矩阵原位替换解算方法     

黑志坚  张洪田  周秋生 《测绘科学》2009,34(4)

研究矩阵原位替换解算方法,包括矩阵行列式、矩阵方程未知数和矩阵逆阵的解算。利用矩阵三角分解原理和矩阵运算的基本法则导出矩阵元素约化值的计算公式,从而进一步导出利用矩阵元素约化值计算矩阵行列式、矩阵方程未知数和矩阵逆阵元素的原位替换解算公式。解算公式用纯量形式表出,有利于编程计算,且可实现按矩阵元素在矩阵中的存储位置原位替换解算。该解算方法可节省计算用内存空间和时间,提高科学计算的效率。  相似文献   

Lewis Ponds, a hybrid carbonate and volcanic-hosted polymetallic massive sulphide deposit, New South Wales, Australia     

Michael W. Agnew  Ross R. Large  Stuart W. Bull 《Mineralium Deposita》2005,39(8):822-844

The Lewis Ponds Zn–Pb–Cu–Ag–Au deposit, located in the eastern Lachlan Fold Belt, central western New South Wales, exhibits the characteristics of both volcanic-hosted massive sulphide and carbonate-hosted replacement deposits. Two stratabound massive to disseminated sulphide zones, Main and Toms, occur in a tightly folded Upper Silurian sequence of marine felsic volcanic and sedimentary rocks. They have a combined indicated resource of 5.7 Mt grading 3.5% Zn, 2.0% Pb, 0.19% Cu, 97 g/t Ag and 1.9 g/t Au. Main Zone is hosted by a thick unit of poorly sorted mixed provenance breccia, limestone-clast breccia and quartz crystal-rich sandstone, whereas Toms Zone occurs in the overlying siltstone. Pretectonic carbonate–chalcopyrite–pyrite and quartz–pyrite stringer veins occur in the footwall porphyritic dacite, south of Toms Zone. Strongly sheared dolomite–chalcopyrite–pyrrhotite veins directly underlie the Toms massive sulphide lens. The mineralized zones consist predominantly of pyrite, sphalerite and galena. Paragenetically early framboidal, dendritic and botryoidal pyrite aggregates and tabular pyrrhotite pseudomorphs of sulphate occur throughout the breccia and sandstone beds that host Main Zone, but are rarely preserved in the annealed massive sulphide in Toms Zone. Main and Toms zones are associated with a semi-conformable hydrothermal alteration envelope, characterized by texturally destructive chlorite-, dolomite- and quartz-rich assemblages. Dolomite, chlorite, quartz, calcite and sulphides have selectively replaced breccia and sandstone beds in the Main Zone host sequence, whereas the underlying porphyritic dacite is weakly sericite altered. Vuggy and botryoidal textures resulted from partial dissolution of the dolomite-altered sedimentary rocks and unimpeded growth of base metal sulphides, carbonate and quartz into open cavities. The intense chlorite-rich alteration assemblage, underlying Toms Zone, grades outward into a weak pervasive sericite–quartz assemblage with distance from the massive sulphide lens. Limestone clasts and hydrothermal dolomite at Lewis Ponds are enriched in light carbon and oxygen isotopes. The dolomite yielded ¹³C_VPDB values of –11 to +1 and ¹⁸O_VSMOW values of 6 to 16. Liquid–vapour fluid inclusions in the dolomite have low salinities (1.4–7.7 equiv. wt% NaCl) and homogenization temperatures (166–232°C for 1,000 m water depth). Dolomitization probably involved fluid mixing or fluid–rock interactions between evolved heated seawater and the limestone-bearing facies, prior to and during mineralization. ³⁴S_VCDT values range from 2.0 to 5.0 in the massive sulphide and 3.9 to 7.4 in the footwall carbonate–chalcopyrite–pyrite stringer veins, indicating that the hydrothermal fluid may have contained mamgatic sulphur and a component of partially reduced seawater. The sulphide mineral assemblages at Lewis Ponds are consistent with moderate to strongly reduced conditions during diagenesis and mineralization. Low temperature dolomitization of limestone-bearing facies in the Main Zone host sequence created secondary porosity and provided a reactive host for fluid-rock interactions. Main Zone formed by lateral fluid flow and sub-seafloor replacement of the poorly sorted breccia and sandstone beds. Base metal sulphide deposition probably resulted from dissolution of dolomite, fluid mixing and increased fluid pH. Pyrite, sphalerite and galena precipitated from a relatively low temperature, 150–250°C hydrothermal fluid. In contrast, Toms Zone was emplaced into fine-grained sediment at or near the seafloor, above a zone of focused up-flowing hydrothermal fluids. Copper-rich assemblages were deposited in the Toms Zone footwall and massive sulphide lenses in Main and Toms zones as the hydrothermal system intensified. During the D₁ deformation, fracture-controlled fluids within the Lewis Ponds fault zone and adjacent footwall volcanic succession remobilized sulphides into syntectonic quartz veins. Lewis Ponds is a rare example of a synvolcanic sub-seafloor hydrothermal system developed within fossiliferous limestone-bearing facies. The close spatial association between limestone, hydrothermal dolomite, massive sulphide and dacite provides a basis for new exploration targets elsewhere in New South Wales.Editorial handling: D. Lentz  相似文献   

强夯置换技术处理公路软土地基试验研究     

余开彪  王宗国  张成顺 《岩土力学》2006,27(Z1):969-972

分析了抛石强夯置换加固软土地基的原理,并通过监测和分析试验段的孔隙水压力在施工过程中的变化规律,以及研究静力触探、沉降观测和复合地基静载试验结果,说明通过该技术的应用,公路路基的承载力由软土地基的承载力90 kPa提高到复合地基的承载力245 kPa以上,加固深度达到6 m以上,且能够加快公路软土地基沉降过程。  相似文献   

变参数刚-柔性桩复合地基研究     

朱奎  徐日庆  郭印  周鹏飞 《岩土力学》2006,27(Z1):869-874

为了研究刚-柔性桩复合地基的承载和变形特性,在温州地区进行了6个大型不同试验参数条件下刚-柔性桩复合地基试验,并在静荷载试验中对刚性承压板下压力盒进行同步检测。根据检测成果较系统地分析了褥垫层的设置与否、褥垫层厚度及材料、刚性桩置换率对刚-柔性桩复合地基特性的影响,为工程设计提供一些可以借鉴的结论。  相似文献   

柴达木盆地东部表土花粉分析   总被引：21，自引：1，他引：20  

陈辉  吕新苗  李双成 《地理研究》2004,23(2):201-210

柴达木盆地东部荒漠区 8个样地、 2 3个样点的表土花粉分析较好地揭示了荒漠区花粉组合的特点及其与植被、环境的关系。研究发现 ,荒漠区表土花粉以藜科 (Chenopodiaceae)和蒿属 (Artemisia)为主 ,并以前者占优势地位 ,麻黄属 (Ephedra)亦较常见 ,禾本科(Gramineae)、菊科 (Compositae)植物在群落中也占有一定的比例。花粉百分比含量DCA排序与相关分析发现 ,荒漠区不同植物群落下表土花粉组合特征各不相同 ,而且与相应的植物群落及其所代表的环境特征相一致。荒漠区表土花粉蒿 /藜 (Artemisia/Chenopodiaceae)比对干旱程度具有指示作用 ,比值越小 ,越干旱。  相似文献   

用换填法及刚性桩复合地基处理桩基质量事故     

周青春  李海波  刘亚群 《岩土力学》2003,24(5):845-848

通过对某一工程桩基质量事故的分析,提出了一种经济合理有效地处理方案。该方案在充分利用原有桩基的同时,用人工级配的砂石料对原设计基底土进行换填,组合成刚性桩复合地基,有效地提高了地基承载力,使建筑物的沉降控制在允许范围内。  相似文献   

基于广义强度准则的地基土换填防冻胀能力评估   总被引：1，自引：1，他引：0  

李洪升  杨海天  刘增利  王悦东 《岩土力学》2003,24(5):682-685

基于广义强度准则,提出了一种评价地基土换填抗冻胀能力的新方法。将冻胀力作为外载荷考虑,将冻土缺陷考虑为裂纹,并把冻土断裂韧度作为重要因素引进新准则。通过一个挡墙基础的算例,对换填前后的稳定性和强度进行了分析,与传统方法相比,由于考虑了更多的因素,从而更加合理。  相似文献   

大型洞室群软岩置换方案优化的并行实现   总被引：1，自引：1，他引：0  

李邵军  冯夏庭  安红刚 《岩土力学》2003,24(3):335-338

并行计算己成为求解大规模岩土工程问题的一种强大趋势 。 以水布娅大型洞室群软岩置换方案优化为例 , 探讨了方案优化中的并行计算问题,分析了并行计算中的编程模式 、 任务划分 、负载平衡和编程方法等问题,在 W id n o w s 环境下的 PC 机群上成功实现了软岩置换方案优化的并行计算,并获得了近乎线性的加速比 , 从而大大提高了方案优化的计算速度和效率 , 为岩土工程计算并行化思路提供了重要参考 。  相似文献   

在线渗析-离子色谱法测定土壤中有效氟   总被引：1，自引：1，他引：0  

林琳  劳月娥  许健  倪晓芳  杨国祥 《岩矿测试》2011,30(4):497-500

土壤样品经超声波超声静置,提取上清液,经渗析进入色谱柱,采用Metrohm A Supp 4-250阴离子交换柱,以1.8 mmol/L碳酸钠-1.7 mmol/L碳酸氢钠混合溶液作为流动相,用在线渗析技术与离子色谱法联用测定土壤中的有效氟。与常规方法相比,建立的方法操作简单,避免了繁琐的样品前处理。加标回收率为90.5%～95.7%,精密度(RSD,n=6)为1.60%。该方法具有高效、快速、灵敏等特点,能够用于环境土壤样品中有效氟的检测。  相似文献   

河北平原表层土壤重金属环境质量及污染评价   总被引：9，自引：1，他引：8       下载免费PDF全文

郭海全杨志宏  李宏亮马文静 任久峰 《中国地质》2011,38(1):218-225

土壤环境质量评价是了解土壤环境质量状况、采取保护措施的重要前提,本文用土壤环境质量标准(GB15618-1995),对河北平原表层土壤重金属环境质量进行了评价,结果表明:河北平原表层土壤环境质量优良,一、二级土壤分别占全区93.02%和6.62%。同时又根据重金属元素的环境地球化学行为,采用富集因子,有效地区分了重金属污染的自然影响和人为影响,结果显示,河北平原表层土壤人为污染的面积较大,但以轻微污染为主。  相似文献