河流水污染定量研究进展

水质模型可定量地反映出水质状况与污染物排放之间的关系,从而为进行水质评价与预测、选择污染控制方案以及制定水质标准和排放污染规定提供可靠的依据.文章从建立模型所采用的数学方法角度出发,较为详细的概述了近年来水质模拟的研究进展,并对确定性模型所存在的问题和河流水质模型的发展趋势做出评价.     

甲烷高温自燃诱导过程实验与数值模拟研究

甲烷的转化在化工产业中具有举足轻重的地位与战略意义,近年来涌现的氧化偶联制烯烃等多种新型化工工艺涉及高温条件的甲烷-纯氧等体系的混合与反应过程,明确甲烷高温自燃诱导与爆炸规律是实现工艺安全设计与运行的前提,然而相关研究与基础数据仍较为欠缺。通过利用基于快速压缩装置的高温高压燃爆测试系统开展甲烷-纯氧等典型混合体系的自燃诱导过程研究,同时基于GRI-Mech 3.0机理的数值模拟方法进行了数值模拟研究。实验结果与数值模拟结果吻合较好,随着温度/压力的增加及氧气含量的下降,混合体系自燃诱导时间均缩短;燃料气中加入乙烷或氢气则会大幅缩短自燃诱导过程。对于多个工艺过程中涉及的低氧含量体系率先开展了研究,得到了不同当量比及温度条件下的典型体系自燃诱导时间,同时考察了惰性气的加入对于自燃诱导过程的延长作用。研究结果有助于深入理解甲烷自燃诱导机理,同时指导高温条件的甲烷转化工艺的本质安全化设计与爆炸防控。     

碳酸锶废水对生态环境的影响调查及治理方案

碳酸锶因电子工业飞速发展而身价百倍，但其生产废水的直接排放则造成了严重的环境污染，本文通过对水体、农业、渔业、人体健康和水生生物等多种因素调查，掌握了碳酸锶废水污染成因，同时提出了资源再利用方案。     

液氯泄漏事故模拟分析

针对1996年1月21日在西班牙发生的一起液氯泄漏事故的后果进行了模拟分析。模拟分析结果同事故实际所造成的后果是一致的。表明采用基于数学模型的事故后果模拟分析具有一定程度的可靠性。对于救灾和对重大危险源编制应急事故预案有一定程度的指导意义。     

The Water Poverty Index: Development and application at the community scale

The article details the development and uses of the water poverty index (WPI). The index was developed as a holistic tool to measure water stress at the household and community levels, designed to aid national decision makers, at community and central government level, as well as donor agencies, to determine priority needs for interventions in the water sector. The index combines into a single number a cluster of data directly and indirectly relevant to water stress. Subcomponents of the index include measures of: access to water; water quantity, quality and variability; water uses (domestic, food, productive purposes); capacity for water management; and environmental aspects.
The WPI methodology was developed through pilot projects in South Africa, Tanzania and Sri Lanka and involved intensive participation and consultation with all stakeholders, including water users, politicians, water sector professionals, aid agency personnel and others. The article discusses approaches for the further implementation of the water poverty index, including the possibilities of acquiring the necessary data through existing national surveys or by establishing interdisciplinary water modules in school curricula. The article argues that the WPI fills the need for a simple, open and transparent tool, one that will appeal to politicians and decision makers, and at the same time can empower poor people to participate in the better targeting of water sector interventions and development budgets in general.     

Numerical Simulation of Synoptic Condition on a Severe Sand Dust Storm

By using observational data and MM5, an observational analysisand numerical study was conducted on the synoptic condition of a severe dust storm that was caused by a Mongolian cyclone whichoccurred from 6 to 8 April 2001. Results illustrated thatthe cyclogenesis was due to the isentropic potential vorticity (IPV) advection in the upper troposphere and the terrain modifiedbaroclinicity in the mid-lower troposphere. The Altai-Sayan complex of mountains blocked the lower level cold air and made the isentropic surface sharply steep. When the air slid down along the isentropic surface the increasing of baroclinicity anddecreasing of stability blew up the vertical vorticity development.The formation of the dust storm was a result of a cyclonic cold front passing across the area. The occurrence of this dust stormwas closely related to the strong surface wind, which was accompanied by a cold front passing, rather than the cyclogenesis, itself. Hence, the reason for the pre-front dust storm formulation was the formation of heating convection. Reasons behind the formation of a black storm (visibilitylower than 50 m), which occurred in the mid-north part ofInner Mongolia, lay in several aspects. Firstly, in thisarea the surface wind was strong, a direct result of thedownward transport in mid-lower troposphere. Secondly,the cold front passed over the effected area near sunsetso the air obtained much more surface heating to form adeeper mixed layer (ML). Thirdly, cooperation between thelower level wind and the terrain made the atmosphere inthis area and acquired the maximum advective contributionnecessary to form a deep post-front ML. The sensitivityexperiment revealed that surface heat flux was important to the frontal lifting. In addition, the forcing of surface heating wasalso seen as the primary forcing mechanism of frontogenesis. Meanwhile, removal of the surface heat flux made the atmosphericstratification became stable and the pre-storm ML very shallow,which weakened the strength of the dust storm.     

土地利用变化驱动下的上海市区水灾灾情模拟

对上海市区近50年来的土地利用结构变化进行了重建，并计算了由土地利用变化引起的上海市区水位变化量。以特定的1962年水灾为参照，模拟在同等雨强情况下，由土地利用结构变化和地面沉降引起的淹没范围的变化以及由此带来的水灾损失的变化。结果表明，在49mm／d降水条件下，由于土地利用的变化，使2001年的径流系数比1950年增大了34．0％，2001年的水位比1950年增高了45．9％；2001年的水灾灾情为1950年的1．0629倍；即使在目前千年一遇的防洪标准下，亦可造成相当于2001年地均GDP值0．088％(约为4．5亿元人民币)的损失，这是1991年相应数值的220倍。     

关于环评中的景观影响评价问题

环境影响评价制度对控制环境污染和防止生态破坏取得明显的成效。随着社会的进步和人们对环境质量的高要求,景观环境影响评价已成为旅游资源、森林资源、矿产资源开发以及交通运输等建设项目环境影响报告书中的重要内容。但由于目前尚缺乏评价规范和评价标准,在开展景观影响评价中存在着不少的困难,评价标准和评价等级的缺乏,使评价的深度和广度以及景观污染的界定上难以满足评价结果的要求;评价方法的不确定,又使评价过程难以统一,难以预测项目建设对景观的影响程度,而人才的缺乏则是困扰持证单位的主要问题。所以目前急切需要解决问题的办法是尽快制定景观评价的标准和规范,研究评价的方法,以加速人才的培养,使景观影响评价真正能达到保护景观的目的。     

秦皇岛市生态状况及资源开发利用水平分析综述

秦皇岛市区内生态类型多样,各类生态系统功能突出,自然资源丰富,尤其是海、旅游资源优势突出,为区域经济发展提供了良好的基础条件。该文对秦皇岛市生态系统平衡及资源开发利用水平进行了定量分析。     

关于制定连云港市水土保持生态建设规划的思考

连云港市地处欧亚大陆桥的东桥头堡,是沿海十四个开放城市之一,国家定位是将其建设成为连接太平洋沿岸与中亚地区的国际商贸中心和全国性的旅游城市。而目前的山丘区水土流失严重,植被稀少,生态环境恶化,与国家定位目标和连云港市发展目标相差甚远。因此在制定水土保持生态环境建设规划时,必须紧紧围绕改善生态环境这条主线,以增加农民收入和改善生存条件为突破口,因地制宜,坚持长期综合治理,方能实现“山川秀美”之目标。