一种橡胶材料的大变形分析

对于橡胶材料,高玉臣在1990年和1997年分别提出两个本构关系,一个是将应力偏量与静水应力分离,另一个是将拉应力与压应力分离.本文提出了一种简单的橡胶材料本构关系,通过对立方体单元的典型大变形分析,揭示了这类材料的大变形特征并得出了对材料常数的限制条件.     

总体比例的分级Bayes估计

在总体比例的Bayes估计中，引入超先验，得到总体比例的分层先验分布，在此先验下，给出总体比例的分级Bayes估计量，当总体比例值较小时，Bayes估计量是分级Bayes估计量的一个特例。     

湖南省信息化水平测算及预测

用信息化指数模型对湖南省1985－2000年信息化水平进行测算和分析，并对湖南省信息化未来发展水平状况进行预测，就如何提高湖南省信息化水平提出了若干对策。     

时效性对单桩极限承载力的影响分析

目前，盐城地区正广泛采用打入式预制桩和泥浆护壁成孔灌注桩。从这两种桩的成桩工艺，结合地基条件，对盐城地区饱和软粘土层中这两种桩成桩后休止时间对单桩极限承载力的影响规律进行了分析研究，并对载荷试验的间歇时间的确定问题作一些有益的探讨。     

高应变动测和静载荷试验对比检测单桩承载力

介绍了高应变与静荷载对比检测单桩承载力的发展概况；对盐城市大直径钻孔灌注桩，利用高应变动测与静载荷试验相结合检测承载力，并对检测结果进行对比分析，为在本地区推广应用高应变动测应技术提供依据。     

西部沙漠化与沙尘风暴问题的探讨

根据我国西部地表植被向恶性循环方向发展，土地沙漠化面积迅速增长，沙尘风暴日趋频繁的具体情况，以生态系统科学为指导，采用多学科紧密合作方式，分析了中国西部沙漠化和沙尘风暴存在的主要问题，并进一步探讨了沙漠化和沙尘风暴形成的原因和对发展所造成的危害，因地制宜提出了相应的治理对策。     

氯化十六烷基三甲基季铵盐减阻流体试验

通过对不同工况下氯化十六烷基三甲基季铵盐（Cetyltrimethyl Ammonium,Chloride,CTAC)减阻流体在二维流道中减阻性能的测量，分析了温度，浓度，配比变化对流体减阻性能的影响，同时使用相位多普勒测速仪测量了流体的速度场，利用信号处理中的相关方法分析了运动结构，结果表明，减阻流体在主流速度方向上存在较低频率的周期运动，而在垂直方向上的运动则是随机的，减阻流体的各向异性强于非减阻流体。     

超声化学的研究与应用

回顾了超声化学研究发展的历史，简要说明了超声化学的反应机理，并详细介绍了超声化学在催化领域，水处理，电化学及纳米材料中的应用。     

Carbon isotopic records in paleosols over the Pliocene in Northern China: Implication on vegetation development and Tibetan uplift

Carbon isotopic composition of pedogenic carbonate can be used to estimate the proportion of C₄ and C₃ plants. Here we present carbon isotopic data of carbonate in a red earth section at Xifeng, central Loess Plateau. Results show that C₄ vegetation increased in ∼4.4 Ma B.P., stabilized between 4.0 and 3.0 Ma B.P. The character and timing of C₄ expansion on the Loess Plateau are similar, but different with other localities, e.g. Pakistan and Africa, implying that regional climate changes were main factors driving the expansion of C₄ plants. This event is comparable in timing with increased aridity evidenced by Xifeng grain size and North Pacific eolian dust records. Therefore we argue that the Pliocene expansion of C₄ plants in northern China might have been caused by the increased aridity, which in turn might be related to rapid uplift of the Tibetan Plateau.     

Palaeolake and palaeoenvironment between 42 and 18 kaBP in tengger desert, NW China

Comprehensive field investigations and laboratory analyses show that palaeolakes, including fresh- mesohaline water Megalake Tengger and other semi-con- nected, isolated water bodies, during late Pleistocene covered an area of more than 20000 km², which is more than half of the Tengger Desert in NW China. Stratigraphic correlation and chronological evidence indicate that before ca. 42000 aBP the area was more arid. The palaeolakes started to develop around 40000 uncal. ¹⁴C aBP but until 37000 ¹⁴C aBP their scope was limited. High water levels established from 35000 ¹⁴C aBP lasted until 22000 ¹⁴CaBP. Lake levels regressed between 22000 and 20000 ¹⁴C aBP but transgressed from 20000 to 18600 ¹⁴C aBP. Subsequently, water level declined further and the Megalake Tengger finally desiccated at around 18000 ¹⁴C aBP. Megalake Tengger possessed a fresh-mesohaline water property, implying that the regional precipitation increased significantly. During the period of Megalake Tengger, the climate was warmer-humid than present. The annual rainfall was 250 to 350 mm more than that of today and the temperature was 1.5 to 3.0℃ higher.