关于长江产业带建设总体布局的初步思考

重点开发长江是90年代中国经济重大战略布署。将长江产业带建设成具有强大经济实力的国家一级经济轴线,宜采用分层次推进与中心辐射相结合的发展战略,以浦东开发和三峡建设为契机,加强基础产业,发展新兴产业和第三产业,优化产业结构,以能源和交通建设先行,改善基础设施。同时,要协调产业带建设与浦东开发、三峡工程建设的关系。     

视力与环境

眼睛,是心灵的窗口,没有它,多精彩的世界也会黯然无色.世之贵者莫过于人,人之贵者莫过于眼.眼睛,视物之宝、灵魂之窗、情感之镜、智慧之源,眼为万物色之美,人凭眼目以为光.美丽的世界只有通过眼睛才得以体现.可是近段时期,人们的视力总体水平不断下降,最明显的是表现在近视、白内障等眼疾的患者急剧增加,给患者的生活、工作带来许多的行动不便.身患视力障     

城市空气中多环芳烃定量测定方法

本文发展了一种对城市空气中多环芳烃(PAH)定量测定的方法。该方法可以用极少量溶剂,相当快地完成测定工作。     

生态足迹影响因子的定量分析

人口的膨胀和人类工业化进程的加剧，使得人类向自然界获取越来越多的资源，同时向环境源源不断的输入废弃物，已经严重超过了自然生态系统的供给能力和环境容量，生态环境日益恶化，水土流失、草场退化、植被消亡、生物多样性锐减、全球变暖等情况已经严重到难以遏制的地步，危及到人类自身的生存。在和平与发展成为世界两大主题的今天，人们越来越关注可持续发展的问题。在现有资料的基础上，利用主成分分析方法，定量地讨论了中国各省（区市）1999年生态足迹大小与其影响因子间的关系。结果表明，生态足迹的大小是各省（区市）的大中型企业个数、全社会固定生产投资等众多因子共同作用的结果，其中总人口和GDP是生态足迹大小的主要影响因子，其因子载荷量分别达到了0.940和0.913。值得一提的是非农业人口与生态足迹的相关系数超过了农业人口，这说明由于消费模式和生活水平等的差异，非农业人口对生态足迹的影响大于农业人口对生态足迹的影响。在此基础上建立了生态足迹影响因子的多元线性回归模型，以期为生态足迹在进行区域可持续发展评价的方法上提供新的思路。     

OPC技术在安防系统中的应用

OPC是一种建立在COM技术基础上的用于加工控制的OLE。从本质上说，OPC定义一种共用接口，这种接口能够使接口开发工作一经完成就很容易重新使用。     

新型污水生化参数测试仪的研制和应用

介绍了ＤＯ、ＢＯＤｓ、Ｒｓ、ＫＬａ及α、β、θ等污水处理工程常用生化参数的测试原理和仪器应用。用ＢＯＤｓ替代ＢＯＤ５使测试时间从５天缩短到２０分钟，参数值一致。上述参数的测试仪器已鉴定投产。     

离子色谱法分离La系元素——电子选择性不同可同时测定过渡金属和镧系金属

稀土元素的测定,特别是镧系元素,在各种工业中是很重要的。例如,在核动力工业中,对处置放射燃料的镧系分裂产物的测定就是称为燃耗(burnup)参数的衡量尺度。在矿业中各种岩石样中的痕量镧系元素的测量有助于勘探者寻找镧系矿藏。 同样,地质样中痕量镧系元素的浓度可为判断一些地质形成过程提供线索。岩石中镧系元素的浓度一般都不随时间而变。因此分析镧系物对探索地质成因及其运动可提供一个“指痕”(fingerprint),因为没有任何两个取自不同地点的样品是具有相同断     

塞浦路斯的地震危险性

<正> 1 地震危险性评定历史地震危险性评定在塞浦路斯虽处于初始阶段,但并未忽视其重要性。地震危险性评定对结构(如构筑物和大坝)的设计安全性参数确定所起的关键作用已有充分认识。到目前为止,已进行了两个场地的地震危险性评定。第一项是确定一大坝坝址预期最大可能地面加速度(Neophyton,1981),第二项估计尼科西亚老城墙以内地区不同烈度地震过程中人员及财产可能损失(Constantinon,1990),研究结果公布于地质调查局的内部报告上。对市区及近郊的岩土工程编图方面,也做了大量工作。测定了Larnaca镇沿海地区的潜在疑难层,如冲积层和高有机含量沉积层(Michaelides,1988)。在塞浦路斯,尽管全国地震危险性图有震中分布图(公元前180～公元1972年)、具有预期最大地面加速度值的观测烈度带图(公元前180～公元1980)和最大能量释放带图(1901～1972),但至今尚未进行综合地震危险性评定研究。     

The role of socio-economic data in food needs assessment and monitoring

This paper reviews six case studies examined as part of a project to review targetting methodologies employed by non-government organisations in Africa during the 1984-6 food crisis. Most agencies have not yet fully evaluated the role of data in informing policy decisions during their respective emergency programmes. The case studies presented reflect a wide variety of approaches to targetting emergency food aid that are based largely on the use of 'socio-economic' data. The recent emergency relief operations in Africa seem to indicate a change in relief agencies' approaches to the assessment and monitoring of needs of the affected populations. Earlier dependance on nutritional data has given way to an increasing reliance on the use of socio-economic indicators. There was a wide variation in the case studies of the type of indicators collected and utilised in needs assessment and monitoring. There were those who relied almost exclusively on nutritional data to target resources during the 1984-86 African crisis, and others whose experiences during that period lead them to attach more weight to socio-economic data. Other agencies appear to have recognised the problems of relying solely on nutritional data to target food aid during their 1984–86 emergency programmes, and thus more or less abandoned classical anthropometric surveys in their needs assessment and monitoring methodologies during this period. Thus nutritional data has a less significant role in the decision making process than previously had been the case.     

The qiongshan earthquake of july 1605

In 1605 a destructive earthquake affected the northern region of Hainan Island and adjacent parts of the Chinese mainland. Based on a detailed analysis of contemporary chronicles, the authors present a revision of the effects of the earthquake, and show that a sequence of strong shocks throughout 1605 caused cumulative damage and relatively heavy loss of life in Qiongshan. The subsidence of large areas of coast round Puqian Bay and Dongzhai Port is shown to be due to a combination of liquefaction caused by the shock, the occurrence of a typhoon associated with flooding and exacerbated by a high surge tide, as well as a long-term process of active tectonic movement in the area; the subsidence was not caused by downthrow of the earth's crust during the shock. Topographical changes in the area, traced from historical maps, suggest that subsidence is continuing, but a survey of the long-term seismicity of Hainan Island indicates that it is not an area of exceptional seismic risk.