近50年来黄河流域400 mm等雨量线空间变化研究

以黄河流域及周边地区1 026个雨量（水文）站1956—2000年逐日降水过程资料为基础，以GIS技术为关键数据处理平台，建立等值线加权平均位置的定量化表征方法，采用时间序列分析技术，对黄河流域近50年来400 mm等雨量线的空间位移特征进行了系统揭示。1956—2000年间，黄河流域多年平均降雨量为454.62 mm；400 mm等雨量线加权平均位置坐标为（105°0′4″E，36°57′54″N）。整体上看，近50年来，黄河流域400 mm等雨量在纬向上的移动是典型的平稳随机序列过程；在经向上的移动尚不能满足平稳随机序列过程。趋势检验结果表明，黄河流域400 mm等雨量线有向东和向南发生移动的趋势，且向东移动的趋势显著。功率谱分析表明，黄河流域400 mm等雨量线在经向上发生迁移的显著周期为3年；在经向和纬向上均有7年和2年周期；同时，位移具有反向持久性。     

乡村旅游区选址问题研究 --以昆明市为例

和一般旅游区一样,乡村旅游区具有满足旅游者不同需求的功能要素,由多个乡村旅游园区组成。在对昆明市周边乡村旅游区调查的基础上,对乡村旅游区的选址问题进行了探讨。与依托城市的时空距离、乡村旅游地的整体经济水平、农村特色和自驾车旅游是乡村旅游发展的4个背景条件。乡村旅游区选址受宏观和微观两个层次因子的影响:依托城市的出游能力、乡村旅游区的交通区位、旅游区位是3个宏观因素,乡村旅游区的聚集与屏蔽、乡村园区的周边环境状况是两个微观因素。最后从政策因素和旅游者品位变化的角度提出了影响乡村旅游区选址问题的两点补充意见。     

区位能研究

区位、区位选择和区位优势分析的基础是该文中提出的区位能,即分析各极点因其区位条件 而对区位能客体的吸引力.通过考察极点自身的属性和因极点位于某一区域而具有的该区域 内的属性,并设立一定的程序来确定不同目的类型极点的理论区位能、可置信区位能和可实践区位能.区域的各种区位能由其内各类极点的相应区位能组成.     

湖北省春季暴雨落区数值预报模型和指标

数值预报产品已广泛应用于基层台站，但对于其丰富的物理量预报产品的解释应用还不够。文章利用T106物理量预报产品，结合常规气象资料，对1998～2001年湖北省春季暴雨天气过程进行了诊断分析，重点分析了有利于产生暴雨的多个物理要素，发现了产生暴雨的一些物理量及其值的结构特征，包括不同的物理要素场形态的走向、预报值的大小、上下层的配置，加深了对暴雨发生机制的认识，归纳出湖北省春季暴雨落区、落点的预报模型和指标，在促使暴雨预报准确率有所提高的同时，使暴雨预报更加精细化。     

GPS-RTK技术在油田井位测量中的应用

结合新疆油田地形地貌特点，阐述了RTK技术在油田井位测量中的应用，分析了影响RTK作业的原因，指出了RTK技术在井位测量中的注意事项，并就RTK技术在实际工作中遇到的问题提出了有益的见解。     

CASS测图软件中DTM的建立与应用

本文探讨了CASS测图软件中DTM的建立及其在工程中的应用,并提出了在建立过程中应该注意的一些实际问题,供有关人员参考应用.     

Study on the earthquake fault of the Lulong ML=6.2 earthquake by precise relocation of aftershock

Introduction The Lulong county is about 75 km northeast to Tangshan in Hebei Province. An earthquake of ML=6.2 took place on October 19, 1982 about 4 km northeast to the county town. The epicenter of the mainshock is located at 39°57′N, 119°04′E by the Beijing seismic network. The 1976 Tang- shan 7.8 earthquake and the successive Luanxian 7.1, Ninghe 6.9 and the Lulong earthquake spread in NE-SW direction in space. SONG and WANG et al of Institute of Geophysics, China Seismolog…     

Quantitative analysis on tectonic deformation of active rupture zones

Introduction The Global Position System (GPS) may provide information about the crust movement of high precision in a large area, which significantly improve the capability of monitoring crustal movement over the area. In the last decade, studies on the global plate movement, the large scale block motions, the high-resolution crust movement of related monitored regions and tectonic de-formation fields have become the hotspot of spatial geodesy (ZHU et al, 2003; Wang et al, 2001; HUANG et…     

One-Dimensional qP-Wave Velocity Model of the Upper Crust for the West Bohemia/Vogtland Earthquake Swarm Region

The western part of the Bohemian Massif (West Bohemia/Vogtland region) is characteristic in the relatively frequent recurrence of intraplate earthquake swarms and in other manifestations of past-to-recent geodynamic activity. In this study we derived 1D anisotropic qP-wave model of the upper crust in the seismogenic West Bohemia/Vogtland region by means of joint inversion of two independent data sets - travel times from controlled shots and arrival times from local earthquakes extracted from the WEBNET seismograms. We derived also simple 1-D P-wave and S-wave isotropic models. Reasons for deriving these models were: (a) only simplified crustal velocity models, homogeneous half-space or 1D isotropic layered models of this region, have been derived up to now and (b) a significant effective anisotropy of the upper crust in the region which was indicated recently by S-wave splitting. Both our anisotropic qP-wave and isotropic P-and S-wave velocity models are constrained by four layers with the constant velocity gradient. Weak anisotropy for P-waves is assumed. The isotropic model is represented by 9 parameters and the anisotropic one is represented by 24 parameters. A new robust and effective optimization algorithm - isometric algorithm - was used for the joint inversion. A two-step inversion algorithm was used. During the first step the isotropic P- and S-wave velocity model was derived. In the second step, it was used as a background model and the parameters of anisotropy were sought. Our 1D models are adequate for the upper crust in the West Bohemia/Vogtland swarm region up to a depth of 15 km. The qP-wave velocity model shows 5% anisotropy, the minimum velocity in the horizontal direction corresponds to an azimuth of 170°. The isotropic model indicates the V_P/V_S ratio variation with depth. The difference between the hypocentre locations based on the derived isotropic and anisotropic models was found to be several hundreds of meters.