基于改进人工蜂群算法的概率积分法参数反演

针对传统算法在反演概率积分法参数时易发散且难以获得全局最优解的问题,提出利用自适应人工蜂群算法反演概率积分法参数。根据该算法在求解过程中收敛速度快,获得全局最优解的特点,将参数反演问题转化为组合优化问题,建立了自适应人工蜂群算法的概率积分法预计参数反演流程,并将计算结果与实际值进行对比分析。通过理论分析与实验证明,自适应人工蜂群算法反演概率积分法参数精度高,较最小二乘法和模矢法拟合效果好,可应用于矿山开采沉陷预计。     

吉林省松花江流域产业系统与环境系统时空耦合特征

采用耦合协调模型对2001-2014年吉林省松花江流域产业系统与环境系统时空耦合特征进行了分析,并对两大系统耦合关系的影响因素进行研究。结果表明:流域产业-环境系统耦合度呈现"M"型曲线特征,具有明显的经济烙印。耦合发展度不断升高,流域产业系统对环境系统的胁迫作用不断降低,环境系统对于产业系统的支撑作用不断增强;产业-环境系统耦合度经历了流域特征明显到不明显的过程,且耦合发展度区域差距不断缩小反映了资源型城市产业-环境系统耦合状况趋佳,产业生态化得到一定程度发展;二三产业增加值总额和人均工业废水排放量是影响产业-环境系统耦合发展度的主要障碍指标,并且人均水资源量以及外商合同投资额/GDP的障碍作用愈加突出。另外产业结构与产业规模是影响产业-环境系统耦合发展度的主要障碍子系统,而产业效率与环境污染是潜在障碍子系统。     

Simulation of structural phase transition in NaNO3 and CaCO3

 The order-disorder phase transitions in NaNO₃ and CaCO₃ are simulated by molecular dynamics. The simulations are based on the potentials calculated from the Gordon–Kim modified electron gas formalism extended to molecular ions. We successfully reproduced the transition temperature T _c and the abnormally large c axis thermal expansion observed in experiment. The phase transitions in NaNO₃ and CaCO₃ were found to be initiated by ±60 and ±180° reorientation of the NO₃ and CO₃ ions about the c axis. The orientations of NO₃ and CO₃ ions are continuous with six preferred calcite-type orientations above the phase-transition temperature. Received: 30 January 2001 / Accepted: 11 May 2001     

共接收点倾斜叠加波动方程偏移

共接收点倾斜叠加波动方程偏移,本质上是一种叠前偏移方法.每给定一个斜率P,对经过叠前（动校正前）常规处理的地震记录中的各共接收点道集,沿直线t=τ+px进行倾斜叠加,就形成一个共接收点倾斜叠加剖面.对之进行波动方程偏移,该偏移剖面将代表地下真实构造.对一系列的p,我们可以得到一系列这样的偏移剖面.对它们作共接收点叠加,偏移叠加剖面的信噪比将超过水平叠加剖面.本文导出了在均匀、水平层状及非均匀介质条件下的共接收点倾斜叠加波动方程偏移算法.     

Genesis and Geological—Geochemical Characters of the ushan Gold Deposit,Shandong,China

The Rushan gold deposit, explored in recent years in the Jiaodong area, Shandong Province, is a quartz vein-type gold deposit hosted in granite. The temperature of its major mineralization episode is between 220°C and 280°C. The salinity of the ore-forming fluid is 5 % to 9% NaCl equivalent, with H₂O and CO₂ as the dominant gas constituents. The fluid is rich in Na⁺, Ca²⁺ and Cl⁻, but relatively impoverished in K⁺ and F⁻, characterized by either Ca²⁺ > Na⁺ > K⁺ (in three samples) or Na⁺ > Ca²⁺ > K⁺ (in six samples). Hydrogen and oxygen isotopes in the ore-forming fluid are highly variable with δ¹⁸ ranging between − 7.70‰ and 5. 97‰ and between − 128‰ and − 71‰. The possibility of lamprophyre serving as the source of gold can be excluded in view of its low gold content on the order of 2.5 × 10⁻⁹. Rb-Sr isochron ages of the deposit and the host Kunyushan granite are ( 104.8 ± 1.5) Ma and 134.6 Ma respectively with the respective initial Sr ratios of 0. 71307 and 0.7096. It is considered that the emplacement of the lamprophyre under a tensile environment had provided sufficient heat energy to facilitate deep circulation of meteoric water by which ore metals were extracted from the Kunyushan granite through long-term water-rock reaction. This project was financially supported by the National Natural Science Foundation of China.     

An Elastoplastic Model for Partially Saturated Collapsible Rocks

A unified elastoplastic model for describing the stress–strain behavior of partially saturated collapsible rocks is proposed. The elastic–plastic response due to loading and unloading is captured using bounding surface plasticity. The coupling effect of hydraulic and mechanical responses is addressed by applying the effective stress concept. Special attention is paid to the rock–fluid characteristic curve (RFCC), effective stress parameter, and suction hardening. A wide range of saturation degree is considered. The characteristics of mechanical behavior in partially saturated collapsible rocks are captured for all cases considered.     

未来百年夏季青藏高原臭氧变化趋势及可能机制

利用全大气气候通用模式(WACCM3)对政府间气候变化专门委员会排放情景特别报告中2001年到2099年A1B、A2、B1三种排放情景进行了模拟,分析了三种排放情景下青藏高原地区未来百年臭氧总量在夏季(6—8月)的变化趋势及引起该变化的可能机制。结果表明:在三种排放情景下未来百年夏季高原区臭氧总量均呈现增长趋势,其中A2情景下臭氧增长最快,B1情景下增长最慢,但相对于同纬度其他地区,高原区的臭氧总量增长较慢,即高原区臭氧谷加深。高原区高空污染物的减少以及局域Hadley环流的减弱是未来高原区臭氧总量增加的原因;而南亚高压的增强,以及与之相对应的辐散增强则可能是高原区臭氧谷继续加深的原因。     

粤东北仁差盆地早侏罗世花岗岩基底LA-ICP-MS锆石U-Pb年龄及其地质意义

钻探勘查揭露表明,粤东北仁差盆地基底主要由古生代变质岩和文象花岗岩组成。为进一步查明其基底岩体形成的时代,提高对该地区地质演化的认识,对盆地内2个勘查钻孔内的文象花岗岩岩心取样,进行LA-ICP-MS锆石U-Pb同位素定年,测得谐和年龄为179±1Ma和186Ma。此结果表明,仁差盆地基底文象花岗岩的形成时代为早侏罗世晚期,即其为燕山期第一幕岩浆活动的产物。此年龄不仅加深了对仁差盆地形成演化的认识,也为粤东北地区早侏罗世时期缺乏岩浆岩活动的报道提供了新的年代学资料。     

长螺旋钻机在粘性坚硬地层中的应用探讨

以许昌市三国大剧院桩基工程为例,从普通长螺旋钻机、液压动力头钻机、利用变频技术的高自重大扭矩动力头钻机在坚硬地层钻进中遇到的问题和应对措施等几方面,论述了各款型长螺旋钻机对地层的适应性,为以后类似工程施工选择施工机械提供参考。     

“煤铀兼探”找矿新思路在云南的初次应用——以滇西户撒盆地铀矿勘探为例

通过对滇西户撒盆地煤田资料二次开发利用,文章首次提出"潜在储铀层"的概念,即煤田等勘探钻孔测井资料中自然伽马值显示高于50γ(或3.5PA/kg或150API或12.6纳库(n·C)/Kg·小时)时所对应的砂岩、砾岩层,并筛查出主要赋存在新近系芒棒组一至三段的潜在储铀层40层。自然伽马异常等厚图与等值线图指示盆地北东部姐来-小寨地区、中部曼统-曼燕地区、南西部帕董-老汪寨地区可作为首选钻探验证靶区,验证孔当优先部署在以上区域。芒棒组一、二段因赋存的潜在储铀层数量多、伽马异常厚度较大、伽马异常值高,赋矿潜力大,可作为重点验证层位。