土体侧向变形性状的真三轴试验研究

对标准砂和风干粘土的击实试样进行了真三轴应力应变关系试验研究，发现当某一方向给土体施加力应力增量而其侧向应力保持不变时，侧向变形未必都是膨胀的，也有可能是压缩的，即泊松比未比总是正值，而有时可能为负，这是一个值得重视的有异于经典力学理论的现象，本文研究了这一现象出现的规律，并从机理上分析了其发生的必然性和存在的条件。     

浅孔密集钻注浆及有关参数的确定

本文阐述采用浅孔密集钻注浆时,钻孔的布置和设计,注浆材料的粒度分级和水土比的简易测定方法,以及泥浆输送中计算水力坡度、临界流速和倍线时有关参数的确定。     

卸载对软土伸长强度的影响分析

基于Hvorslev强度理论,以卸荷前应力状态为基准,推导了软土等向卸载后,土体处于类似超压密状态时卸载土体强度与卸载前正常固结土强度之间的关系式;采用太沙基一维固结理论,编制了内嵌固结计算的修正剑桥模型程序,分析不同卸载量、不同卸载固结时间、不同卸载级数对强度的影响,从而提供了全面系统分析卸载对软土伸长强度影响的方法,计算结果与试验数据对比,表明分析方法具有良好的可信度。     

模糊层次分析法在地基处理方案优选中的应用

简要介绍了模糊层次分析法的基本原理和分析问题的步骤。基于模糊层次分析法的软土地基处理方案优选，结果表明选择结果与实际相符合。     

中国北方新近纪红黏土记录的古气候意义——与动物群化石序列对比

目的研究中国北方新近纪红黏土序列的古气候演化特征。方法对中国北方4个新近纪红黏土剖面沉积物的粒度、磁化率和化石动物群时间序列进行区域对比。结果黄土高原新近纪红黏土沉积以来发生了5次大的气候事件,气候事件的分界线在粒度、磁化率年龄曲线上特征明显,反映的气候特点与化石动物群演替性质完全一致。结论中国北方新近纪红黏土序列古气候演化过程的气候事件均与青藏高原隆升和东亚季风的发展相联系。时间上,南北气候演化事件基本同步;空间上,北部较南部地区变化剧烈。5次气候事件从下到上表现为半湿润、半干旱、湿润、干旱与湿润交替、干旱的气候演化特征;相应动物群生态类型表现为草原-疏林草原、草原为主的疏林草原、森林、草原荒漠与森林交替到草原的演化特点。     

哺乳动物胚胎冷冻技术研究进展

报道了胚胎冷冻技术的发展及现状。根据它的发展分别介绍了慢冻慢解法、常规快速解冻法、玻璃化冷冻、1步细管法冷冻、1步冷冻和半胚冷冻，并且就胚胎冷冻保护剂、冷冻方法、解冷方法、冷冻保护剂的脱除及胚胎发育时期等对胚胎冷冻效果的影响进行了探讨。     

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。     

The ecological sequence of Hipparion fauna in the mid-dle reaches of the Yellow River during Neogene

The faunal ecological type and sequence in the Tertiary red clay indicate that Hipparion fauna during the period 7.4-6.1 Ma in the middle reaches of the Yellow River is composed mainly of dorcadoides and mixed types. This represents semiarid veld environment with small fluctuation. The fossil assemblages characterized by the abundance of gaudryi types and even the occurrence of some Hominoid and Chalicotherium indicate an obviously warm and humid period since 5.3 Ma. The fossil assemblages during 3.4 Ma show the typical steppe fauna representing dry climate. It is indicated by the changes of ecological sequence that the climatic conditions in Pliocene are drier than that in late Miocene. The clay-skin content of red clay, which has a synchronous change with faunal features, is a rather good replacing palaeoclimatic index.     

The ecological sequence of Hipparion fauna in the middle reaches of the Yellow River during Neogene

The faunal ecological type and sequence in the Tertiary red clay indicate that Hipparion fauna during the period 7.4–6.1 Ma in the middle reaches of the Yellow River is composed mainly of dorcadoides and mixed types. This represents semiarid veld environment with small fluctuation. The fossil assemblages characterized by the abundance of gaudryi types and even the occurrence of some Hominoid and Chalicotherium indicate an obviously warm and humi period since 5.3 Ma. The fossil assemblages during 3.4 Ma show the typical steppe fauna representing dry climate. It is indicated by the changes of ecological sequence that the climatic conditions in Pliocene are drier than that in late Miocene. The clay-skin content of red clay, which has a synchronous change with faunal features, is a rather good replacing palaeoclimatic index.     

尼龙6/粘土纳米复合材料的熔融挤出制备及表征

为了研究尼龙6／粘土纳米复合材料制备和结构，采用合适的改性剂对粘土进行有机改性，改性后的有有机土与尼龙按一定比例在具有反螺旋段的双螺杆挤出机中熔融复合。TEM测试结果表明：大多数粘土以单层层均匀分解于基体中（即使有少数以多晶层出现，厚度大约20nm），形成纳米复合材料。