软土地基水泥深层搅拌加固土物理力学特性研究

通过对水泥深层搅拌桩加固土的各种影响因素和大量物理力学性质的试验研究,得出如下主要结论：（ａ）影响加固效果的主要因素依次为水泥掺入比、含水量、龄期等;（ｂ）水泥掺入比一般应力１０％￣１５％,不宜低于８％;（ｃ）土壤含水量较高时宜选用粉喷搅拌工艺,含水量小于３０％宜采用浆喷湿搅工艺;（ｄ）水泥土声波速度与其强度之间有很好的相关关系,可将声速作为水泥深层搅拌桩检测的重要物理量。     

新型常温自干道路标志涂料的研究

以不饱和聚酯树脂为成膜物质,加入一定量的填料、助剂和颜料经充分混合、搅拌制成常温自干路标涂料．通过正交实验,确定了最佳配方,并对该涂料的耐磨性、干燥时间、流动性、附着力等性能进行测试．     

竖直下喷流化床射流区相间的传质

为了准确设计流化床反应器,对三维统化床中射流区下喷射流与乳化相之间的传质过程进行了理论及实验研究,利用一个简单的模型计算了传质系数,并给出了射流与乳化相间的传质数与射流速度的关联式,还考察了流化气速对传质系数的影响。     

镍-磷-金刚石复合镀层的耐磨性

研究镍－磷－金刚石复合镀层的耐磨性,实验表明经过一定方式前处理的金刚石在ＰＨ值４．５,温度８０℃,负载量８－１０ｍ＾２．ｍ＾－３的工艺条件下,可以获得耐磨性优异的镍－磷－金刚石复合镀层。经粗化亲水前处理的金刚石所得到的镍－磷－金刚石复合镀层,其耐磨性优于经活化亲水前处理金刚石所得到的复合镍层,经粗化亲水前处理的金刚石镀液中添加少量时,就可以获得优异的镍－磷－金刚石复合镀层。镍－磷－金刚石复合镀层的     

磁悬浮液体中颗粒对分散体系流变性的影响

研究了磁悬浮液体中固相质点浓度、质点形状和大小对分散体系流变性质、沉降速度以及分散体系结构的影响。对Ｅｉｎｓｅｉｎ黏度关系式进行了适用性验证：提出一种估算吸附－溶剂化层有效厚度δ的方法。认为,质点间的作用力、质点深度以及质点的形状和大小是决定分散体系结构和流变性质的主要因素。     

晶种涂层对合成ZSM-5沸石膜影响

分别利用打磨法和浸涂法在载体管上引入晶种,然后１７０℃水热晶化,成功地合成了ＺＳＭ－５沸石膜。实验发现引入晶种可减少水热晶化次数,在孔径为０．６μｍ的载体上一次水热晶化即可完成。ＸＲＤ、ＳＥＭ和单组分气体渗透对膜表征表明,该膜为完整、致密的ＺＳＭ－５膜,Ｈ２／Ｃ３Ｈ８的最大理想选择因数达到３３,显示子分子筛分性质。     

镍-磷-Si3N4纳米粒子复合镀工艺研究

通过正交试验法确定了镍-磷-Si3N4纳米粒子复合镀最佳施镀工艺,对正交试验进行了详细的分析,从而确定了镀层最佳施镀工艺：纳米粒子含量为1．0g／L,施镀温度为82℃,镀液pH=4．8。     

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.     

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 .