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     

红会一矿煤层对比分析及主要标志层的确定

通过对一、二层煤的对比分析 ,证实二层煤为一层煤的分支煤层 ;确定了一、二层煤间的主要标志层。     

电导法研究环己烷/水/CTAB乳状液的稳定性

制备了不同组成的环己彬水／十六烷基三甲基溴化铵（CTAB）乳状液,用电导法测定了正己醇、聚乙二醇等添加剂存在下乳状液富水相不同时间的电导率、通过提出增比电导率Kr的新概念,描绘了dkr／dt与时间的关系曲线,并由dkr／dt—t曲线求得了该曲线上的极值点tmax和（dkr／dt）max,定量判断了乳状液的稳定性,结果与分相法观察到油水分层的时间tp基本吻合。     

图库中光栅与矢量化技术的应用研究

通过产库中光栅与矢量化应用技术的分析和研究,合理有效地利用扫描技术实现“甩掉图纸”的目标,进而实现真正意义上的电子图档管理。     

5种抗寒剂对早稻湘早籼25号幼苗的耐寒生理鉴定及其利用

试验结果表明,在相同低温胁迫条件下,经聚乙二醇处理的湘早籼２５号秧苗不仅电导率低,干重大,而且可溶性糖和叶绿素总含量高,表明５种抗寒剂中聚乙二醇对水稻秧苗具有较好的抗寒效果。     

自构形神经网络模型在天然气储量评价中的应用初探

在ＢＰ（Ｅｒｒｏｒ Ｂａｃｋ－Ｐｒｏｐａｇａｔｉｏｎ）算法基础上,采用ＢＩ（ＢａｃｋＩｍｐｅｄａｎｃｅ）算法,运用了自组织优化隐层节点数和自动化优化网络因子的方法,使得人工神经网络ＡＮＮ的计算速度、精度和柔韧性有所提高,且在微机上其操作变得更加容易。在勘探成熟的气藏中,按照天然气成藏理论,选取能够系统反映气藏的８个储量评估参数,进行网络学习,建立储量评估模型。应用所建的网络模型对正处于勘探阶段的气