203HgCl2在紫贻贝(Mytilus cdulis)体内的累积和结合以及锌对其影响的实验研究

本文研究了紫贻贝（Mytilus edulis）对无机汞²⁰³HgCl₂的累积和结合.实验结果表明:紫贻贝累积汞速度很快,能力很强.用Sephadex G75凝胶层析表明:所有的²⁰³Hg几乎都以生物大分子存在（M.W.>1000）.其中大部分²⁰³Hg的分子量大于50000,小部分分子量在1000—50000之间.本文还讨论了汞的累积机制,并研究了Zn²⁺对于²⁰³Hg累积的影响.     

Die Bestimmung des Turnovers von ATP,Kreatinphosphat und Orthophosphat in lebenden Muskeln mittels H2O18 und anschließender Aktivierung durch Protonen-Beschuß

The Science of Nature -     

建立绿色包装系统的可行性研究报告

笔者从我国包装的现状分析入手，探讨建立绿色包装系统的可行性和必要性，提出建立绿色包装系统的具体措施和实施方案。     

Rapid prediction of disinfection by-product formation potential by fluorescence

Recent drinking water regulations have lowered the disinfection by-product standards as well as added new disinfection by-products for regulation. Natural organic matter (NOM) plays a major role in the formation of undesirable organic by-products following disinfection/oxidation of drinking water. It is suspected that most precursors to disinfection by-products are humic, although nonhumic substances are also suspected of contributing to these by-products. Many of the disinfection by-products have adverse health effects in humans (i.e., carcinogenic or mutagenic effects). The primary chlorinated disinfection by-products of concern include trihalomethanes, haloacetic acids, and haloacetonitrile. Fluorescence spectroscopy was used to study humic and fulvic acids. The two fractions of humic substances, humic and fulvic acids, were characterized by a double-peak phenomena in an overlapping fluorescing region. Disinfection by-product formation potentials of humic and fulvic acids have been correlated with total organic carbon, UV absorbance at 254 nm, specific absorbance and fluorescence. River humic and fulvic acid was found to have the highest reactivity to disinfection by-product formation as compared to soil and peat humic and fulvic acid. Fluorescence spectroscopy has shown to be a rapid and predictive tool for disinfection by-products formation potential of humic and fulvic acids.     

长江中下游火山-侵入杂岩研究中值得探讨的几个问题(一)

长江中下游燕山期中酸性-酸性火山-侵入杂岩大家公认为具有偏碱性到碱性特点，但对富碱原因即碱质来石源则存在不同意见，大多数人认为壳幔亮混源，碱质来源于富集地幔的部分熔融，也受到地壳物质的混染．另一种意见强调富碱是由于岩浆侵位或分异过程中受到蒸发岩（特别是膏盐层）的混染与同化。笔者根据长江中下游有关岩体的大量岩石化学分析数据．分地区、分岩体、也按时代对其K2O、Na2O、CaO、MgO与SiO2的相关性作了直观性对比分析，事实表现出Na2O对SiO2几乎完全没有相关性，Na2O对SiO2可以说是独立变化的；K2O与MgO对SiO2具有不同程度的相关性；而CaO－SiO2则具有明显的直线性相关。据此提出：除了原始岩浆具有的碱质外，在岩浆分导过程中不时地有外来碱质加入，这些外来的碱质主要由中、下三叠统中的膏盐层提供。文中根据岩浆硫的δ34S值偏高、膏盐层主要矿物的自由能在高温下熔融及分解温度与低温下在水中的溶解度、石膏矿山的矿泉水中K＋、Na＋、C1＋、SO32-等的浓度，以及斜长石的环带构造方面作了论证．     

Biologie und Biochemie des Elements Selen

The importance of selenium as an essential trace element has progressively emerged during the last years due to the analysis of selenium deficiency diseases and to the identification and characterization of a number of selenoenzymes. Selenium is incorporated in the catalytic site of the enzymes as an integral selenocysteine residue. The pathway of selenocysteine biosynthesis and incorporation has been elucidated recently for Escherichia coli. This article presents an overview on these subjects and describes the mechanisms which confer selenocysteine specificity in the framework of protein biosynthesis. In addition, some considerations concerning the phylogeny of selenocysteine incorporation are presented and a model for the evolution of the selenocysteine pathway is proposed.     

A polyiodide with regular I 4 2− chains: Tl6PbI10

The Science of Nature -     

西部干旱半干旱地区水资源再生利用分析

结合西部干旱半干旱地区的地域特点、水文特征和水资源开发利用状况，分析论述了该地区水资源短缺与水污染加剧这一矛盾所决定的西部地区水资源开发利用的特点及其对地区经济发展的制约，认为水资源的再生利用是解决西部地区水资源危机的一条有效途径。以城市污水为再生水源，根据该区域特点，提出了西部干旱半干旱地区水资源再生利用的研究内容。