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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">nznistu</journal-id><journal-title-group><journal-title xml:lang="ru">Науки о Земле и недропользование</journal-title><trans-title-group xml:lang="en"><trans-title>Earth sciences and subsoil use</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2686-9993</issn><issn pub-type="epub">2686-7931</issn><publisher><publisher-name>Federal State Budget Educational Institution of Higher Education "Irkutsk National Research Technical University"</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.21285/2686-9993-2022-45-2-172-183</article-id><article-id custom-type="elpub" pub-id-type="custom">nznistu-225</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>Гидрогеология и инженерная геология</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Hydrogeology and Engineering Geology</subject></subj-group></article-categories><title-group><article-title>Прогноз подъема уровня грунтовых вод в районе исторических построек города Иркутска</article-title><trans-title-group xml:lang="en"><trans-title>Forecasting groundwater rise in the historic downtown area of Irkutsk city</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-4702-7863</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Аузина</surname><given-names>Л. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Auzina</surname><given-names>L. I.</given-names></name></name-alternatives><bio xml:lang="ru"><p> Аузина Лариса Ивановна, кандидат геолого-минералогических наук, доцент, доцент кафедры прикладной геологии, геофизики и геоинформационных систем, Институт недропользования</p><p>г. Иркутск</p></bio><bio xml:lang="en"><p> Larisa I. Auzina, Cand. Sci. (Geol. &amp; Mineral.), Associate Professor,Assosiate Professor of the Department of Applied Geology</p><p>Irkutsk </p></bio><email xlink:type="simple">lauzina@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Иркутский национальный исследовательский технический университет</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Irkutsk National Research Technical University</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2022</year></pub-date><pub-date pub-type="epub"><day>03</day><month>07</month><year>2022</year></pub-date><volume>45</volume><issue>2</issue><fpage>172</fpage><lpage>183</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Аузина Л.И., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Аузина Л.И.</copyright-holder><copyright-holder xml:lang="en">Auzina L.I.</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://www.nznj.ru/jour/article/view/225">https://www.nznj.ru/jour/article/view/225</self-uri><abstract><p>Цель работы заключалась в разработке аналитической модели для прогноза подъема уровня грунтовых вод в условиях барражного эффекта. В результате обработки значительного объема производственных решений разработана аналитическая модель, позволяющая прогнозировать изменение уровня грунтовых вод, которое происходит при строительстве инженерных сооружений с глубоким заложением фундаментов, создающих эффект подпорной стенки (барража). Работа проводилась на участках, расположенных в исторических центрах городов Восточной Сибири, в том числе города Иркутска. Разработаны прогнозные схемы глубин формирования уровня подземных вод первых от поверхности водоносных горизонтов, проведена оценка территорий по условиям подтопления в соответствии с существующими нормативными документами. Анализ результатов исследований показывает, что наибольшее влияние на подъем грунтовых вод оказывают гидравлический уклон потока подземных вод и ширина проектного сооружения. Значительную роль в формировании нового подпорного горизонта в пределах исследуемой территории играют вертикальная планировка застраиваемой территории и использование свайных фундаментов. Кроме того, при разработке профилактических и защитных мероприятий необходимо учитывать многолетние сезонные колебания уровня грунтовых вод. Представленная аналитическая модель достаточно проста, универсальна и может применяться в различных геолого-гидрогеологических условиях.</p></abstract><trans-abstract xml:lang="en"><p>The purpose of this investigation is to develop an analytical model for predicting the groundwater level rise due to the barrage effect. Processing of a significant volume of production decisions for multiple objects has resulted an analytical model that allows predicting the dynamics of groundwater rise due to the barrage effect when building deep foundation structures. The study has been conducted for the downtown areas of Irkutsk and other cities of Eastern Siberia. Prediction schemes for the groundwater level formation have been made, and an assessment of the study areas by their underflooding conditions has been carried out. Being adequately simple and multi-purpose. The analysis of the research results shows that the hydraulic gradient of the underground water flow and the project structure width have the biggest effect on the groundwater rise. Vertical planning of the territory and the use of pile foundations play a significant role in the formation of the groundwater level. Besides, when evaluating the depth of the underground water formation level and developing the prevention and protection measures, it is necessary to take into account the seasonal rise of the underground waters. The developed model can be applied in the corresponding geological and hydrogeological conditions.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>подпор</kwd><kwd>уровень грунтовых вод</kwd><kwd>аналитическая модель</kwd><kwd>прогноз</kwd><kwd>перезаглубленный фундамент</kwd></kwd-group><kwd-group xml:lang="en"><kwd>groundwater rise</kwd><kwd>groundwater level</kwd><kwd>analytical model</kwd><kwd>prediction</kwd><kwd>deep foundation</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">Davies J. A. Groundwater control in the design and construction of a deep excavation // Proceedings of the 9th European Conference on Soil Mechanics and Foundation Engineering. 1987. Vol. 1. P. 139–144.</mixed-citation><mixed-citation xml:lang="en">Davies J. A. Groundwater control in the design and construction of a deep excavation. 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