岩溶地区不整合地层系统地基评价——以贵州省天柱碳酸钡工程场地为例

岩溶地区不整合地层系统之岩土构成复杂。通过对贵州省天柱碳酸钡工程场地的勘察,选择卵(碎)石土层作地基持力层,采用浅基础方案及碎石层褥垫等地基处理措施,避让了岩溶等对地基稳定性的影响,为该地区的工程建设提供了岩土工程治理的经验。     

废弃矿井地下水污染特征及防治技术

分析了我国目前废弃煤矿的现状，阐述了废弃煤矿将会造成的地下水污染特征及污染机理，并提出对废弃矿井地下水污染进行了研究和治理的技术思路。     

二维地下水水量水质管理模型

通过数值方法建立了抽水井水质与注水井水质的非线性响应关系，采用非线性的多项式函数形式，应用Ｍａｒｑｕａｒｄｔ法拟合，在管理模型的求解中应用Ａｖｒｉｅｌ－Ｗｉｌｌｉａｍｓ法处理负系数问题。实例计算结果表明，几何规划法的应用是可行的，该方法可应用于多排注水，抽水井情况。     

裂隙地下水中残留LNAPL物理驱替冲洗实验

利用透明复制裂隙模型，选择两种典型LNAPL（轻非水相液体）-邻二甲苯和十二烷残留体，开展一系列水流驱替冲刷和SDS（十二烷基磺酸钠）表面活性剂增强驱替实验，直接获取了裂隙内部LNAPL残留体几何形状与分布情况，结果表明：水流驱替冲刷和SDS驱替裂隙内残留体的去除率分别为8.3%~12.3%和65.9%~82.1%.残留体累积去除率随着驱替流体雷诺数的增加而增加.水流驱替冲刷条件下，残留体离散为小液滴，数量比初始残留状态增加1.3~2.2倍.SDS表面活性剂降低了"LNAPL-水"间的界面张力，能够有效去除裂隙内较大残留体，驱替后仅残余单个面积为1mm²左右的微小液滴.由于粗糙裂隙的非均质性，水流冲刷易导致系统内的"LNAPL-水"有效界面面积增加，对LNAPL污染修复不利，表面活性剂增强修复是一种更有效的方法.     

焦作市某赤泥堆放场周围地下水水质评价

焦作市某赤泥堆放场一期工程采用了在堆放场底部铺设赤泥加石灰垫层和防渗膜的工程防渗处理措施.基于其防渗处理现状,文章探讨了该区域地下水对赤泥冲灰水的日最大允许入渗量,和赤泥冲灰水的实际日渗透量.评价了该防渗处理措施的可行性和在地下水日活动量稳定的状况下,该赤泥堆放场对周围地下水的影响.结果表明:将赤泥加石灰垫层用作防渗的措施值得大力推广;该堆放场在使用年限内不会对周围区域地下水水质造成太大的影响.     

污灌区地下水中有机污染物的分离鉴定与致突变活性研究

应用XAD系列大孔网状树脂萃取富集法,结合GC、GC/MS/DS1的分离鉴定技术,研究了北京东郊污灌区深层(90m)和浅层(18m)地下水中的有机污染物。采用LSC-GC/MS/DS装置测定了地下水中的挥发性有机物,并对水样进行了Ames试验以检验水样的致突变活性。结果从深井水样中检出32种非挥发性有机物,未检出挥发性有机物,致突变试验阴性。浅井水样中同时检出非挥发性和挥发性有机物。两种菌株在所有试验条件下均呈现阳性致突变反应。     

河北省藁城市蔬菜种植区化肥施用与地下水硝酸盐污染研究

通过农户问卷调查和地下水田间取样分析 ,主要对河北省藁城市蔬菜种植区的化肥施用与地下水硝酸盐污染现状进行了研究。结果表明 :2 0 0 1年藁城市蔬菜种植区化肥施用纯量为 1 4 0 8.6kg·hm-2 ,其中氮肥施用纯量为 84 0 .8kg·hm-2 ;藁城市各蔬菜种植模式下氮肥施用量由高到低的顺序依次为大棚 >温室 >中棚 >小棚 >地膜 >露地 ;温室、中棚和露地蔬菜区地下水硝酸盐含量最高值出现在 8月 ,而地膜蔬菜区则在 1 1月 ;各蔬菜种植模式对地下水影响的大小顺序为地膜 >中棚 >温室 >露地 ,影响因素主要有密集度、种植模式、种植年限、氮肥施用量和土壤质地等。     

涕灭威对地下水污染敏感区的预测与区划试点

本文根据涕灭威在室内模拟试验与田间试验的结果，详细剖析了影响涕灭威农药在土壤中残留和移动的各种因子，建立了涕灭威农药对地下水污染的敏感性模型，并就涕灭威农药在江苏使用后对地下水可能造成污染的情况进行了预测与区划试点，结果与用美国环保局提供的ＰＲＺＭ模型计算结果和田间实测结果基本一致，本模型可用于预测涕灭威农药在其它地区使用后对地下水可能造成污染的情况。     

Impact of urbanization on hydrochemical evolution of groundwater and on unsaturated-zone gas composition in the coastal city of Tel Aviv, Israel

The coastal city of Tel Aviv was founded at the beginning of the 20th century. The number of its inhabitants and its water consumption increased rapidly. This study analyses a 15-year record (1934-1948) of pre-industrial development of groundwater chemistry in the urban area. Archive data on concentrations of major ions, dissolved gases (CO2 and O2), organic matter, and pH were available for each half-year during the period of 1934-1948. The major factors causing changes in the chemistry of groundwater flowing in three sandy sub-aquifers have been seawater encroachment due to overpumping, and infiltration of effluents from pit-latrine collectors. Influence of these factors decreases with depth. Landward-penetrating seawater passed through clayey coastal sediments, interbedded among sands and calcareous sandstones, and spread into the Kurkar Group aquifer. This has led to exchange of sodium (dominant in seawater) with calcium adsorbed on clay particles, enriching groundwater with calcium. Intensity of cation exchange decreases inland and with depth. Infiltration of pit-latrine effluents has introduced large amounts of ammonium into the unsaturated zone. Its rapid oxidation in unsaturated sediments has caused massive nitrate production, accompanied by pore-water acidification. This process induces dissolution of vadose carbonate, resulting in enrichment of groundwater recharge in calcium. Anthropogenically induced dissolution of calcite in the unsaturated zone has been the major factor for the increase of Ca2+ concentration in groundwater, accounting for about 80% of this increase. In the interface zone, an additional 20% of calcium has been supplied by cation exchange. Owing to pH increase caused by denitrification in the aquifer, Ca(2+)-rich waters supersaturated with calcite could be formed, especially in the capillary fringe of the uppermost sub-aquifer, which could induce calcite precipitation and ultimately lead to the cementation of sandy aquifers. Urban development has caused drastic changes in the gas content in the unsaturated zone and in groundwater. Carbon dioxide was intensively generated by nitrification-denitrification processes, by hydration of urea, to a lesser degree by oxidation of organic matter, and probably by anoxic biodegradation of organics. Between 1934 and 1948, concentrations of CO2 in unsaturated sediment air rose from 3.2% to 7.6%. In the unsaturated zone, oxygen consumption for oxidation of ammonium and organic matter lowered O2 concentrations in sediment air to unusually low values of 3.9-12.9%. Nitrification in the urban unsaturated zone could thus serve as a pump, sucking in atmospheric oxygen at a rate of about 0.3-0.5 g m-2 day-1. The extreme concentrations of CO2 and O2 in unsaturated sediments have been preserved due to production and consumption of gas under conditions of diminishing areas open to the atmosphere, uncovered by buildings and by roads.     

Use of environmental isotopes and hydrochemistry as indicators for the origin of groundwater resources in El Dabaa area,northwestern coastal zone of Egypt

The EI-Dabaa area is located on the northwestern coastal zone of Egypt and is considered to be one of the most important regions for land reclamation and agriculture. In addition, it has been selected as a potential site for constructing Egypt's first nuclear power plant.In April 1989, 14 groundwater samples were collected from the area as well as collecting samples from the Mediterranean sea and from local rainwater. These samples were subjected to chemical and environmental isotope analyses. The results of the analyses for stable isotopes (oxygen-18 and deuterium) indicate that the main recharge source of the groundwater in El-Dabaa is the local precipitation during the rainy season. Variation of the environmental tritium content as well as in the chemical composition of both major cations (Na,K,Ca,Mg) and major anions (Cl,SO₄,HCO₃) between different groundwaters in the studied area reflect the high degree of inhomogeneity of the aquifer and different recharging conditions due to permeability of the water bearing formation.The chemical water type of the El-Dabaa groundwater is sodium sulphate (Na₂SO₄) and the SAR values illustrate the suitability of these groundwaters for agricultural purposes.