Unmanned aerial vehicle based remote sensing method for monitoring a steep mountainous slope in the Three Gorges Reservoir,China     

Haifeng Huang  Jingjing Long  Haiyu Lin  Lei Zhang  Wu Yi  Bangjun Lei 《Earth Science Informatics》2017,10(3):287-301

Monitoring has been considered to be the most effective means of preventing and mitigating geo-hazards. Unmanned aerial vehicle (UAV) based remote sensing has been proven to be a viable method for monitoring relatively flat areas, but has typically encountered challenges on steep mountainous slopes. The Qinglingou Slope, which is located at the head of the Three Gorges Reservoir, China, was selected as a case study, and a UAV-based remote sensing method was applied to monitor this steep mountainous slope. The UAV, which was equipped with a camera, was used to acquire images on May 10 and Sept. 13, 2015. At the same time, a plan for establishing and measuring a detailed network of ground control points (GCPs) and check points was carefully designed and implemented, according to the local conditions. Georeferenced digital surface models (DSMs) and digital orthophotos were obtained by photogrammetric processing. Based on the results, a simple and quick method that identified and quantified slope deformation by calculating and analyzing the changes in the DSMs was developed. The results showed that the UAV-based remote sensing method was rapid, safe and effective, and it could be valuable for monitoring a large number of steep mountainous slopes in the Three Gorges Reservoir.  相似文献   

政区多粒度时空对象建模及其Geodatabase实现     

程星华  胡迪  俞肇元  龙毅  周如财 《地球信息科学学报》2017,19(9):1228-1237

全空间信息系统是将现实世界抽象为由多粒度时空对象组成的数据世界,对动态且复杂的现实世界中的各类时空实体对象进行表达、分析等。时空数据模型是时态地理信息系统（TGIS）核心,在一些特定领域上取得了较好的应用效果,对时空对象的时态信息进行了一定程度的表达,但仍旧无法完整地描述时空对象的变化以及联系。本文在分析时空数据模型的研究现状和存在问题的基础上,以全空间多粒度时空对象建模为指导思想,以北京近百年来的政区演变为例,分析了政区的基本特征,进而将政区看作是多粒度时空对象,探索了多粒度时空对象的建模方法,对政区进行了多粒度时空对象表达,并采用可视化表达的方法进行了实验验证。结果表明：多粒度时空对象建模能较好地反映政区的空间特征、属性特征和时间特征,反映其在时空上的演变过程以及便于更好地支持时空对象的查询、分析和可视化表达等。  相似文献   

Simulation of morphological development of soil cracks in Yuanmou Dry-hot Valley region,Southwest China   总被引：2，自引：0，他引：2  

Donghong Xiong  Dongchun Yan  Yi Long  Xiaoning Lu  Jianning Han  Xueqin Han  Liangtao Shi 《中国地理科学(英文版)》2010,20(2):112-122

Soil cracking is an important process influencing water and solutes transport in the Yuanmou Dry-hot Valley region of Southwest China. Studying the morphological development of soil cracks helps to further reveal the close relationship between the soil cracking process and water movement in such semi-arid regions. Here we report regular changes on surface morphology of soil cracks with decreasing water in four different soils (Typ-Ustic Ferrisols,Ver-Ustic Ferrisols,Tru-Ustic Vertisols and Typ-Ustic Vertiso...  相似文献   

广义线性高程拟合法在物探中的应用     

滕龙  朱红兵  高卫华 《火山地质与矿产》2010,(3):209-215

地球物理勘探工作需要三维坐标为其定位,尤其是重力勘探,对高程有较高的要求。作为一种先进的现代化测量技术,GPS能实时提供高精度的平面坐标,但因其使用W G S-84坐标系统,高程为大地高,没有实际的地球物理意义。地球物理勘探用的是正常高,故GPS测量的大地高无法直接使用。若联测高程,不仅增加工作难度,时间成本和经济成本也将大大增加。本文以长江中下游某些地区地球物理矿产勘查为例,介绍利用广义线性拟合法来获取高程。该模型不仅能对拟合结果进行评价,亦能评价模型参数的优劣。  相似文献   

Study on Potential Strong Earthquake Risks Around the Mabian Area,Southern Sichuan     

Yi Guixi  Wen Xueze  Zhang Zhiwei  Long Feng  Ruan Xiang  Du Fang 《中国地震研究》2010,24(4):478-490

Based on seismic data from the regional network for the last 34 years,we analyzed the present fault behavior of major fault zones around the Mabian area,southern Sichuan,and identified the risky fault-segments for potential strong and large earthquakes in the future.The method of analysis is a combination of spatial distribution of b-values with activity background of historical strong earthquakes and current seismicity.Our results mainly show:(1) The spatial distribution of b-values indicates significant heterogeneity in the studied area,which reflects the spatial difference of cumulative stress levels along various fault zones and segments.(2) Three anomalously low b-value areas with different dimensions were identified along the Mabian-Yanjin fault zone.These anomalies can be asperities under relatively high cumulated stress levels.Two asperities are located in the north of Mabian county,in Lidian town in western Muchuan county,and near Yanjin at the south end of the fault zone.These two areas represent potential large earthquake seismogenic sites around the Mabian area in the near future.Besides them,the third relatively smaller asperity is identified at southern Suijiang,as another potential strongearthquake source.(3) An asperity along the southwestern segment of the Longquanshan fault zone indicates the site of potential moderate-to-strong earthquakes.(4) The asperity along the segment between Huangmu town in Hanyuan county and Longchi town in Emeishan city on Jinkouhe-Meigu fault has potential for a moderate-strong earthquake.  相似文献   

体波谱振幅相关系数法在肥东地震序列震后判定中的应用   总被引：2，自引：1，他引：1  

刘泽民  刘东旺  夏仕安  徐鑫  龙爱军  缪鹏 《地震地磁观测与研究》2010,31(5):13-16

地震直达体波记录的观测谱包含震源、传播路径和台站信息,而发生在同一震源区的不同地震,如:序列地震,在同一地震台站的记录,受传播路径影响基本相同,地震台站的场地响应、仪器响应也完全相同。因此,序列地震体波观测零频谱的相关系数直接反映震源辐射图型因子的相似性,即震源机制解的相似性。将该方法用于2009年安徽肥东地震序列,与传统方法计算的震源机制解作比较,结果显示,谱振幅相关系数法能反映序列地震震源机制解的变化过程。  相似文献   

基于多源数据的活动断裂遥感图像处理技术   总被引：1，自引：0，他引：1  

窦爱霞  王晓青  王栋梁  丁香  王龙 《地震》2010,30(3):123-128

本文在综合分析活动断裂遥感影像特征的基础上, 主要研究了活动断裂与隐伏断裂调查中遥感图像处理。基于SAR影像、 ETM+影像、 SPOT-5影像及高精度DEM数据, 运用SAR图像与ETM+多光谱图像融合方法、 ETM+图像纹理特征和光谱特征组合增强方法等, 结合断裂周围高分辨率影像及其三维影像, 综合分析解译了济南市周边活动断裂, 为该地区地震地质调查和精确定位活动隐伏构造提供了依据。  相似文献   

卫星钟差实时估计的收敛分析     

李黎  朱建军  陈永奇  匡翠林  龙四春  李洪玉 《大地测量与地球动力学》2011,31(4):80-83

就测站数量、观测时间和测站分布对估计钟差的影响进行了研究,结果表明：增加测站数量和观测时间,均有利于提高卫星钟差的估计精度;但随着测站个数的增加,计算耗时会随之增加,从而影响钟差的实时使用,因此,从兼顾钟差的精度和实时应用两方面考虑,只有选择适当的测站分布和测站个数,才有利于钟差的实时估计和应用。PPP定位中,基于估计钟差的收敛时间比基于IGS最终钟差的收敛时间更长。  相似文献   

2014年震情述评     

龙海云  李纲  黎明晓  孟令媛 《中国地震》2015,31(1):168-175

<正>1全球地震活动概况据中国地震台网中心测定,2014年全球共发生7级以上地震13次(表1),其中包括1次8级以上地震,即2014年4月2日智利北部沿岸近海8.1级地震(图1)。2014年全球7级以上地震主要发生在环太平洋地震带,欧亚地震带活动较弱。与2013年相比,全球地震频次显著减少,能量释放略有降低。2014年全球7级以上地震活动有以下特点。  相似文献   

2008年攀枝花6.1级地震序列精定位     

傅莺  龙锋 《中国地震》2015,31(1):56-64

利用四川和云南区域数字地震台网震相到时资料,并结合Hypo2000+Hypo DD对2008年8月30日攀枝花MS6.1地震序列进行了定位。定位结果表明,地震序列的震中在空间上呈近SN向展布,余震密集区长度约为30km,主震震源深度约为14km。序列深度的分布范围主要为0~4、5~20km,而4~5km范围显示为明显的少震层。沿序列长轴的深度剖面显示,余震区中段存在1个不规则的少震的"空区",为1955年634级地震的破裂区,该地震发生在空区的南端。分析认为,2008年8月30日攀枝花MS6.1地震是因汶川8.0级地震后的应力调整造成未破裂的小凹凸体发生破裂所致。余震密集分布区沿垂直于破裂长轴的两个剖面则显示了在其北端地震震源分布更深,且断层面向NW倾斜,与已知的红格断裂的倾向一致。  相似文献