鄱阳湖生态系统长期变化对气候——人为环境的响应研究

作者： 郭娅  来源：中国科学院大学 年份：2016 文献类型 ：学位论文

描述：鄱阳湖生态系统长期变化对气候——人为环境的响应研究

鄱阳湖生态系统长期变化对气候——人为环境的响应研究

作者： 郭娅  来源：中国科学院大学 年份：2016 文献类型 ：学位论文

描述：鄱阳湖生态系统长期变化对气候——人为环境的响应研究

鄱阳湖生态系统长期变化对气候——人为环境的响应研究

作者： 郭娅  来源：中国科学院大学 年份：2016 文献类型 ：学位论文

描述：鄱阳湖生态系统长期变化对气候——人为环境的响应研究

鄱阳湖流域史前人类遗址时空分布及其环境响应

作者： 徐佳佳 贾玉连 马春梅 朱诚 吴立 李育远 王鑫浩  来源：地理学报(英文版) 年份：2016 文献类型 ：期刊 关键词： expanded  northward  geographic  records  环境响应  鄱阳湖流域  climatic  ancient  Holocene  southeast 

描述：The temporal-spatial geographic distribution of archaeological sites and its feature between 10.0–2.8 ka BP(ka BP= thousands of years before 0 BP, where “0 BP” is defined as the year AD 1950) were determined, based on GIS spatial analysis in the Poyang Lake Basin. The relationship between geographic distribution of sites of different periods under subsistence existence of ancient civilizations, climate and environmental change was investigated. The results revealed numerous archaeological sites of the Neolithic Age(10.0–3.6 ka BP). The sites were mainly located in the northern part of the Poyang Lake Basin, a hilly and mountainous area with many river terraces suitable for the development of human civilization. The number of archaeological sites rapidly increased during the Shang and Zhou dynasties(3.6–2.8 ka BP) and spread widely on the floodplains of the middle and lower reaches of Ganjiang River and onto the west, south, and southeast beach areas of the Poyang Lake. Holocene records of climate change suggested that it was possible that climate fluctuations had a great impact on human evolution in the study area. Before 3.6 ka BP, westward and northward expansion of Neolithic cultures in the Poyang Lake watershed occurred under the background of climate amelioration(becoming warmer and wetter). The ancient people lived in the hilly areas with high elevation. The simple mode of a fishing and gathering economy was mostly suited to this area in the early Neolithic Age. The scope of human activities was expanded and cultural diversity developed in the late Neolithic Age. However, with population growth and increasing survival pressure in a dry-cold climatic stage after 3.6 ka BP, this simple living mode had to be abandoned, and various forms of economy, the majority being agriculture, were developed on flood plains of the lower reaches of numerous rivers around Poyang Lake. This promoted flourishing of the Bronze culture of South China.

全文：The temporal-spatial geographic distribution of archaeological sites and its feature between 10.0–2.8 ka BP(ka BP= thousands of years before 0 BP, where “0 BP” is defined as the year AD 1950) were determined, based on GIS spatial analysis in the Poyang Lake Basin. The relationship between geographic distribution of sites of different periods under subsistence existence of ancient civilizations, climate and environmental change was investigated. The results revealed numerous archaeological sites of the Neolithic Age(10.0–3.6 ka BP). The sites were mainly located in the northern part of the Poyang Lake Basin, a hilly and mountainous area with many river terraces suitable for the development of human civilization. The number of archaeological sites rapidly increased during the Shang and Zhou dynasties(3.6–2.8 ka BP) and spread widely on the floodplains of the middle and lower reaches of Ganjiang River and onto the west, south, and southeast beach areas of the Poyang Lake. Holocene records of climate change suggested that it was possible that climate fluctuations had a great impact on human evolution in the study area. Before 3.6 ka BP, westward and northward expansion of Neolithic cultures in the Poyang Lake watershed occurred under the background of climate amelioration(becoming warmer and wetter). The ancient people lived in the hilly areas with high elevation. The simple mode of a fishing and gathering economy was mostly suited to this area in the early Neolithic Age. The scope of human activities was expanded and cultural diversity developed in the late Neolithic Age. However, with population growth and increasing survival pressure in a dry-cold climatic stage after 3.6 ka BP, this simple living mode had to be abandoned, and various forms of economy, the majority being agriculture, were developed on flood plains of the lower reaches of numerous rivers around Poyang Lake. This promoted flourishing of the Bronze culture of South China.

鄱阳湖生态系统长期变化对气候——人为环境的响应研究

作者： 郭娅  来源：中国科学院大学 年份：2016 文献类型 ：学位论文

描述：鄱阳湖生态系统长期变化对气候——人为环境的响应研究

基于粗糙集和突变模型的鄱阳湖域生态经济区划

作者： 张延飞 唐鑫 张振东 丁木华  来源：人民长江 年份：2016 文献类型 ：期刊 关键词： 突变模型  生态经济区划  粗糙集  鄱阳湖域 

描述：级数模型计算鄱阳湖域32个区划单元的生态经济综合量化值。根据各区划单元的生态经济综合值,通过模糊聚类方法,将区划单元按生态经济系统状态区划为优、良、中、一般、差5个等级。区划结果表明,研究区域呈现

全文：级数模型计算鄱阳湖域32个区划单元的生态经济综合量化值。根据各区划单元的生态经济综合值,通过模糊聚类方法,将区划单元按生态经济系统状态区划为优、良、中、一般、差5个等级。区划结果表明,研究区域呈现

基于GWR模型的鄱阳湖地区城镇用地空间扩张差异及其影响因素研究

作者： 李欣 叶长盛  来源：江西农业学报 年份：2016 文献类型 ：期刊 关键词： 空间自相关  GWR模型  城镇用地  扩张  鄱阳湖地区 

描述：利用鄱阳湖地区2000、2005、2010、2013年4期土地利用现状图,采用扩张强度、扩张动态度、空间自相关等方法,分析了2000~2013年鄱阳湖地区城镇用地扩张的空间差异,利用GWR模型

全文：利用鄱阳湖地区2000、2005、2010、2013年4期土地利用现状图,采用扩张强度、扩张动态度、空间自相关等方法,分析了2000~2013年鄱阳湖地区城镇用地扩张的空间差异,利用GWR模型

鄱阳湖湿地农户生态补偿受偿意愿及其影响因素分析——基于CVM和排序Logistic模型的实证

作者： 熊凯 孔凡斌 陈胜东  来源：江西财经大学学报 年份：2016 文献类型 ：期刊 关键词： 鄱阳湖湿地  st  条件价值评估法  c模型  i  生态补偿  受偿意愿  排序Logi 

描述：基于农户调查数据,采用条件价值评估法(CVM)和排序Logi st i c模型,对鄱阳湖湿地农户生态补偿受偿意愿及其影响因素进行分析。研究结果表明:研究区内具有生态补偿受偿意愿的农户占被调查农户总数

全文：基于农户调查数据,采用条件价值评估法(CVM)和排序Logi st i c模型,对鄱阳湖湿地农户生态补偿受偿意愿及其影响因素进行分析。研究结果表明:研究区内具有生态补偿受偿意愿的农户占被调查农户总数

鄱阳湖湿地农户生态补偿受偿意愿及其影响因素分析——基于CVM和排序Logistic模型的实证

作者： 熊凯 孔凡斌 陈胜东  来源：江西财经大学学报 年份：2016 文献类型 ：期刊 关键词： 鄱阳湖湿地  st  条件价值评估法  c模型  i  生态补偿  受偿意愿  排序Logi 

描述：基于农户调查数据,采用条件价值评估法(CVM)和排序Logi st i c模型,对鄱阳湖湿地农户生态补偿受偿意愿及其影响因素进行分析。研究结果表明:研究区内具有生态补偿受偿意愿的农户占被调查农户总数

全文：基于农户调查数据,采用条件价值评估法(CVM)和排序Logi st i c模型,对鄱阳湖湿地农户生态补偿受偿意愿及其影响因素进行分析。研究结果表明:研究区内具有生态补偿受偿意愿的农户占被调查农户总数

浅水三角洲动态生长过程模型与有利砂体分布——以鄱阳湖赣江三角洲为例

作者： 高志勇 周川闽 董文彤 白斌 李雯  来源：现代地质 年份：2016 文献类型 ：期刊 关键词： 砂体预测  沉积演化  鄱阳湖  生长过程模型  浅水三角洲 

描述：上平原堤岸相沙泥质互层的沉积演化特征。结合鄱阳湖枯水期与洪水期的水文地质特征,建立了赣江浅水三角洲的动态生长过程模型,其动态成因演化过程可分为先期枯水期湖泊沉积,湖平面上升至最大洪泛期和再次枯水期

全文：上平原堤岸相沙泥质互层的沉积演化特征。结合鄱阳湖枯水期与洪水期的水文地质特征,建立了赣江浅水三角洲的动态生长过程模型,其动态成因演化过程可分为先期枯水期湖泊沉积,湖平面上升至最大洪泛期和再次枯水期