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- 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
- 垂向归纳模型下鄱阳湖丰、枯水期初级生产力特征及与环境因子相关性分析
- 作者： 李艳红 葛刚 王茂林 周晓岚 胡春华 来源：湖泊科学 年份：2016 文献类型 ：期刊 关键词： 相关分析 鄱阳湖 影响因子 丰枯水期 初级生产力 垂向归纳模型
- 描述：于2014年1月(枯水期)、7月(丰水期)对鄱阳湖湖水进行采集,测定相应的理化参数、叶绿素a浓度和光合有效辐射,结合初级生产力垂向归纳模型估算浮游植物初级生产力,分析湖区初级生产力特征及与环境因子
- 全文：于2014年1月(枯水期)、7月(丰水期)对鄱阳湖湖水进行采集,测定相应的理化参数、叶绿素a浓度和光合有效辐射,结合初级生产力垂向归纳模型估算浮游植物初级生产力,分析湖区初级生产力特征及与环境因子
- MERIS影像水环境遥感大气校正算法评价——以鄱阳湖叶绿素a浓度反演为例
- 作者： 曾群 张海东 陈晓玲 田礼乔 李文凯 王国良 来源：湖泊科学 年份：2016 文献类型 ：期刊 关键词： QUAC BEAM 水色遥感 大气校正 鄱阳湖 MERIS FLAASH 叶绿素a 6S
- 描述：MERIS是2002年发射的在轨运行近10年的ENVISAT-1卫星上搭载的主要传感器之一,在波段设置和辐射灵敏度等方面有非常突出的优势,能够较好地运用于Ⅱ类水体叶绿素a浓度反演,但Ⅱ类水体的大气
- 全文：MERIS是2002年发射的在轨运行近10年的ENVISAT-1卫星上搭载的主要传感器之一,在波段设置和辐射灵敏度等方面有非常突出的优势,能够较好地运用于Ⅱ类水体叶绿素a浓度反演,但Ⅱ类水体的大气
- 赣北鄱阳湖地区第四纪黄土的粒度特征及环境意义
- 作者： 徐传奇 贾玉连 刘倩 凌超豪 王鹏岭 来源：干旱区资源与环境 年份：2016 文献类型 ：期刊 关键词： 鄱阳湖 黄土 风积成因 古土壤 粒度特征
- 描述：对长江中游南岸鄱阳湖东侧砂山下风向的太平关黄土剖面进行了粒度测试分析,与南京下蜀黄土、巫山黄土和长江河流沉积物进行了对比。结果表明:1)太平关剖面粉砂(5-50μm)含量达到了50%以上,粘土次之
- 全文：对长江中游南岸鄱阳湖东侧砂山下风向的太平关黄土剖面进行了粒度测试分析,与南京下蜀黄土、巫山黄土和长江河流沉积物进行了对比。结果表明:1)太平关剖面粉砂(5-50μm)含量达到了50%以上,粘土次之
- 民政创新环境分析——基于鄱阳湖生态经济区的调查
- 作者： 刘翀 邹晓文 来源：社会工作(上半月实务) 年份：2016 文献类型 ：期刊 关键词： 民政工作 创新环境 鄱阳湖生态经济区
- 描述：民政创新环境分析——基于鄱阳湖生态经济区的调查
- [0图]鄱阳湖生态经济区发展报告（2015-2016） 畜禽养殖的环境影响及其治理政策研究
- 作者： 孔凡斌 潘丹 来源：北京：中国环境科学出版社 年份：2016 文献类型 ：图书
- 描述：鄱阳湖生态经济区发展报告（2015-2016） 畜禽养殖的环境影响及其治理政策研究
- 鄱阳湖湿地土壤有机碳氮同位素特征及其环境意义
- 作者： 王毛兰 赖建平 胡珂图 张丁苓 来源：中国环境科学 年份：2016 文献类型 ：期刊 关键词： 氮同位素 鄱阳湖 物质来源 湿地土壤 碳同位素
- 描述：通过对2011年鄱阳湖及其主要入湖河流（赣江、抚河、信江、修水及饶河）15个湿地土壤样品中δ13C及δ15N的测定,分析探讨了鄱阳湖及其主支流湿地土壤有机质和氮素来源、结果表明:鄱阳湖湖区湿地土壤中总有机碳（TOC）的含量在0.45%1.58%之间,总氮（TN）含量变化范围为0.06%0.17%;各入湖河流TOC含量为0.41%1.18%,TN含量在0.05%0.13%之间.鄱阳湖湖区湿地土壤有机质δ13C及δ15N变化范围分别为-28.35‰18.58‰和3.27‰6.84‰;各入湖河流湿地土壤δ13C和δ15N分别为-25.93‰-22.66‰和2.97‰5.41‰.有机质来源分析表明:除湖口处主要来源于C4植物外,鄱阳湖区及其入湖河流湿地土壤有机质的主要来源是C3植物.湖区湿地土壤氮素来源分析表明吴城处主要受农业化肥使用的影响,而其他采样点湿地土壤有机质氮素主要来源于生活污水;入湖河流湿地土壤氮素来源较复杂,生活污水、化肥及工业污水是其主要来源.
- 全文：通过对2011年鄱阳湖及其主要入湖河流（赣江、抚河、信江、修水及饶河）15个湿地土壤样品中δ13C及δ15N的测定,分析探讨了鄱阳湖及其主支流湿地土壤有机质和氮素来源、结果表明:鄱阳湖湖区湿地土壤中总有机碳（TOC）的含量在0.45%1.58%之间,总氮（TN）含量变化范围为0.06%0.17%;各入湖河流TOC含量为0.41%1.18%,TN含量在0.05%0.13%之间.鄱阳湖湖区湿地土壤有机质δ13C及δ15N变化范围分别为-28.35‰18.58‰和3.27‰6.84‰;各入湖河流湿地土壤δ13C和δ15N分别为-25.93‰-22.66‰和2.97‰5.41‰.有机质来源分析表明:除湖口处主要来源于C4植物外,鄱阳湖区及其入湖河流湿地土壤有机质的主要来源是C3植物.湖区湿地土壤氮素来源分析表明吴城处主要受农业化肥使用的影响,而其他采样点湿地土壤有机质氮素主要来源于生活污水;入湖河流湿地土壤氮素来源较复杂,生活污水、化肥及工业污水是其主要来源.