浅谈上海地区的总稀土

1 概述稀土(Rare Earth)元素,位于元素周期表第57～71号,由性质十分相近的镧、铈、镨、钕等15种镧系元素以及钪、钇2个元素组成。通常,把57～63号的7个元素称为轻稀土元素,其它10个元素称为重稀土元素。地壳中,稀土元素含量与锌、铜、铅等元素含量不相上下。我国的稀土资源,居世界首位,共约3600万吨(R_2O_3),其中90％分布在包头地区。土壤及生物链中,均有稀土元素。进入环境中的稀土化合物,大部分来自岩石的风化物,其次来自煤的燃烧。稀土元素,主要用于冶金、石油化工、电子器械、玻璃陶瓷等工业上。稀土元素,通过口、呼吸道及皮肤的伤口进入人体。吸收后的稀土元素,从人体内排泄的半衰期为一年至十几年。     

Complex behaviour of trivalent rare earth elements by humic acids

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煤中部分潜在毒害微量元素在表生条件下的化学活动性

利用连续化学浸取实验方法，对采自贵州省二叠经龙潭组的３２个煤样中的１０种潜在毒害微量元素化学的活动性进行了研究，结果表明：煤中Ｈｇ、Ａｓ、Ｓｅ、Ｃｄ等元素具有极强的化学活动性，其中平均８３．８％的Ｈｇ、９３．５％的Ａｓ、８０．３％的Ｓｅ．６３．３％的Ｃ在．１％的Ｃｕ的８６．８％的Ｐｂ可以被带出煤中而进入表生环境；煤中Ｚｎ的化学活动性次之，只有平均４６．６％的Ｚｎ可能迁移进行环境中；Ｔｌ、Ｃｒ、Ｎｉ     

燃烧型煤排放可吸入尘中的成分分析

主要运用X 射线荧光光谱的半定量分析方法 ,测量了民用炉灶燃烧型煤排放的可吸入尘中的主要成分 ,从而得出在可吸入尘中的主要元素为Cl、S、Na、K ,并研究了其产生的原因     

地质样品中27项元素的粉末压片法x射线荧光光谱测定

本文报导了用x射线荧光光谱法—次粉末压片制样同时测定Na. Mg. Al. Si.P. S. K. Ca. Ti. V. Cr. Mn. Fe. Co. Ni. Cu. Zn. Rb. Sr. Y. Zr. Nb. Ba. Hf. Pb. Th. U等27项元素的快速分析方法。从理论上提出了新的基体效应学校正模式,首次引入了非荧光分析的物质(筒称NFAM)的新概念;并计算了理论α系数,使理论α系数在粉末压片法x射线荧光分析中获得了应用。本方法测定的对象可以是岩石,土壤和水系沉积物等地质样品。     

Status of air pollution in Beijing

A study has been made on elements organic constituents, TSP, SO2,NO2 of atmospheric pollutants in Beijing. 17 elements, and some PAHs, e. g. B(a)P, B(b, j, k)P, and B(g, h, i)P, in airborne particles by X-ray fluorescence spectroscopy and HPLC, GC/MS, have been determined respectively. It has been shown that the elements Pb, Zn, S and Cu were more enriched in fine particles and different valence states of sulfur at various sites. It was found that the concentrations of S6+ and S2-were more than 85% and less than 15% of the total sulfur respectively. Concentrations of major PAHs and sulfur-containing compounds increased in winter and in urban area. High values for Pb and Zn in city, Fe and Mn at industrial area and Cu, Al rural sites were obtained respectively. This implies the functions of different elemental sources of various sites. Thus, elements can be from distingushed anthropogenic and natural sources.The main contribution of SO2 was found of to have same seasonal variation as the anthropogenic el     

长江铜陵段表层水中重金属含量及存在形态分布研究

通过测定长江铜陵段枯、丰水期江水中cu、Pb、Zn和cd不同形态的含量,分析了4种金属在江水中的存在形态分布,不同水期含量变化,水中悬浮物对金属吸附能力大小,以及近20年来含量的变化情况。结果表明,长江铜陵段江水中各重金属总量丰水期时大于枯水期,重金属各形态含量之间均有差异:丰水期时,各金属会被悬浮物以不同的方式携带进入水体中,cu、zn、Pb以活跃态和稳定态为主,Cd以活跃态为主;枯水期时,Zn主要以溶解态和稳定态为主,Pb以稳定态方式被携带,而80％的Cu、Cd是以溶解态形式存于水中。悬浮物(丰水期)对重金属的吸附能力大小顺序为Pb>Cu>Zn>Cd。与近20年江水中的重金属背景值比较,长江铜陵段重金属含量有普遍升高的趋势。     

孟连,丽江地震前云南天文台时纬残差异常

本文分析了云南天文台光电等高仪自有观测以来的时纬残差异常与云南及其周邻地区大地震的对应关系；并报导了孟连、丽江地震前云南天文台的时纬残差均有明显异常。这再次证明时纬残差的明显异常可为台站周围的强震预测提供可靠信息     

基于神经网络的重大危险源动态分级研究

利用自组织神经网络对重大危险源进行动态分级研究，介绍了神经网络的模式聚类即分级法的自组织学习过程和算法，克服了以往危险源分级方法的某些局限性。在计算机上进行的模拟计算表明：基于自组织神经网络的重大危险源动态分级方法是合理可行的     

Study of Pollution of the Plitvice Lakes by Water and Sediment Analyses

The process of eutrophication in form of intense plant growth has been observed in some lakes and water streams at the Plitvice Lakes National Park in central Croatia. Here we investigate whether this phenomenon is a consequence of anthropogenic pollution or due to naturally produced organic matter in the lakes. We applied chemical analysis of water at two springs and four lakes (nutrients, dissolved organic carbon (DOC), trace elements) and measurements of surface lake sediments (mineral and organic fraction analyses, trace elements) in four different lakes/five sites. The chemical composition of water does not indicate recent anthropogenic pollution of water because the concentrations of most trace elements are below detection limits. The concentrations of DOC and nutrients are slightly higher in the area of increased eutrophication-plant growth. Also the content of organic matter in the sediment is at the highest level in areas with highest C/N ratio indicating that the organic fraction of this sediment is mainly of terrestrial origin. There is no significant difference among the trace element concentration in the upper segment of all cores, deposited approximately during last 50 years when higher anthropogenic influence is expected due to development and touristic activity, and the lower part of the cores, corresponding to the period approximately 100–200 years before present. The content of trace elements and organic matter in sediments decreases from the uppermost lake downstream. According to our results there is no indication of recent anthropogenic pollution in water and sediment. Higher concentrations of DOC in water as well as phosphorus and some other elements in the lake sediment can be a consequence of input of natural organic matter to the lake water.