GPS卫星伪广播星历技术研究

通过GPS广播星历求出一个时间段内间隔一定时间的离散卫星三维坐标,以这些卫星坐标序列为已知数据反求星历参数的方法,论述和验证了当卫星坐标发生旋转变化时,解算得到的相应地面点坐标的旋转矩阵与卫星坐标发生旋转变化的矩阵具有相同的值。这对于实现GPS加密具有很大的意义。     

安丘台定点形变监测与地震活动性的相关性分析

应用安丘台跨断层定点形变的水准观测资料进行一般多项式曲线分段拟合,结合周边的地震活动背景．研究断层活动与地震活动之间的关系。结果表明,断层活动和周边的地震活动在频度上存在对应关系。可利用断层活动与地震活动的对应关系,为台站周边地区的地震预报提供参考指标。     

Numerical modelling of stream–aquifer interaction: Quantifying the impact of transient streambed permeability and aquifer heterogeneity

Stream–aquifer interaction plays a vital role in the water cycle, and a proper study of this interaction is needed for understanding groundwater recharge, contaminants migration, and for managing surface water and groundwater resources. A model‐based investigation of a field experiment in a riparian zone of the Schwarzbach river, a tributary of the Rhine River in Germany, was conducted to understand stream–aquifer interaction under alternative gaining and losing streamflow conditions. An equivalent streambed permeability, estimated by inverting aquifer responses to flood waves, shows that streambed permeability increased during infiltration of stream water to aquifer and decreased during exfiltration. Aquifer permeability realizations generated by multiple‐point geostatistics exhibit a high degree of heterogeneity and anisotropy. A coupled surface water groundwater flow model was developed incorporating the time‐varying streambed permeability and heterogeneous aquifer permeability realizations. The model was able to reproduce varying pressure heads at two observation wells near the stream over a period of 55 days. A Monte Carlo analysis was also carried out to simulate groundwater flow, its age distribution, and the release of a hypothetical wastewater plume into the aquifer from the stream. Results of this uncertainty analysis suggest (a) stream–aquifer exchange flux during the infiltration periods was constrained by aquifer permeability; (b) during exfiltration, this flux was constrained by the reduced streambed permeability; (c) the effect of temporally variable streambed permeability and aquifer heterogeneity were found important to improve the accurate capture of the uncertainty; and (d) probabilistic infiltration paths in the aquifer reveal that such pathways and the associated prediction of the extent of the contaminant plume are highly dependent on aquifer heterogeneity.     

基于点面关系构建的线基元点云配准算法

针对传统的点特征点云配准算法不能解决缺失同名点的配准问题,从点在平面上的几何关系出发,利用具有较强几何约束能力的直线特征,推导出基于单位四元数表征的无需同名直线端点完全对应的点云配准模型。结果表明,该模型不仅能够同步求解配准参数,还适用于大旋转角的配准问题,同时降低了配准模型对参数初值的要求,增强了配准模型的稳定性和实用性。     

天球参考架零点的测定（Ⅱ）－小行星可观测弧段长度

全轨道均匀分布的小行星观测对天球参考架零点的测定，以及其它一些相关课题的研究非常有利。本文就低纬子午环的观测能力，计算分析了小行星在全轨道观测的星等范围和弧段分布，给出了可观测弧段长度的计算公式，并进行了模拟计算。     

天球参考架零点的测定（Ⅰ）－观测对象和观测方法的分析

本文叙述了测定天球参考架零点位置的意义和途径，通过比较，认为小行星是最合适的观测对象，并且在分析了过去用小行星观测测定天球参考架零点位置的误差较大的原因后，提出了用低纬子午环高精度地测定小行星瞬时位置的观测方法。     

渐近非扩张映象多步迭代序列的收敛性

研究了凸度量空间中用多步迭代序列来逼近渐近非扩张映象的不动点,并给出了其收敛于不动点的充分必要条件.     

宇宙弦和星系两点相关函数

本文对宇宙弦模型中的星系两点相关函数ξ进行了计算,并同Davis和Peebles的观测结果进行了比较,发现宇宙弦模型能较好地解释ξ的观测曲线。一个有意义的结果是我们利用宇宙弦图象自然地给出了其他宇宙模型难以给出的r_c≈3Mpch~(-1)处从1+ξ∝r~(-2)幂律到1+ξ∝r~(-0.85)幂律的转变点。