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Investigation of iodine concentration in salt water and soil along the coast of Zhejiang China

机译:浙江沿海盐水和土壤中碘含量的调查

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摘要

Objective: We aim to describe the environment iodine concentration in salt, water and soil along Zhejiang Province coast in the China foreland. It will be helpful for us to judge whether this area is insufficient in iodine and universal iodized salt is necessary or not. Methods: We collected iodized salt samples, drinking water samples (tap water in the towns, and well water or spring water in the villages), water samples from different sources (ditches, lakes, rivers) and soil samples through random sampling in June, 2005. Salt, water and soil iodine was detected by arsenic-cerium redox method. Statistical analysis was expressed as mean±SEM by Windows SPSS 13.0. Results: (1) The iodine concentration in salt was 27.9±4.33 mg/kg (n=108). (2) Seventy-five water samples were collected. The water iodine value was 0.6~84.8 μg/L (mean of 11.66 μg/L). The watershed along the Qiantang River has significantly higher iodine content than the water in Lin’an in mountain area (P<0.01). The iodine content and mean iodine content of tap water, well or spring water and natural water sources were 4.30±2.43 μg/L (n=34), 23.59±27.74 μg/L (n=19) and 12.72±10.72 μg/L (n=22) respectively. This indicated that among environmental water sources, the ditch iodine content was the highest with river water iodine being the lowest (P<0.01). (3) Soil iodine value was 0.11~2.93 mg/kg (mean of 1.32 mg/kg). Though there was no statistical difference of soil iodine in different districts (P=0.131), soil iodine content correlated positively with water iodine content. Conclusion: Iodine concentration in salt accords with national policy of adding iodine in salt. Foreland has more iodine in water than mountain area. The data reflected that water and soil iodine in foreland area was not high, which suggests universal iodized salt should be necessary. Environment iodine has relatively close association with pollution.
机译:目的:我们旨在描述中国前陆浙江省沿海地区盐,水和土壤中环境碘的浓度。判断该区域的碘是否不足,是否需要普遍加碘盐将对我们有帮助。方法:我们于6月份通过随机抽样收集了加碘盐样品,饮用水样品(城镇的自来水以及村庄的井水或泉水),不同来源(沟渠,湖泊,河流)的水样品和土壤样品, 2005年。砷,铈,氧化还原法检测到了盐,水和土壤中的碘。 Windows SPSS 13.0将统计分析表示为平均值±SEM。结果:(1)盐中的碘浓度为27.9±4.33 mg / kg(n = 108)。 (2)收集了75个水样本。水碘值为0.6〜84.8μg/ L(平均11.66μg/ L)。钱塘江沿岸的流域碘含量明显高于山区临安市的水(P <0.01)。自来水,井水或泉水和天然水的碘含量和平均碘含量分别为4.30±2.43μg/ L(n = 34),23.59±27.74μg/ L(n = 19)和12.72±10.72μg/ L (n = 22)。这表明,在环境水源中,沟碘含量最高,河水碘最低(P <0.01)。 (3)土壤碘值为0.11〜2.93 mg / kg(平均1.32 mg / kg)。尽管不同地区的土壤碘含量无统计学差异(P = 0.131),但土壤碘含量与水碘含量呈正相关。结论:盐中的碘含量符合国家在盐中添加碘的政策。前陆地区水中的碘含量高于山区。数据表明,前陆地区的水和土壤碘含量不高,这表明普遍需要加碘盐。环境碘与污染有相对密切的联系。

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