安全也需送“清凉”

今年夏季高温天气来的快、来的早,给人们正常的生活和各行各业工作带来了一定的影响。企业如何做好高温季节的安全生产工作,这里就有一个送“清凉”的问题。按照以往惯例,每逢这个季节,也是一些单位各类事故频率最高的时候,这是因为天气炎热而造成人体的不舒适和设备安全运行参数下降的关键所在。所以,防暑降温工作是这个时间段安全生产的重头戏。但是如何做好送“清凉”工作,笔者以为关键是三点:     

使用紫外闪光灯处理受污染的水,气,土壤

本文介绍了一种新的有效的处理挥发性有机化合物(VOC′S)、聚氯联苯化合物(PCB′S)和其他有机毒物的方法。这个新方法是采用高强宽谱的紫外光线(UV)直接光解有机物,分解的最终产物是无毒的单质物质。新方法的效靛优于使用中压汞灯做光源的传统 UV 处理工艺。     

责任关怀--罗门哈斯的安全理念

何谓“责任关怀”（ResponsibleCare）？责任关怀是指一个化学品制造厂商在开展其业务的同时，对人身安全、健康和环境的重要性所采取的高度重视态度。其中特别强调社区的认知权和参与性。责任关怀的概念源于加拿大，起源于上世纪80年代后期，现已为全世界45个国家的化学品制造     

西澳大利亚布罗克曼火山岩型稀有金属矿床──奈厄比厄姆凝灰岩的矿物学和地球化学

西澳大利亚布罗克曼稀有金属矿化，是富含挥发份和不相容元素（例如Zr、IJf、Nb、Ta、Be、Y和REE及Ga等）的粗面岩岩浆发生早期火山碎屑喷发的结果。矿化呈三。粒状（＜20μm），是由于相对简单的岩浆前身矿物（如铌铁矿和钻石），在岩浆喷发后保存于灰流凝灰岩［奈厄比厄姆（Niobium）凝灰岩］中的岩浆期后富F溶液的作用下，发生蚀变和再活化的结果。球粒陨石标准化的REE分布模式显示，矿体强烈富集HREE。胶质锆石是HREE主要载体，浸染状氟碳铈矿（±氟碳钙铈矿和直氟碳钙铈矿）是LREE的载体，晚期方解石脉中的羟硅滚石是Be的载体。Ga赋存于基质K云母中。上覆于奈厄比厄姆凝灰岩的粗面岩流含有许多类似的矿石矿物，但含量略有不同。     

天马腾飞──德阳市市中区经济开发区一瞥

天马腾飞──德阳市市中区经济开发区一瞥邓永德，田柯（本刊记者）在“德政如阳”的德阳市区西侧，一直流传着从西方“极乐世界”——如来佛座下飞来了一匹金色的天马，造福这方故土的神话故事。这里的人，祖祖辈辈都盼望着“天马”带来“福气”，时光流逝，夙愿依旧！但...     

Effect of nickel on some aspects of protein metabolism in the gill and kidney of the freshwater fish, Cyprinus carpio L

Nickel has an adverse effect on some aspects of protein metabolism of the freshwater fish, Cyprinus carpio. The main changes observed were: (a) Decrease in soluble, structural and total proteins, AlAT and AAT activities with an increase in the levels of free amino acids, protease and GDH activities and ammonia in the gill and kidney at 1, 2, 3, and 4 days of exposure to a lethal concentration, 40 mg litre(-1) of nickel; (b) Increase in soluble, structural and total proteins, free amino acids and the activities of protease, AlAT, AAT and GDH with a decrease in ammonia and urea in these organs at 1, 5, 10 and 15 days of exposure to sublethal concentration, 8 mg litre(-1); (c) The magnitude in these changes increased over time with both concentrations of the metal, and was more marked in gill than in kidney.     

Fluxes of ions in precipitation, throughfall and stemflow in an urban forest in Kuala Lumpur, Malaysia

A study was carried out to determine the chemical composition of bulk precipitation, throughfall and stemflow in an urban forest in Kuala Lumpur, Malaysia. The mean weekly rainfall recorded during the period of study was 63.2 mm. Throughfall, stemflow and canopy interception of incident precipitation were 77.1%, 1.2% and 21.7% respectively. Bulk precipitation, througfall and stemflow were acidic, the pH recorded being 4.37, 4.71 and 4.15 respectively. In all cases the dominant ions were NO3, SO4, Cl, NH4, K, Ca and Na. Of the ions studied Ca, K, Cl, SO4, Mg and Mn showed net increases in passing through the forest canopy, while NH4, Na, NO3, Zn, H and Fe showed net retention. This study shows that the urban environment of Kuala Lumpur contributes considerable amounts of materials to the atmosphere, as reflected by the high ionic contents in bulk precipitation, throughfall and stemflow.     

Impacts of afforestation on water quality trends in two catchments in mid-Wales

The impact of afforestation on stream-water chemistry for two catchments in central Wales is investigated. Trends in water chemistry are evaluated with forest age progressing at 8-15 years and 20-27 years. To assess the possible exacerbating effect of afforestation on surface-water acidification two moorland catchments are used as controls. Absolute differences in inter-catchment streamwater chemistry are evident. Differences in acidity between the moorland and the young forest site reflect site preparation and modifications to water pathways. Differences in the observed present day chemistry between the young and old forest result from past interactions between deposition changes during forest development. An estimate of the future impact of forest growth was attained from model predictions. The model was calibrated to present day stream-water chemistry and incorporates, cation uptake, evapotranspiration/ concentration effect and increased scavenging of occult and dry deposition. Predictions suggest the pH will decline to 5.3 when the young forest progresses to 20 years of age, which is still much higher than the pH recorded at the older forest site at the age of 20 years.