长江三峡库区玉溪遗址地层沉积特征研究   总被引：1，自引：0，他引：1  

徐伟峰  朱诚 《地层学杂志》2008,32(1):21-26

在考古断代和AMS14C测年基础上,通过对洪水沉积环境以及三峡库区中坝遗址1981年洪水沉积和玉溪疑似古洪水沉积的粒度对比分析,发现它们的平均粒径、分选系数、偏度和峰度都在同一值域范围内;概率累积曲线都呈明显的三段式,从而推断出玉溪遗址的文化间隙层为古洪水沉积。  相似文献   

扬子地块东南缘多期构造变形及其油气意义   总被引：1，自引：0，他引：1  

陈科  林伟  王清晨 《地质学报》2008,82(3):308-315

扬子地块的构造演化及其动力学机制约束着古生代海相油气成藏,而扬子地块东南缘的构造变形特征是理解整个扬子地块构造变形的关键所在.通过对武夷、云开和肇庆地区的构造特征研究,初步划分出扬子地块东南缘的三期重要变形①早古生代末期云开地区NW向剪切变形,武夷山地区ESE向剪切变形;②中生代早期云开、肇庆地区NE向逆冲推覆作用;③中生代晚期武夷山地区的脆性构造变形.在重新认识区内构造演化的基础上,对其动力学作了初步探讨.这些认识有助于今后中国南方碳酸盐岩含油气远景的评价.  相似文献   

长江中下游典型湖泊近代环境变化研究   总被引：7，自引：0，他引：7  

薛滨  姚书春  夏威岚 《地质学报》2008,82(8):1135-1141

选择长江中下游的典型湖泊洪湖、巢湖、石臼湖和太湖,采集了沉积柱样,测定了总有机碳、总氮、总磷,并采用210Pb和137Cs定年以研究湖泊近代环境演变。根据洪湖137Cs蓄积峰得到过去50 a里洪湖沉积速率经历了一个由慢到快再变慢的过程,1963~1986年之间沉积速率最大,达0.174 cm/a,这可能是因为当时湖区大规模开垦有关。巢湖钻孔核素的研究发现20世纪70年代以来随着深度的减少,巢湖钻孔中沉积通量在增加,可能与流域内水土流失逐步加重有关。对营养盐的分析表明,洪湖50年代以来沉积物中营养元素急剧增加,巢湖70年代以来营养元素开始增加,在太湖中体现为80年代,石臼湖中则为近百年来营养元素开始快速增加。从营养盐增加的幅度来看,草型湖的洪湖、石臼湖要大于藻型的巢湖以及太湖藻型区域。本文尝试利用总有机碳、总磷获取了湖泊环境变化的速率。研究表明总有机碳和总磷的变化速率存在波动性,这可能与湖泊的自我调节有关。而总有机碳的变化速率在最近时间阶段内基本呈正值,对于洪湖来说在80年代初,石臼湖在1970年左右,太湖在80年代初,巢湖在60年代。总有机碳、总磷变化速率的振荡幅度与周期也许对理解当今湖泊处于何种位置,由此采取何种湖泊管理手段提供重要认识。  相似文献   

The development and control of the land subsidence in the Yangtze Delta,China   总被引：3，自引：0，他引：3  

Jichun Wu  Xiaoqing Shi  Yuqun Xue  Yun Zhang  Zixin Wei  Jun Yu 《Environmental Geology》2008,55(8):1725-1735

Land subsidence in China occurs predominantly in 17 provinces (cities) situated in the eastern and middle regions of the country, including Shanghai, Tianjin and Jiangsu, and Hebei provinces. It is primarily caused by groundwater overpumping. One of the areas most severely affected by land subsidence is the Yangtze Delta, most of which consists of Shanghai City, the Su-Xi-Chang area (Suzhou, Wuxi and Changzhou cities) of Jiangsu Province, and the Hang-Jia-Hu area (Hangzhou, Jiaxing and Huzhou cities) of Zhejiang Province. The excessive exploitation of groundwater forms in a large regional cone of depression and, consequently, land subsidence is also regional, currently centered in the Shanghai and Su-Xi-Chang areas. In 2002, the maximum cumulative subsidence of Shanghai, Su-Xi-Chang and Hang-Jia-Hu were 2.63 m, 2.00 and 1.06 m, respectively. The land subsidence area is continuing to expand throughout the Yangtze Delta. To study the characteristics and the pattern of this land subsidence, the government has implemented a monitoring system involving the placement of 37 groups of extensometers (layers marks) and drilling of more than 1000 observation wells. These provide an invaluable historical record of deformation and pore water pressure and facilitate studies on the special features of soil deformation when the groundwater level changes due to pumping. Several measures have been taken in recent years to control the development of the land subsidence in the different areas; these include groundwater injection, prohibition of pumping deep confined groundwater, and an adjustment of the pumping depth and magnitude of the groundwater withdrawn. At present, although the subsidence area is still increasing slowly, the subsidence rate is controlled.  相似文献   

Migration patterns of Neolithic settlements on the abandoned Yellow and Yangtze River deltas of China   总被引：4，自引：0，他引：4  

Zhongyuan Chen  Yongqiang Zong  Hui Wang 《Quaternary Research》2008,70(2):301-314

Archaeological records of the Neolithic settlements on the eastern China coast between 35°N and 30°N, an area covering the abandoned Yellow River and the Yangtze River delta plains, reveal that Neolithic people moved from the Yellow River basin onto the northern coast for fishing, hunting and dry-land agriculture ~ 7000 yr ago. Marine transgression interrupted their activities on the low-lying (2-5 m in elevation) coastal wetlands between 6000 and 5000 yr ago, after which they reclaimed their land near the river mouths. Their migration routes on the southern Yangtze delta plain indicate another scenario: early Neolithic communities moved onto the plain for wet-rice cultivation. Despite relative sea-level rise from 7000 to 4000 yr ago, a large number of settlements were established on the lowlands between the eastern Chenier Ridges and the western Taihu Lake depression. The Chenier Ridges, with ~ 1.0 m higher topography than the adjacent coastal area, played a role in sheltering the Neolithic people. Subsequently, settlements waned considerably, possibly due to further marine inundation combined with cold climate. The present study shows that migration patterns of the Neolithic settlements are closely associated with a gradually rising sea level between 7000 and 4000 yr ago.  相似文献   

气候变化背景下中国沿海地区典型区域脆弱性评价——以长三角为例     

王洁  王卫安  王守芬 《测绘与空间地理信息》2017,(3)

采用静态情景模拟与基于GIS的淹没分析相结合的情景分析方法和指标体系方法综合的脆弱性分析方法开展研究,重点探讨了中国沿海地区典型区域在全球气候变化背景下的脆弱性情况。从危险性、暴露性、敏感性和恢复性等方面开展脆弱性分析,探讨了指标间的权重分配方法,并将脆弱性评估结果划分为低、中、高、极高4个等级,从而为区域的防灾降险提供决策依据。  相似文献   

Statistical Modeling and Trend Detection of Extreme Sea Level Records in the Pearl River Estuary     

Weiwen WANG  Wen ZHOU 《大气科学进展》2017,34(3):383-396

Sea level rise has become an important issue in global climate change studies. This study investigates trends in sea level records, particularly extreme records, in the Pearl River Estuary, using measurements from two tide gauge stations in Macau and Hong Kong. Extremes in the original sea level records(daily higher high water heights) and in tidal residuals with and without the 18.6-year nodal modulation are investigated separately. Thresholds for defining extreme sea levels are calibrated based on extreme value theory. Extreme events are then modeled by peaks-over-threshold models. The model applied to extremes in original sea level records does not include modeling of their durations, while a geometric distribution is added to model the duration of extremes in tidal residuals. Realistic modeling results are recommended in all stationary models. Parametric trends of extreme sea level records are then introduced to nonstationary models through a generalized linear model framework. The result shows that, in recent decades, since the 1960 s, no significant trends can be found in any type of extreme at any station, which may be related to a reduction in the influence of tropical cyclones in the region. For the longer-term record since the 1920 s at Macau, a regime shift of tidal amplitudes around the 1970 s may partially explain the diverse trend of extremes in original sea level records and tidal residuals.  相似文献   

自然环境高温对长江中下游地区中稻结实率的影响及模拟     

宣守丽  石春林  刘杨 《气象与环境科学》2017,40(1):73-77

利用长江中下游地区6个代表站2004—2011年中籼迟熟水稻品种区试资料及1984—2013年逐日最高气温资料,通过分析田间环境下逐日最高气温与水稻结实率的关系发现,长江中下游地区中稻高温敏感时段主要在水稻齐穗期前36天至齐穗期前4天。其中,齐穗期前14天左右(减数分裂期前后)高温对结实率的影响最为显著。在此基础上,利用水稻高温败育模型,根据各样本水稻减数分裂期逐日最高气温,实现研究区域站点尺度水稻高温败育的定量模拟预测。模型对高温年份2004年和2007年各站点水稻相对结实率模拟和预测的均方根误差分别为4.74%和2.84%。分析表明,利用基于水稻高温败育模型的定量模拟方法,可对长江中下游地区水稻高温热害情况进行较好预测。  相似文献   

长江三角洲人口与经济空间格局演变及影响因素   总被引：3，自引：1，他引：2  

闫东升  杨槿 《地理科学进展》2017,36(7):820-831

人口与经济是反映区域差异的两大主要指标,其空间分布与区域差异的形成有密切关联。产业作为经济发展的基本载体,产业结构是影响人口与经济空间分布协调性的重要因素。在产业转移加快的背景下,长三角人口与经济空间分布格局也出现了一定的变化,对二者空间演变协调性研究具有重要的现实意义。本文运用重心、不一致指数及不均衡指数等方法,分析2000-2013年长三角人口与经济空间格局演变趋势及影响因素。结果表明,核心区经济增长有所放缓、边缘区经济增长加快,但人口向核心区集聚态势依然存在;基于不一致指数与不均衡指数的分析表明,与边缘区GDP快速增长导致区域GDP格局显著变化不同,边缘城市的人口增长并不显著且集中在部分城市;尽管人口与经济不一致指数分布格局呈现相对稳定的“核心—边缘”格局,但人口与经济增长不协调性增强推动了长三角人口与经济总体协调性的提高。本文尝试从市场、政府及人均GDP等因素对长三角人口与经济分布不协调的现象进行了解释。  相似文献   

基于生境质量的城市增长边界研究——以长三角地区为例   总被引：5，自引：1，他引：4  

吴健生  毛家颖  林倩  李嘉诚 《地理科学》2017,37(1):28-36

基于“生态优先”理念,提出一种利用生境质量评估策略的城市增长边界划定方法。结合ArcGIS和InVEST模型,通过综合评估生境自身及其在威胁情境下的质量,模拟各市独立规划、建设用地指标再分配及区域一体化发展的三类建设用地扩张情景,分别划定2024和2034年的长三角地区城市增长边界。结果表明：研究区生境质量总体呈南高北低格局,平均生态系统服务价值密度为10 770.604元/（hm²·a）,高质生境位于西南地区;根据指标再分配及一体化发展情景模拟的2024年研究区建设用地总量分别为10 583.273 km2和10 489.090 km2,2034年达到13 603.535 km2和13 252.370 km2;模拟的建设用地集中在东部沿海地区,并向北部及环杭州湾区域拓展;建设用地指标再分配能从整体上减少建设用地对优质生境的占用,区域一体化发展则能进一步降低城市发展造成的生态压力。  相似文献