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斯里兰卡卡卢特勒地方性甲状腺肿的医学地质学;分布及可能成因。

Medical geology of endemic goiter in Kalutara, Sri Lanka; distribution and possible causes.

机构信息

Department of Physics, Faculty of Natural Sciences, The Open University of Sri Lanka, Nugegoda, Sri Lanka.

Department of Basic Sciences, Faculty of Health Sciences, The Open University of Sri Lanka, Nugegoda, Sri Lanka.

出版信息

Environ Geochem Health. 2017 Dec;39(6):1501-1511. doi: 10.1007/s10653-017-9985-7. Epub 2017 May 27.

Abstract

This study assesses the distribution of goiter in the Kalutara District, Sri Lanka in order to find causative factors for the occurrence of goiter even after the salt iodization. A questionnaire survey was conducted at the household level and at the same time iodine and selenium levels of the water sources were analyzed. Questionnaire survey results indicated the highest numbers of goiter patients in the northern part where the lowest were found in the southern sector which may be due to the presence of acid sulfate soils. Females were more susceptible and it even showed a transmittance between generations. Average iodine concentrations in subsurface water of goiter endemic regions are 28.25 ± 15.47 μg/L whereas non-goiter regions show identical values at 24.74 ± 18.29 μg/L. Surface water exhibited relatively high values at 30.87 ± 16.13 μg/L. Endemic goiter was reported in some isolated patches where iodine and selenium concentrations low, latter was <10 μg/L. The formation of acid sulfate soils in the marshy lands in Kalutara district may lead to transformation of biological available iodine oxidation into volatile iodine by humic substances, at the same time organic matter rich peaty soil may have strong held of iodine and selenium which again induced by low pH and high temperature were suggested as the instrumental factors in the endemic goiter in Kalutara district. Hence, geochemical features such as soil pH, organic matter and thick lateritic cap in the Kalutara goiter endemic area play a role in controlling the available selenium and iodine for food chain through plant uptake and in water.

摘要

本研究评估了斯里兰卡卡卢特勒地区甲状腺肿的分布情况,以寻找甲状腺肿发生的原因,即使在盐碘化之后。在家庭层面进行了问卷调查,同时分析了水源的碘和硒水平。问卷调查结果表明,甲状腺肿患者数量最多的是北部地区,而南部地区则最少,这可能是由于存在酸性硫酸盐土壤。女性更容易受到影响,甚至存在代际传播。甲状腺肿流行地区地下水的平均碘浓度为 28.25±15.47μg/L,而非甲状腺肿地区的相同值为 24.74±18.29μg/L。地表水的碘浓度相对较高,为 30.87±16.13μg/L。一些孤立的斑块报告有地方性甲状腺肿,这些地区的碘和硒浓度较低,后者低于 10μg/L。卡卢特勒区沼泽地酸性硫酸盐土壤的形成可能导致生物可利用碘氧化为挥发性碘,同时富含有机物的泥炭土可能对碘和硒具有很强的吸附能力,而低 pH 值和高温再次被认为是卡卢特勒区地方性甲状腺肿的影响因素。因此,卡卢特勒地区地方性甲状腺肿流行地区的土壤 pH 值、有机质和厚层红土等地球化学特征通过植物吸收和在水中控制食物链中硒和碘的可用性。

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