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孟加拉国植酸盐-铁摩尔比与铁的生物利用度。

Phytate-iron molar ratio and bioavailability of iron in Bangladesh.

机构信息

Public Health, School of Medicine, Griffith University, Gold Coast Campus, Southport, Queensland, Australia.

Institute of Nutrition and Food Science, University of Dhaka, Dhaka, Bangladesh.

出版信息

Trop Med Int Health. 2022 May;27(5):509-514. doi: 10.1111/tmi.13750. Epub 2022 Apr 19.

DOI:10.1111/tmi.13750
PMID:35383403
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC9322336/
Abstract

OBJECTIVE

Phytate, an important component of plant origin foods, works as a chelator for mineral nutrients such as iron. Estimating the phytate-iron molar ratio is a traditional method to assess the bioavailability of dietary iron, and a ratio >1 is suggestive of poor absorption of iron through the intestinal mucosa. In Bangladesh, the ratio is considerably higher; nonetheless, the haemoglobin and ferritin status are satisfactory. Hence, we appraised phytate-iron molar ratios and concomitant haemoglobin and ferritin status.

METHODS

Dietary intake of iron and phytate was estimated in non-pregnant non-lactating women and school-age children from a nationally representative survey. The phytate-iron molar ratios were estimated. Linear regressions on haemoglobin for the phytate-iron molar ratios and on molar ratios predicting inflammation-adjusted ferritin were performed.

RESULTS

The median ratios were 6.12 in women and 5.47 in children, with corresponding haemoglobin concentrations of 12.6 and 12.5 g/dl. Hypothetical lowering of the ratios by ~50% revealed a nominal increment of haemoglobin and ferritin.

CONCLUSION

The standard cut-off phytate-iron molar ratio of >1 is inconsistent with the iron and haemoglobin status of the Bangladeshi population. One plausible explanation for the inconsistency is a non-dietary environmental factor-groundwater iron. Isotope studies incorporating the iron from dietary and the drinking groundwater sources are needed to establish a ratio which might better explain iron bioavailability.

摘要

目的

植酸是植物性食物的重要组成部分,它可以作为矿物质营养素(如铁)的螯合剂。估计植酸盐-铁摩尔比是评估膳食铁生物利用度的传统方法,比值>1 表明铁通过肠黏膜吸收不良。在孟加拉国,该比值相当高;尽管如此,血红蛋白和铁蛋白状况仍令人满意。因此,我们评估了植酸盐-铁摩尔比以及伴随的血红蛋白和铁蛋白状况。

方法

我们在一项具有全国代表性的调查中,估计了非妊娠非哺乳期妇女和学龄儿童的铁和植酸的膳食摄入量。估计了植酸盐-铁摩尔比。对血红蛋白进行线性回归,以评估植酸盐-铁摩尔比和预测炎症调整铁蛋白的摩尔比。

结果

女性的中位数比值为 6.12,儿童为 5.47,相应的血红蛋白浓度为 12.6 和 12.5g/dl。假设将比值降低约 50%,血红蛋白和铁蛋白的数值略有增加。

结论

标准的>1 的植酸盐-铁摩尔比值与孟加拉国人的铁和血红蛋白状况不一致。不一致的一个合理解释是一种非饮食环境因素——地下水铁。需要进行同位素研究,将来自膳食和饮用水源的铁纳入其中,以建立一个可能更好地解释铁生物利用度的比值。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b915/9322336/f94a366110e7/TMI-27-509-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b915/9322336/b802315cb291/TMI-27-509-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b915/9322336/f94a366110e7/TMI-27-509-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b915/9322336/b802315cb291/TMI-27-509-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b915/9322336/f94a366110e7/TMI-27-509-g002.jpg

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