共查询到19条相似文献,搜索用时 156 毫秒
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海(咸)水入侵与浅层地下水水化学特征及变化研究 总被引:9,自引:1,他引:8
利用山东莱州湾沿岸海水入侵监测剖面的水化学监测数据,从水化学指标与Cl^-含量的关系入手,采用不同侵染程度组段钭所选定的水化学指标对Cl^-含量作回归分析的方法,对海水入侵过程中浅层一上水水化学特征变化作了研究。研究表明,多数水化学指标及几项灌溉水质指标与侵染程度有较明显的宏观相关性,但不是简单的线性关系,两个剖面分析数据的对比揭示出莱州湾东部与南部沿岸海水入侵的区域差异性。 相似文献
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长江与黄河沉积物金属元素地球化学特征及其比较 总被引:27,自引:0,他引:27
研究了长江干流和黄河干流沉积物中金属元素(Li,Na,K,Ca,Ba,Ti,V,Cr,Mn,Fe,Co,Ni,Cu,Zn,Al等共16种)_总量与形态特征。 相似文献
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运用数理统计和模糊数学评价秦皇岛洋戴河平原的海水入侵程度 总被引:4,自引:1,他引:3
运用数理统计方法获取秦皇岛洋戴河平原地下潜水和海水的水化学统计特征,据此优选出4项海水入侵评判指标,建立各评判指标的背景值及指标等级体系,并将模糊数学综合评价法和地理信息系统结合起来评价研究区潜水含水层的海水入侵程度。研究结果表明:氯离子Cl-、电导率EC、溶解总固体TDS和潜在盐度是指示本区潜水含水层海水入侵程度的最佳指标,其判别海水入侵发生的下限值分别为250 mg/L、1 250μs/cm、700mg/L和8.5 meq/L;洋戴河平原潜水含水层的海水入侵程度总体上为中等水平,洋、戴河间浦河一带的潜水含水层海水入侵程度最为强烈。 相似文献
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本文测定了三元系RECl3(RE=La,Pr,Sm)-HOAc-H2O(30℃)的平衡态的溶度数据并绘制了相应的溶度图.在三个体系中分别形成LaCl3·7H2O,PrCl3·6H2O,SmCl3·6H2O三种物质.HOAc对LsCl3·7H2O,PrCl3·6H2O,SmCl3·6H2O盐析作用程度的不同,表明了轻稀土元素的“一分组效应”,同时依据HOAc对LaCl3·7H2O,PrCl3·6H2O,SmCl3·6H2O有盐折作用这一结论,提出了一种制备LaCl3·7H2O,PrCl3·6H2O,SmCl3·6H2O的新方法. 相似文献
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1991年12月~1992年1月,在中国第八次南极考察途中,用分级撞击式采样器采集了13个气溶胶样品,用PIXE法分析了样品中的Al、Si、P、S、Cl、K、Ca、Ti、V、Cr、Mn、Fe、Ni、Cu、Zn、Br、Pb等17种元素,并应用富集因子分析、相关分析和主因子分析,研究了气溶胶粒子中的元素组成、浓度粒度分布、气溶胶的地球化学类型、主要来源及其贡献。结果表明:研究区气溶胶中元素的来源、组成、浓度粒度分布具有明显的地理规律性;气溶胶的来源,如海洋气溶胶除主要来源于海水、受所在洋区及其周围环境的影响外,还受全球性和局地性大气环流的控制,如近岸大气明显受陆源(地壳源和人为源)传输的影响;该年内发生的菲律宾皮纳图博火山和智利哈得逊火山爆发,以及海湾地区的战争等突发事件,对研究区大气也产生了影响。 相似文献
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测定了三元体系RECl3(RE=Dy,Yb)-HOAc-H2O(30℃)的平衡态的溶度数据并绘制了相应的溶度图。在两个体系中分别得到了DyCl3.6H2O和YbCl3.6H2O两种固相。依据HOAc和DyCl3.6H2O和YbCl3.6H2O有盐析作用这一结论得到了一种制备DyCl3.6H2O和YbCl3.6H2O的HCl-HOAc法。同时, 在分析测定酸的重百分浓度时,利用“差减法”得到了H的准 相似文献
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针对海水入侵现状评价中单指标(Cl-或矿化度)评价方法的片面性和不确定性等问题,本文将熵值理论和属性识别模型相结合,建立了熵权属性识别模型,并将其应用于滨海地区海水入侵现状评价中。以潍北平原8 个海水入侵实测点为应用实例进行研究。结果表明,潍北平原大部分地区海水入侵属于轻度侵染,水质为微咸水,东部地区(6、8 号点位)在5 月份海水入侵属于较严重侵染,但在11 月份侵染程度减缓,可能的原因是气候因素(降水增加、海平面上升)以及人为因素(地下水抽水量减少)等共同影响的结果。同时,5 月及11 月各个测点海水入侵侵染排序略有差异,但是差异较小。通过实例证明,该方法通俗易懂,计算方法简洁明了,便于掌握和应用,为海水入侵现状评价提供了一种可行有效的方法。 相似文献
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Eastern and southern coastal zones of Laizhou Bay are the most representative seawater intruded areas in the world, with two intrusion sources of contemporary seawater and paleobrine. In order to reveal the complicated hydrochemical changing process and the mechanism of fresh groundwater being polluted by saltwater, we conducted long-term observation and hydrochemical analysis at four observing sections of typical salt-fresh water transitional zone. The study indicates that seawater and brine intrusion processes have different hydrochemical features, and that ion exchange and adsorption actions between water and aquifer produce great influence on the intrusion. 相似文献
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Seawater intrusion is a special process of groundwater pollution. The contemporary seawater intrusion and buried paleobrine intrusion especially the latter in eastern and southern coasts of Laizhou Bay are the most representative ones in the world [1]. According to the research on seawater intrusion at home and abroad, In-depth studies on change process and mechanism of hydrochemical composition, while ion adsorption and exchange between the permeable stratum and groundwater are studied shall… 相似文献
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The south coastal plain of Laizhou Bay is one of the typical salt-water intrusion areas in China, the occurrence and development of which was closely related with the palaeoenvironment evolution. Systematic analyses of pollen, foraminifera and grain size composition based on ^14C and luminescence dating from two sediment cores were performed for the purpose of understanding the salt-water intrusion in the coastal plain of Laizhou Bay from the perspective of environmental evolution since late Pleistocene. It could be classified into seven evolution stages since 120 kaBP: 120-85 kaBP was a transition period from cold to warm; 85-76 kaBP was a period with warm and wet climate having swamp lakes developed in the lower reaches of the Weihe River, south coastal plain of Laizhou Bay; 76-50 kaBP was characterized by grassland vegetation and coarse sediments in terrestrial environment, which was the early stage of Dali Ice-Age; 50-24 kaBP was a period with alternate sea deposition in the south coastal plain of Laizhou Bay; 24-10 kaBP was the late stage of Dali Ice-Age with coldest period of Quaternary, the south coastal plain of Laizhou Bay was dry grassland and loess deposition environment; 10-4 kaBP was another warm and wet climate period, sea level was high and regressed at 4 kaBP; and has been the modern sedimentary environment since 4 kaBP. Among the three warm stages, including 85-76 kaBP, 50-24 kaBP and 10-4 kaBP, corresponded to late Yangkou, Guangrao and Kenli seawater transgression respectively. The duration of the latter one in south coastal plain of Laizhou Bay was longer than that in west coast of Bohai Sea and east coast of Laizhou Bay. The three periods of seawater transgression formed the foundation of salt-water intrusion in this area. 相似文献
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The south coastal plain of Laizhou Bay is one of the typical salt-water intrusion areas in China, the occurrence and development of which was closely related with the pa-laeoenvironment evolution. Systematic analyses of pollen, foraminifera and grain size com-position based on 14C and luminescence dating from two sediment cores were performed for the purpose of understanding the salt-water intrusion in the coastal plain of Laizhou Bay from the perspective of environmental evolution since late Pleistocene. It could be classified into seven evolution stages since 120 kaBP: 120–85 kaBP was a transition period from cold to warm; 85–76 kaBP was a period with warm and wet climate having swamp lakes developed in the lower reaches of the Weihe River, south coastal plain of Laizhou Bay; 76–50 kaBP was characterized by grassland vegetation and coarse sediments in terrestrial environment, which was the early stage of Dali Ice-Age; 50–24 kaBP was a period with alternate sea deposition in the south coastal plain of Laizhou Bay; 24–10 kaBP was the late stage of Dali Ice-Age with coldest period of Quaternary, the south coastal plain of Laizhou Bay was dry grassland and loess deposition environment; 10–4 kaBP was another warm and wet climate period, sea level was high and regressed at 4 kaBP; and has been the modern sedimentary environment since 4 kaBP. Among the three warm stages, including 85–76 kaBP, 50–24 kaBP and 10–4 kaBP, corresponded to late Yangkou, Guangrao and Kenli seawater transgression respec-tively. The duration of the latter one in south coastal plain of Laizhou Bay was longer than that in west coast of Bohai Sea and east coast of Laizhou Bay. The three periods of seawater transgression formed the foundation of salt-water intrusion in this area. 相似文献
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莱州湾南岸咸水入侵区晚更新世以来的古环境演变 总被引:8,自引:0,他引:8
莱州湾南岸是我国典型的咸水入侵区,古环境变化构成了现代咸水入侵发生的背景。本文通过对潍河下游地区A1、A5孔岩芯系统的孢粉、有孔虫、粒度、14C及热释光测年资料的分析,结合100余个钻孔的沉积特征,论述了莱州湾南岸地区晚更新世以来的古环境演化特征。本区经历了三次明显的冷暖气候波动,三次显著的暖湿期为85~76kaBP、50~24kaBP、10~4kaBP,为海陆过渡相沉积环境,这三个时期分别与晚更新以来的三次海侵相对应,与相邻区域相比,全新世海侵开始早、结束晚;两次冷干期为76~50kaBP、24~10kaBP,分别对应于早大理冰期、晚大理冰期,为陆相沉积环境。 相似文献
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A rapid increase in the number of tourists has placed a heavy demand for freshwater on Manukan Island, a small island located
offcoast of Kota Kinabalu, Sabah. Hydrochemical and numerical approaches have been applied in this study to evaluate the groundwater
quality of unconfined aquifer lying in Manukan Island, Sabah, East Malaysia. This is vital to enhance better understanding
about groundwater management. Hydrochemical analysis output indicated NaCl water type in sampling locations. Seawater intrusion
is marked by its relatively high Na+, Mg2+, Cl− and SO4
2− concentrations. Hydrochemical analysis output clearly showed the influence of seawater in groundwater of Manukan Island.
The numerical model output proved the influence of seawater in groundwater of Manukan Island by indicating the upconing process
at the beneath of the pumping well. Current status of seawater intrusion in Manukan Island is about 14.6% of freshwater and
seawater mixing ratio in low lying area of Manukan Island as simulated by SEAWAT-2000 model output. Numerical model SEAWAT-2000
output showed clearly that the upconing process is the possible route of seawater to influence the fresh groundwater aquifer
chemistry in Manukan Island. The results have enhanced the current understanding of seawater intrusion in the study area.
Future studies will focus on using numerical models to simulate and suggest suitable groundwater management plans in Manukan
Island. 相似文献