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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">resar</journal-id><journal-title-group><journal-title xml:lang="ru">Природные ресурсы Арктики и Субарктики</journal-title><trans-title-group xml:lang="en"><trans-title>Arctic and Subarctic Natural Resources</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2618-9712</issn><issn pub-type="epub">2686-9683</issn><publisher><publisher-name>Академия наук Республики Саха (Якутия)</publisher-name></publisher></journal-meta><article-meta><article-id custom-type="elpub" pub-id-type="custom">resar-717</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>Науки о Земле</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Earth sciences</subject></subj-group></article-categories><title-group><article-title>Исследование изменения параметров георадиолокационных сигналов в процессе оттайки мерзлых дисперсных горных пород различной влажности</article-title><trans-title-group xml:lang="en"><trans-title>Investigation of GPR Signals Parameters Changes during Defrosting Process of Frozen Dispersed Rocks of Different Humidity</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>Федорова</surname><given-names>Лариса Лукинична</given-names></name><name name-style="western" xml:lang="en"><surname>Fedorova</surname><given-names>Larisa Lukinichna</given-names></name></name-alternatives><bio xml:lang="ru"><p>ФЕДОРОВА Лариса Лукинична – к.т.н., зав. лаб., Lar-fed–90@rambler.ru;</p></bio><email xlink:type="simple">Lar-fed-90@rambler.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Саввин</surname><given-names>Денис Валерьевич</given-names></name><name name-style="western" xml:lang="en"><surname>Savvin</surname><given-names>Denis Valerievich</given-names></name></name-alternatives><bio xml:lang="ru"><p>САВВИН Денис Валерьевич – к.т.н., н.с., deophysic@mail.ru; </p></bio><email xlink:type="simple">deophysic@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Соколов</surname><given-names>Кирилл Олегович</given-names></name><name name-style="western" xml:lang="en"><surname>Sokolov</surname><given-names>Kirill Olegovich</given-names></name></name-alternatives><bio xml:lang="ru"><p>СОКОЛОВ Кирилл Олегович – к.т.н., н.с., k.sokolov@ro.ru;</p></bio><email xlink:type="simple">k.sokolov@ro.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Куляндин</surname><given-names>Гаврил Александрович</given-names></name><name name-style="western" xml:lang="en"><surname>Kulyandin</surname><given-names>Gavril Aleksandrovich</given-names></name></name-alternatives><bio xml:lang="ru"><p>КУЛЯНДИН Гаврил Алек- сандрович – м.н.с., kgavrilu@yandex.ru.</p></bio><email xlink:type="simple">kgavrilu@yandex.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт горного дела Севера им. Н.В. Черского СО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Chersky Institute of Mining of the North SB RAS</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2016</year></pub-date><pub-date pub-type="epub"><day>05</day><month>03</month><year>2025</year></pub-date><volume>21</volume><issue>3</issue><fpage>42</fpage><lpage>46</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Федорова Л.Л., Саввин Д.В., Соколов К.О., Куляндин Г.А., 2025</copyright-statement><copyright-year>2025</copyright-year><copyright-holder xml:lang="ru">Федорова Л.Л., Саввин Д.В., Соколов К.О., Куляндин Г.А.</copyright-holder><copyright-holder xml:lang="en">Fedorova L.L., Savvin D.V., Sokolov K.O., Kulyandin G.A.</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://resar.elpub.ru/jour/article/view/717">https://resar.elpub.ru/jour/article/view/717</self-uri><abstract><p>Представлены результаты лабораторных зондирований георадаром «ОКО-2» с центральной частотой 1200 МГц образцов дисперсных горных пород различной влажности, замороженных в холодильной камере, с последующей оттайкой при температуре 22°С. Рассчитаны скорости распространения георадиолокационных сигналов в образцах при влажности от 3 до 22% и изменении температуры от –15ºС до 15ºС. В результате исследований установлено, что существенное различие скоростей распространения георадиолокационных сигналов при отрицательных и положительных температурах в двух типах песков четвертичных отложений наблюдается при влажности более 7%. Также описаны амплитудные значения георадиолокационных сигналов и их частотный состав в зависимости от температуры и влажности исследуемых образцов. Полученные результаты будут способствовать созданию автоматизированной системы контроля динамики влажности пород на горных объектах с последующим отображением данных в геоинформационной системе, применение которой перспективно для мониторинга физико-механических свойств горных пород бортов карьеров, кровли подземных горных выработок и грунтов оснований инженерных сооружений.</p></abstract><trans-abstract xml:lang="en"><p>Laboratory studies are conducted on dispersed rock samples of different moisture content frozen in a refrigerating chamber, with the subsequent defrosting at temperature 22°С. According to the results of sensing by GPR OKO-2 with a center frequency of 1200 MHz delay time, amplitudes and spectral characteristic of the signals at varying moisture (from 3 to 20%) and temperature (from -15 to 15 °C) of rocks were determined. The results of the research showed a significant difference between the velocity of GPR signals at negative and positive temperatures for two types of sands of Quaternary deposits with a moisture content more than 7%. GPR amplitude values of signals and their frequency composition are described, depending on the temperature and humidity of the samples. The obtained results will serve as a basis for creation of automated system for determining the variation of the moisture in the rocks and display the data through geographic information system, which will greatly facilitate the control of moisture content of rocks in the mining industry. Application of the developed system is promising for monitoring of rock properties of pit walls and roofs of mine openings and soil foundations of engineering structures.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>георадиолокация</kwd><kwd>дисперсные горные породы</kwd><kwd>оттайка</kwd><kwd>влажность</kwd><kwd>температура</kwd><kwd>диэлектрическая проницаемость</kwd><kwd>горные объекты</kwd><kwd>криолитозона</kwd></kwd-group><kwd-group xml:lang="en"><kwd>ground penetrating radar</kwd><kwd>dispersed rocks</kwd><kwd>defrost</kwd><kwd>humidity</kwd><kwd>temperature</kwd><kwd>dielectric permittivi- ty</kwd><kwd>mining facilities</kwd><kwd>permafrost</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">Омельяненко А.В. Георадиолокационные ис- следования многолетнемерзлых пород: моно- графия / А.В. Омельяненко, Л.Л. 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