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Influence of socioeconomic disparities, temperature and humidity in kidney stone composition
INTRODUCTION: Large variations in demographic, economic and environmental factors might influence the worldwide distribution of urolithiasis, but scarce data are available concerning their associations with stone composition. We aimed to evaluate the frequency and composition of kidney stones and th...
Autores principales: | , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Sociedade Brasileira de Nefrologia
2020
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7860642/ https://www.ncbi.nlm.nih.gov/pubmed/32716471 http://dx.doi.org/10.1590/2175-8239-JBN-2019-0206 |
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author | Cunha, Tamara da Silva Rodriguez, Adrian Heilberg, Ita Pfeferman |
author_facet | Cunha, Tamara da Silva Rodriguez, Adrian Heilberg, Ita Pfeferman |
author_sort | Cunha, Tamara da Silva |
collection | PubMed |
description | INTRODUCTION: Large variations in demographic, economic and environmental factors might influence the worldwide distribution of urolithiasis, but scarce data are available concerning their associations with stone composition. We aimed to evaluate the frequency and composition of kidney stones and their associations with temperature, humidity, and human development index (HDI). MATERIALS AND METHODS: A total of 1,158 stones from distinct patients (47±14 years old, male/female 2:1) were included. The mean annual temperature and relative humidity of each town were considered separately. RESULTS: Calcium oxalate monohydrate (COM) was disclosed in 38.8% of patients, calcium oxalate dihydrate (COD) in 22.1%, mixed COD/apatite in 9.4%, pure apatite in 1.9%, brushite in 1.8%, struvite in 8.3%, pure uric acid in 11.1%, mixed uric acid/COM in 5.6%, and cystine/rare types in 0.8%. Mean HDI of all pooled cities was 0.780±0.03. However, people living in HDI<0.800 regions had twice the odds of having a struvite stone versus those living in HDI>0.800 (OR=2.14, 95% CI 1.11-4.11). Furthermore, a progressive increase in the struvite stones frequency from 4.5 to 22.8% was detected from HDI>0.800 through HDI<0.700. No significant difference for other stone types was disclosed. Separate logistic regression models assessed the association of each stone composition with gender, temperature, humidity and HDI as covariates. CONCLUSION: Patients living in low HDI areas are more prone to develop struvite stones, possibly due to lower access to healthcare. Temperature and humidity did not represent a specific risk factor for any stone type in the present sample. |
format | Online Article Text |
id | pubmed-7860642 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2020 |
publisher | Sociedade Brasileira de Nefrologia |
record_format | MEDLINE/PubMed |
spelling | pubmed-78606422021-02-16 Influence of socioeconomic disparities, temperature and humidity in kidney stone composition Cunha, Tamara da Silva Rodriguez, Adrian Heilberg, Ita Pfeferman J Bras Nefrol Original Article INTRODUCTION: Large variations in demographic, economic and environmental factors might influence the worldwide distribution of urolithiasis, but scarce data are available concerning their associations with stone composition. We aimed to evaluate the frequency and composition of kidney stones and their associations with temperature, humidity, and human development index (HDI). MATERIALS AND METHODS: A total of 1,158 stones from distinct patients (47±14 years old, male/female 2:1) were included. The mean annual temperature and relative humidity of each town were considered separately. RESULTS: Calcium oxalate monohydrate (COM) was disclosed in 38.8% of patients, calcium oxalate dihydrate (COD) in 22.1%, mixed COD/apatite in 9.4%, pure apatite in 1.9%, brushite in 1.8%, struvite in 8.3%, pure uric acid in 11.1%, mixed uric acid/COM in 5.6%, and cystine/rare types in 0.8%. Mean HDI of all pooled cities was 0.780±0.03. However, people living in HDI<0.800 regions had twice the odds of having a struvite stone versus those living in HDI>0.800 (OR=2.14, 95% CI 1.11-4.11). Furthermore, a progressive increase in the struvite stones frequency from 4.5 to 22.8% was detected from HDI>0.800 through HDI<0.700. No significant difference for other stone types was disclosed. Separate logistic regression models assessed the association of each stone composition with gender, temperature, humidity and HDI as covariates. CONCLUSION: Patients living in low HDI areas are more prone to develop struvite stones, possibly due to lower access to healthcare. Temperature and humidity did not represent a specific risk factor for any stone type in the present sample. Sociedade Brasileira de Nefrologia 2020-07-20 2020 /pmc/articles/PMC7860642/ /pubmed/32716471 http://dx.doi.org/10.1590/2175-8239-JBN-2019-0206 Text en https://creativecommons.org/licenses/by/4.0/ This is an Open Access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. |
spellingShingle | Original Article Cunha, Tamara da Silva Rodriguez, Adrian Heilberg, Ita Pfeferman Influence of socioeconomic disparities, temperature and humidity in kidney stone composition |
title | Influence of socioeconomic disparities, temperature and humidity in kidney stone composition |
title_full | Influence of socioeconomic disparities, temperature and humidity in kidney stone composition |
title_fullStr | Influence of socioeconomic disparities, temperature and humidity in kidney stone composition |
title_full_unstemmed | Influence of socioeconomic disparities, temperature and humidity in kidney stone composition |
title_short | Influence of socioeconomic disparities, temperature and humidity in kidney stone composition |
title_sort | influence of socioeconomic disparities, temperature and humidity in kidney stone composition |
topic | Original Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7860642/ https://www.ncbi.nlm.nih.gov/pubmed/32716471 http://dx.doi.org/10.1590/2175-8239-JBN-2019-0206 |
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