城市水资源水环境系统多阶段灰色动态仿真模型

本文依据城市人口,经济,水资源和水环境之间的相互影响,相互制约关系,建立了城市水资源水环境系统阶段灰色动态仿真模型,以预测不同仿真方案下城市水资源与水环境系统的变化。     

水分在季节性冻土中的运动

季节性冻土是一种冰水共存的特殊土水体系,在分析冻土中水分运动的驱动力及其影响因素,冻土介质的物理特性（热特性和水力特性）及其参数测定方法的基础上,综述了水分在冻土中运动的基本规律及定量研究水分运动的试验与数值模拟方法。     

矿山排水泵站微机通信测控系统

针对目前平庄矿务局元宝山露 天矿的实际情况,利用ＭＣＳ－９６系列单片机成了矿山排水泵站微机通信测控系统。该系统由调度端和终端站组成,调度端与终端站之间的信息伟递采用无线通讯方式。且具有多机通信功能,故系统具有高可靠性和高性能价格比。     

美东地区罗德河流域地下水中铝形态分布的化学平衡模式计算

美东地区的罗德河流域遭受着严重的酸沉降侵蚀．在酸性条件下,铝从土壤中大量溶解并迁移到水环境中．地表水中升高的铝浓度对鱼类产生毒害,监测地表水和土壤水中的铝形态及浓度变化已成为问题的关键．本文报导了用化学平衡模式计算法分析美东地区罗德河流域地下水中的铝形态分布,获得了有价值的结论     

给水度与饱和差关系的初步研究

通过对给水度与饱和差的理论分析,明确了给水度与饱和差在基本概念上的差别;得出了饱和差通常是大于给水度而小于孔隙度,以及只有岩土体积含水率达到持水度时饱和差与给水度才相等的结论;给出了饱和差与给水度之间的定量关系式。这些结果得到了室内试验的验证。     

水库二维水流泥沙数学模型及应用

建立水库坝区平面二维水流泥沙数学模型,考虑了悬移质非均匀,非饱和输沙特性,采用正交曲线坐标拟合复杂边界、ＳＩＭＰＬＥＣ程式离散求解及动边界技术。用该模型对白沙水库流场和河床变形进行了数值验证,计算了典型年条件下,水库取水口附近流场和河床局部形态。结果表明,坝前取水口漏斗基本保持稳定状态。     

流动显示技术及其在温排放模型试验中的应用

简介了作者的流动显示方法（包括应用塑料示踪剂、间隙曝光装置、定时控制器和普通照相机来拍摄水工整体试验中大范围流动的照片（流谱图））;并利用微机图形处理系统,对实拍流谱图进行图／数处理（包括光学修正、网格插补等预处理和信息处理）,从中识别出流体物理参数及其等值线分布图（包括流速场、流函数场和涡度场等）。作为实例,介绍了应用本流动显示技术和方法,在某电厂温排水整体试验中获得取排水口近区流场定量信息的情     

木兰溪两岸浅井水对紫露草四分体微核率的影响

采用紫露草四分体微核技术,对莆田木兰溪下游河溪水和饮用的浅井水进行致突变性监测。结果表明,１０份河溪水能明显诱发紫露草四分体微核率的增高;与对照组相比１０份浅井水也均不同程度提高了四分体微核效应,８份已达到显著或极显著水平（Ｐ〈０．０５或Ｐ〈０．０１）,且与诱发的紫竹梅四分体微核效应显著相关,ｒ＝０．９７７７。说明浅井水内存在致植物细胞染色体畸变物质,提示当地居民上消化道肿瘤高发与饮水污染有一定相     

Isolation of Some Soluble and Dispersed Materials of Oregano Water

Recent results obtained on determining the extraction efficiency and composition of organic volatiles in Oregano Water obtained from Origanum onites L. are described. Oregano Water was subjected to liquid-liquid extraction with a range of solvents with different polarities and each extract was analyzed by GC/MS.     

Voltammetry in Undiluted Acetic Acid. In Situ Determination of Water

Water present in undiluted acetic acid can be monitored in situ with Pt and Au microelectrodes using differential pulse and square‐wave voltammetries. Both reduction and oxidation peaks can be obtained. The best quantitative analytical results were obtained for the anodic peak, the Pt microelectrode, and differential pulse voltammetry. The anodic water peak is located at +1.55 V vs. the quasi reference Pt electrode. The voltammetric peak obtained at Pt electrode is apparently not a diffusional one, however, the calibration plot obtained by employing this peak is linear over a wide concentration range, up to 4 mol dm^?3. The detection limit has been estimated as 2.3 mM or 0.0043 v/v%. The developed method may be particularly useful, since the Karl Fischer method can not be used to determine water in glacial acetic acid due to the estrification reaction of acetic acid with methanol. A voltammetric wave of undiluted acetic acid could not be obtained in the positive and negative ranges of potential.