共查询到20条相似文献，搜索用时 62 毫秒
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边坡稳定性类比评价的定量实现 总被引：9，自引：1，他引：8
岩土边坡是一个受多因素影响、随时空变异的动态系统 ,它具有数据有限、不确定和没有原型等特点 ,因此 ,已有成功经验知识的运用在边坡稳定性评价中具有重要的意义。本文基于类比推理和灰色系统理论 ,提出了一种定量开发利用经验知识的新方法 ,并将其成功地应用于边坡稳定性分析和评价。结果表明 ,在运用经验知识方面 ,该法与目前广泛使用的神经网络方法有异曲同工之妙。此外 ,本文所提出的方法还具有简单、方便和实用等许多优点。 相似文献
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基于蚁群聚类算法的岩石边坡稳定性分析 总被引：2，自引：0，他引：2
由于岩石边坡影响因素众多且关系复杂,不能用简单的方法进行分析和判断。在工程类比的基础上,一般采用聚类的方法。但由于边坡工程问题环境的复杂性,岩石边坡稳定分析的聚类问题是一个复杂的模糊、随机优化问题,采用传统方法难免带来很多局限性。为了更好地解决这类问题,首次把蚁群聚类算法这种新近提出的仿生聚类算法引入岩石边坡工程领域,以解决其稳定分析问题,提出一种分析岩石边坡稳定问题的新方法。该方法在分析岩石边坡工程实例资料的基础上,采用蚁群聚类算法,以工程类比的思想判断岩石边坡的稳定状态。工程应用证明,该算法可以自动把岩石边坡分成几种类似的状态,判断准确率较高、计算速度较快,是一种比较实用的岩石边坡稳定分析方法,值得在岩石边坡分析领域推广应用。 相似文献
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突变级数法在边坡稳定综合评判中的应用 总被引：11，自引：1，他引：10
边坡的稳定性受地质、工程等众多因素影响,且其变形破坏机理复杂,危害巨大,因而边坡稳定问题分析研究一直是理论和实践研究的热点。引入突变理论对边坡的稳定性问题进行研究,利用突变数学和模糊数学结合引出的突变级数法,提出边坡稳定性评判指标--突变级数, 从而建立了新的稳定性评判模型。基于突变级数法的边坡稳定性评判法,综合考虑了边坡各种要素对其稳定性的不同影响程度,真实地描绘了边坡系统的稳定状态。实例分析结果表明,该方法评判结果准确,精度较高,具有良好的实际应用价值。 相似文献
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由于岩土工程的复杂性及其数据的不确定性、不完备性,需要发展经验评价边坡稳定性的体系,以适应中国山区交通工程建设的需要。基于Bieniawski的RMR体系、Barton的Q体系、Romana的SMR体系和Palmström的RMi体系发展出来一种边坡稳定性评分体系。新体系建立了新的不连续面状态描述和评分标准;考虑了天然降水的影响;对应控制性不连续面,考虑了其不连续面状态,并给出了评分方法。通过实例展示了新体系的易用性和一定的客观性。 相似文献
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岩坡系统分析与可靠性评价 总被引：14，自引：0，他引：14
优势面分析原理是边坡工程地质问题的一种新的研究观点和模式。它认为岩坡稳定性以及破坏模式、边界条件受优势面的控制，将边坡隐定性评价问题转化为边坡优势面的寻找与优势分离体的确定。在边坡稳定性的定量评价和预测中运用了系统工程原理和可靠性分析的研究模式和方法，使确定性模型和非确定性模型达到了有机的结合，本文给出了三峡工程、马鞍山露采场等工程边坡研究成果的实例。 相似文献
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基于灰色关联分析和案例推理的边坡稳定性评价方法 总被引：6，自引：0，他引：6
采用基于案例推理的方法 (CBR)来评价边坡稳定性 ,并利用灰色关联理论 ,提出基于灰色关联分析的案例检索方法 ,应用于边坡工程实例 ,效果良好 ,且将实例应用结果与同等条件下欧式距离的检索结果比较 ,说明此方法合理有效、具有明显的优越性 相似文献
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基于案例的边坡治理方案选择决策支持系统研究 总被引：1，自引：0，他引：1
边坡治理是边坡工程研究的核心问题,其治理方案的选择直接关系到边坡治理的成功与否。边坡的治理需要很丰富的经验和知识,但知识的获取一直是边坡治理决策的瓶颈问题。长期以来,边坡治理工程实践已积累了大量的工程案例,这些案例中蕴涵了大量的经验和知识,急需挖掘与开发,并应用于边坡治理决策中,进而指导边坡治理工程实践。为此,针对边坡治理决策中的边坡治理方案选择问题,提出了一种基于案例的边坡治理方案选择系统,用以对边坡治理方案选择提供有效的决策支持。该研究具有较好的工程应用价值。 相似文献
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Emily Keeble David I. Whiteside Michael J. Benton 《Proceedings of the Geologists' Association. Geologists' Association》2018,129(2):99-119
Pant-y-ffynnon Quarry in South Wales yielded a rich cache of fossils in the early 1950s, including articulated specimens of new species (the small sauropodomorph dinosaur Pantydraco caducus and the crocodylomorph Terrestrisuchus gracilis), but no substantial study of the wider fauna of the Pant-y-ffynnon fissure systems has been published. Here, our overview of existing specimens, a few described but mostly undescribed, as well as freshly processed material, provides a comprehensive picture of the Pant-y-ffynnon palaeo-island of the Late Triassic. This was an island with a relatively impoverished fauna dominated by small clevosaurs (rhynchocephalians), including a new species, Clevosaurus cambrica, described here from a partially articulated specimen and isolated bones. The new species has a dental morphology that is intermediate between the Late Triassic Clevosaurus hudsoni, from Cromhall Quarry to the east, and the younger C. convallis from Pant Quarry to the west, suggesting adaptive radiation of clevosaurs in the palaeo-archipelago. The larger reptiles on the palaeo-island do not exceed 1.5?m in length, including a small carnivorous crocodylomorph, Terrestrisuchus, and a possible example of insular dwarfism in the basal dinosaur Pantydraco. 相似文献
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Gilles Serge Odin 《Comptes Rendus Geoscience》2002,334(6):409-414
Lithostratigraphy, physicochemical stratigraphy, biostratigraphy, and geochronology of the 77–70 Ma old series bracketing the Campanian–Maastrichtian boundary have been investigated by 70 experts. For the first time, direct relationships between macro- and microfossils have been established, as well as direct and indirect relationships between chemo-physical and biostratigraphical tools. A combination of criteria for selecting the boundary level, duration estimates, uncertainties on durations and on the location of biohorizons have been considered; new chronostratigraphic units are proposed. The geological site at Tercis is accepted by the Commission on Stratigraphy as the international reference for the stratigraphy of the studied interval. To cite this article: G.S. Odin, C. R. Geoscience 334 (2002) 409–414. 相似文献
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The effect of water on accessory phase solubility in subaluminous and peralkaline granitic melts 总被引：4，自引：0，他引：4
The solubilities of columbite, tantalite, wolframite, rutile, zircon and hafnon were determined as a function of the water contents in peralkaline and subaluminous granite melts. All experiments were conducted at 1035 °C and 2 kbar and the water contents of the melts ranged from nominally dry to approximately 6 wt.% H2O. Accessory phase solubilities are not affected by the water content of the peralkaline melt. By contrast, solubilities are affected by the water content of the subaluminous melt, where the solubilities of all the accessory phases examined increase with the water content of the melt, up to 2 wt.% H2O. At higher water contents, solubilities are nearly constant. It can be concluded that water is not an important control of accessory phase solubility, although the water content will affect diffusivities of components in the melt, thus whether or not accessory phases will be present as restite material. The solubility behaviour in the subaluminous and peralkaline melts supports previous spectroscopic studies, which have observed differences in the coordination of high field strength elements in dry vs. wet subaluminous granitic glasses, but not for peralkaline granitic glasses. Lastly, the fact that wolframite solubility increases with increasing water content in the subaluminous melt suggests that tungsten dissolved as a hexavalent species. 相似文献
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Muriel Rocher Stéphane Baize Stéphane Jaillet Edward Marc Cushing Yannick Lozac&#x;h Francis Lemeille 《Comptes Rendus Geoscience》2003,335(8):701-708
Calcite samples were extracted both from the rock matrix and the superficial coating of a karstified fault plane of an underground quarry, located in the eastern border of the Paris basin. The karstification is dated as Quaternary. Analysis of mechanical calcite twinning reveals that only the calcite matrix has also undergone a compression trending WNW that can be attributed to the Mio-Pliocene alpine collision. Both coating and matrix have undergone a strike-slip regime with σ1 roughly trending north–south, that could correspond to the regional present-day state of stress, a strike-slip compression rather trending NNW, modified by local phenomena. To cite this article: M. Rocher et al., C. R. Geoscience 335 (2003). 相似文献
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正20141756 Chen Ruige(Mathematical College,China University of Geosciences,Beijing100083,China);Zhou Xun Numerical Simulation of Groundwater Level Fluctuation in a Coastal Confined Aquifer with Sloping Initial Groundwater Level Induced by the Tide(Geological Bulletin of China,ISSN1671-2552,CN11-4648/P,32(7),2013,p.1099-1104,6 illus.,16 refs.) Key words:confined water,groundwater level 相似文献
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正20141408 Cai Jia(Institute of Geology,Chinese Academy of Geological Sciences,Beijing100037,China);Liu Fulai Petrogenesis and Metamorphic P-T Conditions of Garnet-Spinel-Biotitebearing Paragneiss in Danangou Area,Daqingshan-Wulashan Metamorphic Complex Belt(Acta Petrologica Sinica,ISSN1000-0569,CN11-1922/P,29(7), 相似文献
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正20142386An Guoying(China Aero Geophysical Survey and Remote Sensing Center for Land and Resources,Beijing 100083,China)Application of Satellite Remote Sensing in Regional Hydrogeological Investigation:Taking Cenozoic Strata in Wenquan Sheet(1∶250 000)of Karakoram Range as an Example(Geosci- 相似文献
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正20141016An Chengbang(Key Laboratory of Western China’s Environmental Systems,Ministry of Education,Lanzhou University,Lanzhou 730000,China);Zhao Yongtao Lake Records during the Last Glacial Maximum from Xinjiang,NW China and Their Climatic Impli- 相似文献
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正20141538 Cao Qing(School of Earth Sciences and Engineering,Xi’an Petroleum University,Xi’an 710065,China);Zhao Jingzhou Characteristics and Significance of Fluid Inclusions from Majiagou Formation,Yichuan Huangling Area,Ordos Basin(Advances in Earth Science,ISSN1001-8166,CN62-1091/P,28(7),2013,p.819-828,7 illus.,3 tables,43 refs.) 相似文献