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.     

Trichloroacetate affects the EPR SignalⅡslow and SignalⅠin the thylakoid of Chlamydomonas reinhardtii

One electron paramagnetic resonance (EPR) signal, named SignalⅡslow, originates from the oxidized Tyrosine 160 (YDo) of D2 polypeptide of photosystemⅡ reaction center. After adding high concentration trichloroacetate (TCA) to the Chlamydomonas reinhardtii thylakoid suspension, this signal was abolished in a minute. Treatment of TCA also removes a few of polypeptides, including three extrinsic polypeptides of oxygen-evolving complex, from the thylakoid membrane. Based upon the analysis of the microenvironment around YD with a three-dimensional model, it is indicated that relatively high hydrophobicity of this microenvironment may be the essential prerequisite for TCA to affect YD. It has been observed that TCA treatment also retards the decay of the SignalⅠ, produced by the oxidized reaction center chlorophyll dimer (P700+) of photosys- temⅠ.     

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     

三维编织复合材料构件机器人优化设计

用有限单元法建立三维编织复合材料构件机器人的动力学模型 ,并用数值积分法求解执行件端点动态响应 通过构件材料阻尼的极大优化 ,显著地减短机器人执行件端点的残余振动时间 图 2 ,表 1,参 5     

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。     

区域分裂法:一种精确高效的三维微波结构全波分析方法

提出了三维微波结构的全波区域分裂算法.和其他方法相比,该算法可以大幅度地降低计算规模和计算的复杂性.文中详细讨论了不重叠型区域分裂法及其在差分格式下的实现,并利用差分格式下的区域分裂法计算了矩形波导内部三维分层结构和多层微带贴片天线的散射参数.所得结果和直接采用FDFD所得结果几乎完全吻合,证明了算法的正确性和有效性.     

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。     

利用OpenGL实现对黄河小浪底发电洞的三维图形模拟

ＯｐｅｎＧＬ是目前应用最广泛且性能非常优越的三维图形应用程序库,本文重点介绍了其在黄河小浪底发电洞的三维图形模拟中的一些应用。