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501.
Weiwei LI Yuegang TANG Shifeng DAI 《中国地球化学学报》2006,25(B08):70-70
The dental and skeletal fluorosis is highly prevalent in Zhijin, Guizhou, especially at Hualuo Village, Hehua Village and Majiazhuang Village. The contents of fluorine in coal, clay used for coal combustion, mixed fuel of coal and clay, corn, and chili from households of the three villages were determined by the pyrohydrolysis-fluorine ion-selective electrode method. The average contents of fluorine in the above samples respectively are 237 mg/g, 2262 mg/g, 828 mg/g, 1419 mg/g, and 110 mg/g. The clay used for coal combustions is the main fluorine source of endemic fluorosis and the inferior coal and weathered coal are the secondary source of fluorine. During the combustion of mixed fuel of coal and clay, about eighty percent of fluorine was volatilized, approximately two thirds of which was from the clay and the other one third from the coal. The occurrence of fluorine in clay used for coal combustion is closely related to apatite and hornblende. The contents of fluorine in corn and chili, dried by coal-clay mixed fuel are about 1400 and 73 times higher than the permitted level of fluorine in foods according to the Chinese Standard. It is worth paying attention to the high-fluorine indoor surroundings, such as coal, clay, corn, and chili, particularly ash from boiler bottom with the fluorine content of 15738 μg/g. Besides the technologies of fluorine fixation during the combustion, 相似文献
502.
Orlando Vaselli Franco Tassi Dario Tedesco Nisi Barbara Capaccioni Bruno Mapendano Yalire 《中国地球化学学报》2006,25(B08):71-72
The Nyiragongo volcano is located in the Virunga volcanic chain (Western Branch Rift, Eastern African Rift System). On January 17-18, 2002 a NS-oriented fracture network quickly propagated down-slope up to 16 km from the crater and two of the several lava flows emitted reached the city of Goma (about 500000 inhabitants). On May 2002 the volcanic activity resumed in the main crater with the formation of an active lava lake, which produced a volcanic plume mainly displaced west towards by the dominant winds. TOMS data suggest a release of SO2 of up to 60000 tons per day with relevant amounts of HF, HC1 and CO2. About 50000 people living in the villages around the western flank of Nyiragongo were forced to use rainwater, having no direct access to drinkable water Furthermore, crops and plants located in the western sector lie below the main direction of the volcanic plume. In order to evaluate the effects on the environment and public health caused by the Nyiragongo degassing system, rain waters, ashes, scorias and Pelee's hairs have been collected in a span of time of more than three years from different sites: (1) Nyiragongo crater; 相似文献
503.
Binbin WANG Baoshan ZHENG 《中国地球化学学报》2006,25(B08):80-80
Background: Fluorine is an important element to human health. Overloading of fluorine may cause dental and/or skeletal fluorosis, while in fluorine deficiency distracts, fluoride drinking water supply or other methods of fluoridation may greatly reduce the ratio of dental caries of local residents. The benefit of drinking water fluoridation has been widely accepted as a public sanitation measure in most western countries, but in China it faces big challenges. Method: Investigation of oral health and fluorine level in drinking water, main food and urine in some big cities of China. Result and conclusion: (1) Fluorine content in drinking water in 70% of the whole research cities is lower than 0.3 mg/L, and in 90% of the research cities, it is lower than 0.5 mg/L. (2) Fluorine concentrations in main foodstuff of respective cities in China were low and did not have too much difference. (3) Drinking water was the main source of fluorine intake for Chinese residents. (4) With the data of the epidemiological research by NCOH in 1995, in the range of fluorine content in drinking water below 1.0 mg/L, the ratio of dental caries and DMFT decreases with the increase of fluorine concentration. The relation between fluorine concentration in drinking water and dental index did not have a good linear relationship. 相似文献
504.
Xiaoyu ZHAO Wuyi WANG Hairong LI Fujian FENG Lizhen WANG 《中国地球化学学报》2006,25(B08):80-81
Brick-tea-type fluorosis is a peculiar endemic disease in China, which had been discovered in minority areas of western China since 1980, and distributed mainly in Tibet, Inner Mongolia, Gansu, Xinjiang, Qinghai and parts of Sichuan Province. The prevalence rate of fluorosis in Tibetan and Mongolian nationality people was higher. Epidemiological investigation showed that fluorosis morbidity and degrees were different in different brick-tea drinking areas, and it was probably caused by drinking various kinds of brick tea from different regions. Therefore, we collected 33 samples of brick tea from six provinces where minority nationalities were accustomed to drinking a large quantity of brick tea. F concentrations were determined by the combustion hydrolysis-ion selective electrode method. The results showed that among the brick teas, the F concentrations ranged from the minimum 74.1 mg/kg in Yunnan Province to the maximum 991.2 mg/kg in Sichuan Province. Besides, there was a great difference among the various kinds of brick tea, and F concentrations decreased in the order of Kang brick tea, Green brick tea, Black brick tea, Mi brick tea, Fu brick tea, Chitsu ping tea, Puerh tea, and Tuo tea. The average F concentration in brick teas was 431.92 mg/kg. 相似文献
505.
单扫描极谱法测定地质样品、土壤和蔬菜中的氟 总被引:1,自引:0,他引:1
采用三电极系统(工作电极:滴汞电极;参比电极:甘汞电极;辅助电极:铂丝电极),在pH=4.9的六次甲基四胺缓冲溶液中,利用P r3 -ALC-F-三元络合体系及单扫描极谱法测定地质样品、土壤及生物样品中微量氟,该方法操作方便、快速、灵敏,测量的回收率为96%~99%。其起始电位为-0.20 V(vs.SCE),峰电位在-0.58 V(vs.SCE)左右,线性范围为1.0×10-6m o l/L~4.0×1-0 5m o l/L,检出限为:8.0×1-0 7m o l/L。 相似文献
506.
507.
508.
氟是自然界广泛分布的非金属元素,也是人体必须的微量元素之一。环境微生物作为自然界中物质迁移的主动力之一,积极地参与着多种元素的水文生物地球化学循环。研究微生物参与下沉积物中氟的释出行为,对深入理解环境氟迁移行为具有重要意义。以山西运城高氟区沉积物样品为代表,采用野外沉积物调查采集、室内环境地球化学分析和微宇宙培养实验等研究手段,从环境生物地球化学作用的角度探讨了微生物介导下沉积物中氟的迁移释出行为。研究证明,高氟区沉积物总氟质量分数介于206.2~781.0 mg/kg之间,主要含氟矿物为长石、云母、方解石、绿泥石、角闪石等。培养条件下,溶液中的氟质量浓度与微生物生长曲线呈现良好的一致性;在培养初期,溶液中的氟质量浓度迅速上升,而后逐渐缓和,14 d后呈下降趋势。其中,黏土类沉积物的释氟量较大,砂土类沉积物释氟量较小。有、无碳源对照培养说明,沉积物中一定量的碳源可被微生物代谢利用,但碳源不是影响微生物在此环境中作用的主要因素。研究证明,原生微生物代谢活动可以显著促进沉积物中氟的迁移释出,微生物作用下不同岩性沉积物中氟的释出特征也有显著的差异,本研究工作有助于进一步丰富环境氟循环的理论认识。 相似文献
509.
510.
<正>近日,辽宁地质七队在丹东五龙山风景区西侧成功打成一眼温泉井,成井深度2,127米,水温46摄氏度,日出水量610吨。经检测,该温泉水含有多种矿物元素,其中氟含量达到国家理疗矿水命名标准,属氟理疗热矿泉水。技术人员称,该井属增温、对流复合型深井温泉水,区内地热流体储热层主要为印支期花岗岩中的热储构造带, 相似文献