电阻抗CT技术在人体上肢图象重建中的应用

人体实验是电阻抗ＣＴ技术应用于临床的重要研究课题之一。在研制了适用于人体上肢的环状无源３２－电极系统的基础之上,对不同受试者的上臂和前臂作了多组测试工作。文中给出了电阻抗ＣＴ逆问题计算的数学模型和人体实验的结果。结果表明：经过图象重建和处理后,基本符合人体上肢的解剖学特征,可以清晰地分辨出骨骼与肌肉组织。     

焦耳热效应和矿物质对煤导电性的影响

主要讨论了焦耳热效应和矿物质对煤导电性质的影响。结果表明,因焦耳热的影响煤体温度升高,使得通过煤体的电流增大,且这种效应随时间的增加,由于散热影响而减弱,从而导致一定时间后导电性随时间而减弱;煤在脱除方解石、石英等矿物质后电导率增大１～２个数量级,煤的堆密度增大及煤粒度减小时其电导率将增大。     

一类斯泰勒三元系(STS)的上色数

反超图及其上色数的概念是由ＶｉｔａｌｙＩＶｏｌｏｓｈｉｎ（１９９５）提出来的,该文主要研究斯泰勒三元系及其着色理论,构造了一类ＳＴＳ,并给出了它们的上色数。     

Terrestrial heat flow in Junggar Basin, Northwest China

Based on temperature logs of 117 boreholes and thermal conductivity of 119 rock samples, the first group of 35 heat flow data in the Junggar Basin are presented. The thermal gradients vary between 11.6 and 26.5°C/km, and the thermal conductivity changes from 0.17 to 3.6 W/mK. Heat flow ranges from 23.4 to 53.7 mw/m² with a mean of (42.3±7.7) mW/m². The heat flow pattern shows that heat flow is higher in the uplifts and lower in the depressions. The factors affecting the heat flow and its distribution include basin type, basement structure, sediment thickness, radioactive heat generation, etc. The overall low present-day heat flow in the Junggar Basin reflected its tectonothermal evolution characterized by lithospheric thickening, thrust and fault at shallow crust as well as consequently quick subsidence during the Late Cenozoic.     

Geologic relationships and geochronology of the Cenozoic volcanoes and interbedded weathered mantles of Yulinshan in Qiangtang, North Tibet

The Yulinshan accumulations of volcanic rocks and interbedded weathered mantles provide a unique chance for studying the processes and environment of the formation of the planation surface in central Tibetan Plateau. Geochemical,⁴⁰Ar/³⁹Ar and K/Ar geochronologic investigations of the weathered mantles and high-potassium volcanic rocks reveal that the volcano-weathered mantle accumulations formed under arid or semi-arid subtropic environment in 30–24 Ma. The sole planation surface of the Qiangtang region finally formed in about 20 Ma.     

Thawing and freezing processes of active layer in Wudaoliang region of Tibetan Plateau

The interaction between permafrost and atmosphere is accomplished through transfer of heat and moisture in the overlay active layer. Thus, the research on the thermal and hydrodynamics of active layer during the thawing and freezing processes was considered a key to revealing the heat and moisture exchanges between permafrost and atmosphere. The monitoring and research on active layer were conducted because permafrost occupies about two thirds of the total area of the Tibetan Plateau. Based on the analysis of the ground temperature data and soil moisture data of monitoring near the Wudaoliang region of the Tibetan Plateau, the thawing and freezing processes of active layer were divided into four stages, i.e. summer thawing stage (ST), autumn freezing stage (AF), winter cooling stage (WC) and spring warming stage (SW). Coupled heat and water flow is much more complicated in ST and AF, and more amount of water is migrating in these two stages. Heat is transferred mainly via conductive heat flow in the other two stages, and less water migrated. Four water migration and coupled heat flow processes were addressed for the thawing and freezing stages, which are water infiltration driven by gravity, moisture advection and distillation driven by temperature and osmotic gradients, water migration driven by capillarity and unfrozen water migration driven by temperature gradient. The water content near the permafrost table tends to increase after one thawing and freezing cycle, which is the main reason for the development of thick ground ice layer near permafrost table.     

收敛无穷积分的若干问题

研究在无穷积分∫ ∞a f(x)dx ,收敛的条件下 ,被积函数f(x)的一些性质以及f(x) → 0 (x→ ∞ )的几个充分条件。     

交互初至波检测与表层模型正反演

初至波表层速度模型层析反演是层析静校正的重要基础。作者研究了一套完整的方法和软件系统 ,利用计算机可视化技术进行人机交互初至波检测、表层模型正演及反演 ,可直观地分析、监控初至波检测的合理性及模型层析反演的质量 ,提高表层速度模型层析反演的可靠性 ,为层析静校正提供合理的表层速度模型。     

黄土物理性质变化规律研究

研究了黄土孔隙度和湿陷性在垂向上变化的规律和原因 .结果表明 ,孔隙度高和湿陷强的层位是风化成壤弱的黄土层 ,孔隙度低和湿陷弱的层位是红色古土壤或风化成壤强的黄土层 .第四纪冷干与温湿气候的交替和由此产生的成壤过程的变化是造成黄土地层孔隙度和湿陷性波动变化的根本原因 .黄土湿陷性是在干旱与半干旱地区弱的成壤过程中产生的 ,是草原地带灰黄色土壤具有的特征 .     

可编程控制器在多层喷射沉积制备管坯工艺中的应用

多层喷射沉积是一种新型的喷射沉积工艺 .对制备大厚壁管有着其优越性 ,但存在着开头难以保证的缺点 .作者分析了开头难以保证所形成的原因 .介绍了QA2 2 1 2系列可编程控制器在解决多层喷射沉积管坯形状问题中的应用 ,可更加有效地控制管坯的形状