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1.
崔仲元  李洪文 《黑龙江地质》2001,12(3):38-46,62
七星泡矿泉水是特定的水文地球化学环境下形成的酸性矿泉水。它含适量的常量元素和丰富的微量元素,多项指标达到国家医疗矿泉水和饮用水天然矿泉水界限指标要求。酸性矿泉水有较强的杀虫灭菌力。由于它含适量的常量化学组份和人体必需的微量元素,因此具有一定的医疗保健用,可以预防和治疗多种外科疾病和慢性疾病。文章论述了人体必需的微量元素的生理功能与生物学作用,讨论了各种元素对的适应症和过量、缺乏不适的不适症。提出了对酸性矿泉水的开发利用建议。  相似文献   

2.
文章叙述了饮用天然矿泉水的特点及其保健功能。因各种饮用天然矿泉水的保健功能取决于它所含的特征性生物微量元素,故文章又叙述了生物微量元素的定义,介绍了几种生物微量元素I、F、Zn、Se、Ge在人体内的生理功能,以及在国外矿泉水生产销售中的新动向,并简要介绍了部队的低矿化度饮用水矿化卫生标准。  相似文献   

3.
高亚峰 《城市地质》2001,13(3):43-45
主要叙述了饮用天然矿泉水、纯净水、超纯水及其它常见饮用水的各自特点,并进行了综合对比分析。详细阐述了天然饮用矿泉水的保健作用,其主要取决于天然饮用矿泉水所含的特征性微量元素,并介绍了所含Si、Sr、Zn、Li、Se、I等几种微量元素对人体的保健作用,进而说明天然饮用矿泉水是最理想的饮用水。  相似文献   

4.
经科学测定,人体血液中各种化学元素,微量元素平均值与地壳中元素的丰度值密切相关。矿泉水溶解了地壳中相关地层的矿物质,所以矿泉水中所含人体必需的微量元素和矿物质也最接近人体的自然状态。从营养学上讲,矿物质、微量元素在人体中所起的作用不亚于维生素,它的作用要比我们认识到的大得多。而且维生素可在人体内合成,矿物质则不行,只能外补。  相似文献   

5.
《地下水》2016,(3)
对凉州区高坝镇饮用天然矿泉水水源地进行了水文地质调查、分析测试等相关工作,分析了该矿泉水形成条件及水质特征。其中微量元素锶含量为0.506~0.640 mg/L,已达到国家饮用天然矿泉水标准,具有较高开发利用价值。本文对其矿泉水形成条件进行了初步探讨,并对该矿泉水的水质进行了分析,对今后该矿泉水合理开发利用资源提供参考依据。  相似文献   

6.
随着营养学和微量元素研究的发展,人们进一步认识到饮用矿泉水对于增强体质,去病延年的作用。但天然饮用矿泉水受多种因素限制,难以满足人们需要。地质学家、矿物学家开始模拟天然矿泉水形成作  相似文献   

7.
草帽顶子矿泉水为偏硅酸矿泉水.含有钴、锶等多种人体必需的微量元素,是一处优质天然矿泉水。起源于大气降水.矿化时间约15年.流量较大,具有重要的开发利用价值.  相似文献   

8.
饮用天然矿泉水的保健作用   总被引:2,自引:0,他引:2  
饮用天然矿泉水受到消费者的广泛欢迎,畅销于消费市场,主要是它来自地下深处,富含对人体健康有益的多种适量矿物组分与微量元素。西方人嗜饮矿泉水已有两个世纪的历史,我国近二十年来也有越来越多的人饮用,突显饮用天然矿泉水的神秘魅力。  相似文献   

9.
王娟  龚庆红 《吉林地质》2013,(4):120-123
红丰泉为偏硅酸型矿泉水,含有锶、锂、锌多种对人体健康有益的微量元素,是一处优质天然矿泉水,流量大,具有重要的开发利用价值。  相似文献   

10.
承德作为京津冀水源涵养地,其天然矿泉水和山泉水等水资源丰富,分布广、流量大、水质优,且多为弱碱性或中性淡水,富含钾、钙、镁、锶、锂、锌、偏硅酸等多种矿物质及微量元素。通过对承德地区矿泉水资源分布情况的研究,总结不同类型的矿泉水在承德地区的分布规律,并对不同类型矿泉水形成的地球化学条件做了阐述。  相似文献   

11.
矿泉水中的饮用天然矿泉水在地下深循环条件下形成,化学成分稳定,水源卫生,细菌学指标安全。有一定含量的矿物盐、微量元素或二氧化碳气体,作为一种天然饮料,是其他饮用水无法比拟的,无须医生指导,长期饮用也不会对人体产生危害。  相似文献   

12.
福建省饮用天然矿泉水资源丰富,但主要为偏硅酸型,水源地遍布全省,但规模一般较小,根据我省已鉴定的饮用天然矿泉水资源的基本概况,特点进行总结,并对福建省饮用天然矿泉水资源评价中存在的若干主要问题进行探讨,同时对资源评价,开发提出了建议。  相似文献   

13.
黄镜友 《湖南地质》1992,11(2):134-139
湘乡市东山天然饮用矿泉水,是我省首次发现的大型含锌矿泉。它发育在北东向东台山含水断层带上,该断层长60km以上,倾向北西,斜贯湘乡境内,向西南通过歇马花岗岩体。在泉区,沿断层带发育一条硅化破碎带,最厚处达150m。断层上盘为白垩—第三系红层,下盘为板溪群,均为不透水层,对矿泉起遮挡保护作用。本矿泉水量丰富,每昼夜可取水2000t。泉水中锌和偏硅酸含量,已达到国家天然饮用矿泉水标准,另含10种人体必需的微量元素,属少见的优质矿泉。  相似文献   

14.
盘山花岗岩裂隙水研究   总被引:2,自引:0,他引:2  
张伟  王作友 《地质论评》1996,42(1):87-92
盘山花岗岩裂隙水起源于大气降水,赋存于各种成因的裂隙中,裂隙水年龄从小于4a到接近40a,差异较大。裂隙水中常量元素和微量元素主要来源于长石类矿物的水解,特别是钙长石的水解,其中SiO2和Sr在裂隙水中含量较高,已达到饮用矿泉水标准。裂隙水可开采资源量多年平均为1291.56万m^3/a,富水规律明显。  相似文献   

15.
《Applied Geochemistry》1995,10(2):133-144
The effect of local geology and land-use practices on dissolved U was investigated by analysis of surface water and some springs in the Arkansas River valley of southeastern Colorado. Water samples were collected during a 2 week period in April, 1991. The rate of increase of U concentration with distance downriver increased markedly as the river flowed from predominantly undeveloped lands underlain by igneous and metamorphic rocks to agriculturally developed lands underlain by marine shale and limestone. An additional abrupt increase in dissolved U was observed along the section of river where discharge is often greatly reduced because of extensive diversions for irrigation and where remaining flow is largely composed of irrigation return water. Dissolved U in this last section of river and in most of its tributaries exceeded the proposed U.S. drinking water standard of 20 μ/L In water samples collected from agricultural areas dissolved U showed strong positive correlation with major dissolved constituents Na, Ca, Mg, and SO4 that increase as a result of sulfate mineral dissolution and clay mineral ion-exchange reactions in weathered shale bedrock and shaley soils. Highly soluble minor and trace elements Cl, Li, B, Sr, and Se that are not subject to strong sorptive uptake or precipitation in this setting also correlated positively with U. These combined observations indicate that natural leaching of U-bearing shale bedrock and derivative soils, additional leaching of rock and soil by irrigation water, and evaporative concentration in a semi-arid climate can produce concentrations of dissolved U in surface water and shallow ground water that may threaten nearby drinking water supplies. Other agriculturally developed areas of the semi-arid Western U.S. with similar geology are likely to contain high concentrations of U in irrigation drain water.  相似文献   

16.
The market for mineral water has been growing steadily over the last few years. Germany is the country with the highest number of bottled mineral water brands (908 bottled water samples from 502 wells/brands were analyzed). The per capita consumption of mineral water in Germany in 2003 was 129 L. A wide range of values of one to seven orders of magnitude was determined for 71 elements in the bottled water samples analyzed by ICP-QMS, ICP-AES, IC, titration, photometric, conductometric and potentiometric methods. A comparison of the element concentrations and the legal limits for both bottled and tap water (EU, Germany, US EPA, WHO) shows that only 70% of the 908 mineral water samples fulfill the German and EU drinking water (i.e., tap water) regulations for all parameters (not including pH) for which action levels are defined. Nearly 5% of the bottled water samples not fulfill the German and EU regulations for mineral and table water. Comparison of our results with the current German and European action levels for mineral and table water shows that only 42 of the bottled water samples exceed the limits for one or more of the following elements: arsenic, nitrate, nitrite, manganese, nickel and barium concentrations. Ten of the bottled water samples contain uranium concentrations above the 10 μg/L recommended limit.  相似文献   

17.
至2002年,本市已勘查鉴定了80处矿泉水。矿泉水主要赋存于第四纪孔隙承压含水层及岩溶裂隙含水层中,矿泉水达标元素较单一,水化学类型繁多,单井允许开采量相差悬殊及区域分布不均。勘查评价和开发的重点将是寻找符合人们饮水习惯的低矿化度矿泉水。  相似文献   

18.
Twenty-two bottled mineral and spring waters from Norway, Sweden, Finland and Iceland have been analysed for 71 inorganic chemical parameters with low detection limits as a subset of a large European survey of bottled groundwater chemistry (N = 884). The Nordic bottled groundwaters comprise mainly Ca–Na–HCO3–Cl water types, but more distinct Ca–HCO3, Na HCO3 and Na–Cl water types are also offered. The distributions for most elements fall between groundwater from Fennoscandian Quaternary unconsolidated aquifers and groundwater from Norwegian crystalline bedrock boreholes. Treated tap waters have slightly lower median values for many parameters, but elements associated with plumbing have significantly higher concentrations in tap waters than in bottled waters. The small dataset is able to show that excessive fluoride and uranium contents are potential drinking water problems in Fennoscandia. Nitrate and arsenic displayed low to moderate concentrations, but the number of samples from Finland and Northern Sweden was too low to detect that elevated concentrations of arsenic occur in bedrock boreholes in some regions. The data shows clearly that water sold in plastic bottles is contaminated with antimony. Antimony is toxic and suspected to be carcinogenic, but the levels are well below the EU drinking water limit. The study does not provide any health-based arguments for buying bottled mineral and spring waters for those who are served with drinking water from public waterworks. Drinking water from crystalline bedrock aquifers should be analysed. In case of elevated concentrations of fluoride, uranium or arsenic, most bottled waters, but not all, will be better alternatives when treatment of the well water is not practicable.  相似文献   

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