颗粒增强复合材料相界面的动态应力分析

针对硬微粒填充高聚物复合材料因相界面脱粘开裂生成微孔洞的微损伤成核机制，取材料的代表体积单元进行动力分析，通过对粘弹性基体本构关系作Laplace变换建立了基本方程，并引入Hankel变换，得到了球对称动荷载作用下的相界面应力变化规律的解析解，据此分析了惯性效应和粘性效应对界面脱粘的影响。

异育银鲫对鱼粉等11种饲料中磷的利用率

于1988年,以三氧化二铬间接指示法,在水温22±2℃条件下,测定了平均体重为55±5g/尾的异育银鲫对鱼粉、肉骨粉、芝麻饼、虾粉、骨粉、菜籽饼、玉米粉、脱氟磷酸氢钙、磷酸二氢钙、磷酸氢钙、磷酸钙的表观消化吸收率。结果表明:异育银鲫对第一、第二、第三磷酸钙的消化吸收率是不同的,分别为81％,65％和32％,此顺序与其溶解性由大到小的顺序一致;在所测试的八种商品饲料中,对骨粉、虾粉和菜籽饼中磷的表观消化吸收率较高,分别为65％,68％和65％;对鱼粉、芝麻饼、肉骨粉三种原料中磷的表观消化吸收率较低,分别是1

高精度GPS,三维激光扫描和测针板三种测量技术监测沟蚀过程的对比研究

采用连续模拟降雨试验,对坡沟系统概化模型进行坡面沟蚀发育过程模拟,再现坡面片蚀—细沟侵蚀—切沟侵蚀演变过程。结合3种测量技术从测量精度、测量人员要求、数据处理、数据通用性、配套软件使用、前期投入、测量条件等几个方面入手,对比分析高精度GPS(Trimble 5700)、三维激光扫描仪(Leica HDS 3000)和测针板的3种测量方法的优缺点,同时对3种测量方法在沟蚀过程监测和侵蚀量估算方面进行对比研究。结果表明,激光扫描仪能很好地监测沟蚀演变过程,且对侵蚀量估算精度较高,误差仅为4.5%。高精度GPS也能很好地监测沟蚀演变过程,对侵蚀量估算精度误差为7.38%。测针板法不能很好的反映沟蚀演变过程,但是对于侵蚀量的估算可以满足日常要求,误差为-12.78%。

原油萃取汽提水中的酚

渣油催化裂化装置产生的含硫污水经汽提后虽脱除了大部分的硫、氮化合物，但仍含有较高浓度的酚类物质直接排入污水处理厂，其酚负荷约占全厂进水总酚的一半以上，极易造成对生物处理设施的冲击，导致活性污泥恶化，严重影响总排污水综合合格率。因此，在汽提水进入污水厂...

岱海岩芯沉积的粒度组成与湖区全新世降水变化历史

Sediment cores DH99a and DH99b recovered in the central part of Daihai Lake in north-central China were analysed at 2- to 4-crn intervals for grain-size distribution. Grain-size distributions of the lake sediments are inferred to be a proxy for past changes in East Asian monsoon precipitation, such that greater silt-size percentage and higher median grain size reflect increased monsoonal precipitation rates. The grain-size record of Daihai Lake sediments spanning the last ca 11,000 yr indicates that the monsoonal precipitation in the lake region can be divided into three stages: the Early, Middle and Late Holocene. During the Early Holocene before ca 7900 cal yr BP, the median grain size (Md) and the silt-fraction content were relatively low and constant, suggesting relatively low precipitation over the lake region. The Middle Holocene between ca 7900 and 3100 cal yr BP was marked by intensified and highly variable monsoonal precipitation, as indicated by high and variable Md values and silt contents of the lake sediments. During this period, average precipitation rate gradually increased from ca 7900 to 6900 cal yr BP, displayed intense oscillations between ca 6900 and 4400 cal yr BP, and exhibited a decreasing trend while fluctuating from ca 4400 to 3100 cal yr BP Although generally high during the Middle Holocene, both the Md and the silt content assumed distinctly low values at the short intervals of ca 6500-6400, 6000-5900, 5700-5600, 4400-4200 cal yr BP, implying that monsoonal precipitation might have been significantly reduced during these intervals. During the Late Holocene since ca 3100 cal yr BP, grain-size values suggest that precipitation decreased. However, during the Late Holocene, relatively higher Md values and silt contents occurring between ca 1700 to 1000 cal yr BP may denote an intensification of hydrological cycles in the lake area. Changes in the East Asian monsoonal precipitation were not only directly linked with the changing seasonality of solar insolation resulting from progressive changes in the Earth's orbital parameters, but also may have been closely related to variations in the temperature and size of the Western Pacific Warm Pool, in the intensity of the El Nino-Southern Oscillation, and in the path and strength of the North Equatorial Current in the western Pacific.