一种融合测高仪与地面GPS数据的单站电离层反演方法     

欧明  甄卫民  刘钝  於晓 《全球定位系统》2009,34(1):1-4

电离层层析成像技术非常适用于检测电离层电子密度的大尺度空间分布及其扰动。利用地面单站的GPSTEC值和另一站的数字测高仪观测数据，结合国际参考电离层（IRI），利用MART算法反演得到测站上空电子密度的垂直分布。利用白天和夜间的实测数据进行了CIT反演，结果表明了该方法的可靠性。  相似文献   

Geology and geochemistry of the adjacent Changkeng gold and Fuwang silver deposits, Guangdong Province, South China   总被引：2，自引：0，他引：2  

Hua-Ying Liang  Ping Xia  Xiu-Zhang Wang  Jing-Ping Cheng  Zhen-Hua Zhao  Cong-Qiang Liu 《Ore Geology Reviews》2007,31(1-4):304-318

The Changkeng Au and Fuwang Ag deposits represent an economically significant and distinct member of the Au–Ag deposit association in China. The two deposits are immediately adjacent, but the Au and Ag orebodies separated from each other. Ores in the Au deposit, located at the upper stratigraphic section and in the southern parts of the orefield, contain low Ag contents (< 11 ppm); the Ag orebodies, in the lower stratigraphic section, are Au-poor (< 0.2 ppm). Changkeng is hosted in brecciated cherts and jasperoidal quartz and is characterized by disseminated ore minerals. Fuwang, hosted in the Lower Carboniferous Zimenqiao group bioclastic limestone, has vein and veinlet mineralization associated with alteration comprised of quartz, carbonate, sericite, and sulfides. Homogenization temperatures of fluid inclusions from quartz veinlets in the Changkeng and Fuwang deposits are in the range of 210 ± 80 °C and 230 ± 50 °C, respectively. Salinities of fluid inclusions from the two deposits range from 1.6 to 7.3 wt.% and 1.6 to 2.6 wt.% equiv. NaCl, respectively. The δD_H2O, δ¹⁸O_H2O, δ¹³C_CO2 and ³He/⁴He values of the fluid inclusions from the Changkeng deposit range from − 80‰ to − 30‰, − 7.8‰ to − 3.0‰, − 16.6‰ to − 17.0‰ and 0.0100 to 0.0054 Ra, respectively. The δD_H2O, δ¹⁸O_H2O, δ¹³C_CO2 and ³He/⁴He values of fluid inclusions from the Fuwang deposit range from − 59‰ to − 45‰, − 0.9‰ to 4.1‰, − 6.7‰ to − 0.6‰ and 0.5930 to 0.8357 Ra, respectively. The δD_H2O, δ¹⁸O_H2O, δ¹³C_CO2 and ³He/⁴He values of the fluid inclusions suggest the ore fluids of the Changkeng Au-ore come from the meteoric water and the ore fluids of the Fuwang Ag-ore are derived from mixing of magmatic water and meteoric water. The two deposits also show different Pb-isotopic signatures. The Changkeng deposit has Pb isotope ratios (²⁰⁶Pb/²⁰⁴Pb: 18.580 to 19.251, ²⁰⁷Pb/²⁰⁴Pb: 15.672 to 15.801, ²⁰⁸Pb/²⁰⁴Pb: 38.700 to 39.104) similar to those (²⁰⁶Pb/²⁰⁴Pb: 18.578 to 19.433, ²⁰⁷Pb/²⁰⁴Pb: 15.640 to 15.775, ²⁰⁸Pb/²⁰⁴Pb: 38.925 to 39.920) of its host rocks and different from those (²⁰⁶Pb/²⁰⁴Pb: 18.820 to 18.891, ²⁰⁷Pb/²⁰⁴Pb: 15.848 to 15.914, ²⁰⁸Pb/²⁰⁴Pb: 39.579 to 39.786) of the Fuwang deposit. The different signatures indicate different sources of ore-forming material. Rb–Sr isochron age (68 ± 6 Ma) and ⁴⁰Ar–³⁹Ar age (64.3 ± 0.1 Ma) of the ore-related quartz veins from the Ag deposit indicate that the Fuwang deposit formed during the Cenozoic Himalayan tectonomagmatic event. Crosscutting relationships suggests that Au-ore predates Ag-ore. The adjacent Changkeng and Fuwang deposits could, however, represent a single evolved hydrothermal system. The ore fluids initially deposited Au in the brecciated siliceous rocks, and then mixing with the magmatic water resulted in Ag deposition within fracture zones in the limestone. The deposits are alternatively the product of the superposition of two different geological events. Age evidence for the Fuwang deposit, together with the Xiqiaoshan Tertiary volcanic-hosted Ag deposit in the same area, indicates that the Pacific Coastal Volcanic Belt in the South China Fold Belt has greater potential for Himalayan precious metal mineralization than previous realized.  相似文献   

基于3DEC的岩质边坡安全系数影响因素敏感性研究          下载免费PDF全文

臧浩  陈鹏  赵盾  董玉芬 《山东国土资源》2021,37(8)

为研究岩质边坡中结构面几何参数及力学参数对边坡安全稳定性的影响,文中采用离散元软件3DEC进行数值模拟试验;以安全系数为指标,结合响应面分析法,研究边坡结构面几何参数倾向、倾角及力学参数法向刚度(Kn)、切向刚度(Ks)、粘聚力(c)、内摩擦角(φ)对影响边坡稳定性敏感程度;结果显示,结构面的几何参数是边坡的稳定性的前提条件,在具备滑塌条件的情况下,结构面的力学参数,将进一步影响边坡的稳定性;其中结构面的切向刚度和内摩擦角对边坡稳定性有高敏感度,按照敏感度由大到小排序,为切向刚度内摩擦角粘聚力法向刚度;同时发现内摩擦角和切向刚度与边坡安全性因素之间呈相互促进作用。  相似文献   

A Fourteen-Year Climatology of the Southwest Vortex in Summer   总被引：4，自引：0，他引：4       下载免费PDF全文

FU Shen-Ming  ZHANG Jing-Ping  SUN Jian-Hua  SHEN Xin-Yong 《大气和海洋科学快报》2014,7(6):510-514

Statistical studies were conducted on the southwest vortex（SWV） during the summers of 2000–13 using high-resolution reanalysis data with a horizontal resolution of 0.5°× 0.5°. A total of 578 SWVs were detected, with a maximum interannual frequency of 55. The variation of the interannual frequency featured a period of around six years. The most active period of SWVs was early July and the maximum occurrence of SWVs appeared in early morning（0200–0800 Beijing Standard Time（BST））. Most of the SWVs were short-lived, with only 66 cases（11.4%） lasting for more than 24 h. In addition, the moving tracks and three-dimensional shape of long-lived（≥ 36 h） SWVs are also presented. For those SWVs that lasted for more than 12 h, four types of SWVs（Types I–IV） were identified using a new method, and the results indicated that the dynamical and thermodynamical conditions before the formation of SWVs are effective indicators of the subsequent evolution of the vortex and associated severe weathers. Moreover, a further level of classification was also constructed for Type II SWVs, which accounted for the largest proportion out of Types I–IV, and the results indicated that the lifespan, radius and maximum 6-h precipitation were all closely related to the intensity of precipitation before the formation of SWVs.  相似文献   

三峡水库巴东库段地震成因机制研究     

王墩  王秋良  李井冈  袁丽 《大地测量与地球动力学》2007,27(Z1):32-34

震源机制解表明：长江三峡水库巴东库段地震的发震应力是由库水荷载作用造成的。进一步分析认为，地震可能是库岸区浅地表岩层在库水荷载为主的水岩耦合作用下沿易滑结构面滑动的结果。  相似文献   

淮南丁集矿地表移动和变形规律分析     

王帅  吴盾  刘桂建 《中国煤炭地质》2013,25(2):48-51,59

淮南丁集矿井1262(1)工作面为该矿-826m水平西一采区首采工作面,地质条件特殊(如深厚松散含水层和大采深),且地表移动变形规律研究得较少。因此,为了研究该矿地表移动变形规律,在1262(1)工作面建立地表移动观测站。以实测数据为基础,结合概率积分法获得了在该地质采矿条件下地表移动的相关参数。结果表明:地表下沉系数为1.16;起动距为1/7～1/6倍的平均采深;超前影响距为380m。在此基础上,计算出该矿的地表最大下沉速度及最大下沉速度滞后角分别为Vmax=21.9 mm/d和φ后=77.2°,表明在该地质采矿条件下,该矿的地表移动剧烈、地表下沉速度较快、起动距偏小等特点。在对综合移动角理论公式推导的基础上,获得了矿区综合移动角的误差值,并得出了矿区综合移动角经验值,对指导矿山开采具有一定的实际意义。  相似文献   

卫星信号仿真电离层闪烁模型研究   总被引：1，自引：0，他引：1  

冯健  刘钝  甄卫民 《全球定位系统》2013,38(3)

电离层闪烁会导致地空无线电信号产生随机起伏,影响各种地空信息系统的工作性能.为了满足电离层闪烁影响效应评估的应用需求,建立了一个卫星信号电离层闪烁模型.该模型是在对闪烁信号衰落特性进行统计分析的基础上建立的,它将信道函数分为直接分量和随机多径成分两部分.模型可根据输入的电离层闪烁指数和去相关时间仿真出信号振幅和相位的变化,并可直接嵌入到各类卫星信号模拟器中,用于卫星导航、卫星通信等系统的衰落信道仿真.  相似文献   

A Multi‐Grid Method of High Accuracy Surface Modeling and Its Validation     

Tian‐Xiang Yue  Na Zhao  Hai Yang  Yin‐Jun Song  Zheng‐Ping Du  Ze‐Meng Fan  Dun‐Jiang Song 《Transactions in GIS》2013,17(6):943-952

A method of high accuracy surface modeling (HASM) has been constructed to find a solution for error problems that had long troubled surface modeling in geographical information systems (GIS). It is found that when a preconditioned conjugate gradient (PCG) algorithm is used to solve the large sparse linear system, which HASM can be transferred into, HASM performs best in terms of simulation compared with all other algorithms. But its computing speed is not fast enough for all applications. A multi‐grid method is introduced into HASM to try to shorten its computing time. Both numerical and real‐world tests demonstrate that there is a range of stop error (SE). The multi‐grid method of HASM (HASM‐MG) greatly increases computing speed when SEs are within this range, compared with the PCG algorithm of HASM (HASM‐PCG). HASM‐MG is suitable for applications with a need for less accuracy and a shorter computing time. HASM‐PCG is appropriate for issues needing higher accuracy. HASM‐MG performs better than HASM‐PCG in flat areas, while HASM‐PCG does better in complex terrainm in terms of accuracy and computing time.  相似文献   

海蜇(Rhopilema esculenta)浮浪幼虫及早期螅状体摄食行为的研究     

刘春胜  邹安革  庄志猛  陈四清  王相杰  王绍军  燕敬平  李旭  刘长琳 《海洋与湖沼》2012,43(3):545-549

采用对比实验与显微观察的方法,对海蜇浮浪幼虫及早期螅状体的摄食行为进行了研究。结果表明,海蜇浮浪幼虫期不摄食外界食物;浮浪幼虫附着变态发育成海蜇螅状体1d后,开始摄食其它浮浪幼虫,螅状体发育到第3天摄食能力迅速增强,能够捕食卤虫无节幼体。海蜇早期螅状体的捕食实验结果表明,早期螅状体开始捕食主要受两方面影响,一方面是口的发育,另一方面是刺细胞的发育。  相似文献   

斜坡浅埋水平条形锚板抗拔承载力的极限分析          下载免费PDF全文

黄明华  李盾  李嘉成 《水文地质工程地质》2019,(1):116-116

针对山区和丘陵等复杂地形下浅埋锚板抗拔承载力计算问题,基于极限分析上限定理、非线性Mohr-Coulomb强度准则及其关联流动法则,构造了斜坡浅埋水平条形锚板的曲线型破裂机制和机动许可速度场,采用变分极值原理获得了其上方土体破裂面方程和抗拔承载力的上限解,分析了斜坡倾角和锚板埋深对锚板抗拔承载力的影响。结果表明:随着斜坡倾角的增大,锚板抗拔承载力逐渐减小,此时其上方两侧土体破裂面不再对称且整体向下坡侧偏移;锚板抗拔承载力及其上方两侧土体破裂面宽度均随着埋深增大而增加;锚板埋深越小,斜坡倾角对其抗拔承载力的影响越大,应在计算中予以考虑,以更合理地反映斜坡浅埋水平条形锚板的抗拔承载特性。  相似文献