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NaOH溶液浓度对硅质集料和白云质集料岩石柱膨胀的影响
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作者 杨文文 邓敏 +2 位作者 黄蓓 陈维佳 王志磊 《南京工业大学学报(自然科学版)》 CAS 北大核心 2018年第3期18-23,共6页
改进岩石柱法研究硅质碱活性组分分散分布在岩石中的硅质集料和白云质集料岩石柱在80℃不同浓度的NaOH溶液中的膨胀性。结果表明:当NaOH溶液浓度分别为1.00和0.50 mol/L时,硅质集料和白云质集料岩石柱均可产生显著膨胀,当NaOH浓度低至0.... 改进岩石柱法研究硅质碱活性组分分散分布在岩石中的硅质集料和白云质集料岩石柱在80℃不同浓度的NaOH溶液中的膨胀性。结果表明:当NaOH溶液浓度分别为1.00和0.50 mol/L时,硅质集料和白云质集料岩石柱均可产生显著膨胀,当NaOH浓度低至0.25 mol/L时,硅质集料岩石柱不膨胀或轻微膨胀,白云质集料岩石柱膨胀显著。当NaOH浓度为0.10 mol/L时,硅质集料岩石柱不膨胀,白云质集料岩石柱膨胀。岩石柱法可以用于评定硅质碱活性组分分散分布集料的碱硅酸反应活性,当养护溶液为80℃、0.25 mol/L的NaOH溶液时,采用岩石柱法可判定白云质集料是否具有碱碳酸盐反应活性。 展开更多
关键词 硅质集料 白云质集料 岩石柱 NaOH溶液浓度
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集料碱活性岩石柱法自动测试仪的应用研究 被引量:1
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作者 高峰 《山西建筑》 2017年第9期106-108,共3页
针对岩石柱法碱活性试验过程自动化程度低、误差大的问题,研发了一种新型自动测试仪,并将位移传感器与自动化控制系统相结合,实现了试件养护、数据采集、数据分析的自动化控制,大大提高了测量精度和工作效率。
关键词 碱活性 岩石柱 测试方法 自动测试仪
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峨眉山大火成岩省的岩石圈结构:对地幔柱-岩石圈相互作用的启示
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作者 陈赟 赵与同 +3 位作者 刘佳乐 梁晓峰 李玮 徐义刚 《岩石学报》 SCIE EI CAS CSCD 北大核心 2023年第9期2541-2553,共13页
峨眉山大火成岩省位于扬子克拉通西缘,是中-晚二叠世峨眉山古地幔柱头熔融的产物。因此,该区岩石圈结构特征对于揭示地幔柱-岩石圈相互作用方式与机制具有重要的指示意义。本文基于COMPASS-ELIP宽频带地震台阵资料,开展S波接收函数成像... 峨眉山大火成岩省位于扬子克拉通西缘,是中-晚二叠世峨眉山古地幔柱头熔融的产物。因此,该区岩石圈结构特征对于揭示地幔柱-岩石圈相互作用方式与机制具有重要的指示意义。本文基于COMPASS-ELIP宽频带地震台阵资料,开展S波接收函数成像研究,并与同剖面远震S波有限频层析成像、区域面波层析成像结果进行对比分析,识别了沿剖面岩石圈内部主要间断面,从而获得了峨眉山大火成岩省岩石圈结构的横向变化特征。结果显示,相对中带和外带,内带具有地壳增厚(增厚15~20km)、岩石圈减薄(减薄~50km)现象,且岩石圈地幔具有高速、分层特征,但下层底界面转换波震相并不明显;中带岩石圈厚度大(~170km),局部地段岩石圈-软流圈边界(LAB)缺失,对应位置存在地幔低速异常;外带岩石圈厚度略小(~150km),中带和外带均发育岩石圈中部不连续面(MLD)。结合地球化学、岩石学、物理/数值模拟等研究成果,本文推测上述特征记录了古地幔柱作用引起的不同程度岩石圈变形:地幔柱在内带以纵向作用为主,通过热-动力冲击方式造成岩石圈大幅度快速减薄,地幔柱头高程度减压熔融,产生的大规模岩浆穿透岩石圈地幔,在地壳发生底侵和内侵,部分喷出地表形成溢流玄武岩;地幔柱在中带以横向作用为主,通过底部剪切引起岩石圈地幔横向伸展,甚至造成局部撕裂,在撕裂部位进一步引发热-化学侵蚀并导致岩石圈破坏;地幔柱在外带以垂向拖曳为主,造成岩石圈的局部拆沉而减薄。此外,内带下方地幔的高速、分层特征,可能指示经历地幔柱作用减薄后的岩石圈,减薄产生的岩石圈空区因捕获地幔柱头熔融残留物而得到一定程度愈合,而受地幔柱改造后的残存岩石圈,因经历大量熔体抽取更加亏损而得到强化。综上,本文揭示的峨眉山大火成岩省岩石圈结构,为进一步理解地幔柱-岩石圈相互作用的方式与机制提供了新的地球物理观测证据。 展开更多
关键词 峨眉山大火成岩省 地幔-岩石圈相互作用 S波接收函数 岩石圈-软流圈边界 岩石圈中部不连续面
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峨眉地幔柱-岩石圈的相互作用:来自低钛和高钛玄武岩的Sr-Nd和O同位素证据 被引量:58
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作者 肖龙 徐义刚 何斌 《高校地质学报》 CAS CSCD 2003年第2期207-217,共11页
峨眉山玄武岩总体具有较高的87Sr/ 86Sr比值和较低的εNd(t)值 ,并具有富集地幔源区的特点。而低钛玄武岩 (LT)与高钛玄武岩 (HT)间又表现出一定的差异性 ,即早期低钛玄武岩(LT1)的87Sr/ 86Sr比值最高 (0 .70 6 3~ 0 .70 78) ,而其εNd... 峨眉山玄武岩总体具有较高的87Sr/ 86Sr比值和较低的εNd(t)值 ,并具有富集地幔源区的特点。而低钛玄武岩 (LT)与高钛玄武岩 (HT)间又表现出一定的差异性 ,即早期低钛玄武岩(LT1)的87Sr/ 86Sr比值最高 (0 .70 6 3~ 0 .70 78) ,而其εNd(t)最低 (- 6 .74~ - 0 .34) ;晚期高钛玄武岩 (HT)具有最低的87Sr/ 86Sr比值 (0 .70 4 9~ 0 .70 6 4 )和最高的εNd(t)值 (- 0 .71~ 1.5 )。峨眉山低钛玄武岩中单斜辉石的氧同位素变化范围为 6 .2‰~ 7.86‰ ,高于洋岛拉斑玄武岩的平均值5 .4‰。研究样品较地幔岩石偏高的δ18O值说明在其形成和演化过程中有壳源物质的参与。结合前人的研究成果和对元素地球化学的研究认为 ,壳源物质可能主要来自于新元古代富集的扬子西缘次大陆岩石圈地幔。地幔柱 -岩石圈的相互作用过程中表现在时间和空间的系统变化 ,即早期西岩区形成含大量壳源组分的低钛玄武岩 ,晚期为壳源组分相对较少的高钛玄武岩。空间上低钛玄武岩仅分布在西岩区 ,而中、东岩区皆为高钛玄武岩。壳源组分随着时间演化逐渐减少 ,在空间上由西而东也逐渐减少。表明峨眉山火成岩省形成早 (主 )期地幔柱头卷入并熔融了较多交代富集的次大陆岩石圈物质 ,晚期则有较少的壳源物质参与。 展开更多
关键词 蛾眉山玄武岩 Sr-Nd同位素 氧同位素 地幔岩石圈相互作用
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峨眉山玄武岩区两类玄武岩的地球化学:地幔柱-岩石圈相互作用的证据 被引量:7
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作者 张招崇 王福生 《地质学报》 EI CAS CSCD 北大核心 2002年第2期281-288,共8页
野外地质和地球化学研究表明,峨眉山玄武岩区主要由玄武岩以及顶部少量的粗面岩组成。与其他地区的溢流玄武岩相似,峨眉山玄武岩区也可以分成低Ti和高Ti两种。由于 Ti和 P具有正相关性,并且 TiO2的含量具有连续性(1%
关键词 峨眉山 玄武岩 地球化学 地幔-岩石圈相互作用
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柱状节理岩石的旋转椭球纤维丛力学模型 被引量:2
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作者 苑宝军 邓荣贵 杨涛 《地下空间与工程学报》 CSCD 北大核心 2015年第6期1390-1395,共6页
根据柱状节理岩石形成的地质特征,基于细观层面,将单根柱状岩石在重力方向上视为纤维丛,轴对称状态下,纤维丛将根据外荷的变化有机地进行调整,假设纤维丛根据变形协调条件排列为细观椭球体胞群,则通过分析典型椭球体胞的本构行为即可进... 根据柱状节理岩石形成的地质特征,基于细观层面,将单根柱状岩石在重力方向上视为纤维丛,轴对称状态下,纤维丛将根据外荷的变化有机地进行调整,假设纤维丛根据变形协调条件排列为细观椭球体胞群,则通过分析典型椭球体胞的本构行为即可进一步探讨整个岩石的宏观力学性质。根据纤维椭球体胞的几何方程,通过Banach不动点定理和Brouwer不动点定理证明了轴对称状态下椭球体胞中存在着旋转效应并给出了旋转附加应力的表达式,揭示了柱状岩石存在通过周界粘滞剪切耗散局部应变能的过程;通过引入Freudenthal率相关方程并联合有旋转效应的平衡方程构建了分析椭球体胞的本构微分方程组并对之进行了Laplace变换;根据纤维丛细观本构模型及理论并结合泥巴山柱状流纹岩的岩石试验分析了不同应力路径下椭球体胞的几何特征与宏观破坏结果之间的内在联系。 展开更多
关键词 状节理岩石 细观本构模型 椭球体胞 旋转纤维丛
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受均布围压岩石试件的三维应力函数 被引量:1
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作者 王永岩 时秀文 李剑光 《科学技术与工程》 北大核心 2019年第31期298-303,共6页
以圆柱体标准岩石试件受均布围压时的弹性阶段为研究对象,以弹性力学空间轴对称理论为依据,采用半逆解法,构造出试件的三维应力函数。根据应力函数推导出应力分量。为岩石内部力学性质的研究提供了便利。并与ANSYS模拟结果进行对比,发... 以圆柱体标准岩石试件受均布围压时的弹性阶段为研究对象,以弹性力学空间轴对称理论为依据,采用半逆解法,构造出试件的三维应力函数。根据应力函数推导出应力分量。为岩石内部力学性质的研究提供了便利。并与ANSYS模拟结果进行对比,发现两者结果非常吻合,从而表明构造的应力函数是可取的。 展开更多
关键词 岩石 均布围压 三维应力函数 半逆解法
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湄洲湾输电线路岩石锚杆试验及其基础设计 被引量:1
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作者 吴登峰 赵金飞 陈孝湘 《福建建筑》 2010年第9期60-63,共4页
福建输电线路工程多分布在山区,通过以湄洲湾大跨越高塔岩石锚杆试验基础为背景,针对在强风化花岗岩地质条件下的普通斜柱基础与岩锚结合的基础进行抗拔、水平极限承载力的设计计算,扩展岩石锚杆基础在山区线路工程中的应用范围,为强风... 福建输电线路工程多分布在山区,通过以湄洲湾大跨越高塔岩石锚杆试验基础为背景,针对在强风化花岗岩地质条件下的普通斜柱基础与岩锚结合的基础进行抗拔、水平极限承载力的设计计算,扩展岩石锚杆基础在山区线路工程中的应用范围,为强风化地质条件下岩石锚杆基础设计提供参考。 展开更多
关键词 输电线路 普通斜基础与岩石锚杆 试验基础 承载力
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塔里木大火成岩省碱性岩浆活动与稀有金属成矿作用 被引量:2
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作者 朱圣柱 黄小龙 +3 位作者 于洋 贺鹏丽 杨帆 李梦静 《大地构造与成矿学》 EI CAS CSCD 北大核心 2023年第3期631-660,共30页
地幔柱活动导致大火成岩省的形成,并伴随大规模岩浆作用和成矿事件。碱性岩型稀有金属矿床是地幔柱成矿作用中非常重要的一类,但目前对该类矿床形成过程中稀有金属元素超常富集机制仍缺少系统性研究。本文搜集了塔里木大火成岩省两大构... 地幔柱活动导致大火成岩省的形成,并伴随大规模岩浆作用和成矿事件。碱性岩型稀有金属矿床是地幔柱成矿作用中非常重要的一类,但目前对该类矿床形成过程中稀有金属元素超常富集机制仍缺少系统性研究。本文搜集了塔里木大火成岩省两大构造域(塔里木克拉通及边缘地区和中亚造山带)碱性岩浆岩的年代学和岩石地球化学数据,分析其岩浆活动和成矿作用的基本特点,探讨地幔柱与不同类型大陆岩石圈相互作用导致稀有金属元素富集的差异性。塔里木克拉通及边缘地区碱性岩浆岩主要为碱性正长岩‒花岗岩和碳酸岩,形成于291~268 Ma,峰期年龄为~278 Ma,主要属于塔里木大火成岩省最晚阶段的岩浆活动;其中碱性正长岩‒花岗岩富碱、Th、REE、Nb、Zr,高Ga/Al、Nb/Ta值,多数显示典型A1型花岗岩的地球化学特征。中亚造山带碱性岩浆岩为碱性正长岩‒花岗岩,形成于325~255 Ma,大部分与塔里木大火成岩省岩浆活动时代一致,其碱、Th、REE、Nb、Zr含量和Ga/Al、Nb/Ta值明显低于塔里木克拉通及边缘地区的碱性正长岩‒花岗岩,并且多数显示典型A2型花岗岩的地球化学特征。塔里木克拉通及边缘地区的碱性正长岩‒花岗岩和碳酸岩赋存Nb-Zr-REE矿床,而中亚造山带的碱性正长岩‒花岗岩则赋存Li-Be-Ta-Nb-W-Sn-Mo矿床。地幔柱和再循环洋壳物质加入地幔源区导致塔里木克拉通及边缘地区的碱性岩浆岩富集Nb、Zr、REE;中亚造山带碱性岩浆岩的源区因近期俯冲交代影响的岩石圈地幔和新生地壳物质的参与而显著富集Li、Be、W、Sn、Mo等流体活动元素。塔里木克拉通及边缘地区碱性正长岩‒花岗岩贫硅、钠质、过碱性的特征有利于熔体中Nb、Zr、REE的富集;而中亚造山带碱性正长岩‒花岗岩富硅、钾质、过铝质的特征有利于Ta、Li、W、Sn的富集。塔里木克拉通和中亚造山带具有不同的地幔柱‒岩石圈相互作用,其碱性岩浆岩的岩浆源区不同,并经历了不同的岩浆演化过程,导致塔里木大火成岩省两大构造域具有不同的稀有金属成矿作用。 展开更多
关键词 碱性岩浆岩 稀有金属成矿 地幔岩石圈相互作用 塔里木大火成岩省 中亚造山带
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判定混凝土骨料ACR活性反应的试验方法
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作者 秦海峰 《水科学与工程技术》 2007年第2期32-33,共2页
南水北调中线京石段应急供水工程各类建筑物及渠道需大量混凝土骨料,鉴于半个世纪以来碱活性骨料反应在世界各地造成混凝土工程的严重破坏,尤其是骨料的ACR活性反应被誉为“混凝土的癌症”,且不可抑制,因此判定骨料是否具有ACR活性对工... 南水北调中线京石段应急供水工程各类建筑物及渠道需大量混凝土骨料,鉴于半个世纪以来碱活性骨料反应在世界各地造成混凝土工程的严重破坏,尤其是骨料的ACR活性反应被誉为“混凝土的癌症”,且不可抑制,因此判定骨料是否具有ACR活性对工程安全至关重要。通过试验,对3种判定试验方法进行分析,得出在不同情况下应用不同的试验方法检测骨料是否具有ACR活性的结论。 展开更多
关键词 ACR活性 岩相法 岩石柱 岩石柱快速蒸压法
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Experimental studies on pillar failure characteristics based on acoustic emission location technique 被引量:11
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作者 徐帅 刘建坡 +3 位作者 徐世达 魏炯 黄文柏 东龙宾 《Transactions of Nonferrous Metals Society of China》 SCIE EI CAS CSCD 2012年第11期2792-2798,共7页
Acoustic emission (AE) technique is a useful tool for investigating rock damage mechanism, and is used to study the temporal-spatial evolution process of microcracks during the similar pillar material experiment. A ... Acoustic emission (AE) technique is a useful tool for investigating rock damage mechanism, and is used to study the temporal-spatial evolution process of microcracks during the similar pillar material experiment. A combined AE location algorithm was developed based on the Least square algorithm and Geiger location algorithm. The pencil break test results show that the location precision can meet the demand of microcrack monitoring. The 3D location of AE events can directly reflect the process of initiation, propagation and evolutionary of microcracks. During the loading process, stress is much likely concentrated on the area between pillar and roof of the specimen, where belongs to danger zone of macroscopic failure. When rock reaches its plastic deformation stage, AE events begin to decrease, which indicates that AE quiet period can be seen as precursor characteristic of rock failure. 展开更多
关键词 rock damage mechanism pillar specimen failure characteristics temporal-spatial evolution microracks acousticemission location algorithm quiet period
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小秦岭崤山地区晚太古代基底变质岩系划分与对比 被引量:4
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作者 喻积贤 《河南地质》 1998年第2期106-113,共8页
小秦岭、崤山地区第二轮1∶5万区调查明,两地区晚太古代基底变质岩系均包括变质表壳岩系和变质花岗岩系。据此划分了构造岩石地层单位和构造岩石单位。根据其间的层序、时序关系,建立了各自统一的地层—岩石柱,拟出了新的划分对比... 小秦岭、崤山地区第二轮1∶5万区调查明,两地区晚太古代基底变质岩系均包括变质表壳岩系和变质花岗岩系。据此划分了构造岩石地层单位和构造岩石单位。根据其间的层序、时序关系,建立了各自统一的地层—岩石柱,拟出了新的划分对比方案。指出小秦岭地区观音堂组与崤山地区杨寺沟岩组是同一次沉积事件的产物,应属同一构造岩石地层单位,可作为区域对比的标志层位。根据接触关系,将小秦岭地区呈异岩不整合伏于观音堂组之下的变质花岗岩系划属晚太古代阜平期花岗岩,将崤山地区侵入于杨寺沟岩组的变质花岗岩系划属晚太古代五台期花岗岩。 展开更多
关键词 晚太古代 变质岩系 地层 岩石柱 划分 对比
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Cancelling ore pillars in large-scale coastal gold deposit: A case study in Sanshandao gold mine, China 被引量:10
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作者 刘志祥 党文刚 +1 位作者 贺显群 李地元 《Transactions of Nonferrous Metals Society of China》 SCIE EI CAS CSCD 2013年第10期3046-3054,共9页
According to the actual conditions in Sanshandao Gold Mine, the cancelling ore pillars mining method was researched. Firstly, a series of tests for the physical and mechanical characteristics of rock mass were carried... According to the actual conditions in Sanshandao Gold Mine, the cancelling ore pillars mining method was researched. Firstly, a series of tests for the physical and mechanical characteristics of rock mass were carried out and a quality classification system of rock mass applied in coastal metal deposit was established. Secondly, the reasonable demarcation depth of cancelling ore pillars was simulated using the finite element method, and the simulation results show that the ore pillars can be cancelled below the level of-555 m. Thirdly, a novel layer-backfill mining method of room-pillar alternation was designed to reduce the disturbance and settlement of terrain in mining area. Engineering practice shows that the new mining method enhanced the mining output and relieved rock disturbance. Furthermore, the settlement of the roof strata was small and no disaster occurred. The new mining technology effectively controlled the deformation of the terrain, indicating that the mining of the large-scale gold coastal deposit in Sanshandao Gold Mine was achieved safely, efficiently, and with a low loss rate. 展开更多
关键词 coastal deposit rock quality evaluation numerical simulation layer-backfill mining method of room-pillar alternation monitoring system
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Ilvaite as a thermodynamic recorder of multistage retrograde alteration in large Galinge skarn Fe deposit, western China 被引量:1
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作者 YU Miao Jeffrey MDICK +5 位作者 MAO Jing-wen FENG Cheng-you LI Bin LU An-huai ZHU Yong-feng LAI Jian-qing 《Journal of Central South University》 SCIE EI CAS CSCD 2019年第12期3534-3550,共17页
The ilvaite-bearing skarn associations in the Galinge skarn deposit were studied to determine their physicochemical formation conditions.A thermodynamic model setting pressure of 50 MPa(Pf=Ps=50 MPa)was set up to trac... The ilvaite-bearing skarn associations in the Galinge skarn deposit were studied to determine their physicochemical formation conditions.A thermodynamic model setting pressure of 50 MPa(Pf=Ps=50 MPa)was set up to trace the skarn evolution.Petrographic evidence for replacement of garnet and magnetite by ilvaite in the early retrograde stage(Stage I)combined with thermodynamic modeling suggests that the alteration may have occurred at 400470°C under moderately high fO withΔlgfO(HM)ranges from 4 to 4.2.The model is based on a maximum 22 pressure of 50 MPa calculated from magmatic amphibole geobarometer.The continuous breakdown of ilvaite with quartz to form ferro-actinolite and magnetite occur in the late retrograde stage(Stage II).The reactions occurred at 400440°C under moderate fO(ΔlgfO(HM):4 to 4.4).In Stage III,the breakdown of ilvaite to form calcite,pyrite 22 and ferroactinolite depends on XCO which can be estimated to be in a range of 0.005 to 0.05,and the reaction would 2 occur at higher temperatures with increasing XCO.Under these conditions,the breakdown occurs at 270350°C and 2 low fO(ΔlgfO(HM):up to 5.2).The thermodynamic model for continuous evolution from Stage I to Stage III 22 completely records the conditions of the retrograde alteration,which is inconsistent with the thermobarometry imprints of fluid inclusions.Therefore,the petrography and phase relations of ilvaite are useful indicators of reaction conditions in various skarn deposit types. 展开更多
关键词 Galinge skarn deposit ILVAITE retrograde alteration thermodynamic properties
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Analysis of roof and pillar failure associated with weak floor at a limestone mine 被引量:5
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作者 Murphy Michael M. Ellenberger John L. +1 位作者 Esterhuizen Gabriel S. Miller Tim 《International Journal of Mining Science and Technology》 SCIE EI CSCD 2016年第3期471-476,共6页
A limestone mine in Ohio has had instability problems that have led to massive roof falls extending to the surface. This study focuses on the role that weak, moisture-sensitive floor has in the instability issues.Prev... A limestone mine in Ohio has had instability problems that have led to massive roof falls extending to the surface. This study focuses on the role that weak, moisture-sensitive floor has in the instability issues.Previous NIOSH research related to this subject did not include analysis for weak floor or weak bands and recommended that when such issues arise they should be investigated further using a more advanced analysis. Therefore, to further investigate the observed instability occurring on a large scale at the Ohio mine, FLAC3 D numerical models were employed to demonstrate the effect that a weak floor has on roof and pillar stability. This case study will provide important information to limestone mine operators regarding the impact of weak floor causing the potential for roof collapse, pillar failure, and subsequent subsidence of the ground surface. 展开更多
关键词 Underground limestone Ground control Case study Weak floor Instability
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THE RELATION BETWEEN THE CHAIN PILLAR WIDTH AND THE SURROUNDING ROCK DEFORMATION OF ROADWAY
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作者 郭育光 陆士良 《Journal of China University of Mining and Technology》 1992年第1期1-10,共10页
Based on the analysis and research into ground pressure behavior law and surrounding rock deformation of a large number of roadways affected by mining activity,this paper proposed a relation between the surrounding ro... Based on the analysis and research into ground pressure behavior law and surrounding rock deformation of a large number of roadways affected by mining activity,this paper proposed a relation between the surrounding rock deformation during mining ,the surrounding rock deformation rate during stable stage of mining and the chain pillar width. Moreover,it established the relation between the total amount of surrounding rock deformation during service period of roadway and the chain pillar width,which provides a principal basis for choosing the chain pillar width. 展开更多
关键词 ROADWAY surrounding rock deformation chain pillar width
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Stability analysis and determination of rock pillar between two adjacent caverns in different regions of Asmari formation in Iran
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作者 Abdollahipour Abolfazl Ghannadshirazi Hossein 《International Journal of Mining Science and Technology》 SCIE EI 2014年第5期593-596,共4页
Large underground caverns are commonly used in variety of applications. In many cases, because of the geomechanical limitations of dimensions and requirement of high volume, several parallel caverns are used. Plastic ... Large underground caverns are commonly used in variety of applications. In many cases, because of the geomechanical limitations of dimensions and requirement of high volume, several parallel caverns are used. Plastic zone integration requires a larger rock pillar distance of theses adjacent caverns while eco- nomic and access reasons require smaller distance. In lran many underground projects are located in West and South West, Asmari formation covers a large part of these regions. The stability of underground spaces that are constructed or will be constructed in this formation has been investigated. A proper cross section based on plastic analysis and a stability criterion has been proposed for each region. Finally, in each case, allowable rock pillar between adjacent caverns with similar dimension was determined with two methods (numerical analysis and fire service law). Results show that Fire Service Law uses a very con- servative safety factor and it was proposed to use a correction factor for allowable distance based on application of underground space. 展开更多
关键词 Stability analysis Storage cavern Numerical analysis Rock pillar Asmari formation
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Characterization and application of tourmaline and beryl from Brazilian pegmatite in adsorption process with divalent metals 被引量:3
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作者 Denis L.Guerra Silze P.Oliveira +2 位作者 Ricardo A.R.Silva Victor Leidens Adriano C.Batista 《International Journal of Mining Science and Technology》 SCIE EI 2012年第5期711-718,共8页
In this study,the original tourmaline and beryl mineral samples have been collected from a Brazilian pegmatite.The objective of this study was to examine the adsorption behavior of Brazilian ciclosilicate samples,towa... In this study,the original tourmaline and beryl mineral samples have been collected from a Brazilian pegmatite.The objective of this study was to examine the adsorption behavior of Brazilian ciclosilicate samples,towards divalent metals(Pb 2+,Mn 2+,and Zn 2+) in ethanol solution has been studies by a batch technique.The ciclosilicate samples were characterized by elemental analysis,Fourier transform infrared spectroscopy,helium picnometry,mercury porosity,and nitrogen adsorption-desorption.The Langmuir expression for adsorption isotherm was applied in order to determine the adsorption capacity to form a monolayer and the constant related to the adsorption intensity.In aqueous solution there was a significant adsorption increase with the temperature and pronounced synergistic effects were observed.The maximum number of moles adsorbed was determined to be 12.48 and 11.49 mmol/g for systems Pb 2+ /beryl and Pb 2+ /tourmaline,respectively.The energetic effects caused by metal cations adsorption were determined through calorimetric titrations.Thermodynamics indicated the existence of favorable conditions for such Pb 2+-,Mn 2+-,and Zn 2+-OH interactions. 展开更多
关键词 Industrial minerals Environmental Pollution Surface modification Wasteprocesing
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Effects of overburden, rock strength and pillar width on the safety of a three-parallel-hole tunnel 被引量:3
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作者 Shong-loong CHEN Guo-wei LI Meen-wah GUI 《Journal of Zhejiang University-Science A(Applied Physics & Engineering)》 SCIE EI CAS CSCD 2009年第11期1581-1588,共8页
During the excavation of three-parallel-hole tunnel, the tunnel might collapse due to over-stress as a result of inadequate rock pillar width. Treating the rock overburden depth, rock strength, and rock pillar width a... During the excavation of three-parallel-hole tunnel, the tunnel might collapse due to over-stress as a result of inadequate rock pillar width. Treating the rock overburden depth, rock strength, and rock pillar width as variables, a series of 3D numerical analysis was carried out to examine the effect of each variable on the safety of the tunnel, in particular the rock pillar. A stress strength ratio (SSR) was used to define whether the safety of the rock pillar was exceeded. A simple design chart for the case of three-parallel-hole tunnel, which took into account the influence of overburden depth, rock pillar width, and rock strength, was also proposed for used in the preliminary design stage. 展开更多
关键词 Three-parallel-hole tunnel Tunnels interaction Rock pillar Numerical analysis Stress strength ratio (SSR)
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Thermal evolution and dynamic mechanism of the Sichuan Basin during the Early Permian-Middle Triassic 被引量:12
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作者 HE LiJuan XU HeHua WANG JiYang 《Science China Earth Sciences》 SCIE EI CAS 2011年第12期1948-1954,共7页
The Sichuan Basin, located in the western margin of Yangtze Plate, is one of the important oil-gas-bearing basins in China. During the Early Permian-Middle Triassic, the Sichuan Basin experienced regional lithospheric... The Sichuan Basin, located in the western margin of Yangtze Plate, is one of the important oil-gas-bearing basins in China. During the Early Permian-Middle Triassic, the Sichuan Basin experienced regional lithospheric extension and Emeishan basalt activities, both of which influenced the basin development and thermal evolution. Here we simulated the thermal effects of lithospheric extension and the Emeishan mantle plume based on different geodynamical models. Modeling results indicated that the lithospheric temperature together with the basement heat flow was generally increasing with time due to extension. As the stretching factor was relatively small, the thinning of lithosphere, and consequently the thermal disturbance, was not great. The lithospheric extension yielded about 20% increase of the basement heat flow, with maximum value of 60?62 mW m?2 in the Early Triassic. Mantle plume model shows that the thermal evolution of the inner zone above the plume head was influenced greatly by plume activity. But the outer zone and its outside area where the Sichuan Basin is located were affected only slightly. The basalts that had erupted in the southwestern basin might disturb the basin temperature significantly, although shortly and locally. Generally, the thermal history of the Sichuan basin during the Early Permian-Middle Triassic was controlled by the lithospheric extension, but locally it superimposed thermal effects of basalt activities in its southwestern area. 展开更多
关键词 tectono-thermal evolution numerical modeling lithospheric extension Emeishan basalt Sichuan Basin
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