CSS集群技术在地震核心网中的应用     

常俊  李瑞华 《震灾防御技术》2015,10(3):664-672

随着网络虚拟化技术的发展,以及地震系统业务内容的扩展,原地震行业网络核心层从性能上已逐渐难以满足需求。为保障网络可靠高效运转,同时为满足地震行业网络零中断的需求,利用新一代CSS交换机集群技术,采用中间设备临时接管的方法,对地震核心网进行了平滑改造升级,通过升级简化了网络结构,提高了网络效能。  相似文献   

Variations of the alpine precipitation from an ice core record of the Laohugou glacier basin during 1960-2006 in western Qilian Mountains,China     

Xiang QIN  Xiaoqing CUI  Wentao DU  Zhiwen DONG  Jiawen REN  Jizu CHEN 《地理学报(英文版)》2015,25(2):165-176

The net accumulation record of ice core is one of the most reliable indicators for reconstructing precipitation changes in high mountains. A 20.12 m ice core was drilled in 2006 from the accumulation zone of Laohugou Glacier No.12 in the northeastern Tibetan Plateau, China. We obtained the precipitation from the ice core net accumulation during 1960-2006, and found out the relationship between Laohugou ice core record and other data from surrounding sites of the northeastern Tibetan Plateau. Results showed that during 1960-2006, the precipitation in the high mountains showed firstly an increasing trend, while during 1980 to 2006 it showed an obvious decreasing trend. Reconstructed precipitation change in the Laohugou glacier basin was consistent with the measured data from the nearby weather stations in the lower mountain of Subei, and the correlation coefficient was 0.619 (P<0.001). However, the precipitation in the high mountain was about 3 times more than that of the lower mountain. The precipitation in Laohugou Glacier No.12 of the western Qilian Mountains corresponded well to the net accumulation of Dunde ice core during the same period, tree-ring reconstructed precipitation, the measured data of multiple meteorological stations in the northeastern Tibetan Plateau, and also the changes of adjacent PDSI drought index. Precipitation changes of the Laohugou glacier basin and other sites of the northeastern Tibetan Plateau had significantly positive correlation with ENSO, which implied that the regional alpine precipitation change was very likely to be influenced by ENSO.  相似文献   

基于ISSR分子标记数据的兰州百合核心种质构建方法研究     

李谋强  师桂英  叶树辉  黄彦玮  边小荣 《中国沙漠》2015,35(6):1573-1578

利用ISSR分析获得的数据,研究了依据Nei & Li、SM和Jaccard遗传距离,采用UPGMA聚类法进行逐步聚类筛选核心种质的效果,并最终采用SM遗传距离逐步聚类从175份兰州百合种质中筛选出了37份核心种质。保留了初始种质21.14%的样品,多态性位点数、多态性位点百分率、Nei's遗传多样性指数和Shannon's信息指数的保留率分别为96.08%、96.59%、105.27%、103.62%,t检验表明核心种质的Nei's遗传多样性指数和Shannon's信息指数与原种质没有显著差异,表明构建的核心种质能很好的代表原始种质的遗传多样性。  相似文献   

Fluctuational mechanism for the formation of proton vortices in the superfluid core of neutron stars     

K. M. Shahabasyan  M. K. Shahabasyan 《Astrophysics》2008,51(1):112-120

The Gibbs thermodynamic potential of a proton vortex interacting with the normal core of a neutron vortex of radius r << λ (λ is the penetration depth) that is parallel to it and has an outer boundary of radius b is calculated. It is shown that, under this assumption, the capture of only one vortex by the core is energetically favorable. The force acting on the proton vortex owing to the entrained current is found and it is always directed toward the core. The corresponding force for a proton antivortex is directed toward the outer boundary of the neutron vortex. The Ginzburg-Landau equation is solved for a vortex-antivortex system and its Gibbs function is calculated. It is shown that at large distances from the core, vortex-antivortex pairs can form because of fluctuations. Acted on by the entrainment current, the antivortex moves outward, while the vortex stays inside the neutron vortex. It is shown that the best conditions for fluctuational pair production, followed by separation, exist near the outer boundary. It is shown that new proton vortices can develop only in a region where the entrainment magnetic field strength H (ρ) > H_C1 (H_C1 is the lower critical field). __________ Translated from Astrofizika, Vol. 51, No. 1, pp. 139–149 (February 2008).  相似文献   

南黄海CSDP-2井晚泥盆世早期真蕨类Shougangia的形态观察     

白姣  徐洪河  郭兴伟  卢辉楠 《吉林大学学报(地球科学版)》2019,49(1):65-73

南黄海CSDP-2钻井上泥盆统五通组擂鼓台段2 068.00~2 069.02 m段岩心识别出了早期真蕨类植物。该植物具有至少三次羽状复叶,末二次羽片互生,小羽片扁平,呈扇状、楔状或舌状,基部收缩,至少一次深裂,裂片边缘钝圆,二分叉的叶脉明显。据此,可鉴定为优美守刚蕨（比较种）（Shougangia cf.S.bella）。本研究为南黄海地区上泥盆统五通组增加了古植物学新资料。  相似文献   

中下部地壳拆离断层带演化中的褶皱作用:以辽南变质核杂岩为例     

郑媛媛  张若愚  甘浩男  李弘珂  蒋浩  张雎易  刘俊来 《地学前缘》2019,26(2):58-71

作为变质核杂岩构造的重要组成部分,拆离断层带内广泛发育的褶皱构造与其寄主岩石一样记录了中下地壳拆离作用过程。选取辽南变质核杂岩金州拆离断层带内褶皱构造作为研究对象,基于叶理与褶皱构造关系分析,划分了褶皱期次与阶段性;通过形态组构分析、结晶学组构分析及石英古温度计等技术方法的应用,初步分析了拆离断层内褶皱的形成机制,为辽南地区拆离作用过程提供约束。根据褶皱形成与拆离作用的时间关系,将拆离带内褶皱分为拆离前褶皱、拆离同期褶皱和拆离后褶皱;拆离作用同期的褶皱按时间早晚分为早期(a1)阶段、中期(a2)阶段、晚期(a3)阶段。不同阶段褶皱的野外形态、叶理与褶皱关系等方面的差异,以及形态组构与结晶学组构的特征,为判断和恢复褶皱的形成机制提供了佐证,揭示出拆离断层带褶皱是在纵弯压扁和顺层流变的共同作用下递进剪切变形的产物。在拆离作用过程中, a1阶段和a2阶段褶皱以纵弯、压扁褶皱作用为主,a3阶段褶皱以弯滑作用为主。褶皱作用记录了拆离断层一定温度范围内(主要集中在380~500 ℃)的变形特征,拆离作用从早期到晚期的演化整体处于相对稳定的应变状态下。对金州拆离断层带而言,在区域NW-SE向伸展过程中,还伴随着NE-SW向微弱的收缩。  相似文献   

深海底钻机动力头的钻杆自行抛弃和冲击卸扣机构          下载免费PDF全文

魏治利  钟路  谢振权  臧龙  彭莹 《探矿工程》2017,44(10):84-87,83

文章介绍了深海岩心取样钻机的主要部件动力头的结构及特点。根据深海钻进的特殊情况,专门在动力头上设计了钻杆自行抛弃机构和冲击卸扣机构。这两种机构可在发生卡钻事故钻机无法回收已经深入孔内的钻杆串时,可将其自行抛弃,或由于动力头扭矩液压马达出现故障不能拧卸钻杆时,冲击卸扣机构将对钻杆丝扣进行冲击使其松动而卸扣。文章重点介绍了钻杆自行抛弃机构和冲击卸扣机构的结构及工作原理。  相似文献   

塔里木盆地塔河油田奥陶系数字岩心图像中生物扰动的定量表征^*   总被引：1，自引：0，他引：1       下载免费PDF全文

牛永斌  崔胜利  胡亚洲  钟建华  王培俊 《古地理学报》2017,19(2):353-363

生物扰动对塔里木盆地塔河油田奥陶系碳酸盐岩“基质储集体”储集性能的改造效应具有重要影响。以塔河油田奥陶系岩心为研究对象,利用Adobe^® Photoshop^® CS6软件提供的生物扰动数字图像分析软件包,对岩心数字图像中生物扰动区域进行了识别和定量表征。结果表明: (1)在生物扰动数字图像分析软件包提供的方法中,“相似像素选择法”和“魔棒法”是对生物扰动识别与定量表征最为有效的方法,但二者适用范围不同;(2)“相似像素选择法”适用于生物扰动程度较大,单个形体相对较小且离散度相对较高的情况:当生物扰动充填物和围岩基质边界对比度较大时,应用“选取相似”操作效果最好;而当生物扰动充填物和围岩基质边界对比度较小时,应用“色彩范围”操作识别效果最好;这2种操作都仅能执行1次;(3)“魔棒法”对于识别生物扰动区域形体大而分布连续,且充填物颜色不同的情况具有独到优势;该方法可以通过多次重复操作以及调整“容差”来提高生物扰动区域与围岩基质的识别度。该研究对从生物成因角度解释碳酸盐岩“基质储集体”的非均质性与分布规律、实现增强储集性能生物扰动属性表征、丰富海相碳酸盐岩储集层地质学理论、指导该类油气藏远景勘探和储量计算以及选择合理的开发方案等具有重要意义。  相似文献   

The Pelona–Orocopia–Rand and related schists of southern California: a review of the best-known archive of shallow subduction on the planet     

Alan D. Chapman 《International Geology Review》2017,59(5-6):664-701

ABSTRACT

The Pelona–Orocopia–Rand and related schists of southern California are an archetypal example of an exhumed shallow subduction complex. ‘The schist’ comprises mainly trench materials underthust beneath continental arc rocks during Late Cretaceous–early Cenozoic collision of one or more oceanic plateaux with southern California. The arc-on-trench relationship, without intervening mantle or lowermost crust, implies that significant subduction erosion accompanied shallow subduction. Upsection increases in metamorphic grade (~150 ± 100°C/km) and spatial variations in age and peak temperature provide an ~50 million year long record of tectonic underplating within a cooling system. Evidence for palaeoseismic events in earliest formed and hottest (locally transitional granulite grade) schists provides a possible field-based record of episodic tremor and slow slip events such as detected in several modern shallow subduction zones. Structural ascent of the schist was achieved in distinct Late Cretaceous–early Eocene and late Oligocene–early Miocene extensional pulses, the first during collapse of gravitationally unstable upper plate assemblages and accompanied by trench-directed (top-NE) lower plate extrusion and the second corresponding temporally, spatially, and in character with core complex formation in the SW United States. The line between schist and core complex belts is blurred by the recent discovery of schist within 40 km of the nearest core complex and containing synkinematic Miocene intrusions, a hallmark of SW U.S. core complexes. The history of schist assembly, metamorphism, and exhumation provides the most complete field-based record of thermo-mechanical processes, subduction erosion and tectonic underplating in particular, that operated during a shallow subduction event. Future cross-disciplinary investigations of, and comparisons between, the schist and other possible ancient (e.g. Swakane gneiss, Sanbagawa belt, Qiangtang terrane) and modern (e.g. Cascadia, SW Japan, central Mexico, Chile) shallow subduction zones will yield new insights into the tectonic and petrologic processes that operate within such systems.  相似文献   

绳索取心复合钻柱的动力学行为研究   总被引：1，自引：1，他引：0       下载免费PDF全文

梁健  郭宝科  王志刚  孙建华  李鑫淼  尹浩 《探矿工程》2017,44(7):34-40

绳索取心复合钻柱在岩心钻探“满眼钻进”过程中,钻杆易出现不同程度的划痕、压痕及磨痕等情况。本文利用非线性有限元方法,采用三维管单元对绳索取心复合钻柱拉压两处截面的涡动轨迹、涡动速度、横向振动、纵向振动规律进行了分析。结果表明：转速的增加和钻压的增大会显著增加钻柱与井壁的碰撞次数;在相同钻压条件下,随着钻柱回转速度的增大,钻柱与井壁的碰撞机率增加、接触轨迹增长,致使钻柱与孔壁的滑动摩擦机会增多;钻柱的涡动速度均值将随钻压和转速的增加而增大,转速大于钻压的影响;转速的增加则会加大钻柱的横向振荡频率,钻压的增大会增加钻柱横截面的纵向振荡幅值。  相似文献