川西可尔因地区1:5万水系沉积物测量异常评价及找矿预测

以可尔因地区1∶5万水系沉积测量成果为基础,对该地区8种与稀有金属矿床密切相关的元素进行了R型聚类分析、因子分析。结果表明,该地区各元素间的相关性较好,主成矿元素为Li。各元素异常强度高,规模大,套合性好,主要分布在可尔因岩体外接触带。结合地质、物探成果,圈定了8处锂多金属矿找矿靶区。     

多成分水体的光学性质与遥感

不同水体的水的性质显示了极大的多变性，这与水体的湖泊学／光学类型、季节、生物活动的周期变化和人类影响有关。根据光学及其他性质，将水体放在线性的尺度上是不可能的。光学性质是由除了水体本身之外的光学灵敏水体组成物所决定的，这些组成物被称为水成份。     

蒸汽透平积盐及防治

1积盐的形成 1.1汽盐机积盐的种类汽轮机内沉积物含有大量硅盐其含量超过30%,其中氯化钠占22%,其它盐类很少.在汽轮机沉积的盐类中,SiO2的增加几乎是与NaGl的含量的减少成比例的.SiO2大量沉积的温度,有人认为380～60℃之间.     

湖泊富营养化灰色评价模型及其应用

将待评价湖泊富营养化指标组成参考数列,湖泊富营养化评价标准指标组成被比较数列,根据灰色关联度定义,运用扩展的最小二乘方准则构造目标函数,通过求条件极值建立了湖泊富营养化灰色评价模型。应用该模型对我国１８个主要湖泊的富营养化进行了评价,并与用其它方法评价的结果进行了对比.     

北京的地下明珠

提到北京的溶洞，石花洞、银狐洞的名字会立刻浮现于人们的脑海中。作为京城的地下明珠，它们每年都吸引着八方来客，尤其在盛夏的日子里，它们的“消暑功力”更是“游山玩水”所不能比拟的。     

Clay mineral distributions in the southern Yellow Sea and their significance

To better understand the characteristics of the clay minerals in the southern Yellow Sea, the X-ray quantitative determinations have been carried out for the surface samples obtained from the Yellow Sea. With newly compiled clay mineral synoptic maps, the depositional processes were described for four main clay minerals (illite, chlorite, kaolinite and smectite). The analysis shows that most clay minerals are of terrigenous source with the Huanghe River acting as the major sediment supplier. Besides, the source of muddy sediments in the Yellow Sea was also discussed. As for the central Yellow Sea mud (CYSM), the sediments in its northern part mainly come from the Huanghe River, and those in the rest are of multi-origin. Very similarly, a large amount of sediments in the northern part of the southeastern Yellow Sea Mud (SEYSM) derive from the Keum River and Yeongsan River, while those in the southern part are of multi-origin.     

南京市区坳沟地貌探讨

本文论述了南京市区坳沟地貌的形成过程及其主要地貌特征,分析了沟内沉积物的岩性岩相及其垂向沉积序列,进而阐述了坳沟地貌的发育演变史。     

Distribution of diatoms in the water and surface sediments of southern South China Sea

The relationship of species and abundance between the diatoms in the water and sediments from the southern South China Sea （SCS） were discussed, and the key environmental controlling factors were also investigated. Studies show that the diatom abundance is high in both water and sediments in the southeast part of the southern SCS and the varying trend is similar, while in the northwest part, the abundance is low, and the varying trend is different. The dominant diatom species are Thalassionema nitzschioides and Nitzschia bicapitata in water, and T. nitzschioides and Chaetoceros messanensis in sediments. The diatom species of small size and thin shell in water are more than in the sediments, while the diatom species of large size and thick shell in water are less. The percentage of species T. nitzschioides is higher in water of southeast part than in that of northwest part, but it is similar in sediments of both areas. It is shown that the southwest monsoon is the important factor influencing diatom abundance and T. nitzschioides percentage, and when the southwest monsoon is well developed, the distribution of diatom abundance and T. nitzschioides percentage are consistent in both water and sediments of the study area.     

嫩江水系沉积物中若干元素背景值的研究

本文从嫩江水系环境特征出发,在大面积采样调查的基础上,用地球化学和数理统计方法计算了嫩江水系Cu、Pb、Zn、Cd、Cr、Ni、Hg、A■等元素在沉积物中的背景值,讨论了沉积物粒度和岩石化学组成对沉积物背景值的影响,以及沉积物中元素的分布规律。     

土壤和沉积物中1,2,4-三氯苯的超声波提取

以土壤和沉积物中的1,2,4-三氯苯为研究对象,应用超声波提取并以气相色谱进行定量分析。研究结果表明：在一定的超声波处理条件下,1,2,4-三氯苯较为稳定且降解比率很小;最适宜的超声波提取条件为：超声波功率20W、提取温度35℃、提取时间60min、提取剂为石油醚-丙酮混合溶剂(体积比1：1);三种不同提取方法(索氏、振荡和超声波)相比较以超声波提取法最优;该方法的平均回收率为92．18％、变异系数0．82%、检测限0．000μg／g,可满足土壤中微量有机物定量分析要求。