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<article article-type="research-article" dtd-version="1.3" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xml:lang="ru"><front><journal-meta><journal-id journal-id-type="publisher-id">zhps</journal-id><journal-title-group><journal-title xml:lang="ru">Журнал прикладной спектроскопии</journal-title><trans-title-group xml:lang="en"><trans-title>Zhurnal Prikladnoii Spektroskopii</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">0514-7506</issn><publisher><publisher-name>B. I. Stepanov Institute of Physics of the National Academy of Sciences</publisher-name></publisher></journal-meta><article-meta><article-id custom-type="elpub" pub-id-type="custom">zhps-786</article-id><article-categories><subj-group subj-group-type="heading"><subject>Research Article</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="ru"><subject>Статьи</subject></subj-group></article-categories><title-group><article-title>АНАЛИЗ КАМНЕЙ В МОЧЕВОМ И ЖЕЛЧНОМ ПУЗЫРЕ ЧЕЛОВЕКА С ПОМОЩЬЮ ИК-ФУРЬЕ-СПЕКТРОСКОПИИ НАРУШЕННОГО ПОЛНОГО ВНУТРЕННЕГО ОТРАЖЕНИЯ</article-title><trans-title-group xml:lang="en"><trans-title>ANALYSIS OF HUMAN URINARY STONES AND GALLSTONES BY FOURIER TRANSFORM INFRARED ATTENUATED TOTAL REFLECTANCE SPECTROSCOPY</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Hermida</surname><given-names>F. J.</given-names></name><name name-style="western" xml:lang="en"><surname>Hermida</surname><given-names>F. J.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Ла-Корунья</p></bio><bio xml:lang="en"><p>A Coruña</p></bio><email xlink:type="simple">fernandojesus.hermida.ameijeiras@sergas.es</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Университетская клиника Сантьяго-де-Компостела</institution></aff><aff xml:lang="en"><institution>Department of Clinical Analysis, Hospital Clínico Universitario de Santiago de Compostela</institution></aff></aff-alternatives><pub-date pub-type="collection"><year>2021</year></pub-date><pub-date pub-type="epub"><day>29</day><month>01</month><year>2021</year></pub-date><volume>88</volume><issue>1</issue><elocation-id>172(1)-172(10)</elocation-id><permissions><copyright-statement>Copyright &amp;#x00A9; Hermida F.J., 2021</copyright-statement><copyright-year>2021</copyright-year><copyright-holder xml:lang="ru">Hermida F.J.</copyright-holder><copyright-holder xml:lang="en">Hermida F.J.</copyright-holder><license xml:lang="ru" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>Данная работа распространяется под лицензией Creative Commons Attribution 4.0.</license-p></license><license xml:lang="en" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>This work is licensed under a Creative Commons Attribution 4.0 License.</license-p></license></permissions><self-uri xlink:href="https://zhps.ejournal.by/jour/article/view/786">https://zhps.ejournal.by/jour/article/view/786</self-uri><abstract><p>Проанализирован состав камней в мочевом и желчном пузыре и оценена степень распространенности отдельных компонентов камней в зависимости от возраста и пола. Составы 425 мочевых камней и 108 желчных камней проанализированы с помощью ИК-Фурье-спектроскопии нарушенного полного внутреннего отражения (FTIR-ATR). По спектрам поглощения, полученным с помощью FTIR-ATR, камни в мочевом пузыре разделены на группы: оксалат кальция (55.6%), мочевая кислота (24.1%), гидроксиапатит (7.3%), струвит (9.0%), бруцит (2.1%), цистин (1.0%) и урат аммония (0.2%). Камни в желчном пузыре разделены на холестериновые (66.7%) и пигментные (33.3%). Камни в мочевом пузыре чаще встречаются у мужчин (62.0%), чем у женщин (38.0%) (соотношение 1.7), причем камни из оксалата кальция распространены у представителей обоих полов. Для женщин характерна более высокая частота гидроксиапатита и струвита, чем для мужчин (вероятность ошибки p&lt;0.05), а для мужчин — более высокая частота оксалата кальция и мочевой кислоты (p&lt;0.05). Камни из оксалата кальция чаще встречаются в возрастной группе 30–69 лет (p&lt;0.05), камни из мочевой кислоты — у лиц старше 50 лет (p&lt;0.05). Камни в желчном пузыре чаще встречаются у женщин (59.3%), чем у мужчин (40.7%) (соотношение 1.4), причем холестериновые камни — у представителей обоих полов. У женщин холестериновые камни находят чаще, чем у мужчин (p&lt;0.05), а мужчины имеют более высокую частоту пигментных камней (p&lt;0.05). Холестериновые камни характерны для лиц в возрасте до 60 лет (p&lt;0.05), тогда как пигментные — для пациентов в возрасте свыше 60 лет (p&lt;0.05). Физический анализ камней с помощью FTIR-ATR дает достаточно точную информацию о его составе. На тип образовавшегося камня оказывают влияние пол и возраст.</p></abstract><trans-abstract xml:lang="en"><p>The aim of this study was to analyze the composition of urinary stones and gallstones and assess their prevalence as a function of age and sex. A total of 425 urinary stones and 108 gallstones was analyzed for composition using FTIR-ATR spectroscopy. According to the absorption band spectra obtained using FTIR-ATR, urinary stones were classified into the following groups: calcium oxalate (55.6%), uric acid (24.1%), hydroxyapatite (7.3%), struvite (9.0%), brucite (2.1%), cystine (1.0%) and ammonium urate (0.2%). Gallstones were classified into cholesterol (66.7%) and pigment stones (33.3%). As to urinary stones, they are more common in males (62.0%) than in females (38.0%) (ratio ♂/♀: 1.7), calcium oxalate stones being the most common ones in both sexes. Women have a higher frequency of hydroxyapatite and struvite than men (p&lt;0.05) whereas males have a higher frequency of calcium oxalate and uric acid than women (p&lt;0.05). Calcium oxalate stones are more common in the 30–69 years age group (p&lt;0.05), while uric acid stones are more common in ages &gt;50 years (p&lt;0.05). As to gallstones, they are more common in women (59.3%) than in men (40.7%) (ratio ♀/♂: 1.4), cholesterol stones being the most prevalent in both sexes. Women have greater frequency of cholesterol stones than men (p&lt;0.05) and men have higher frequency of pigment stones than women (p&lt;0.05). Cholesterol stones were more common in ages &lt;60 year (p&lt;0.05), whereas pigment stones were more common in ages ³60 years (p&lt;0.05). The results of this study show that the physical analysis of stones using FTIR-ATR spectroscopy provides fairly accurate information on its composition, and sex and age have been seen to have an influence on the type of stone formed.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>камень мочевого пузыря</kwd><kwd>камень желчного пузыря</kwd><kwd>пол</kwd><kwd>возрастная группа</kwd><kwd>ИК-Фурье-спектроскопия нарушенного полного отражения</kwd></kwd-group><kwd-group xml:lang="en"><kwd>urinary stone</kwd><kwd>gallstone</kwd><kwd>gender</kwd><kwd>age groups</kwd><kwd>Fourier transform infrared attenuated total reflectance spectroscopy</kwd></kwd-group></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">O. W. Moe, Lancet, 367, 333–344 (2006).</mixed-citation><mixed-citation xml:lang="en">O. W. 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