深圳妈湾排海工程非设计条件下海水入侵与冲洗研究

本文从微观的角度，分析了排海工程扩散管内海水入侵与冲洗的临界水力特点，并通过理论分析和物理模型试验的相互验证，得出了上述临界水力条件的判别关系式，提出了判别方法，并由此得到了深圳妈湾排海工程防止海水入侵的临界排放流量和出现海水入侵后的最小冲洗流量，为排海工程在非设计条件下的运行管理提供了依据。     

滨海地带地下水面与咸淡水界面伴随着潮汐波动而变化的规律的探讨研究(Ⅰ)二维数值仿真数学模型的建立及其效度的验证

在研究海岸带广泛存在的凸凹不平的不透水层的几何及地质特性的基础上,结合地下水渗流运动的特征,运用数理分析的手法,建立了不同于以往的模拟海岸带含水层咸淡水界面变动规律的二维数值仿真数学模型.其后,通过与实验数据的对比验证了其效度.     

莱州湾滨海平原咸水入侵分析与趋势预测——以山东省广饶县为例

文章以鲁北平原山东省广饶县为例,阐述了咸、淡水形成的地质背景、咸淡水变化带形成与演化;分析了大规模开发利用地下水引起的咸水入侵的历史与现状;采用非确定性模型方法对咸水入侵趋势进行了预测,提出了缓解咸水入侵的对策与建议。取得的主要认识和结论为:(1)鲁北平原自山前冲洪积扇向莱州湾滨海平原,地下水水质具有水平和垂直分带特征;(2)20世纪70年代中期大量开采南部地下淡水后,地下淡水水位持续下降,破坏了咸淡水之间的水动力平衡,北部咸水向南入侵,引起淡水咸水、机井报废等一系列环境地质问题;(3)预测结果表明,在不采取调控措施情况下,咸淡水界面以每年平均240m速度向南部推进;(4)人工回灌、营造淡水帷幕并减少淡水区开采量是防止咸水入侵的有效途径。     

秦皇岛洋河－戴河沿海平原海水入侵数值模拟分析

在分析洋河-戴河沿海平原水文地质条件的基础上,运用FEFLOW软件,建立了三维变密度溶质运移模型。以2002-12至2004-12的地下水位和水质观测资料,对模型进行了率定。用检验后的模型对研究区海水入侵原因进行了模拟分析,对不同开采条件、不同防治措施下的海水入侵发展趋势进行了预测。模拟结果表明：滨海地区超采地下水是造成海水入侵的根本原因,河流长期低水位导致海水倒灌加剧了海水入侵的程度;在滨海地区,只要地下水降落漏斗存在,就会引发海水入侵进一步向内陆移动;同时,根据预测结果,提出了防止和减缓海水入侵的措施。     

RATIONAL PROTECTION OF WATER RESOURCES IN COASTAL ZONES THROUGH PLANNED DEVELOPMENT1

ABSTRACT: A significant water-resources problem in Florida and other coastal states where the ground-water resources are threatened by salt-water intrusion or direct pollution from septic tanks, canals or marinas, is the almost explosive urban development of the limited coastal zone without or with only little water related planning. The reported study deals with the establishment of methods for identification of areas which are suitable for development and of areas where complete preservation or controlled and limited development should be encouraged. A methodology using data input available from such federal and state agencies as the USGS, the U. S. Weather Bureau, and the various State Geological Surveys is developed and brought on a graphic form that will guide the planning process and allow the urban planner even without a background in geohydrology or water-resources engineering to identify the problem areas.     

FRESH GROUND WATER STORED IN AQUIFERS UNDER THE CONTINENTAL SHELF: IMPLICATIONS FROM A DEEP TEST,NANTUCKET ISLAND,MASSACHUSETTS1

ABSTRACT: A deep water-resource and stratigraphic test well near the center of Nantucket Island, about 40 miles (64 km) off the New England Coast, has encountered freshwater at greater depth than predicted by the Ghyben-Herzberg principle. An uppermost lens of fresh-water, which occupies relatively permeable glacial-outwash sand and gravel to a depth of 520 ft. (158 m), is probably in hydrodynamic equilibrium with the present level of the sea and the height of the water table. However, two zones of freshwater between 730-820 ft. (222-250 m) and 900-930 ft. (274-283 m) are anomalously deep. A third zone extending from 1150-1500 ft. (350-457 m) contains slightly salty ground water (2 to 3 parts per thousand dissolved solids). Several explanations are possible, but the most likely is that large areas of the Continental Shelf were exposed to recharge by precipitation during long periods of low sea level in Pleistocene time. After the last retreat of glacial ice, seawater rapidly drowned the shelf around Nantucket Island. Since then, about 8000 years ago, the deep freshwater zones which underlie dense clay layers have not had time to adjust to a new equilibrium. Under similar circumstances freshwater may remain trapped under extensive areas of the Continental Shelf wherever clay confining beds have not permitted saltwater to intrude rapidly to new positions of hydrodynamic equilibrium. The implications are far reaching because all continental shelfs were exposed to similar hydrologic influences during Pleistocene time.     

ADVANCES IN THE BOUNDARY INTEGRAL EQUATION METHOD IN SUBSURFACE FLOW1

ABSTRACT: This paper explores some of the advances of the boundary element method, as applied to ground-water problems, during the last five years. Although the method is still somewhat limited compared to solution by finite elements, the range of solutions has increased considerably. Diffusion and advection-diffusion solutions are done efficiently. These include the incorporation of inhomogeneity, anisotropy, and nonlinear diffusion. The difficult problem of stream-aquifer interaction is an important application as it is much easier to follow a free surface with its multiple configurations. The application must be able to cycle between ground-water connection and disconnection with the stream and include seepage surfaces. Flow in fractured media is a natural application where the flow in fractures can usually be treated without a computational exception in spite of extremely high aspect ratios. The case of seawater intrusion forms a type of free surface problem and thus is a case for which the method has special advantages. For these and other applications the boundary element method provides an inexpensive technique for calculation where the data preparation and setup time is minimal. In most of these cases, programs can and have been written on microcomputers.     

Emission rates of chlorinated volatile organics from new and used consumer products found during vapor intrusion investigations: Impact on indoor air concentrations

Consumer products can emit chlorinated volatile organic compounds (CVOCs) that complicate vapor intrusion (VI) assessments. Assessment protocols acknowledge the need to remove these products during VI investigations, but they can be problematic to identify and locate. Predicting if the products cause detectable air concentrations is also difficult since emission rate information is limited and can vary with product use and age. In this study, the emission rates of 1,2-dichloroethane, trichloroethene, tetrachloroethene, and carbon tetrachloride from four consumer products identified as indoor sources during VI field investigations were measured under laboratory conditions using a flow through system. Emissions of PCE from an adhesive container tube ranged from 1.33 ± 1.13 μg/min (unopened) to 23.9 ± 2.93 μg/min (previously opened). The laboratory-measured emission rates were used to estimate indoor air concentrations, which were then compared to concentrations measured after the products placed were into an actual residence. The estimated and measured indoor air concentrations were generally comparable, showing that emission rate information can be used to determine the relative impact of internal CVOC sources.     

美国污染场地清理的风险评估简介及政策制定

本文主要介绍美国加州污染场地清理的风险评估的概念,方法,计算和风险管理.从而引进挥发性污染物室内入侵风险评估方法来制定污染场地清理标准.讨论如何运用数学模型计算土壤清理浓度和挥发性污染物室内入侵风险评估.在风险评估基础上,加州环保署水质管理局颁布了地下储油罐低风险结案政策.政策中的污染场地清理定量标准是由人体健康风险评估方法计算得出.最后,用一个具体的美国加州洛杉矶案例介绍风险评估方法是怎样运用在污染场地清理修复中,以回答污染场地修复的关键问题"多干净算干净".     

基于实测资料的长江河口南支河段盐水入侵规律分析

为对长江口南支河段盐水入侵规律有清晰的认识,在梳理、总结以往研究成果的基础上,通过对历年咸潮及氯度实测资料的分析,对长江口南支河段盐水入侵的规律进行了较为全面系统的分析研究。研究表明：北支盐水倒灌是长江口南支河段盐水入侵的主要来源;在研究水域,枯季大潮期氯度的沿程分布表现为两头高、中间低的“马鞍形”形式,枯季中潮期则为“高 低 高 低 高”的复杂的“W”形的分布形式;受外海潮汐和上游径流的综合作用,由大潮到中潮,倒灌盐水团在下移过程中,氯度的沿程分布形式发生了变异;近期盐水入侵的程度有加剧的趋势;研究水域2～3月盐水入侵最严重,在这段时间内盐水入侵超标次数多、历时长;当大通流量小于20 000 m3/s时,就可能发生明显的北支盐水倒灌南支现象;盐水入侵程度跟大通流量和潮汐强度密切相关;大通流量越大,盐水入侵程度越低;潮差越大,盐水入侵程度越高