东营市城区第四纪松散堆积物工程建筑适宜性评价     

张金兰 《山东国土资源》2010,26(7):17-20

从工程地质角度,以东营城区0～50m的土体为研究对象,分析了土体的工程地质特征,采用专家类聚法,对一般工业民用建筑和高层重型建筑物场地的工程建筑适宜性做出了评价并进行了区域划分,对东营城区将来的工程建设规划具有重要的指导意义。  相似文献   

边坡稳定性的聚类未确知综合识别方法及应用   总被引：1，自引：0，他引：1  

薛锦春  李夕兵  董陇军 《岩土力学》2010,31(Z1):293-297

影响岩石边坡稳定性的因素众多且关系复杂,且存在大量未确知信息,很难用简单的方法进行分析判断,借鉴工程类比的思想,采用聚类与未确知测度相结合的方法进行研究。针对边坡工程问题环境的复杂性,以大量的历史数据为训练样本,通过动态聚类分析,求得其分类中心。针对大量的未确知信息,利用未确知测度方法对其进行评价,提出一种分析边坡稳定问题的新方法。研究表明,该算法可以对边坡的稳定状态进行预测,正确率在90%以上,为比较合理快速地分析边坡稳定分析方法提供了一条新的途径。  相似文献   

Boulder height – exposure age relationships from a global glacial 10Be compilation     

《Quaternary Geochronology》2016

  相似文献   

基于自适应区间二型模糊聚类的遥感土地覆盖自动分类   总被引：2，自引：0，他引：2       下载免费PDF全文

贺辉  胡丹  余先川 《地球物理学报》2016,59(6):1983-1993

遥感影像土地覆盖分类面临"类别密度差异显著"、"同谱异物"和"同物异谱"等不确定性问题,传统的分类方法(如FCM)因不能描述高阶模糊不确定性,无法完成准确建模,使分类误差较大,而二型模糊集恰是处理此类不确定性的有效工具.在引入二型模糊集新概念和自适应降型新方法的基础上,提出一种自适应二型模糊分类方法(A-IT2FCM):(1)基于样本集模糊距离度量构建面向分类的区间二型模糊集,以尽可能降低对先验知识和预设参数的依赖,从而满足自动分类的要求;(2)给出一种自适应探求等价一型代表(模糊)集合的高效降型方法,在此基础上进行自适应区间二型模糊聚类.实验数据为珠海横琴和北京颐和园的SPOT5影像数据,对比方法有AIT2FCM、基于Karnik-Mendel算法降型和基于Tizhoosh提出的简易降型方法的区间二型模糊C均值聚类以及作者前期研究提出的区间值模糊C-均值算法(IV-FCM).实验结果表明,A-IT2FCM方法分类效果佳,在类别具有较大密度差异和多重模糊性时能得到比FCM及IV-FCM更精确的边界和更连贯的类别,适于处理遥感影像土地覆盖类别的深层不确定性;同时在"光谱混叠"现象严重时,可以获得比对比方法更稳健、精度更高的影像自动分类结果,且时间复杂度明显低于基于Karnik-Mendel方法.  相似文献   

基于时间序列聚类方法分析北京出租车出行量的时空特征   总被引：1，自引：0，他引：1  

程静  刘家骏  高勇 《地球信息科学学报》2016,18(9):1227-1239

受城市资源配置、区域功能分化的影响,城市中居民的出行往往呈现出特定的模式和规律,而这种出行模式的背后反映出城市的功能结构。城市车辆GPS导航的广泛使用,以及车辆轨迹数据的大量获取,为分析城市居民出行模式及理解城市功能结构提供了数据支撑。本文以道路分割城市得到的地块为研究单元,利用北京市一个月的出租车轨迹数据,对北京居民的出行模式及城市功能格局进行分析。在轨迹数据分析中,本文从轨迹数据中提取每个地块的出行量时间序列信息,然后采用结合时间序列距离度量和时间序列自身相关性的聚类方法,对出行量时间序列数据进行聚类分析,从而研究乘客出行的时空分布特征,最后结合北京市POI数据,探讨了不同区域乘客出行规律和区域功能类型的相互关系。结果表明,出租车出行量时间序列模式在工作日和周末间存在明显差异。此外,工作日的2个出行高峰与通常的通勤早晚高峰不同。由出行量所得的区域聚类结构,除具有重要交通枢纽功能的地块外,总体上以市中心为圆心大致呈同心圆分布,且距离市中心越远出行量越小。研究结果对于分析北京市居民出行行为、辅助城市交通规划具有一定的意义。  相似文献   

General multidimensional cloud model and its application on spatial clustering in Zhanjiang, Guangdong     

DENG Yu  LIU Shenghe  ZHANG Wenting  WANG Li  WANG Jianghao 《地理学报》2010,20(5):787-798

Traditional spatial clustering methods have the disadvantage of “hardware division”, and can not describe the physical characteristics of spatial entity effectively. In view of the above, this paper sets forth a general multi-dimensional cloud model, which describes the characteristics of spatial objects more reasonably according to the idea of non-homogeneous and non-symmetry. Based on infrastructures’ classification and demarcation in Zhanjiang, a detailed interpretation of clustering results is made from the spatial distribution of membership degree of clustering, the comparative study of Fuzzy C-means and a coupled analysis of residential land prices. General multi-dimensional cloud model reflects the integrated characteristics of spatial objects better, reveals the spatial distribution of potential information, and realizes spatial division more accurately in complex circumstances. However, due to the complexity of spatial interactions between geographical entities, the generation of cloud model is a specific and challenging task.  相似文献   

模糊聚类在不良地质洞段红外探水中的应用     

张雪峰  叶祖圣 《地震学刊》2010,(6):698-701

在玉昆铁路柿花树隧道不良地质发育的洞段进行红外探水工作期间,常用的分析方法有时无法预判掌子面前方是否存在隐伏水体或含水构造。为了提高红外探水短距离预报的准确率,用模糊聚类法将掌子面测点场强的数据分类,根据开挖传递的地质信息,研究模糊聚类结果的变化规律、突水风险与岩体破碎程度之间的关系。实践证明,模糊聚类法和常用分析方法的结合,使红外探水取得了较好的预判效果。  相似文献   

Evidence for evolution in the clustering of quasars     

Zhu Xing-fen  Chu Yao-quan 《Chinese Astronomy and Astrophysics》1990,14(4):371-380

We discuss the changes in the amplitude of the correlation function of quasar clustering with the redshift. Using the new Hewitt-Burbidge QSO catalogue, we find from a statistical analysis of the quasar pairs that the positive results of quasar clustering are mainly contributed by low-redshift quasars. There is an obvious change in the quasar distribution at z = 2. There is no clustering for z > 2. The difference in clustering is not due to any selection effect on the brightness. The evidence is that quasar clustering evolved with cosmological time.  相似文献   

Self-organized Fractal Seismicity and b Value of Aftershocks of the 2001 Bhuj Earthquake in Kutch (India)   总被引：1，自引：0，他引：1  

Prantik?MandalEmail author  B.K.?Rastogi 《Pure and Applied Geophysics》2005,162(1):53-72

— The devastating intraplate earthquake of M_w 7.7 of 26 January, 2001 took place along the south-dipping reverse fault in the lower crust ( 23 km) of Kutch, Gujarat, India, obliterating some 14,000 people. The aftershock activity has ensued for three years. We analyzed 997 aftershocks of M 3.0 to study the b value and fractal correlation dimensions in time and space. The b value is found to be 0.8 ± 0.03 from the Gutenberg-Richter relation and 0.76 ± 0.02 from the maximum-likelihood, suggesting a typical value for the intraplate region. The spatial correlation is 1.71 ± 0.02, indicating that events are approaching a two-dimensional region. Further, the temporal correlation dimension is estimated to be 0.78 ± 0.02, confirming the structure is mono-fractal in time domain. The depth section of b value shows a peak at 15–35 km depth range coinciding with the maximum occurrence of aftershocks ( 47%), which is inferred as a fluid-filled highly fractured rock matrix with fractures of high density. It will be important to note that tomographic results also suggest a low Vp, low Vs and a large Poissons ratio for the same depth range, further confirming this inference. Additionally, we have studied the variation of D₂^s and b value with time. During the first two months of aftershock activity the results show a marked negative correlation between spatial correlation dimension D₂ (large) and b value (low), indicating the predominance of large events associated with weak clustering. The negative correlation means the stress release along faults of a larger surface area. After two months the fractal dimension (D₂^s) and b value suggests a positive correlation implying more numerous smaller shocks with stress release along faults of a smaller surface area. This would indicate a reduced probability of large magnitude earthquakes due to fragmentation of the fault zone.Acknowledgement. The authors thank Dr. V.P. Dimri, Director, NGRI for his encouragement and kind permission to publish this work. The Department of Science and Technology, New Delhi supported this study.  相似文献   

Paleoearthquake rupture behavior and recurrence of great earthquakes along the Haiyuan fault,northwestern China   总被引：16，自引：0，他引：16  

ZHANG Peizhen  MIN Wei  DENG Qidong & MAO Fengying State Key Laboratory of Earthquake Dynamics  Institute of Geology  China Seismological Bureau  Beijing  China 《中国科学D辑(英文版)》2005,48(3):364-375

Paleoseismological studies have shown that indi-vidual past large-magnitude earthquakes can be recog-nized in the geological record and the timing betweenevents can be measured through Quaternary datingtechniques[1—6]. Thus, through paleoseismological st-udies, it is possible to determine age of each prehis-toric event so that recurrence intervals of large earth-quakes may be evaluated which provides a means toexpand the limited view of earthquakes offered by thehistorical and instrumental re…  相似文献