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采石场开采量计算,由于传统测量方法存在获取数据量少、精度低、复杂地形获取数据困难等问题,利用激光点云数据计算采石场开采量具有重要的研究意义。选择李庄采石场作为研究对象,利用徕卡C10获取点云数据,运用Cyclone软件对点云数据进行预处理,Geomagic软件对预处理数据进行精简。采用Cyclone,HD-3LS-SCENE,CASS软件对开采量分别进行计算,详细对比分析计算结果。研究结果表明:三种软件可满足工程需要。Cyclone软件计算精度最高,CASS软件操作快捷方便。根据软件多种性能指标的对比研究,确定采石场开采量行之有效的计算方法。 相似文献
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采石业对国民经济起到积极作用的同时,给生态、环境和人居安全带来了隐患。目前,石矿区生态修复成为重要的生态文明建设问题。解决该问题的前提是识别采石场且确定石矿区边界。高分遥感对地观测和深度学习技术为高精度识别采石场并确定矿区边界提供了有效的途径。本文基于残差网络,设计了注意力金字塔结构和细节增强模块,以少量参数和极低计算复杂度为代价,从无人机高分遥感图像中有效识别石矿区。试验采用福建省南安市高分遥感图像和人工实地考察获取的石矿区边界真值作为数据源,构建用于卷积神经网络训练的数据集,并对算法精度进行验证。试验结果表明,本文方法速度快、精度高,可为石矿区生态修复提供可靠的支撑材料。 相似文献
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In Carrara marble basins, the long and intensive quarrying activities (which began in the first century BC ) have produced extensive dump deposits, locally known as ravaneti. Ravaneti are of such large dimensions and diffusion as to make them a widespread landform of the Apuane Alps (Tuscany). In recent years these quarry dump deposits have been affected by frequent debris flows, more than 50 in 1996/97. This phenomenon is the most significant currently active geomorphological process in this landscape. The evolution of quarrying techniques produced a variety of sedimentological compositions of ravaneti. The debris flows analysed involve only the surface layers where debris is mixed with fine material with a lower permeability (active ravaneti) than the coarser underlying debris (older ravaneti). The presence of different permeability layers causes a wetting front to move downwards. Source area observations indicate a soil slip movement in the initial phases of the failure. The transformation of landslides into debris flow occurs by means of both soil contractive failure and an increase of granular temperature. The morphological and sedimentological analyses of depositional lobes resulted in a classification of three types of lobe, based on fabric–morphometry relationships allowing the identification of different flow dynamics: (1) type A lobe (platy form), matrix‐supported and well developed fabric with general tendency of ab clast plane strikes to lie generally parallel to flow direction as a consequence of laminar flow; (2) type B lobe (elongated form), clast‐supported and random fabric as a consequence of both turbulent flow and coarser composition of starting material; (3) type C lobe, intermediate type A–B morphometry, tendency for ab clast plane to lie in a semi‐circle around the main flow direction determined by the presence of secondary flow lines divergent from it in the stopping phase. In Carrara marble basins, the anomalous frequency with which debris flows tend to be triggered by medium‐intensity rainstorms (about 30 mm h−1 rainfall) is due to the recent increases in silt dump produced by modern quarrying techniques. This represents a significant example of debris flows as an environmental problem in major anthromorphized landscapes. Copyright © 2000 John Wiley & Sons, Ltd. 相似文献
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以松辽盆地南部团山子采石场辉绿岩侵入露头为例,采用连续密集取样、常规分析和碳氧稳定同位素测试等方法,对围岩储层的成岩及其变质特征进行分析,进而探讨岩浆侵入对围岩的影响及其储层意义。岩浆侵入对角岩围岩的影响包括:1)自生绢云母距离侵入体越远,其含量越少;2)粘土矿物主要为成岩晚期的伊利石和绿泥石;3)角岩中发育特殊“气孔-杏仁”构造。岩浆侵入对上覆砂岩的影响表现为:1)造成自生石英的特征分布;2)造成粘土矿物的不均匀分布;3)形成反映应力挤压特征的颗粒结构。角岩中浊沸石发育和高岭石不发育对应碱性环境,不利于热液微裂缝中碳酸盐矿物的溶蚀。因此,尽管角岩发育微孔、微缝等少量储集空间(平均孔隙度为1.70%),但其渗透能力很低(平均渗透率小于0.1 mD)。侵入活动对研究露头砂岩储层物性造成的不利影响,主要是由于挤压作用和热液流动作用使自生矿物不均匀分布,从而导致或加剧了砂岩储层的非均质性。 相似文献
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观夕硐是古人地下采石活动形成的洞室群。其历史可追溯到1500年前,属于大型地下工程。为解答观夕硐长期稳定,千年不倒的原因,研究洞区的工程地质条件。此研究既为长屿洞天地质公园大型地下古采石场遗址的保护和旅游安全积累地质资料,也可为现代大型地下工程的选址和建设提供工程类比资料。 相似文献
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