Two quantum oscillators coupled with a planar radio frequency ion trap     

陈亮  高克林 《海洋学报(英文版)》2010,29(11)

In this scheme, two quantum oscillators in a planar radio frequency ion trap are coupled by the trap electrodes. The ions motional states encode the quantum bits (qubits), and a swap gate could be achieved. Under different conditions of the experiments, the intensity of the coupling between two quantum oscillators and the dissipation of the system are calculated. We compute fidelities for a quantum swap gate and discuss experimental issues.  相似文献   

美国阿拉斯加异性石研究     

谢意红 《岩矿测试》2009,28(4):361-363

对产于美国阿拉斯加的异性石的物理特性及化学成分进行分析。该异性石呈深红色,为一轴晶正光性;其紫外可见吸收光谱在530nm处有明显的吸收带,在917nm处有较弱的吸收带;穆斯堡尔谱及参数与俄罗斯科拉半岛深红色异性石和辽宁凤城深玫瑰色异性石相近;红外光谱特征与正光性异性石相似。探讨了该异性石的致色机理,认为其颜色主要与Fe2+有关,且异性石中的Fe2+主要以平面四配位存在。  相似文献   

一种基于平面不等式约束法的北斗三频数据组合选取方法     

张建龙  丰勇  隋心 《测绘工程》2017,26(3)

GNSS现代化的标志之一是三频或多频数据的广泛使用,文中在研究北斗三频数据组合原理、优化选取准则的基础上,推导出一种基于平面不等式约束法的三频数据组合选取方法。该方法将长波长条件转化为组合系数的线性关系,将弱电离层条件转化为平面域,将低噪声条件转化为椭圆域,依此建立模型并给出模型的几何解释,最后应用该方法选取特性较优的北斗三频数据组合,并总结了一些组合系数的特点。结果证明,该方法组合系数选取效率大于枚举法等常规方法,从而为多频数据组合理论的研究提供参考。  相似文献   

平面拓扑模型的多边形矢量更新算法     

崇素文  王庆  王慧青 《测绘科学》2016,41(1):170-174

为了提高土地利用变更图斑的更新效率,文章提出了一种平面拓扑图模型下的多边形矢量数据更新算法:采用平面拓扑图的数据结构,实现多边形几何对象间的线段求交计算,解决多边形间在重点和重边情况下的几何裁剪问题;通过对底图几何对象与变更几何对象之间拓扑关系的判别,不仅能够检测出矢量底图数据中发生变化的几何信息,而且可以减少几何运算的次数,提升矢量数据的更新效率。实验结果表明该算法具有良好的适用性及较高的更新效率。  相似文献   

高喜马拉雅普兰地区东西向韧性拆离作用及其构造意义   总被引：3，自引：0，他引：3       下载免费PDF全文

戚学祥许志琴  史仁灯陈方远 《中国地质》2006,33(2):291-298

高喜马拉雅地体西部普兰地区东西向面状韧性拆离作用发育,韧性拆离带内的岩石都经历了不同程度的塑性变形,糜棱岩化作用普遍存在,面理向东缓倾,拉伸线理向东倾伏,倾伏角5～18°.不对称旋转应变构造指示韧性拆离带具有早期自西向东的运动性质,及后期又经历了自东向西脆韧性变形的特点.EBSD组构测定结果反映糜棱岩中变形石英的晶格优选方位具有自西向东的高温柱面{10 -10}《a》、中温菱面{10-1 -1}《a》和自东往西的中温菱面{10-1 -1}《a》、低温底面{0001}《a》两组滑移系,结合糜棱岩中普遍存在的不对称旋转构造特点分析说明构造带早期自西向东韧性拆离作用形成于中高温环境,后期自东向西的脆韧性变形形成于中低温环境.锆石SHRIMP U-Pb定年结果表明普兰地区高喜马拉雅变质基底原岩形成于1863Ma.普兰东西向韧性拆离作用形成于中新世,与高喜马拉雅地体南北两侧的MCT和STDS形成时代相吻合,是印度板块向北俯冲产生的挤压应力作用于弧形喜马拉雅造山带时,分解出平行于造山带方向的剪切应力促使造山带内中下地壳的物质沿平行于造山带方向发生塑性流动形成的,是与MCT和STDS在同一构造事件中同一构造应力场内形成的,是青藏高原大规模南北向缩短、隆升和一部分物质向东逃逸的产物.  相似文献   

Dynamic rupture on a planar fault in three-dimensional half-space – II. Validations and numerical experiments     

Haiming Zhang  Xiaofei Chen 《Geophysical Journal International》2006,167(2):917-932

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Superposed folding in the Honakere arm of the Chitradurga-Karighatta schist belt in the Dharwar tectonic province,southern India,and its bearing on the Sargur-Dharwar relation     

K. Naha  A. Rai Choudhuri  V. Ranjan  R. Srinivasan 《Journal of Earth System Science》1995,104(3):327-347

The supracrustal enclave within the Peninsular Gneiss in the Honakere arm of the Chitradurga-Karighatta belt comprises tremolite-chlorite schists within which occur two bands of quartzite coalescing east of Jakkanahalli(12°39′N; 76°41′E), with an amphibolite band in the core. Very tight to isoclinal mesoscopic folds on compositional bands cut across in the hinge zones by an axial planar schistosity, and the nearly orthogonal relation between compositional bands and this schistosity at the termination of the tremolite-chlorite schist band near Javanahalli, points to the presence of a hinge of a large-scale, isoclinal early fold (F₁). That the map pattern, with an NNE-plunging upright antiform and a complementary synform of macroscopic scale, traces folds 'er generation (F ₂),is proved by the varying attitude of both compositional bands (S₀) and axial pranar schistosity (S ₁), which are effectively parallel in a major part of the area. A crenulation cleavage (S ₂) has developed parallel to the axial planes of theF ₂ folds at places. TheF ₂ folds range usually from open to rarely isoclinal style, with theF ₁ andF ₂ axes nearly parallel. Evidence of type 3 fold interference is also provided by the map pattern of a quartzite band in the Borikoppalu area to the north, coupled with younging directions from current bedding andS ₀ -S ₁ inter-relation. Although statistically theF ₁ andF ₂ linear structures have the same orientation, detailed studies of outcrops and hand specimens indicate that the two may make as high an angle as 90°. Usually, in these instances, theF ₁ lineations are unreliable around theF ₂ axes, implying that theF ₂ folding was by flexural slip. In zones with very tight to almost isoclinalF ₂ folding, however, buckling attendant with flattening has caused a spread of theF ₁ lineations almost in a plane. Initial divergence in orientation of theF ₁ lineations due to extreme flattening duringF ₁ folding has also resulted in a variation in the angle between theF ₁ andF ₂lineations in some instances. Upright later folding (F₃) with nearly E-W strike of axial planes has led to warps on schistosity, plunge reversals of theF ₁ andF ₂ axes, and increase in the angle between theF ₁ andF ₂ lineations at some places. Large-scale mapping in the Borikoppalu sector, where the supposed Sargur rocks with ENE ‘trend’ abut against the N-‘trending’ rocks of the Dharwar Supergroup, shows a continuity of rock formations and structures across the hinge of a large-scaleF ₂ fold. This observation renders the notion, that there is an angular unconformity here between the rocks of the Sargur Group and the Dharwar Supergroup, untenable.  相似文献   

Vectorial Formulation of Direction Cosines for Anisotropic Geologic Structures from Their Geologic Angle Measurements     

Jun-Mo Kim 《Mathematical Geology》2005,37(8):929-941

On the basis of vectorial formulation, a series of relatively simple closed-form mathematical equations is presented to determine the direction cosines of the local coordinate axes associated with planar and linear structures in an anisotropic geologic material from their geologic angle measurements (i.e., strike and dip for planar structures and trend and plunge for linear structures). The equations are then applied to calculation of global anisotropic hydraulic conductivity and elastic stiffness tensors with respect to the geographical coordinate axes from their local counterparts with respect to the material symmetry axes.  相似文献   

Point Mass Method Applied to the Regional Gravimetric Determination of the Geoid   总被引：1，自引：0，他引：1  

Antunes  C.  Pail  R.  Catalão  J. 《Studia Geophysica et Geodaetica》2003,47(3):495-509

The determination of the local gravity field by means of the point mass inversion method can be performed as an alternative to conventional numerical methods, such as the least-squares collocation. Based on the first derivative of the inverse-distance Newtonian potential for the representation of the gravity anomaly data, it is possible to compute any wavelength component of the geoid in planar approximation with sufficient accuracy. In order to exemplify the theoretical concept, two applications are presented of the computation of two different wavelength components of the geoid, the long wavelength component in a local solution and the short wavelength component in a regional solution. The results are compared with corresponding least-squares collocation solutions, using a global geopotential model to remove and to restore the long wavelength component.  相似文献   

幔羽现象与地震电磁流体效应的可能联系——电磁流体效应和平面电流模型   总被引：4，自引：1，他引：4  

曾小苹  刘正彦  林云芳  王吉易  续春荣 《地学前缘》2001,8(2):253-258

综合分析了 2 0世纪 70年代以来发生在中国的 14个强震前地磁和地下流体参量动态图像的时空演化特征 ,发现强震前这些参量均呈现十分明显的异常图形。这些图像十分复杂 ,且随时间不断变化 ,并与孕震过程有某种时空规律性联系。 90年代地学家通过地震资料分析发现了幔羽现象。笔者设想核幔边界的幔羽磁流体物质上涌是地震电磁流体效应的一种可能成因。幔羽中的流体物质螺旋上涌至地壳的底部 ,并形成“蘑菇云”。流体在地壳中扩展或挤压 ,形成异常电流 ,可将其看作在孕震区地下 10 2 0km深处有一等效平面电流。再考虑到近地表的电磁环境———电离层电流体系的局部异常 ,计算了一个地下和电离层组成的等效平面电流模型在地面产生的磁场分布 ,结果与强震前地球磁场的零等变型异常动态图像较吻合。  相似文献