DEM resolution dependencies of terrain attributes across a landscape     

Y. Deng  J. P. Wilson  B. O. Bauer 《International journal of geographical information science》2013,27(2):187-213

This paper documents resolution dependencies in terrain analysis and describes how they vary across landform location. Six terrain attributes were evaluated as a function of DEM resolution—slope, plan curvature, profile curvature, north–south slope orientation, east–west slope orientation, and topographic wetness index. The research highlights the effect of varying spatial resolution through a spatial sampling/resampling scheme while maintaining sets of indexed sample points at various resolutions. Tested sample points therefore coincide exactly between two directly compared resolutions in terms of their location and elevation value. An unsupervised landform classification procedure based on statistical clustering algorithms was employed to define landform classes in a reproducible manner. Correlation and regression analyses identified sensitive and consistent responses for each attribute as resolution was changed, although the tested terrain attributes responded in characteristically different ways. These responses displayed distinguishable patterns among various landform classes, a conclusion that was further verified by a series of two‐sample, two‐tailed t‐tests.  相似文献   

A spatial cognition-based urban building clustering approach and its applications     

Zhang Liqiang  Deng Hao  Chen Dong  Wang Zhen 《International journal of geographical information science》2013,27(4):721-740

This article presents a spatial cognition analysis technique for automated urban building clustering based on urban morphology and Gestalt theory. The proximity graph is selected to present the urban mrphology. The proximity graph considers the local adjacency among buildings, providing a large degree of freedom in object displacement and aggregation. Then, three principles of Gestalt theories, proximity, similarity, and common directions, are considered to extract potential Gestalt building clusters. Next, the Gestalt features are further characterized with seven indicators, that is, area difference, height difference, similarity difference, orientation difference, linear arrangement difference, interval difference, and oblique degree of arrangement. A support vector machine (SVM)-based approach is employed to extract the Gestalt building clusters. This approach transforms the Gestalt cluster extraction into a supervised discrimination process. The method presents a generalized approach for clustering buildings of a given street block into groups, while maintaining the spatial pattern and adjacency of buildings during the displacement operation. In applications of urban building generalization and three-dimensional (3D) urban panoramic-like view, the method presented in this article adequately preserves the spatial patterns, distributions, and arrangements of urban buildings. Moreover, the final 3D panoramic-like views ensure the accurate appearance of important features and landscapes.  相似文献   

The morphological characteristics of glacial deposits during the Last Glaciation, taking the Parlung Zangbo River Basin as an example   总被引：1，自引：0，他引：1  

RenRong Chen  ShangZhe Zhou  YingBin Deng 《寒旱区科学》2013,5(6):0698-0708

Moraine morphology is a valuable indicator of climate change. The glacial deposits of ten valleys were selected in the Parlung Zangbo River Basin, southeastern Tibetan Plateau, to study the glacial characteristics of the Last Glaciation and the climate change processes as revealed by these moraines. Investigation revealed that a huge moraine ridge was formed by ancient glacier in the Marine Isotope Stage 2 （MIS2）, and this main moraine ridge indicates the longest sustained and stable climate. There are at least two smaller moraine ridges that are external extensions of or located at the bottom of the main moraine ridge, indicating that the climate of the glacial stage before MIS2 was severer but the duration was relatively shorter. This distribution may reflect the climate of MIS4 or MIS3b. The glacial valleys show multi-channel, small-scale moraine ridges between the contemporary glacial tongue and the main moraine ridge. Some of these multi-channel mo- raine ridges might be recessional moraine, indicating the significant glacial advance during the Younger Dryas or the Heinrich event. The moraine ridges of the Neoglaciation and the Little Ice Age are near the ends of the contemporary glaciers. Using high-precision system dating, we can fairly well reconstruct the pattern of climate change by studying the shape, extent, and scale characteristics of glacial deposits in southeastern Tibet. This is valuable research to understand the relationship between regional and global climate change.  相似文献   

轮古西奥陶系潜山洞穴型岩溶储层发育特征与充填规律   总被引：2，自引：0，他引：2  

李世银  罗春树  邓兴梁  李保华  常少英  王轩  裴广平 《海相油气地质》2012,(2):70-74

洞穴型岩溶储层是塔里木盆地轮古油田缝洞型碳酸盐岩油藏的主要储集空间类型,多数高效井均钻遇大型洞穴型岩溶储层。依据轮古西奥陶系潜山大量单井资料分析,洞穴型岩溶储层可分为充填洞穴、半充填洞穴和未充填洞穴三种类型。结合古地貌精细刻画与岩溶垂向分带成果,认为古地貌位置由岩溶台地向岩溶缓坡和岩溶盆地逐渐降低,而洞穴发育和充填程度在逐渐增高。未充填与半充填洞穴主要发育在岩溶台地和岩溶缓坡的溶峰边坡、溶丘边坡及沟槽谷洼地边坡等地貌单元。表层岩溶带、径流溶蚀带洞穴型岩溶储层发育频率最高,其次为垂直渗滤带和潜流溶蚀带。未充填与半充填洞穴型岩溶储层主要发育在表层岩溶带。  相似文献   

Relations between density of earthquake-damaged trace and environmental factors in seismic intensity: a case study in Wenchuan County, China     

Hui Yu  Wei Deng  Yong Luo 《Environmental Earth Sciences》2012,67(6):1631-1637

Many studies have been designed to assess seismic hazard and to improve post-earthquake damage evaluation models. Compared with previous studies, the research attempted to solve the problems of the effectiveness differences of seismic intensity on density of Earthquake-damaged trace (D _e) and established the appropriate models for D _e in different scale of seismic intensity. D _e as a relative value reduced the influence of area on earthquake-damaged trace. The research will provide the necessary scientific support to fast post-earthquake damage assessment and modeling. By utilizing GIS, RS and field investigation data, the spatial distribution characteristic of earthquake-damaged traces was analyzed. Effective factors including seismic intensity, distance to rivers and slope were identified through PCA. Specifically, seismic intensity was identified as the key factor. The inherent relations between D _e and seismic intensity, D _e and distance to rivers in seismic intensity, and D _e and slope in seismic intensity were modeled by regression analysis. The results demonstrated that both earthquake energy and D _e have attenuation characteristics. There is a significant positive correlation between D _e and seismic intensity (the pearson correlation is 0.917). That is, the higher the seismic intensity, the greater the D _e was. The erosion of river leads to steep slope, which is in favor of the formation of mountain hazards. D _e showed the decreasing tendency with the increasing distance to river. With the increase of slope, the D _e gradually became stronger. For distance to river, the largest changing rate of D _e appeared on seismic intensity XI, but for slope, the largest changing rate of D _e appeared on seismic intensity X.  相似文献   

Some Fundamental Issues and Verification of 3DEC in Modeling Wave Propagation in Jointed Rock Masses     

X. F. Deng  J. B. Zhu  S. G. Chen  J. Zhao 《Rock Mechanics and Rock Engineering》2012,45(5):943-951

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Late cretaceous tectonic change of the eastern margin of the Tibetan Plateau — results from multisystem thermochronology   总被引：2，自引：0，他引：2  

Bin Deng  Shugen Liu  Zhiwu Li  Junxing Cao  Wei Sun 《Journal of the Geological Society of India》2012,80(2):241-254

Partially due to lack of structural and sedimentary records to constrain the Jurassic-to-Cretaceous evolution, there was a missing process here in the eastern margin of Tibetan Plateau as it changed from the Paleo-Tethyan to Neo-Tethyan regime. Based on the analysis of 125 thermochronology ages (U/Pb, ⁴⁰Ar/³⁹A, ⁸⁷Rb/⁸⁶Sr, FT, U-Th/He) of igneous rocks from the eastern margin of Tibet, we propose a multisystem thermochronology approach to restore the cooling and emplacement of granites and decipher the missing process. Our integrated study suggests that a key Late Cretaceous (about 100Ma) tectonic change from the Paleo-Tethyan to Neo-Tethyan regime took place there. In the Late Triassic period, the initial emplacement of granite in the Songpan-Ganzi Fold Belt (SGFB) was characterized by a decrease in emplacement age and depth from west to east, and from north to south. Subsequently, all were followed by a very long period of slow cooling, which was followed by a rapid emplacement of about 100Ma. The intensive granite emplacement took place all over except northeastern SGFB, with a decrease in emplacement depth from west to east, which was linked with the far-field effect of Lhasa-Qiangtang collision. After this episode, the cooling history of granite in SGFB had a rapid emplacement on the subsurface under the control of the Neo-Tethyan regime. This process has control of the post Late Cretaceous regional magmatic activity and tectonics, as well as the sedimentary response in Sichuan and Xichang basin.  相似文献   

南方红土的磁性矿物组成及其区域性差异     

刘彩彩  邓成龙 《第四纪研究》2012,32(4)

位于我国热带、亚热带地区的南方红土是我国分布最广的第四纪土状沉积,其经历了较强的化学风化作用,具有典型的磁性矿物组成.磁性矿物是沉积物的重要组成成分.磁性矿物的种类、粒度和含量等信息可以反映沉积物形成时的温度、降水等气候条件.因此,了解红土沉积物磁性矿物组成对于研究南方红土区的环境演化具有重要意义.本文综合分析了安徽室城、浙江长兴、江西九江及广西百色4个剖面不同层位红±样品的x-T曲线、三轴等温剩磁热退磁曲线等岩石磁学结果,发现南方红土的磁性矿物组成主要为磁铁矿、磁赤铁矿、赤铁矿及针铁矿,这些磁性矿物的相对含量不仅具有地带性差异,而且在不同风化阶段也存在差异.其中百色剖面顶部棕色土中磁赤铁矿含量相对其他剖面较高,与百色地区现今较强的风化作用相符.同一剖面内网纹红土中赤铁矿的含量较高,磁赤铁矿的含量相对较低,指示网纹化时期较强的成土作用引起磁赤铁矿向赤铁矿的转化.此外,岩石磁学结果显示百色剖面网纹红土及均质红土中含有一种特殊性质的磁性矿物,即粒度较细、解阻温度较低的成土成因赤铁矿,该矿物为后期强烈风化作用的产物.该次生矿物携带了较强的化学剩磁,引起了百色剖面初始碎屑剩磁的重磁化.该研究表明磁性矿物组成的差异还可以用来解释南方红土剩磁记录的多样性.  相似文献   

深部过程中地幔流体现实微观踪迹的实验证据     

刘显凡  赵甫峰  李春晖  楚亚婷  邓碧平  宋祥峰  张民 《地球科学进展》2012,27(10):1161-1166

伴随深部地质过程的地幔流体作用是引发地壳中成矿作用的重要物质源和动力源。由于地幔流体的超深源性及由此决定其性质和演化的复杂性,使人们很难具体捕捉其实际存在,或者多数情况下很难准确界定。通过岩相学、岩石化学、电子探针和扫描电镜及能谱分析的综合研究发现,地幔流体活动的现实微观踪迹和存在方式可以表现为富铁熔浆包体和富铁微晶玻璃,二者在透射偏光显微镜下无光性,呈黑色不透明状;反射偏光显微镜下不反光,但在电子显微镜下呈显微晶质结构,显示微晶金属和非金属矿物之间呈熔离交生,超微晶矿物组成以硅酸盐和石英为主,尤其是经过成分配比换算,得到碳硅石,含铬自然铁、钛铁矿、磷灰石和含钛镜铁矿等地幔标型矿物,反映了地幔流体的熔浆性质。捕捉和揭示深部地质过程中地幔流体作用的现实微观踪迹,对于深入分析和认识地壳地质作用的机制和成矿效应具有重要理论和现实意义。  相似文献   

基于自动气象站业务软件的外挂软件开发     

邓红  张戈 《内蒙古气象》2013,(1):39-40

《地面气象测报业务系统软件》(2004)开发至2012年已经修改多次并不断地完善,但编报过程中各个要素之间的相关检查的辅助提示功能不够完善,目前也没有相应的足够完善的外挂提示软件的推广应用,导致一些最基础的要素之间的检查都需要人工判断,如果不细心很容易导致错误。针对这个情况,下面将介绍能够检查编报过程中各个要素的外挂软件的开发过程(OSSMO V3.019)。  相似文献