微波爆发中具有双峰结构的准周期振荡的初步分析

本文分析了1989年3月9日,11日,13日与AR5395产生的耀斑成协的,叠加在2cm微波爆发上的具有双峰结构的准周期振荡.利用磁流环结合的非线性不稳定性机制,对等离子体和磁场相互作用的过程进行了定性的分析,并计算了几个有关的参数.最后进行了简单的讨论.     

煤矿地区国土总体规划的初步研究

本文通过制定总体规划方案应重点协调的六个关系的探讨,对煤矿地区国上总体规划进行了初步研究。     

传感器信号调制脉冲序列抽样频率的确定

通过对传感器输出信号波形有无振荡进行分类 ,依据传感器响应时间的定义 ,分别找到一阶、二阶及理想动态传感器的频带上限与动态响应时间两者间的关系式 ;提出了传感器“受激系数”的概念 ,推导出输出信号波形有无振荡两种传感器之间的比例关系。并通过一个数值例子 ,说明所推导出关系式的应用。     

Generation of flow nets using fem nodal potentials and bilinear shape functions

A method for generating both equipotential lines and streamlines directly based upon nodal potentials and bilinear shape functions is presented. The method involves post-processing a finite element (FE) solution utilizing typical four-node isoparametric quadrilateral elements. The application of the method can be important in the interpretation of FE analysis results, especially when inhomogeneous, anisotropic, unconfined or/and other complicated conditions exist. Compared with conventional techniques to generate flow nets which depend upon both the potential and stream functions, the method presented is simpler and more powerful.     

Synthesis of todorokite by refluxing process and its primary characteristics

Todorokite is one of the common manganese ox-ides in manganese ore deposits, weathering product of manganese-bearing rocks, soils and sediments. It is also an important component in the abundant marine manganese nodules. Since todorokite was firstly found in Japanese Todoroki mine in 1934, its properties and origination have appeared to be very interesting to many researchers[1—3]. It has a stable structure similar to porous molecular sieves, constructed of triple MnO6 octahedral chains. Th…     

黄河三角洲海岸带陆海相互作用概念模式

根据陆海相互作用的观点,黄河流域、黄河干流、河口三角洲及其邻近海区的生态环境相互联系,组成了一个有机的生态系统链,可称为黄河-渤海生态系统。黄河流域的降水量、土壤植被条件使黄河干流具有水少沙多、水沙异源和水资源缺乏的特征。干流入海水、沙通量变化影响了黄河三角洲地区的侵蚀、堆积和发育过程。黄河物质入海后在河口及邻近海域形成了具有高生产力的生态环境和著名的渔场。据此绘出了黄河-渤海生态环境内各环节相互联系的概念模式图,并提出了黄河流域大面积水土保持和南水北调工程逐步展开等新环境下,本区陆海相互作用的研究方向。     

A mechanism for anomalous decline in radon precursory to an earthquake

Mechanisms for interpreting anomalous decreases in radon in ground water prior to earthquakes are examined with the help of a case study to show that radon potentially is a sensitive tracer of strain changes in the crust preceding an earthquake. The 2003 Chengkung earthquake of magnitude (M) 6.8 on December 10, 2003, was the strongest earthquake near the Chengkung area in eastern Taiwan since 1951. The Antung radon-monitoring station was located 20 km from the epicenter. Approximately 65 d prior to the 2003 Chengkung earthquake, precursory changes in radon concentration in ground water were observed. Specifically, radon decreased from a background level of 780 pCi/L to a minimum of 330 pCi/L. The Antung hot spring is situated in a fractured block of tuffaceous sandstone surrounded by ductile mudstone. Given these geological conditions, we hypothesized that the dilation of brittle rock mass occurred at a rate faster than the recharge of pore water and gas saturation developed in newly created cracks preceding the earthquake. Radon partitioning into the gas phase may explain the anomalous decrease of radon precursory to the 2003 Chengkung earthquake. To support the hypothesis, vapor-liquid, two-phase radon-partitioning experiments were conducted at formation temperature (60 degrees C) using formation brine from the Antung hot spring. Experimental data indicated that the decrease in radon required a gas saturation of 10% developed in rock cracks. The observed decline in radon can be correlated with the increase in gas saturation and then with the volumetric strain change for a given fracture porosity.     

Fluid evolution in the Rushan lode gold deposit of Jiaodong Peninsula, eastern China

The Rushan gold deposit in the Jiaodong Peninsula is currently the largest lode gold in China. Gold occurs mainly in pyrite- and polymetallic sulfide–quartz vein/veinlet stockworks. Fluid inclusions in the deposit are divided into three main types, namely CO₂–H₂O, H₂O–CO₂ ± CH₄ and aqueous ones. Microthermometric data show that the pre-gold fluids were CO₂-dominant (X_CO2 up to 0.53), and the total homogenization temperatures fall in the range of 298377 °C. These fluids, modified by fluid/wallrock reactions, gradually evolved into fluids with less CO₂ (X_CO2 = 0.010.19) in the main ore-forming stage, and the total homogenization temperatures range from 170 to 324 °C. Hydrogen and oxygen stable isotope data suggest that ore-forming fluids were mixture of magmatic and meteoritic origin. Co-occurrence of gold and sulfides implies that gold was most likely transported in the form of gold–sulfide complexes. The wide distribution of CO₂ inclusions means that the pH variation during gold transportation was controlled by CO₂ buffering.     

中间法电磁波测距三角高程代替精密水准测量的研究

本文在简要介绍中间法电磁波测距三角高程测量原理基础上,推导了高差计算及精度估算公式;分析了中间法测量代替精密水准测量的必要条件、重要条件和次要条件。通过大量实测数据对比分析,验证了中间法测量代替精密水准测量的可行性,最后给出了中间法测量的实施方案。     

基于FME的DWG数据到ArcGIS转换的应用研究

本文针对工程实践中DWG数据到ArcGIS转换的实际需要,基于转换工具FME,采用FME Workbench构建转换模块对DWG数据转换的方法,研究了利用FME Workbench构建转换模块的关键技术和对转换后GIS数据的检查。通过以阜新腰梅力板的DWG数据为例,实现了对DWG数据到ArcGIS的Geodatabase数据的转换,并对转换后的数据进行检查、整理。结果证明,本文所采用的转换方法良好,节省了工作时间、提高了工作效率。