首页 | 本学科首页   官方微博 | 高级检索  
相似文献
 共查询到20条相似文献,搜索用时 187 毫秒
1.
长江口深水航道30年空间特征变化研究   总被引:1,自引:1,他引:0  
根据1973-2003年6幅长江口海图资料,建立不同时期长江口深水航道水下数字高程模型, 对航道治理前后30 a的冲淤状况、纵剖面水深变化以及空间模拟等进行研究. 结果表明,30 a来深水航道冲淤交替出现,总变化趋势是冲刷.航道冲淤除与 水动力条件有关外,与治理工程也有密切联系.长江口深水航道治理一期工程结束后,水深明显加深,坡度比变大,主航道呈现平顺的“U”形河道景观.  相似文献   

2.
应用遥感、地理信息系统和计算机制图技术,通过对长江下游河床及江岸形态、结构、组成物质及其时空变化的分析和识别,建立近五十年来长江河道演变图谱。在此基础上研究长江下游河道演变规律,预测河势发展趋势,评价江岸的稳定性,为长江治理、防洪以及岸线资源合理开发利用提供科学依据。  相似文献   

3.
长江下游河道演变图谱研究   总被引:6,自引:0,他引:6  
应用遥感、地理信息系统和计算机制图技术,通过对长江下游河床及江岸形态、结构、组成物质及其时空变化的分析和识别,建立近五十年长江河道演变图谱。在此基础上研究长江 下游河道演变规律,预测河势发展趋势,评价江岸的稳定性,为长江治理、防洪以及岸线资源合理开发利用提供科学依据。  相似文献   

4.
长江皖江段岸线资源的遥感调查及开发利用评价   总被引:1,自引:0,他引:1  
本文应用TM卫片,彩红外航片结合调查与已有资料,牟皖江岸线资源的分布与利用现状进行了遥感解译与评价,并根据地区经济背影区位条件,效能网络等因素的综合分析,进一步提出了可利用岸线的建议,为今后皖江岸线资源的开发利用提供了科学依据。  相似文献   

5.
一直以来,水库泥沙淤积问题一直困扰水库的安全。一些水库建成后投入运行的时间较长,由于早期测量、检测和监测仪器落后等原因,引起库区基础资料的缺失,对了解水库泥沙淤积情况影响较大。文中阐述应用高密度电法对某库区泥沙淤积进行调查,连续、快速、有效的探测出了水深和淤积层厚度,探测成果与水上钻孔验证有很好的对应性,为后续水库清淤设计方案提供技术支撑。  相似文献   

6.
一直以来,水库泥沙淤积问题一直困扰水库的安全。一些水库建成的时间较长、原始测绘数据缺失,早期测量仪器落后等原因而引起库区测绘资料失实,这些都严重影响了准确掌握水库泥沙淤积情况。文中应用高密度电法对某库区泥沙淤积进行调查,连续、快速、有效的探测出了水深和淤积层厚度,探测资料与水上验证钻孔资料有很好的对应性,为后续水库清淤设计方案提供支撑资料。  相似文献   

7.
中国船舶首航东北航道及其展望   总被引:1,自引:0,他引:1       下载免费PDF全文
王洛  赵越  刘建民  韩淑琴 《极地研究》2014,26(2):276-284
北极航道按其处于地球上的地理方位可分为东北航道和西北航道,东北航道按航线所处的纬度范围则可分为北极低纬航线(北极近岸航线)、北极中纬航线(作为国际常规航线)、北极高纬航线、挺极航线。"雪龙"号于2012年夏季书写了中国船舶首航东北航道的航海史。"雪龙"号从东北航道的起点白令海峡开始,沿东北航道抵达冰岛,并沿北极高纬航线返回白令海峡,完成往返穿越北冰洋之旅。据此,本文对北极航道的分类提出了一些看法,对东北航道的商业航行情况进行了总结,在此基础上概述了"雪龙"号此次首航东北航道的整个进程和关键问题,同时对中国建立北极航道战略进行了思考并提出了建议。  相似文献   

8.
董建平 《西部资源》2012,(3):113-114
内蒙古基础地理信息数据库是依托统一的标准体系和质量保障体系,整合基础地理信息数据,建成数据库管理体系,形成完整的数据库系统;以GIS应用为主,兼顾地图产品的制作,建立产品开发体系和分发服务体系,以及支持系统运行的网络交换体系。  相似文献   

9.
本文借助GIS空间分析手段,对"东洛岛港方案"的港区平面做出设计,运用ARC/INFO 8.1和ArcView 3.2软件,建立高程数据库,将港区平面设计的航道等要素图层比对底图进行空间叠置分析.得出结论是:作为福州深水港区的备选方案,东洛岛港方案在技术上是可行的.  相似文献   

10.
传统的水深测量方法是利用测量船上安装的测深设备和定位设备测出水域各点的水深。用遥感方法进行水深反演,基于OLI遥感影像对错戳龙错盐湖进行水深反演研究,确定OLI4波段是研究错戳龙错盐湖遥感水深反演的最佳波段,建立了此盐湖的水深遥感模型。经过对遥感数据和实测点数据的回归分析,建立了拟合方程。根据拟合方程对水深进行反演,反演结果与实测结果基本一致,从而证明了遥感测水深方法的快速有效性,弥补了传统实测水深方法的不足。  相似文献   

11.
长江江苏段末次盛冰期古河槽特征   总被引:1,自引:0,他引:1  
选择长江江苏段作为研究河段,根据南京长江三桥、长江大桥、长江四桥、润扬长江大桥、扬中长江大桥、江阴长江大桥、苏通长江大桥7个断面的285个地质勘探钻孔资料及参考文献中的8个钻孔资料,建立了7个长江古河谷地质剖面图。在拟建南京长江四桥附近、扬中长江大桥附近的7个钻孔进行了采样分析,获得了8个14C年代、1个ESR年代数据。通过分析发现,末次盛冰期长江古河槽镇江以上切割到基岩,镇江以下嵌在老河床相沉积层上,河槽在南京下关-栖霞山段形成局部深切;南京段约-63 m以下的河槽为末次盛冰期的古河槽,相对狭窄陡峭,宽深比较小,向下游宽深比逐渐变大,扬中以下形成分叉河道体系;古河槽中自下而上充填了从粗到细的沉积旋回,河床相沉积物向下游逐渐变细。  相似文献   

12.
The operation of large-scale reservoirs have modified water and sediment transport processes, resulting in adjustments to the river topography and water levels. The polynomial fitting method was applied to analyze the variation characteristics of water levels under different water discharge values in the Jingjiang reach of the Yangtze River from 1991–2016. The segregation variable method was used to estimate the contributions of the varied riverbed evaluation, the downstream-controlled water level, and the comprehensive roughness on the altered water level at an identical flow. We find that low water levels in the Jingjiang reach of the Yangtze River from 1991–2016 are characterized by a significant downward trend, which has intensified since 2009. Riverbed scouring has been the dominate factor causing the reduced low water level while increased roughness alleviated this reduction. From 1991–2016, there was first a decrease followed by an increase in the high water level. The variation characteristic in terms of the "high flood discharge at a high water level" before 2003 transformed into a "middle flood discharge at a high water level" since 2009. The increased comprehensive roughness was the main reason for the increased high water level, where river scouring alleviated this rise. For navigation conditions and flood control, intensified riverbed scouring of the sandy reaches downstream from dams enhanced the effects that the downstream water level has on the upstream water level. This has led to an insufficient water depth in the reaches below the dams, which should receive immediate attention. The alteredvariation characteristics of the high water level have also increased the flood pressure in the middle reaches of the Yangtze River.  相似文献   

13.
Waterfront resources are important and special kind of natural resources in the marginal area between land and water. The Yangtze River, the longest river in China, is not only rich in waterfront resources, but also has favorable development conditions with great potentiality. Aided by large-scale underwater topographic map, the major factors of the waterfront resources in the middle and lower reaches of the Yangtze River, such as the stability, the water depth and the natural conditions for port construction, are assessed in this paper respectively on the basis of the overall investigations. The results show that: (1) the waterfront resources are abundant in the middle and lower reaches of the Yangtze River, but lack of perfectly combined high grade waterfront; (2) there exists an obvious regional difference in the natural quality of the waterfront along the Yangtze; (3) the fore-bank water depth and waterfront stability are the main natural factors related to the waterfront quality in the middle and lower reaches of the Yangtze River; (4) the waterfronts along the Yangtze are mainly used for port, warehouse and industrial purposes; and (5) the waterfronts near important cities are highly used, especially the high-quality waterfronts. In addition, some suggestions for the development and utilization of the waterfront resources are presented in this paper.  相似文献   

14.
The stratigraphical cross-sections of the Yangtze River incised-valley near the No.1,No.3 and No.4 Nanjing Yangtze River bridges were established with respective bore date and documents.By 14C age analysis of the samples of four drilling cores near the No.4 Bridge(to be built),we can find that the time range of paleo-valley is dated in the LGM at a depth of-60 m to-90 m near Nanjing.It is also indicated that the deep incised-valley channel was narrow and the river flowed swiftly.The ancient Yangtze River deep channel presented partially and deeply incised features near the No.1 Bridge.According to previous publications,much research has been done on the main paleo-channel of the Yangtze River,but few results have been achieved on discharge estimation.In this paper,the incipient velocity and average velocity of the LGM was calculated with Vc = 4.60 d 1/3 h1/6,95 Vc 1.28lg 13.15.h.gd,d = 6 * 90 V 6.5u h≈ d,etc.,in terms of the river shape,sedimentary grain size and sequences near the No.3 and No.1 bridges.Moreover,the discharge in Nanjing reach of the Yangtze River during the LGM has been estimated to be around 12,000-16,000 m3/s according to the relationship of discharge,velocity of flow and cross-section.  相似文献   

15.
Waterfront resources are important and special kind of natural resources in the marginal area between land and water.The Yangtze River,the longest river in China,is not only rich in waterfront resources,but also has favorable development conditions with great potentiality.Aided by large-scale underwater topographic map,the major factors of the waterfront resources in the middle and lower reaches of the Yangtze River,such as the stability,the water depth and the natural conditions for port construction,are assessed in this paper rspectively on the basis of the overall investigations.The results show that:(1)the waterfront resources are abundant in the middle and lower reaches of the Yangtze River,but lack of perfectly combined high grade waterfront;(2)there exists and obvious regional difference in the natural quality of the waterfront along the Yangtze;(3)the fore-bank water depth and waterfront stability are the main natural factors related to the waterfront auality in the middle and lower reaches of the Yangtze River;(4)the waterfronts along the Yangtze are mainly used for port,warehouse and industrial pruposes; and (5)the waterfronts near important cities are highly used,especially the high-quality waterfronts.In addition,some suggestions for the development and utilization of the waterfront resources are presented in this paper.  相似文献   

16.
水库运行改变了坝下游水沙输移条件,在河道冲刷的同时,引起水位过程出现适应性调整.本文以长江中游荆江河段为对象,采用多项式拟合法,对比分析1991-2016年间分级流量一水位变化特征,采用基于河流动力学原理的分离变量法,识别河道冲淤、下游控制水位及河床综合糙率等变化对分级流量-水位变化的影响程度.研究表明:1991-20...  相似文献   

17.
长江中下游岸线资源的特征及其开发利用   总被引:14,自引:0,他引:14  
王传胜  王开章 《地理学报》2002,57(6):693-700
运用大比例尺水下地形图,在岸线资源总量勘查的基础上,评价了长江中下游干流岸线的水深条件、岸线稳定性条件和建港自然条件,分析了本区域岸线资源的基本特征,提出了长江岸线资源开发的基本原则和中下游干流岸线利用建议。  相似文献   

18.
长江中下游河道岸线的整治与开发利用   总被引:2,自引:2,他引:2  
通过分析长江中下游河道的各段的整治措施,提出长江中下游河道整治的关键是:(1)控制河势,治理河岸崩塌,增强河床与河岸的稳定性;(2)充分重视三峡工程建成后对河道变化产生的影响;(3)科学合理地控制好长江采砂。并分析了长江岸线开发利用现状及存在问题,提出了岸线利用的原则。在长江中下游河道岸线利用过程中,还存在:河势不稳定,布局不合理,深水浅用浪费岸线资源和水污染严重等问题,提出遵照河道演变规律开发岸线,保护河岸工程的安全,根据河岸水质污污染与河床特点合理布置引水口和排污口,提高引水质量。  相似文献   

19.
1990年代以来,尤其是浦东开发开放以来,日益推进的全球化和市场化使长三角地区的制造业结构发生了深刻的变化。采用shift—share方法,对1993-2008年16年来长三角及其各次区域31个制造业行业的演进历程进行了考察,发现在未来较长时期内,长三角次区域的产业同构还将继续保持并在一定程度上加强。产业同构将迫使上海率先进行产业升级,从而加速上海与江苏和浙江之间的产业异化过程。未来长三角地区的制造业结构将在沿着从同化到异化的路径行进的过程中实现产业结构的动态演进。  相似文献   

20.
徐维祥  张凌燕  刘程军  杨蕾  黄明均 《地理科学》2017,37(11):1659-1667
利用区位熵、耦合协调模型、趋势面分析、引力模型等对长江经济带城市功能与区域创新耦合协调度进行了测算,并对其空间联系进行了分析。得到了以下结论:2004~2014年,各个城市单元整体的耦合协调度均有一定程度的提升,逐渐形成三大连绵较高协调集聚区,长江经济带总体耦合协调度呈现出“下游高-中上游低”的空间趋势;空间联系的最大引力线联结格局比较稳定,长三角城市群是耦合协调发展的重要基地和优势集聚区;长江下游地区空间联系的网络密度与网络结构的复杂程度远高于长江中上游地区,并且逐渐形成由以长三角为核心城市圈,牵引长江中上游城市多极化发展的网络结构。  相似文献   

设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号