冬季城市边界层风场和温度场结构分析

本文根据沈阳地区大气环境容量研究中1984年12月所进行的观测,对沈阳城市边界层的流场和温度场结构做了分析。得出了冬季城市边界层的一些特征。当地面风速微弱时,热岛效应显著。边界层低层辐合抬升,在城市下风边缘可能出现反向气流。当风速较强时,城市的摩擦效应占优势,城市上风部分辐合抬升,下风部分辐散下沉。观测分析还表明,城市建筑对气流的阻滞作用可伸展到几百米的高度。夜间微风时,接地逆温层厚度可达200m,城市内边界层从上风边缘起开始发展,厚度可达100m。白天风力微弱时,重烟尘污染可导致城市冷岛,并推迟对流边界层的发展。     

强震现场流动无线遥测地震台网观测系统的研制

描述了强震现场流动无线遥测地震台网观测系统的技术设计，系统构成，工作原理及应用。     

A THEORETICAL STUDY ON THE URBAN HEAT ISLAND EFFECT

The atmospheric thermodynamic equations are solved analytically to study the urban circulation caused by city heating.The perturbed flow and temperature fields are obtained and compared with observational facts from some urban boundary experiments.The agreement between the theoretical and observational results shows that this study may shed light on the physical characteristics of heat island circulation.     

数字卫星云图估算面雨量的应用试验

使用云分类降水率估计的方法，有静止气象卫星数字云图进行面雨量估算。对１９９３年８月４日华北南部一次降水过程的实测雨量与估算结果的对比分析表明，这种估算方法对雨区的差别有相当高的精度，对雨量的估计有一定的参考价值。     

陇南伏期旱涝指数及预测模型

从陇南气候规律及农业生产实际出发，制定出客观定量衡量陇南伏期旱涝特征的旱涝指数，并利用1967－1996年旱涝指数，用EOF对陇南伏期旱涝进行分片，分析其时空分布特征，建立各片伏期旱涝均生函数预测模型，通过应用，预报准确率有较大提高。     

北衙红色粘土型金矿地质特征和成矿条件

本文系统研究了北衙红色粘土型金矿的地质特征和矿床类型，并从金矿产出的地质背景入手，分析其形成条件，认为是本区很有代表性的一种新的金矿类型，对矿区增储和区域找矿具有重大意义。     

Tectonic Dynamic Metallization of Silver-GoldHydrothermal Fluids in Proterozoic GneissTerrene Shear Zones, Suichang, Zhejiang, China

-,The well-known Suichang silvengold field is located inZhejiang Province of SOutheast China. It is the largest silver-gold deposit associated with copper and zinc in the Cathaysianmetallogenic province.There are a series of silver-gold dePOsits in the shear zonesof Proterozoic gneiss terrene, Suichang region. The volcanicapparatus at Mesozoic has complicated rpineralization. Respectively, there are two pieces of understanding on the origin ofore-formigg nuid: (l ) metamorphic fluid (Lia…     

The relationship between the first Fresnel zone and the normalized geometrical spreading factor1

Conventionally, the Fresnel zone and the geometrical spreading factor are investigated separately, because they belong to different theories of wave propagation. However, if the paraxial ray method is used for establishing the Fresnel–Kirchhoff diffraction formula for a laterally inhomogeneous multilayered medium, it can be shown that the normalized geometrical spreading factor is inversely proportional to the area of the first Fresnel zone associated with the reflection point. Therefore, if no diffracting edge cuts the first Fresnel zone, the geometrical optics approximation represents the principal part of the wavefield obtained by Fresnel–Kirchhoff diffraction theory. Otherwise, the geometrical optics approximation has to be corrected by adding edge diffractions. It is also shown that Kirchhoff-type migration and geometrical spreading factor correction both reduce the first Fresnel zone to a zone with unit area.     

高温高压下蒙脱石显微变形与力学性质的研究

通过研究高温高压条件下蒙脱石的变形特征和机制,着重阐述了蒙脱石的显微变形特征与温度压力之间的关系,以及对应力-应变的影响。研究表明,在围压为200M Pa条件下,温度升高将导致蒙脱石的变形增大。对相同应变量所需的差异应力则随温度上升而下降。但是,当温度>500℃时,相同应变量所需差异应力较300℃时显著增大,其屈服强度和变形模量在T≥500℃,σ≥300MPa时均因脱水明显增大。蒙脱石在高温高压下均为渐进失稳     

^3He／^4He Ratios and Heat Flow in the Continental Rift—valley,Eastern China

Heat flow and the origin of helium in natural gases from fault basins of the continental rift-valley in eastern China are discussed in terms of helium isotope geochemistry.³He/⁴He ratios in natural gases from the rift-valley range from 2.23 × 10⁻⁷ to 7.21 × 10⁻⁶, which are directly proportional to the concentration of helium and ΣNHC/ΣHC ratio in natural gases. Geological and isotope geochemical data suggest that helium in natural gases consists predominantly of crustal radio-genic and upper mantle-derived helium. In a simple mixing pattern between crustal He and mantle-derived He, mantle-derived helium in natural gases would account for 10–60%. Calculated values for heat flow (Q) range from 59.7 to 82.4mWm⁻², of which about 60 percent in the rift-valley is derived from the upper mantle. Natural helium reservoirs would be found in the areas where the upper mantle uplifted greatly and heat flow is large in the continental rift-valley. The project is financially supported by the National Natural Science Foundation of China.