Shomar B, Müller G, Yahya A, Askar S, Sansur R
Institute of Environmental Geochemistry, University of Heidelberg, Im Neuenheimer Feld 236, 69120 Heidelberg, Germany.
J Water Health. 2004 Mar;2(1):23-35.
The purpose of this study was to determine the fluoride levels in water, soil and tea, and to identify the major fluoride minerals in soil that supply water with fluoride ions. Another aim was to study the prevalence of dental fluorosis in permanent dentition of the school children of the Gaza Strip. Monitoring of fluoride levels in 73 groundwater wells and 20 topsoil samples for the last three years revealed a general trend of increasing from north to south of the Gaza Strip. A linear regression analysis found a correlation coefficient of r=0.93 between the fluoride concentrations in groundwater and soil for the same geographic areas. However, the X-ray diffraction technique (XRD) results showed that none of the four major fluoride minerals were detected in the tested soil samples; the PHREEQC model showed that fluorite (CaF2) was the main donating mineral of fluoride ions to groundwater. A high positive correlation was found between fluoride concentrations in groundwater and occurrence of dental fluorosis. Among 353 school children of the five geographic areas of the Gaza Strip the prevalence of dental fluorosis was 60%, and 40% had no signs of fluorosis in their permanent dentitions. The highest occurrence, 94%, was in Khan Yunis, followed by 82% in Rafah, 68% in the middle area, 29% in Gaza and the lowest occurrence of 9% was in the northern area. These percentages were directly proportional to the average content of fluoride in groundwater of each area: 2.6, 0.9, 1.7, 1.2, and 0.7 ppm, respectively. The exception was Rafah where people drank from new groundwater wells that have been dug in the last 10 years. The occurrence of the disease was due to intake of high amounts of fluorides in drinking water, tea and fish. Communication with population indicated a heavy intake of tea starting from a very young age; not uncommonly tea is put in nursing bottles. No significant correlation was found between prevalence figures and gender or age groups. This high prevalence indicates a need to examine other sources of F including diet.
本研究的目的是测定水、土壤和茶叶中的氟含量,并确定土壤中向水体提供氟离子的主要氟化物矿物。另一个目的是研究加沙地带学龄儿童恒牙中氟斑牙的患病率。对过去三年里73口水井和20份表层土壤样本的氟含量监测显示,加沙地带从北到南呈现出总体上升趋势。线性回归分析发现,同一地理区域的地下水和土壤中的氟浓度之间的相关系数r = 0.93。然而,X射线衍射技术(XRD)结果表明,在所测试的土壤样本中未检测到四种主要氟化物矿物中的任何一种;PHREEQC模型显示,萤石(CaF2)是向地下水提供氟离子的主要矿物。地下水氟浓度与氟斑牙的发生之间存在高度正相关。在加沙地带五个地理区域的353名学龄儿童中,氟斑牙的患病率为60%,40%的儿童恒牙中没有氟斑牙迹象。患病率最高的是汗尤尼斯,为94%,其次是拉法,为82%,中部地区为68%,加沙为29%,最低的是北部地区,为9%。这些百分比与每个地区地下水平均氟含量直接成正比,分别为2.6、0.9、1.7、1.2和0.7 ppm。拉法是个例外,那里的人们饮用过去10年新挖的水井中的水。该疾病的发生是由于饮用水、茶和鱼中摄入了大量氟化物。与当地居民的交流表明,从很小的年龄就开始大量饮茶;茶被放入奶瓶中并不罕见。患病率数据与性别或年龄组之间未发现显著相关性。如此高的患病率表明需要检查包括饮食在内的其他氟来源。