river-lake interaction and its impacts on seasonal WLF. The results showed that the magnitude of seasonal WLF has changed considerably since 2003; the seasonal WLF of the Poyang Lake have been significantly altered by the fact that the water levels both rise and retreat earlier in the season and lowered water levels in general. The fluctuations of river-lake interactions, in particular the changes during the retreating season, are mainly responsible for these variations in magnitude of seasonal WLF. This study demonstrates that WSS is a representative parameter to denote river-lake interactions, and the results indicate that more emphasis should be placed on the decrease of the Poyang Lake caused by the lowered water levels of the Yangtze River, especially in the retreating season.
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