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。     

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。     

聚季铵型阳离子聚合物在蒙脱土上的吸附最大值现象

用静态吸附的实验方法对三种聚季铵型阳离子聚合物(COP)在蒙脱土上的吸附现象进行了研究,实验结果表明,COP在蒙脱土上的吸附等温线不符合Langmuir规律,而存在吸附最大值现象,用红外光谱法和岩芯流动试验方法也得到相同的结果。     

贵州陶器的发明及发展

本文收集了较多的史料,论述了贵州在远古时期用火的痕迹及陶器产生的时间。并根据贵州省陶土的资源情况,对贵州陶瓷工业的发展方向提出了自己的看法。     

湖南永和海泡石粘土的矿物学研究

作者应用x射线衍射、红外光谱、差热分析、电子自旋共振及透射电镜研究了湖南浏阳永和海泡石粘土的矿物学特征,确定了由于类质同像替换在海泡石和滑石结构中存在着晶格缺陷,为进一步探讨它的工业利用提供了必要的资料。     

软土地基震陷分析

根据饱和软粘土动三轴试验结果,将循环弱化参数引入等价线性模型。得到描述软土动力特性的循环弱化关系,进而给出一种修正的软化模量法。据此分析软基震陷,阐明软土循环弱化及其它因素对估算软基震陷的影响。     

堆山工程软土地基Biot固结的非线性有限元分析

本文在文献[1]、[2]给出的软土地基Biot固结的有限元构式及程序基础上,对某大型堆山工程分级加荷施工过程中,软土地基的固结变形,附加应力及超孔隙水压力分布,塑性区的开展等进行了弹性非线性有限元的计算分析,得出了在理论和工程应用上一些有意义的结论。本文的计算方法和结果,可供工程技术人员在类似工程的初步设计时借鉴和参考。有些内容尚可进一步研究和探讨。