第聂伯罗彼得罗夫斯克地区居民尿石个体发育的一些特点

IF 0.5 Q4 MINERALOGY Mineralogical Journal-Ukraine Pub Date : 2020-01-01 DOI:10.15407/mineraljournal.42.04.050
V. Ishkov, Ye.S. Kozii, M. Trufanova
{"title":"第聂伯罗彼得罗夫斯克地区居民尿石个体发育的一些特点","authors":"V. Ishkov, Ye.S. Kozii, M. Trufanova","doi":"10.15407/mineraljournal.42.04.050","DOIUrl":null,"url":null,"abstract":"According to the data of World Health Organization, the incidence of a disease of inhabitants with urolithiasis is constantly growing; moreover the number of recurrences of this disease is stable at 70%. The purpose of the work is to identify some features of the ontogenesis of uroliths from the kidneys of the inhabitants of Dnipropetrovsk region, primarily related to the structure and morphology of these formations. Based on comparative analyzes of morphological observations of more than 300 kidney stones investigated in inhabitants of Dnipropetrovsk region, it was found that spherulites and druse-like aggregates as well as their combinations are the most common among them. Moreover areas of attachment to renal papillae are usually observed on the surface of spherulitic formations and, as a rule, druse-like aggregates are formed in free space of a renal pelvis. Therefore, the specific features of the morphology of urinary stones allow to establish the most favorable areas of the urinary system for their predominant formation in each patient. Urolites of spherical shape differ in zonal structure, while the zonal structure is formed by the alternation of both essentially mineral and mainly organic layers, and mineral layers of different composition as well. Mineralogical and petrographic studies of urinary stones revealed the presence of 15 mineral species, mainly urate and oxalate compounds, with monomineral formations occurring in less than 1%. Multiscale microblocking and the presence of organic matter inclusions are characteristic features of the crystals of all established minerals. The central part of the uroliths is usually represented by accumulations of organic matter containing a highly dispersed mineral component. It is proved that such characteristics as color, size, shape and character of the surface of uroliths of the inhabitants of Dnipropetrovsk region are not very informative for the establishment of their predominant mineral composition. The accumulation of analytical material on the ontogenesis of urinary stones, their structure and mineral composition and its generalization, taking into account the medical and biological characteristics of each patient and the geoecological state of the region, could contribute to solution of an important social task — prevention and effective treatment of urolithiasis.","PeriodicalId":53834,"journal":{"name":"Mineralogical Journal-Ukraine","volume":null,"pages":null},"PeriodicalIF":0.5000,"publicationDate":"2020-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":"{\"title\":\"Some Peculiarities of Urolith Ontogeny of the Inhabitants of Dnipropetrovsk Region\",\"authors\":\"V. Ishkov, Ye.S. Kozii, M. Trufanova\",\"doi\":\"10.15407/mineraljournal.42.04.050\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"According to the data of World Health Organization, the incidence of a disease of inhabitants with urolithiasis is constantly growing; moreover the number of recurrences of this disease is stable at 70%. The purpose of the work is to identify some features of the ontogenesis of uroliths from the kidneys of the inhabitants of Dnipropetrovsk region, primarily related to the structure and morphology of these formations. Based on comparative analyzes of morphological observations of more than 300 kidney stones investigated in inhabitants of Dnipropetrovsk region, it was found that spherulites and druse-like aggregates as well as their combinations are the most common among them. Moreover areas of attachment to renal papillae are usually observed on the surface of spherulitic formations and, as a rule, druse-like aggregates are formed in free space of a renal pelvis. Therefore, the specific features of the morphology of urinary stones allow to establish the most favorable areas of the urinary system for their predominant formation in each patient. Urolites of spherical shape differ in zonal structure, while the zonal structure is formed by the alternation of both essentially mineral and mainly organic layers, and mineral layers of different composition as well. Mineralogical and petrographic studies of urinary stones revealed the presence of 15 mineral species, mainly urate and oxalate compounds, with monomineral formations occurring in less than 1%. Multiscale microblocking and the presence of organic matter inclusions are characteristic features of the crystals of all established minerals. The central part of the uroliths is usually represented by accumulations of organic matter containing a highly dispersed mineral component. It is proved that such characteristics as color, size, shape and character of the surface of uroliths of the inhabitants of Dnipropetrovsk region are not very informative for the establishment of their predominant mineral composition. The accumulation of analytical material on the ontogenesis of urinary stones, their structure and mineral composition and its generalization, taking into account the medical and biological characteristics of each patient and the geoecological state of the region, could contribute to solution of an important social task — prevention and effective treatment of urolithiasis.\",\"PeriodicalId\":53834,\"journal\":{\"name\":\"Mineralogical Journal-Ukraine\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":0.5000,\"publicationDate\":\"2020-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"1\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Mineralogical Journal-Ukraine\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.15407/mineraljournal.42.04.050\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q4\",\"JCRName\":\"MINERALOGY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Mineralogical Journal-Ukraine","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.15407/mineraljournal.42.04.050","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"MINERALOGY","Score":null,"Total":0}
引用次数: 1

摘要

根据世界卫生组织的数据,居民尿石症的发病率不断上升;此外,这种疾病的复发率稳定在70%。这项工作的目的是确定第聂伯罗彼得罗夫斯克地区居民肾脏尿石的个体发生的一些特征,主要与这些地层的结构和形态有关。根据对第聂伯罗彼得罗夫斯克地区居民调查的300多例肾结石形态学观察的比较分析,发现球粒和簇状聚集体及其组合是其中最常见的。此外,通常在球形结构的表面观察到附着于肾乳头的区域,并且通常在肾盂的自由空间中形成束状聚集体。因此,尿路结石形态的特定特征允许在每个患者中建立泌尿系统中最有利于其主要形成的区域。球形尿石的分带结构不同,分带结构是由主要矿物层和主要有机层以及不同组成的矿物层交替形成的。尿路结石的矿物学和岩石学研究表明,存在15种矿物,主要是尿酸盐和草酸盐化合物,单矿物形成的发生率不到1%。多尺度微阻塞和有机质包裹体的存在是所有已建立矿物晶体的特征。尿石的中心部分通常由含有高度分散的矿物成分的有机质堆积而成。事实证明,第聂伯罗彼得罗夫斯克地区居民的尿石表面的颜色,大小,形状和特征等特征对于确定其主要矿物组成并不是很有用。考虑到每个患者的医学和生物学特征以及该地区的地质生态状况,关于尿路结石的个体发生、结构和矿物成分及其概论的分析材料的积累可能有助于解决一项重要的社会任务——预防和有效治疗尿路结石。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
查看原文
分享 分享
微信好友 朋友圈 QQ好友 复制链接
本刊更多论文
Some Peculiarities of Urolith Ontogeny of the Inhabitants of Dnipropetrovsk Region
According to the data of World Health Organization, the incidence of a disease of inhabitants with urolithiasis is constantly growing; moreover the number of recurrences of this disease is stable at 70%. The purpose of the work is to identify some features of the ontogenesis of uroliths from the kidneys of the inhabitants of Dnipropetrovsk region, primarily related to the structure and morphology of these formations. Based on comparative analyzes of morphological observations of more than 300 kidney stones investigated in inhabitants of Dnipropetrovsk region, it was found that spherulites and druse-like aggregates as well as their combinations are the most common among them. Moreover areas of attachment to renal papillae are usually observed on the surface of spherulitic formations and, as a rule, druse-like aggregates are formed in free space of a renal pelvis. Therefore, the specific features of the morphology of urinary stones allow to establish the most favorable areas of the urinary system for their predominant formation in each patient. Urolites of spherical shape differ in zonal structure, while the zonal structure is formed by the alternation of both essentially mineral and mainly organic layers, and mineral layers of different composition as well. Mineralogical and petrographic studies of urinary stones revealed the presence of 15 mineral species, mainly urate and oxalate compounds, with monomineral formations occurring in less than 1%. Multiscale microblocking and the presence of organic matter inclusions are characteristic features of the crystals of all established minerals. The central part of the uroliths is usually represented by accumulations of organic matter containing a highly dispersed mineral component. It is proved that such characteristics as color, size, shape and character of the surface of uroliths of the inhabitants of Dnipropetrovsk region are not very informative for the establishment of their predominant mineral composition. The accumulation of analytical material on the ontogenesis of urinary stones, their structure and mineral composition and its generalization, taking into account the medical and biological characteristics of each patient and the geoecological state of the region, could contribute to solution of an important social task — prevention and effective treatment of urolithiasis.
求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
来源期刊
CiteScore
0.70
自引率
0.00%
发文量
18
期刊最新文献
CURRENT STATE’S CONDITION OF LITHIUM ORE DEPOSITS IN UKRAINE A COMPARATIVE ANALYSIS OF DIAMONDS IN NON-KIMBERLITIC ROCKS OF THE WORLD AND NEOGENE SANDS OF UKRAINE GEOCHEMICAL CHARACTERISTICS OF THE SALTYCHIAN GRANITES (WESTERN AZOV AREA) ACCORDING TO THE ICP-MS RESEARCH RESULTS ECOLOGICAL AND GEOCHEMICAL FEATURES OF MANGANESE DISTRIBUTION IN GROUNDWATERS OF UKRAINE PUMPELLYITE FROM METABASALTS OF THE UKRAINIAN CARPATHIANS
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
已复制链接
已复制链接
快去分享给好友吧!
我知道了
×
扫码分享
扫码分享
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1