Al13形态分离纯化方法的初步研究

对ＳＯ＾２－４／Ｂａ＾２＋法分离提纯Ａｌ１３形态的影响因素进行了研究,实验结果表明,聚合铝浓度、ＳＯ４／Ａｌ比、Ｂａ／ＳＯ４摩尔比、以及超声反应时间对分离效果上具有较大的影响。较高浓度的聚合铝利于沉淀的形成与分离。同时选用１：１的ＳＯ４／Ａｌ与Ｂａ＾２＋的共存对形态分析不产生影响,形态鉴定结果表明,经过上述分离条件所得产物形态为Ａｌ１３。     

兰州市大气颗粒物中水溶性离子研究

本文对兰州市不同季节大气颗粒物中水溶性离子的主要理化特性及其与降水的关系进行了研究，认为大气颗粒物中水溶性离子是当地降水中ＳＯ４＾２－，Ｃａ＾２＋，Ｃｌ＾－等主要离子的来源。在１３种被测的水溶物中，ＳＯ４＾２－和Ｃａ＾２＋离子所占比例较高，分别占总离子的３１．４％和２７．８％，年均浓度值为１０．７２μｇ／ｍ＾３和３．９６μｇ／ｍ＾３。同时大气颗粒物中水溶物浓度与ＳＯ２，ＴＳＰ等大气污染物浓度之间也     

PACS的结构特征及絮凝性能研究

制备了碱化度及Ａｌ＾３＋／ＳＯ＾２－４摩尔比不同的系列ＰＡＣＳ，分别进行常压（干燥温度１０５℃）及真空干燥（真空度为－０．０９８ＭＰａ、干燥温度６５℃）制备固体产品。用红外光谱及Ｘ－射线衍射谱研究了碱化度、Ａｌ＾３＋／ＳＯ＾２－４摩尔比、干燥温度对ＰＡＣＳ的结构影响，比较了干燥温度不同对ＰＡＣＳ固体样品的溶解度及絮凝效果的影响，借助于显微电泳测定技术研究不同碱化度及不同Ａｌ＾３＋／ＳＯ＾２－４摩尔     

Al—Ferron逐时络合比色法研究PACS中铝的水解聚合形态

制备了碱化度及不同Ａｌ＾３＋／ＳＯ＾２＝４摩尔比的系列ＰＡＣＳ，用Ａｌ－Ｆｅｒｒｏｎ逐时络合比色法研究了铝的形态分布，考察了碱化度，Ａｌ＾３＝／ＳＯ＾２＝４摩尔比，稀释作用及ｐＨ值对铝的形态分布的影响。     

流动注射荧光分析法用于土壤及水系沉积物中铈（Ⅲ）含量的测定

研究表明Ｃｅ＾３＋在ｐＨ〈６．２ＫＣｌ介质中以２５４．０ｎｍ紫外光激发时，在３５２．０ｎｍ处发出具有恒定强度的荧光。因而可选择ｐＨ５－６作为测定酸度条件，利用Ａｌ２（ＳＯ４）３消除Ｆｅ＾３＋等离子的干扰，建立起Ｃｅ＾３＋的流动注射荧光分析法。方法的线性范围是２．０×１０＾－７—２．０×１０＾－６ｍｏｌ／ｌ，一元回归方程△Ｆ＝６６３６００Ｃ－０．０４１（ｎ＝１０，ｒ＝０．９９９７），检测限６．０×１     

磷和硫对空心菜吸收砷的影响

本文通过水培空心菜中砷与磷以及砷与硫配比试验，研究了ＰＯ＾３－４和ＡｓＯ＾３－４以及ＳＯ＾２－４和ＡｓＯ３＾３－４共存对空心菜生长及砷累积的影响。结果表明：５ｍｇ．ｌ＾－１ＰＯ＾３－４或ＳＯ＾２－４时，ＡｓＯ＾３－４显著降低空心菜产量，ＰＯ＾３－４和ＳＯ＾２－４含量提高到３０－１００ｍｇ．ｌ＾－１时，空心菜产量明显提高。．     

聚硅氯化铝（PASC）的形态分布及转化规律：Ⅱ.^27Al—NMR法研究PASC溶 …

采用＾２７Ａｌ－ＮＭＲ法比较研究了ＰＡＳＣ与ＰＡＣ中铝的形态分布。实验结果表明，在ＰＡＳＣ中，由于聚硅酸与铝水解聚合物产物间的相互作用，使得铝的水解聚合形态分布及转化情况发生了变化。在相同Ｂ值条件下，ＰＡＳＣ中Ａｌ单和Ａｌ１３的含量低于ＰＡＣ中相应Ａｌ单和Ａｌ１３的含量，而ＰＡＳＣ中Ａｌ其它的含量大于ＰＡＣ中Ａｌ其它的含量，其差值随着碱化度（Ｂ）和Ａｌ／Ｓｉ摩尔比的减小而增大。     

阴离子态养分从第四纪红壤中的淋失特征

在实验室条件下，将第四纪红壤进行淋洗试验，旨在研究第四纪红壤中阴离子态养分的含量及其淋失特征。结果表明，第四纪红壤中各种可溶发生 阴离子态养分含量除ＮＯ＾－３和Ｃｌ＾－外，其它都是很低的，６种阴离子在第四纪红壤中的淋失强弱顺序是：Ｃｌ＾－〉ＮＯ＾－３〉Ｈ２ＢＯ＾－３〉ＳＯ＾２－４〉ｍＯｏ＾２－４？〉ｈ２ｐｏ＾－４，而土壤对它们的固定或吸附能力则相反。     

Fe（Ⅲ）水解过程中无机阴离子的影响作用

本文通过ＰＯ＾３－ ４，Ｆ＾－，ＳＯ＾２－ ４，Ｃｌ＾－，ＮＯ＾－ ３和ＣｌＯ＾－ ４存在时，０．１ｍｏｌ／１ ＦｅＣｌ３溶液的碱中和曲线的分析对比，说明了用曲线斜率区分滴定曲线为三个区域：（Ａ）自发水解反应；（Ｂ）聚合反应；（Ｃ）沉淀反应，以及阴离子对中和曲线的影响及其规律，指出阴子子对Ｆｅ（Ⅲ）浓度中和反应影响为不同程度的竞争配位，参与聚合及电中和脱稳，使沉淀反应提前等。并与ＯＨ＾－共同形成Ｆ     

聚硅氯化铝（PASC）的形态分布及转化规律：Ⅲ.Al—Ferron逐时络合比？…

本文对Ａｌ－Ｆｅｒｒｏｎ逐时络合比色法和＾２７Ａｌ－ＮＭＲ法对ＰＡＳＣ和ＰＡＣ中铝的形态分布测定结果进行了对比分析的讨论。结果表明。在ＰＡＣ中，Ａｌ１３和Ａｌｂｈ之间具有良好的对应关系。Ａｌ１３／Ａｌｂ比值为１．０左右。但对ＰＡＳＣ而言，情况有所不同，在低碱化度（Ｂ）和低Ａｌ／Ｓｉ摩尔比情况下，Ａｌ１３和Ａｌｂ之间的不存在对应关系，Ａｌ１３和Ａｌｂ比值远远小于１．０，随着Ｂ值和Ａｌ／Ｓｉ摩尔比的升     

Fluoride content and distribution pattern in groundwater of eastern Yunnan and western Guizhou, China

For study, the fluoride (F) content and distribution pattern in groundwater of eastern Yunnan and western Guizhou fluorosis area in southwestern China, the F content of 93 water samples [groundwater (fissure water, cool spring, and hot springs), rivers water] and 60 rock samples were measured. The result shows the F content of the fissure water and cold spring water is 0.027–0.47 mg/L, and river water is 0.048–0.224 mg/L. The F content of hot spring water is 1.02–6.907 mg/L. The drinking water supplied for local resident is mainly from fissure water, cool spring, and river water. And the F content in all of them is much lower than the Chinese National Standard (1.0 mg/L), which is the safe intake of F in drinking water. The infected people in eastern Yunnan and western Guizhou fluorosis area have very little F intake from the drinking water. The hot spring water in fluorosis area of eastern Yunnan and western Guizhou, southwest China has high F content, which is not suitable for drinking.     

不同地区何首乌无机元素含量的比较

采用ICP法测定了不同地区何首乌植物及其生境土壤中的15种元素(Al、B、Ba、Ca、Cu、Fe、K、Mg、Mn、Na、Ni、P、Sr、Ti、Zn),分析比较了各种元素在不同地区何首乌体内和生境土壤中的分布规律及不同地区何首乌对无机元素的吸收富集能力.结果表明,不同地区何首乌和土壤中无机元素含量存在着显著差异,德庆、井冈山、靖西三地何首乌的Mn含量较高;不同地区何首乌对元素的富集系数无显著性差异,而何首乌对不同无机元素的富集系数则有显著差异,主要表现在对Ca、K、Mg、Sr的吸收富集能力较强.表6参14     

Spatial distribution of calcium in food, water and soil and its possible influence on rickets disease in Northern Nigeria

Since the 1990s, children of the Gbagyi tribe in Northern Nigeria have been suffering severe rickets with an incidence of up to 40% in the children's generation. The disease seems to be prevalent in an area of approximately 100 km(2) south-east of Kaduna. According to broad medical studies in that area, there is no evidence for a genetic disposition but for a nutritional cause of the disease. A lack of calcium was found in blood and was calculated to originate from diet. We therefore checked parent material, soil, maize cobs (Zea mays) and drinking water for their specific Ca contents from a region with rickets problem (study area A) and compared the results to Ca amounts in similar samples from a region where rickets is unknown among the Gbagyi population (study area B). It thereby became apparent that there are no differences in mineralogical composition of the parent material between the study areas, but that Ca contents in soil, maize cobs and drinking water are 47.6%, 26.6%, respectively, 79.1% lower in study area A compared to study area B. This result suggests that there may indeed be a nutritionally and/or environmentally influence on rickets disease. Nevertheless, further research on this topic is required.     

武汉月湖水体主要元素与浮游植物的PCA与CCA分析

通过2007年1—12月对武汉月湖不同的取样点进行监测,并选择汉江琴台段水域作为研究对照,调查了月湖水体硅藻、蓝藻与水体主要元素的种类,采用PCA、CCA分析法探讨了月湖水体硅藻、蓝藻与水体元素种类的关系。结果表明:月湖水体中所含元素全年监测出28种;汉江琴台段水域中所含元素全年监测出27种。经PCA分析表明,月湖水体中累计贡献率较大为磷(P)、砷(As)、铁(Fe)、铜(Cu)、锰(Mn);汉江琴台段水域累计贡献率较大为硅(Si)、锑(Sb)、镉(Cd)、钒(V)、钡(Ba)、Ag(银)、钼(Mo)。月湖水体中蓝藻密度大于硅藻,汉江琴台段水域硅藻密度大于蓝藻。经CCA分析表明,月湖硅藻密度与硒(Se)、锶(Sr)、银(Ag)、Ba、铝(Al)呈正相关关系;月湖蓝藻密度与P、Cu、铬(Cr)呈正相关关系,月湖蓝藻密度与镁(Mg)、镍(Ni)、钙(Ca)、锌(Zn)、硫(S)呈负相关关系。CCA分析中,汉江琴台段硅藻密度与铅(Pb)、硼(B)、As、Cr、Zn、Al、Cu、Mn、Fe、P呈负相关关系,汉江琴台段硅藻密度与Mo、Ca、钴(Co)、V、Sr、Ag呈正相关关系;汉江琴台段蓝藻密度与钠(Na)、S、Mg、Ni、钾(K)呈负相关关系。月湖水体缺乏可溶硅(dissolved silicon,DSi),硅藻会提升对其他元素(Se、Sr、Ag、Ba、Al)的吸收能力,这些元素会起到缺乏元素(Si)近似的作用,替代性可能出现。水中各种元素的组态是导致月湖浮游植物群落发生演变的重要原因之一。     

Inferring the fluoride hydrogeochemistry and effect of consuming fluoride-contaminated drinking water on human health in some endemic areas of Birbhum district,West Bengal

This research work is carried out to evaluate fluoride (F) hydrogeochemistry and its effect on the population of two endemic villages of Birbhum district, West Bengal. Fluoride concentration in drinking water varies from 0.33 to 18.08 mg/L. Hydrogeochemical evolution suggests that ion-exchange mechanism is the major controlling factor for releasing F in the groundwater. Most of the groundwater samples are undersaturated with respect to calcite and fluorite. Health survey shows that out of 235 people, 142 people suffer from dental fluorosis. According to fluoride impact severity, almost 80 and 94 % people in an age group of 11–20 and 41–50 suffer from dental and skeletal fluorosis, respectively. Statistically drinking water F has a positive correlation with dental and skeletal fluorosis. Bone mineral density test reveals that 33 and 45 % of the studied population suffer from osteopenic and osteoporosis disease. IQ test also signifies that F has a bearing on the intelligence development of the study area school children. The existence of significant linear relationship (R ² = 0.77) between drinking water F and urinary F suggests that consumption of F-contaminated drinking water has a major control over urinary F (0.39–20.1 mg/L) excretion.     

Fluoride distribution in groundwater and survey of dental fluorosis among school children in the villages of the Jhajjar District of Haryana,India

Fluoride concentration of groundwater reserves occurs in many places in the world. A critical area for such contamination in India is alluvial soil of the plain region, consisting of five blocks (Jhajjar, Bahadurgarh, Beri, Matanhail, and Sahalawas) of the Jhajjar District adjacent to the National Capital Territory of India, New Delhi. The purpose of this study was to assess the association between water fluoride levels and prevalence of dental fluorosis among school children of the Jhajjar District of Haryana, India. The fluoride content in underground drinking water sources was found to vary in villages. Hence, the villages were categorized as high-fluoride villages (1.52–4.0 mg F/l) and low/normal-fluoride villages (0.30–1.0 mg F/l). The source of dental fluorosis data was school-going children (7–15 years) showing different stages and types of fluorosis who were permanent resident of these villages. The fraction of dental fluorosis-affected children varied from 30% to 94.85% in the high-fluoride villages and from 8.80% to 28.20% in the low/normal-fluoride villages. The results of the present study revealed that there existed a significant positive correlation between fluoride concentration in drinking water and dental fluorosis in high-fluoride villages (r = 0.508; p < 0.001) and insignificant correlation in low-fluoride villages.     

Dental fluorosis associated with drinking water from hot springs in Choma district in southern province,Zambia

This study was conducted to investigate the high incidence of mottled teeth among residents of an area with hot springs in the Choma District of the Southern Province of Zambia. A survey involving 128 pupils was conducted at a Basic School to collect data on pupil’s backgrounds and their main sources of drinking water between birth and age 7. A dental specialist examined the pupils’ teeth and samples of drinking water were collected from locations where the majority of the pupils lived. It was analysed for fluorides and other drinking water quality parameters. Results of the survey showed a highly significant (P < 0.001) association between pupils’ main sources of drinking water between birth and age 7 and the incidence of discoloured teeth. All (100%) pupils who drank water from hot springs before age 7 had moderate to severe fluorosis, while the majority (96.7%) of the pupils who drank water from other sources had no dental fluorosis. Fluoride concentrations ranged from 5.95 to 10.09 mg/l in water from hot springs, and from 0.03 to 0.6 mg/l in water from other sources. Fluoride levels in water from hot spring water samples exceeded the 1.5 mg/l WHO guideline value for drinking water, while those in water from other sources were significantly (P < 0.05) lower than this. We conclude that the high prevalence of mottled teeth among residents of the study area is a case of endemic dental fluorosis associated with drinking water from hot springs containing high concentrations of fluoride.     

Fluoride in Ceylon tea and its implications to dental health

The purpose of this study was to assess the fluoride content of Ceylon Tea, which is a popular beverage throughout the world. The fluoride content of tea infusions prepared from different grades of tea leaves collected from different parts of the tea-growing regions (25 samples) of Sri Lanka was measured using a fluoride-selective electrode. Fluoride leaching was found to vary from 0.32 to 1.69 mg F/l, but there were no significant differences in terms of fluoride leaching between tea from different tea-growing regions or between tea of different grades. Dental fluorosis is widespread throughout the dry zone of Sri Lanka, and drinking water has traditionally been considered to be the main contributory factor to the development of fluorosis. However, diet, the consumption of tea in particular, may also contribute to the manifestation of dental diseases.     

太湖水华蓝藻中元素的组成及其环境意义

利用电感耦合等离子质谱仪对2008年7、9和10月采自太湖南泉水域的水华蓝藻样本中19种元素(Na、Mg、K、Ca、Zn、Mn、Fe、Al、Cu、Cr、Co、Ni、As、Se、Mo、Ag、Tl、Cd和Pb)的质量含量(w)及组成变化进行研究。结果表明,在藻华中w较高(1 000μg.g-1,以干质量计)的常量元素或有益元素为Ca、K、Na、Mg、Al、Fe。其中,w(Ca)和w(K)较高(4 000μg.g-1),w(Ca)随月份变化不大,而w(K)、w(Mg)、w(Na)则逐月升高。w(Al)、w(Fe)变化较大,7月最高(1 000μg.g-1),之后迅速降低(400μg.g-1);藻华中w在10~100μg.g-1之间变化的元素为Mn、Zn、Ni、Cu,其中,7月这4种元素w均最高,9~10月则降低。藻华中还检出痕量元素Co、Mo和Se,Tl未检出。藻华中积累的有毒元素中w(As)较高(5~15μg.g-1),而w(Cr)、w(Cd)、w(Pb)、w(Ag)均较低(5μg.g-1)。有毒元素w最高值均出现在7月。基于上述结果,推算出2007—2009年采取物理方法除藻从太湖中移除的元素量约为:K595.89 t、Ca 544.03 t、Mg 181.18 t、Al 83.06 t、Na 63.97 t、Fe 55.45 t、Mn 2.99t、Zn 2.26 t、Ni 1.67 t、Cu 1.11 t、As 0.76 t、Cr 94.5 kg、Cd 82.70 kg、Se 45.01 kg、Pb 37.64 kg、Co 32.27 kg、Mo5.41 kg和Ag 2.46 kg。该研究不仅可为进一步寻找关键元素在蓝藻水华爆发过程中的限制作用及其机制提供基础数据,同时也可为评价利用物理除藻方法去除太湖中有毒元素和降低有可能促进藻华发展的营养元素的负荷量的有效性,从而保护和修复渔业环境提供理论依据。     

The Contribution of Drinking Water towards Dental Fluorosis: A case study of Njoro Division, Nakuru District, Kenya

This study was carried out to measure the fluoride levels of water consumed in the Njoro division of Nakuru district, Kenya. The sources of drinking water, methods of water storage and utilisation, as well as the perceptions of the local community towards dental fluorosis and the percentage of children with moderate to severe dental fluorosis were also determined. Rainwater had mean fluoride levels of 0.5 mg L^-1, dams 2.4 mg L^-1, wells 4.1 mg L^-1, springs 5.5 mg L^-1, and boreholes 6.6 mg L^-1. Water stored in plastic and cement containers did not show appreciable reduction in fluoride content with storage time; water stored in metal containers reduced fluoride by up to 8.2%; water stored in clay pots had the highest reduction in fluoride content, ranging between 34.3 and 64.7%;. Forty eight point three percent of children observed in the area had moderate to severe dental fluorosis, even though most people in the area did not know the cause of the problem.There is need to educate the community on the causes of fluorosis, and to lay strategies for addressing the issue, such as encouraging more rainwater harvesting, treating drinking water with alum, or using clay pots for storage of drinking water.