土地利用图中线状要素综合的质量评价     

王晓妍 《测绘通报》2020,(4):116-120

作为土地利用图综合的一个重要组成部分，线状要素综合质量的好坏对于有效提高自动制图综合的正确率具有重要意义。本文基于模糊综合评判理论对土地利用图中线状要素的综合进行了质量评价。首先，基于制图综合约束，确定评价指标体系，组成评价因素集；其次，在确定评判集和权重集的基础上，建立线状要素综合质量评价模型；最后，利用试验验证了评价方法的有效性。该研究为客观评价土地利用图中线状要素的综合质量提供了新的思路。  相似文献   

综合Span图和纹理特征的高分三号影像建筑区提取     

盛玉婷  赵争  王童童 《北京测绘》2020,(1):73-78

建筑区的识别和提取是城市环境规划与研究至关重要的工作。本文采用高分三号全极化SAR影像,提出了一种综合Span图和纹理特征的建筑区提取方法。首先基于Span图利用灰度共生矩阵算法提取图像的7种原始纹理特征,通过目视解译选择出4种纹理效果较好的统计量,然后利用主成分分析法去除他们之间的相关性,筛选出2个最佳纹理特征与Span图结合,最后对组合影像进行分类提取。本文将提取结果与综合灰度和纹理特征建筑区提取、无纹理特征提取方法结果进行对比,实验结果表明:本文方法提取建筑区边界轮廓更加清晰,精度可达92%,提取效果明显得到了优化。  相似文献   

北黄海营养盐结构及限制作用时空分布特征分析   总被引：5，自引：0，他引：5  

张辉  石晓勇  张传松  王丽莎 《中国海洋大学学报(自然科学版)》2009,39(4)

根据2006-07～2007-10 4个航次的调查资料,分析讨论了春、夏、秋、冬四季北黄海营养盐结构分布变化特征及营养盐限制状况.结果表明:春夏季表层,10 m层N/P,Si/N和Si/P值分布变化较大,呈现辽东半岛和山东半岛近岸高中部海域低的分布态势,高值区分别自鸭绿江口和夹河河口向外扩散,且均高于Redfield比值.秋冬季表层N/P,Si/N和Si/P值明显降低,且分布变化不大.10 m层,底层各季节分布相近,高值区位于鸭绿江口和夹河口附近.营养盐结构的分析表明,北黄海海域春夏季大部分站位表层浓度低于浮游植物生长的最低阈值,且春、夏、秋三季主要是受P的潜在限制,冬季营养盐限制状况消失.  相似文献   

峡山湖沙坝的现代沉积     

邱隆伟  周军良  姜在兴  王新征 《海洋地质与第四纪地质》2009,(4)

以现代沉积考察为基础,结合粒度分析资料,对湖泊中沙坝的沉积特征进行了详细的探讨。研究认为峡山湖沙坝微相分为坝前、坝主体、坝后3个沉积单元。坝前受湖浪作用明显,沉积物以湖浪作用形成的浪成沙和冲洗沙为主,发育滩脊和席状沙沉积体。坝主体沉积物以厚度较大、受湖水及风改造明显的中细沙为主,可进一步细分为坝-滩复合体和坝-沙丘复合体。坝后受坝主体阻隔,丰水期为局限湖湾沉积,枯水期发育沼泽沉积。湖泊中沙坝的形成是在滨浅湖环境中水动力和岸线、地貌等因素的影响下,受湖浪、湖流以及暴露环境下风的改造等共同作用的结果,湖浪所派生的沿岸流对沙坝的演化起着至关重要的作用;丰水期沙坝体接受湖水动力的改造,枯水期沙坝体接受风的改造。  相似文献   

近三十年来昆明市建成区扩展遥感监测与分析   总被引：5，自引：1，他引：4  

谭文彬  刘斌  张增祥  赵晓丽  易玲  汪潇 《地球信息科学学报》2009,11(1):117-124

以遥感影像为数据源,借助GIS技术提取了6个时期的昆明市建成区扩展及对周边土地占用的信息.在此基础上,利用扩展弹性系数、分形维数等方法分析了昆明市1974～2004年建成区扩展的时空特征、土地利用类型演变过程,以及与人口增长之间的协调关系,并应用相关分析和主成分分析方法,对影响昆明市建成区扩展的社会经济因素进行分析.结果表明:30年来昆明市建成区扩展了3.07倍,1974～1988年的14年间,仅增加了13.36km²,而1988～2004年的16年,增加了144.07km².其增长速度与市区人口增长速度相比,有时超前有时滞后.建成区是以老城区为核心沿东北、西南、东南三个方向呈“星形”扩展.其扩展占用的土地主要是耕地.自然因素对建成区的扩展形态起着限制作用,社会经济因素是建成区扩展的内在推动力,政策和规划对建成区扩展起着引导和促进作用.  相似文献   

Rapid mapping of high resolution SAR scenes     

F. Dell&#x;Acqua  P. Gamba  G. Lisini 《ISPRS Journal of Photogrammetry and Remote Sensing》2009,64(5):482-489

This paper describes a semi-automatic procedure for cartographic mapping using high resolution SAR and interferometric SAR data. Various two-dimensional features are extracted and combined in order to achieve a basic yet effective recognition of the elements in the scene. Many relevant elements of the landscape are automatically extracted without requiring any deep interaction with the operator. Being based on geometric models assuming regularity of shapes and patterns, the procedure is well suited for detecting man-made features, such as the road network (outside and inside human settlements) and built-up areas. It can be used, however, to extract natural features, focusing on different geometric models. Moreover, extracted elements of the scene can be grouped into higher level ones, such as crossroads, bridges and overpasses, through data fusion at the feature level, because the procedure is characterized by a multi-scale, object-based approach.  相似文献   

Tidal analysis in the venturi-shaped area between Zhenhai and Shenjiamen in the East China Sea     

吕华庆  胡建炯 《中国海洋湖沼学报》2009,27(1):103-111

In order to better understand the general tidal features in the venturi-shaped area between Zhenhai and Shenjiamen in the northern coastal region of Zhejiang Province in the East China Sea, the tidal data were obtained from both the three permanent tide stations of Zhenhai, Dinghai and Shenjiamen, and four temporary tide stations of Mamu, Chuanshan, Guoju and Liuheng, along with the current speed being observed at Luotou Waterway. Results from harmonic analysis show that: (1) The area was dominated by shallow water tides with irregular semi-diurnal features, and the smallest tidal range occurred in the area near a crossing line between Zhenhai and Dinghai stations, indicating that a tidal node existed in the southern Hangzhou Bay; (2) Formulae, HS2/HM2 >0.4 and gM2-(gK1+gO1)=270° (where H and g are harmonic constants), could be used as judging criteria for high and low tidal level diurnal inequalities; (3) The duration difference between ebb and flood tides could be roughly assessed by the ratio of HM4 vs. HM2; and the larger the ratio is, the bigger the duration difference is. At the same time, the duration period could be assessed by 2gM2-gM4, the epoch difference between M2 and M4 tidal constituents. If 2gM2-gM4 <180°, then the ebb duration is longer than the flood duration; if 180°< 2gM2-gM4 <360°, the result is reversed; (4) Taking Dinghai station as a center point, the highest tidal levels and the average high tidal levels, as well as the average tidal ranges at all stations became higher and larger both southeastwards and northwestwards, while the lowest tidal levels and the average low tidal levels appeared to be lower both southeastwards and northwestwards; and (5) The tidal patterns were not all in line with the tidal current patterns. As a conclusion, the smallest tidal range occurred in the narrow part of the venturi-shaped area. Along the both sides of the area, the highest tidal level and tidal range became higher and larger, while the lowest tidal level became lower with the increase of the distance from the narrow throat area. This is somehow different from the theory that the tidal level increases gradually when it moves towards the top narrow area of a V-shaped bay or estuary.  相似文献   

土壤热磁组分形貌特征及元素富集方式     

郭志娟  马生明  胡树起  席明杰 《物探与化探》2012,36(3):396-402

利用光学显微镜和带能谱的扫描电子显微镜（SEM）等方法研究了土壤热磁组分的形貌特征、结构、表面性质及矿物组成,并与化学分析相结合,探讨了土壤热磁组分对矿化指示元素的富集作用和机理。研究结果表明,土壤热磁组分以铁锰氧化物为主,是由土壤中非晶质铁锰氧化物转化而来的。通过对土壤、土壤热磁组分、土壤非磁性组分中铁锰氧化物与成矿及其伴生元素的相关关系分析,证实了土壤热磁组分对矿化指示元素的富集作用,为深化土壤热磁组分测量方法的基础理论提供了依据。对比试验结果表明,土壤热磁组分测量较常规土壤测量具有更强的发现由深部矿体引起的微弱矿化信息的能力。  相似文献   

华北地台北缘火山岩型铀钼矿床找矿模型研究          下载免费PDF全文

杜俐  沈光银  林银山 《地质找矿论丛》2012,27(4):458-462

460铀钼矿床具有很好的火山岩型铀钼矿找矿前景。460铀钼矿早期为斑岩型矿化,晚期叠加火山热液型矿化,成矿时代为晚白垩世及新近纪。铀源层(体)为张家口组三段酸性火山岩及次流纹斑岩,由壳源重熔岩浆作用形成。以460矿床区域地质背景、成矿环境、矿床地质特征及找矿标志研究为重点,总结归纳了火山岩型铀钼找矿方法,建立了华北地台北缘火山岩型铀钼矿床的找矿模型。  相似文献   

河南省舞阳铁矿田岗庙刘铁矿床的地质特征及构造控矿分析          下载免费PDF全文

刘昭宜 《地质找矿论丛》2012,27(2):180-185

文章从地层、构造、矿体和矿石等方面总结了河南省舞阳铁矿田岗庙刘铁矿床的地质特征,分析了控制铁矿床的地质构造.铁矿床为沉积变质型铁矿,含矿岩系位于新太古界铁山庙组的上、下混合岩段之间;矿床赋存的空间位置严格受地堑和地垒式断块控制;古侵蚀面不整合构造面只使岗庙刘矿床中部矿块的矿石全部氧化,而对东部和西部矿块没有造成很大的影响.  相似文献