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针对抽出-处理技术修复污染地下水过程中抽水井抽出效率随时间逐渐降低、抽出-处理技术运行终点（以下简称"抽出终点"）难以确定的问题,提出通过评估抽水井抽出效率,以分段、多次优化抽水方案提高抽出效率、降低修复成本、减少修复时间为工作思路,利用层次分析法和专家打分法实现方案优化时间节点选择。以青海某铬盐厂为例,通过建立抽水方案优化时间节点评价指标体系,可定量分析方案优化时间节点,合理确定抽出终点。结果显示：第1次优化结果为抽水井抽出效率在20%~40%时应重新布设抽水方案（P3）,即采用原抽水方案抽水100 d后需重新布设抽水井;第2次优化结果为抽水井抽出效率在20%~40%时应与其他修复技术联用（P7）,即采用一次优化后抽水方案继续抽水300 d后需联合其他修复技术开展治理。经评估,2次优化可有效提高抽水井抽出效率,使修复时间缩短600 d,相同时间内含水层中六价铬去除率增加8.31%。 相似文献
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甲魁煤田地质构造复杂,岩层破碎胶结松散,换层频繁,断层破碎带多。在钻探施工中导致孔内事故多、岩（矿）心采取率低、钻进效率低等问题。通过使用绳索取心液动锤钻进技术,解决了在该矿田钻探施工中遇到的技术难题,减少了辅助时间,提高了钻进效率和岩（矿）心采取率,保证了钻孔质量。 相似文献
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本文根据褶皱的白相似性特征,引用分形概念,分析褶皱的分形分布特性,并利用MichaelBamsley（1986）的分形插值理论首次模拟褶皱的复杂形态,主要利用插值点（x、y）和褶皱扰动系数d模拟各种褶皱,在此基础上,提出褶皱复杂程度的分形分类方案。这种新的分类方案即褶皱形态的传统分类名称附缀分形分类名称,解决了传统分类方法不能区分褶皱复杂性的难题。这种方法使褶皱的形态分析达到较精确的定量描述和分类,分形分类方法是对褶雏形态分类的一个补充。 相似文献
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煤层低压、易塌、易漏造成煤层段井眼不规则,扩径严重,使注水泥过程顶替效率降低,影响水泥浆的封固效果。运用CFD数值模拟方法,结合鹤岗煤层气井测井数据,模拟了煤层段不同扩径长度、扩径率、井斜角、套管居中度、水泥浆流变参数及顶替流态下的体积顶替效率及截面顶替效率值;分析了各因素对顶替效率的影响规律。结果表明,扩径段长度增加,顶替效率提高;扩径率、井斜角及偏心度增加,顶替效率降低;宾汉流体及幂率流体均存在顶替效率最高的流变参数值,顶替流态建议采用塞流顶替。研究成果为煤层气井安全优质固井提供了技术指导。 相似文献
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围岩类别超前分类是隧道施工过程中必须开展的一项工作,其直接关系到后续的开挖及施工支护方案。为有效地进行隧道围岩类别超前分类,提出了基于数字钻进技术和量子遗传（QGA）-径向基函数（RBF）神经网络的围岩类别超前分类方法。以数字钻进技术为基础,从钻进参数中提取有用信息,构建围岩类别超前分类指标体系。采用量子计算原理对遗传算法进行改进,通过量子位编码和量子旋转门更新种群,以此来确定RBF神经网络的参数,建立了基于QGA-RBF神经网络的围岩类别超前识别系统。最后将该方法应用于青岛胶州湾海底隧道的围岩类别超前识别中,结果表明,该方法具有较高的准确性,其结果为围岩类别超前分类提供了一种新思路。 相似文献
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在1:60溢流坝表、中泄水孔断面模型上对密松水电站泄水建筑物的布置方案进行了泄流能力、流速流态、压力分布等相关水力学问题的试验,并通过十多个方案的比较优化,提出了基本可行的泄水建筑物体型和消力池型式。研究成果表明:表孔采用合适的宽尾墩形式,对增加消能率、缩短消力池池长有利,但无法消除宽尾墩形成的水翅击打两侧导墙现象;表孔取消宽尾墩,采用跌坎式消力池方案,可有效降低底流消能时的池底板流速,同时消除宽尾墩形成的水翅击打两侧导墙现象,达到较满意的消能效果。本文中十数个消能方案的研究成果,对类似工程的设计和科研均有参考价值。 相似文献
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在村镇辖区周边矿产勘查中,遇到民居、农田、道路、农业基础设施、山地植被绿化等,为了保护生态环境,满足绿色勘查的要求,提高地质矿产勘查工作质量和效率,在广丰许家桥黑滑石矿详查中,采用无人机航测、便携式全液压岩心钻机等技术设备进行勘查施工.项目通过先进的设备选型、环保的技术工艺、科学的勘查方案及具体的环保措施,取得了缩短勘查周期、提高岩（矿）心采取率、消除传统勘查安全隐患、降低征地搬迁劳动强度与成本及减轻对生态环境的污染与破坏的成效,实现了地质勘查质优高效,经济效益和社会效益双丰收,达到绿色勘察的目标任务。地质矿产勘查工作走绿色勘查之路,不仅保护了绿水青山生态环境,还可通过高标准的绿色勘查技术手段和环境保护要求,提高勘查效率和质量、降低劳动强度和成本、实现节能降耗目标,是一条可持续、高质量发展之路。 相似文献
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自推广小口径金刚石钻探工艺以来，管理水平、操作技术不断提高，钻进效率、台年进尺、钻头进尺等各项技术经济指标显著增长，事故减少，成本降低。但还存在一些值得引起深切注意的技术问题，提出来供同志们分析、解决。 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20141520 Bo Ying(Key Laboratory of Metallogeny and Mineral Assessment,MLR,Beijing 100037,China);Liu Chenglin Saline Spring Hydrochemical Characteristics and Indicators for Potassium Exploration in Southwestern and Northern Tarim Basin,Xinjiang(Acta Geoscientica Sinica,ISSN1006-3021,CN11-3474/P,34(5),2013,p.594-602,5 illus.,3 tables,28 refs.) 相似文献
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正20141243Chen Ge(Hangzhou Research Institute of Petroleum Geology,PetroChina,Hangzhou 310023,China);Si Chunsong Study on Sedimentary Numerical Simulation Method of Fan Delta Sand Body(Journal of Geology, 相似文献
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正20142599Chen Sanming(Guangxi Key Laboratory of Concealed Deposits Exploration,Guilin University of Technology,Guilin541004,China);He Yuzhou Block Model and Reserves Estimation of Panzhihua Iron Deposit Based on 3D Geological Modeling(Journal of Guilin University of Technology,ISSN1674-9057,CN45-1375/N,33(4),2013,p.610-615,9illus.,1table,15refs.) 相似文献
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正20140594 Bai Daoyuan(Hunan Institute of Geology Survey,Changsha 410016,China);Zhong Xiang Faults in the Jingzhou Basin and Their Tectonic Settings(Geotectonica et Metallogenia,ISSN1001-1552,CN44-1595/P,37(2),2013,p.173-183,6illus.,59refs.)Key words:basin evolution,tectonic setting,South China In the Upper Paleozoic and Jurassic se- 相似文献
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正20141912Cao Hui(State Key Laboratory for Continental Tectonics and Dynamics,Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China)Gravitational Collapse and Folding during Orogenesis:A Comparative Study of FIA Trends and Fold Axial Plane Traces(Geology in China,ISSN1000-3657,CN11-1167/P,40(6),2013,p.1818-1828,9illus.,35refs.,with 相似文献