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分形结构是土体中普遍存在的一种现象,通过对分形结构连接部位所占据的影响域(Voronoi域)的分析,将颗粒连接承载能力换算为影响域上的应力强度,由此获得了一些有益的结果。土体颗粒系统结构分维值的大小对土体强度有着明显的影响;基本结构单元的颗粒数越多,形成的环的长度越长,占据的空间就越大,从力学上讲就越不稳定,因此,其强度越低;土体中分形结构的级数实际上决定了土体中最大孔隙的尺寸,分形结构的级数越多,其相应的最大孔隙越大,等效应力强度会越低;发现偶应力强度与基本结构单元的面积(二维)成反比,即基本结构体越大,偶应力强度就越小,由此可推论出:在其他条件相同的情况下,颗粒越大,偶应力强度就会越低。 相似文献
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Previous paleoenvironmental studies reported the δD values of a mixture of coeluting alkenones. Here, we present a semi-preparative normal-phase high-performance liquid chromatography–mass spectrometry (NP-HPLC–MS) method for purifying long chain (C37 and C38) unsaturated methyl and ethyl ketones (alkenones) on the basis of chain length and degree of unsaturation.The method was applied to purify alkenones in suspended particles and surface sediments from a site in Chesapeake Bay, eastern USA. The hydrogen isotopic composition of di- and triunsaturated C37 and C38 alkenones differed significantly on the basis of chain length and the degree of unsaturation, demonstrating the importance of gas chromatography–isotope ratio-mass spectrometry (GC–irMS) analysis of individual alkenones for accurate paleoenvironmental reconstruction. Constant fractionation factors between alkenones with different chain length but the same degree of unsaturation () and those with the same chain length but different degree of unsaturation () in all samples suggest that the values may represent hydrogen isotope fractionation associated with elongation and desaturation during alkenone biosynthesis. 相似文献
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Frédéric Béjina Misha Bystricky Nicolas Tercé Matthew L. Whitaker Haiyan Chen 《Comptes Rendus Geoscience》2019,351(2-3):86-94
In situ X-ray diffraction was used to measure the isothermal bulk modulus at room conditions (KT0) of synthetic olivines with different iron contents. The chemical formulae of the olivine samples were with x = 0.45; 0.64; 0.82; 1, with 1% standard deviation (referenced as Fa45, Fa64, Fa82 and Fa100, respectively). All experiments were performed in the multi-anvil apparatus installed at NSLS beamline X17B2, to pressures up to about 7 GPa. Unit-cell volumes under hydrostatic conditions and differential stresses present in the samples were calculated using the method developed by Singh et al. (1998), and pressures measured using NaCl as a standard were then corrected for these stresses. Using a second-order Birch–Murnaghan equation of state, we obtained the isothermal bulk modulus of each composition: GPa, GPa, GPa and GPa. These values combined with data available in the literature show that the KT0 of Fe-rich olivines increases very slowly with the Fe content, but possibly not in a simple linear trend. 相似文献
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喀英迪铅锌矿主要产于早石炭世阿克沙克组及其与晚奥陶世呼独克达坂组的接触带上。通过普查工作共圈定15个铅锌矿体。其中主要矿体4个,Ⅰ-4矿体处于晚奥陶世呼独克达坂组灰岩与早石炭世阿克沙克组的不整合接触面上及其两侧,工程控制总长度为523m,最大斜深100m。倾向70°~100°,倾角一般20°~50°,连续性较好。该矿体铅单工程厚0.86~5.64m,平均2.86m,厚度变化系数为70.57%;锌单工程厚0.80~5.64m,平均1.81m,厚度变化系数为93.97%,属于变化较稳定型矿体。铅单工程品位0.62%~16.47%,平均4.53%,品位变化系数114.34%;锌单工程品位0.53%~12.37%,平均3.78%,品位变化系数57.47%。属于有用组分分布较均匀型矿体。通过对矿床地质特征的研究,认为该矿床属沉积岩容矿的、层控的、构造控制非岩浆型低温热液矿床。 相似文献
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滇东岩溶石山地区石漠化特征及成因 总被引:35,自引:0,他引:35
滇东地区生态地质环境脆弱,石漠化明显,面积28 320 km2,严重地制约着地区经济的可持续发展。采用三级标准划分石漠化等级,景观差异特征明显,便于野外识别,制定与之相适应的整治措施。滇东地区石漠化分布具有集中连片、自北向南逐渐增多、程度加重的特点。石漠化的成因:地貌的演化过程中存在着石漠化的潜势,广泛分布的岩溶石山是形成石漠化的物质基础,特定的自然地理环境是导致石漠化的基本条件;人口增长过快、不合理的土地开发、工业污染是形成石漠化的主要因素,但自然因素和人为因素的主次因地而异。 相似文献
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本文针对矿井煤层瓦斯抽放及防突中煤层透气性差,瓦斯抽放率低等问题,按照高压水射流技术应用的原理,设计了应用于抽放钻孔中切割煤体的高压水射击流装置,并在现场对喷嘴和射流器进行了试验。试验结果表明,水射流方向采用+100,喷嘴直径为1.5mm,切割速度为0.2m/min,泵压为30MPa时,水射流切割钻孔中煤体效果最佳;煤层采用高压水射流切割缝后,钻孔预抽瓦斯的抽放率提高了18.8%,抽放时间相对缩短90%以上。因此,该项技术对于煤层瓦斯抽放和防治煤与瓦斯突出具有重要作用。 相似文献
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隧道施工时地表沉降监测控制标准探讨 总被引:5,自引:0,他引:5
地表沉降是判断浅埋隧道地层稳定的一个重要指标。在分析地表沉降监测重要性和隧道埋深的关系基础上,阐述了地表沉降控制标准确定的原则;针对隧道无邻近结构物段,从地层围岩稳定、经验公式和相关规范的角度探讨地表沉降控制标准,并以武广客运专线浏阳河隧道为例子进行验证。结果表明,城市隧道变形控制标准要比山岭隧道更严格,浅埋隧道要比深埋隧道控制标准更严格;围岩越坚硬、跨度越小、边墙高度越小,则允许的位移越小,反之则越大;允许的变形控制标准主要影响因素是围岩自身条件,其次是隧道的跨度 相似文献
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江西德兴矿区为我国重要的矿产资源基地, 目前面临资源枯竭的困境, 寻找替代的新矿产迫在眉睫.根据研究区野外土壤实测样品分析, 利用连续统去除的方法提取土壤实测光谱的特征吸收位置, 从而建立粘土矿物含量为因变量的预测方程.检验得知, 高岭石相关系数R为0.811, 拟合系数R2达到0.658, F值为5.275, Sig值为0.047 7, 其小于0.05;绿泥石相关系数R为0.893, 拟合系数R2达到0.797, F值为1.602, Sig值为0.016 6, 其小于0.05;伊利石相关系数R为0.783, 拟合系数R2达到0.619, F值为5.57, 对应的Sig值是0.075 4, 其大于0.05, 说明自变量与因变量之间具有高度相关性, 反演精度较好.从反演结果可知, 研究区的高岭石整体含量较高, 整体上粘土矿物高岭石、绿泥石和伊利石在1号坝、2号坝、4号坝和铜矿区含量较低.由于粘土矿物不断地经过地球化学变化、累积, 产生黄铁矿、黄铜矿及赤铁矿, 所以挑选粘土矿物富集并且地质构造活跃的区域为铁矿石及铜矿石预测区.结合研究区地质解译图与粘土矿物反演结果, 在采矿场与IV号尾矿坝向NE方向沿线上圈定两个遥感找矿有利区. 相似文献
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Pyrolysis of two kerogens isolated from the and source rocks in the Niuzhuang sag, Dongying Depression, Bohai Bay Basin, China, was performed in a confined system. The products were extracted with solvent and separated using micro-column chromatography into group-type fractions (saturates, aromatics, resins and asphaltenes) with the kerogen residue in each case undergoing swelling with a variety of solvents. The kinetics for generation and retention of crude oil and its group-type fractions from the kerogens were studied and the kinetic parameters applied to modeling generation and retention of crude oil and its fractions from the and source rocks on the basis of burial and thermal history of the Niuzhuang sag. The results show that the “normal oil” was generated at about 4.26 Ma and 24.85 Ma ago, but expelled at about 3.96 Ma and 17.46 Ma ago, respectively, from and source rocks. The current proportions of the expelled saturates, aromatics and NSOs are about 60%, 15% and 25%, respectively. 相似文献