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首页> 外文期刊>Tropical Medicine and International Health: TM and IH >Geophagy, iron status and anaemia among primary school children in Western Kenya.
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Geophagy, iron status and anaemia among primary school children in Western Kenya.

机译:肯尼亚西部小学生的地理位置,铁质状况和贫血。

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As part of a cross-sectional study among 156 primary school children (median age 13 years, range 10-18) in Western Kenya, geophagy was assessed through interviews. 114 (73.1%) of these children reported eating soil daily. Haemoglobin levels were determined in all 156 children and serum ferritin concentrations in 135. The mean haemoglobin (Hb) concentration was 12.7 g/dl, and median ferritin concentration 27.2 microg/l. Both the proportion of anaemic (Hb < 11.0 g/dl) and of iron-depleted (ferritin < 12 microg/l) children was significantly higher among the geophageous children than among the nongeophageous (9.6% vs. 0% anaemia; P = 0.037; 18.4% vs. 5.4% iron depletion; P = 0.046). Serum ferritin and haemoglobin concentrations were not correlated (r = 0. 13 5; P = 0. 100). Multiple regression analysis showed that geophagy, hookworm eggs per gram faeces and malaria parasite counts per microl blood were independent predictors of serum ferritin, when controlling for other helminth infections, age and sex, and socio-economic and educational background of the children's families and family size (y = 36.038-11.247(geophagy) -- 0.010(hookworm epg) + 0.001(malaria parasite counts); R2 = 0.17). Multiple regression analysis with haemoglobin as dependent variable and the same independent variables did not reveal any significant predictors. Analysis of the soil eaten by the children revealed a mean HCl-extractable iron content of 168.9 mg/kg (SD 44.9). Based on the data on the amounts eaten daily and this mean iron content, soil could provide on average 4.7 mg iron to a geophageous child (interquartile range 2.1-7.1 mg), which is equivalent to 32% of the Recommended Nutrient Intake (RNI) for girls (interquartile range 14-48%) or 42% of the RNI for boys (interquartile range 19-63%). Iron depletion and anaemia are associated with geophagy, but only serum ferritin concentrations were shown to be dependent upon geophagy in the regression model. From the cross-sectional data no inference about causality can be made. To clarify the possible causal relationships involved, longitudinal studies and iron-supplementation intervention studies are needed.
机译:作为对肯尼亚西部156名小学生(中位年龄13岁,年龄介于10-18岁)的横断面研究的一部分,通过访谈评估了吞噬能力。这些儿童中有114名(73.1%)报告每天吃土壤。测定所有156名儿童的血红蛋白水平,并测定135名儿童的血清铁蛋白浓度。平均血红蛋白(Hb)浓度为12.7 g / dl,中位铁蛋白浓度为27.2 microg / l。贫血儿童的贫血(Hb <11.0 g / dl)和贫铁儿童(铁蛋白<12 microg / l)的比例均显着高于非食管贫血的儿童(9.6%vs. 0%贫血; P = 0.037 ; 18.4%与5.4%的铁耗竭; P = 0.046)。血清铁蛋白和血红蛋白浓度不相关(r = 0. 13 5; P = 0. 100)。多元回归分析表明,在控制其他蠕虫感染,年龄和性别以及儿童家庭和家庭的社会经济和教育背景时,地理位置,每克粪便的钩虫卵和每微升血液的疟疾寄生虫计数是血清铁蛋白的独立预测因子。大小(y = 36.038-11.247(geophagy)-0.010(钩虫epg)+ 0.001(疟原虫计数); R2 = 0.17)。以血红蛋白为因变量且具有相同自变量的多元回归分析未发现任何重要的预测因素。对儿童食用的土壤进行的分析表明,可从HCl提取的铁的平均含量为168.9 mg / kg(标准差44.9)。根据每日进食量和平均铁含量的数据,土壤可为食道性儿童(四分位数范围为2.1-7.1 mg)平均提供4.7 mg铁,相当于建议营养摄入量(RNI)的32%女孩(四分位间距为14-48%)或男孩的RNI的42%(四分位间距为19-63%)。铁消耗和贫血与地吞相关,但在回归模型中仅显示血清铁蛋白浓度与地吞相关。从横截面数据无法推断出因果关系。为了阐明可能涉及的因果关系,需要进行纵向研究和补充铁的干预研究。

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