GPS接收机测试评估系统数据库的建立

为评定GPS接收机的性能,建立的接收机测试评估系统在对接收机进行测试的过程中将涉及到大量的测试相关数据。为了对这些数据进行科学、安全的存储管理,文中通过分析数据的来源、数据的存储类型以及数据的相互关系等,在考虑了数据库运行的安全性和稳定性的基础上,详细地介绍了GPS接收机测试评估系统数据库的建立。     

基于粗细网格的有限元并行分析方法

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。探讨了粗细网格与预处理共轭梯度法结合的并行有限元算法。从多重网格刚度矩阵推得有效的预处理子。该算法在工作站机群上实现。用地基处理时土体强夯的数值模拟分析进行了数值测试,对其并行性能进行了详细分析。计算结果表明：该算法具有良好的并行加速比和效率,是一种有效的并行算法。     

Transition from platemargin to intraplate environment: Geochemistry of basalts in Paleogene Liaohe basin,northeastern China

Mesozoic and Cenozoic volcanic rocks are widely distributed in the circum-Pacific area of eastern China. These rocks have long been genetically linked to westward subduction of the paleo-Pacific oceanic plate to the eastern Asia continent[1,2]. Research in re-cent years[3―6] has attained conclusions that a simple paleo-Pacific subduction model does not work well in interpreting all the volcanic rocks in eastern China, although some of them could be attributed to circum-Pacific interaction …     

国外OTA与传统旅游企业竞合关系研究综述

作为重要的在线营销渠道,OTA一直是传统旅游企业的重要合作伙伴之一。无论是OTA抢夺资源还是传统旅游企业对抗升级,双方之间的竞争趋势愈加明显。由此,相关方面的研究逐步增多。国外研究从OTA与饭店、航空公司等传统旅游企业合作、竞争和竞合平衡三个方面入手,主要围绕OTA与饭店的竞合问题展开。重视实证分析,采用数理统计和模型构建等定量研究方法,针对航空公司和饭店企业,从市场细分、定价、客房分配等角度提出实现双方竞合平衡的方案。建议今后加强对OTA和传统旅游企业合作模式变化的跟踪分析,关注OTA与景区、餐馆等旅游供应商的博弈关系。     

计算机地形分析中的多边形迭加问题

在计算机地形分析中,研究地形多要素迭加分析的关键是解决多边形的迭加问题。本文通过对多边形迭加的数学方法的研究,提出了适合计算机多要素分析的原理和方法。     

Characteristics of particle size for creeping and saltating sand grains in aeolian transport

Creep and saltation are the primary modes of surface transport involved in the fluid‐like movement of aeolian sands. Although numerous studies have focused on saltation, few studies have focused on creep, primarily because of the experimental difficulty and the limited amount of theoretical information available on this process. Grain size and its distribution characteristics are key controls on the modes of sand movement and their transport masses. Based on a series of wind tunnel experiments, this paper presents new data regarding the saltation flux, obtained using a flat sampler, and on the creeping mass, obtained using a specifically designed bed trap, associated with four friction velocities (0·41, 0·47, 0·55 and 0·61 m sec^?1). These data yielded information regarding creeping and saltating sand grains and their particle size characteristics at various heights, which led to the following conclusions: (i) the creeping masses increased as a power function (q = ?1·02 + 14·19u_*³) of friction wind velocities, with a correlation (R²) of 0·95; (ii) the flux of aeolian sand flow decreases exponentially with increasing height (q = a exp(–z/b)) and increases as a power function (q = ?26·30 + 428·40 u_*³) of the friction wind velocity; (iii) the particle size of creeping sand grains is ca 1·15 times of the mean diameter of salting sand grains at a height of 0 to 2 cm, which is 1·14 times of the mean diameter of sand grains in a bed; and (iv) the mean diameter of saltating sand grains decreases rapidly with increasing height whereas, while at a given height, the mean diameter of saltating sand grains is positively correlated with the friction wind velocity. Although these results require additional experimental validation, they provide new information for modelling of aeolian sand transport processes.     

1614年平遥—榆社间61／2级地震的讨论

通过对1614年平遥榆社间6(1/2)级地震的进一步研究,认为前人确定这次地震时所用的史料疑点较多,所确定的基本参数也问题较大.得出是两次地震事件的结论:一次是1614年10月15日(万历四十二年九月十三日),地点武乡,震级约为5(1/2)级;一次是1614年10月23日(万历四十二年九月二十一日),地点榆社,震级约5(3/4)级.     

Propagation of MHD body and surface waves in magnetically structured regions of the solar atmosphere

The fact that magnetically structured regions exist in the solar atmosphere has been known for a number of years. It has been suggested that different kinds of magnetohydrodynamic (MHD) waves can be efficiently damped in these regions and that the dissipated wave energy may be responsible for the observed enhancement in radiative losses. From a theoretical point of view, an important task would be to investigate the propagation and dissipation of MHD waves in these highly structured regions of the solar atmosphere. In this paper, we study the behavior of MHD body and surface waves in a medium with either a single or double (slab) magnetic interface by use of a nonlinear, two-dimensional, time-dependent, ideal MHD numerical model constructed on the basis of a Lagrangean grid and semi-implicit scheme. The processes of wave confinement and wave energy leakage are discussed in detail. It is shown that the obtained results depend strongly on the type of perturbations imposed on the interface or slab and on the plasma parameter, . The relevance of the obtained results to the heating problem of the upper parts of the solar atmosphere is also discussed.     

无线电波透视快速勘探技术及其应用

无线电波透视技术作为探测煤层工作面内地质构造的一种较为成熟方法,具有快速、轻便、透距大、成本低等优点,但也存在现场观测系统单一、耗时长、接收操作员劳动强度大等缺点。通过对无线电波透视技术现场观测系统的改进,提出"一发双收"数据采集方法及数据校正处理技术。由于"一发双收"的数据是由两个接收机同时接收,因此其数据必须经过校正才能使用。在数据采集中:一是要求两台接收机在一条测线同一地点的场强值差别很小;二是要求做到数据采集中至少存在一个重合接收点,且其重合点数据比值应在0.98～1.02范围内。"一发双收"数据使用无线电波透视CT软件系统处理软件进行拼接,若数据曲线出现阶梯跳跃,则应把低值(或者高值)乘以该重合点数据的比值以保证曲线平滑。在张集煤矿1114(3)工作面探测实践中,使用该技术探测画出其工作面存在三个主要异常区:1#异常区在退尺20~100m处为断层影响区;2#异常区退尺480~560m处为断层影响区;3#异常区在退尺1200~1300m处为断层和薄煤影响区。目前该工作面探测区已经回采,探测结果与实际回采验证结果比较吻合,说明一发双收的探测方式可行。     

广义相遇法的拓展

当地表不规则时,用广义相遇法求取的折射层速度存在较大误差,针对于此,这里提出了一种基于广义相遇法的广义相遇静校圆滑法。其步骤如下:①利用广义相遇法求出针对不同XY值的广义相遇速度解析值和时间深度值;②根据时间深度值求出"静校正量",然后从旅行时间中减去静校正量;③绘出广义相遇速度解析曲线,求出速度。其中的步骤②,是把所求的静校正量从旅行时间中减去,就是把地表的影响消除,所以得到的值基本不受地表的影响。对某一模型用此方法,取得了比较理想的效果,尤其是对于地表比较小范围的突然变化,有很明显的效果。实践证明,该方法极大地提高了传统广义相遇法求取折射层波速的精度。