{"id":6045,"date":"2026-01-21T11:56:33","date_gmt":"2026-01-21T11:56:33","guid":{"rendered":"https:\/\/izvestiyakbncran.ru\/?page_id=6045"},"modified":"2026-06-02T10:27:43","modified_gmt":"2026-06-02T09:27:43","slug":"27-6-7-en","status":"publish","type":"page","link":"https:\/\/izvestiyakbncran.ru\/index.php\/en\/27-6-7-en\/","title":{"rendered":"27.6.7 En"},"content":{"rendered":"\n<h1 class=\"wp-block-heading has-lora-font-family\" style=\"font-size:22px\"><strong>Inverse problem on determining variable-order fractional derivative in mathematical model of anomalous variations in radon volumetric activity<\/strong><\/h1>\n\n\n\n<p class=\"has-foreground-color has-text-color has-link-color has-lora-font-family has-extra-small-font-size wp-elements-6d4d44063254381757c479341ca8da97 wp-block-paragraph\" style=\"margin-top:0;margin-bottom:0;padding-top:0;padding-bottom:0\"><strong>D.A. Tverdyi, R.I. Parovik<\/strong><\/p>\n\n\n\n<div class=\"wp-block-group is-vertical is-content-justification-left is-nowrap is-layout-flex wp-container-core-group-is-layout-20193d73 wp-block-group-is-layout-flex\" style=\"border-style:none;border-width:0px;margin-top:0;margin-bottom:0;padding-top:0;padding-bottom:0\">\n<p class=\"has-text-color has-link-color has-lora-font-family wp-elements-1934a6274ad67c2dd8d97ce7471e2bbb wp-block-paragraph\" style=\"color:#5b1919;font-size:12px;text-decoration:underline\"><\/p>\n\n\n\n<div class=\"wp-block-group is-horizontal is-layout-flex wp-container-core-group-is-layout-9076828a wp-block-group-is-layout-flex\" style=\"min-height:0px;margin-top:0;margin-bottom:0;padding-top:0;padding-bottom:0\">\n<div class=\"wp-block-buttons is-content-justification-left is-layout-flex wp-container-core-buttons-is-layout-856cf56e wp-block-buttons-is-layout-flex\" style=\"margin-top:0;margin-bottom:0;padding-top:0;padding-right:0;padding-bottom:0;padding-left:0\">\n<div class=\"wp-block-button has-custom-width wp-block-button__width-100 is-style-outline is-style-outline--1\"><a class=\"wp-block-button__link has-background-background-color has-text-color has-background has-link-color has-border-color has-custom-font-size wp-element-button\" href=\"http:\/\/izvestiyakbncran.ru\/wp-content\/uploads\/2026\/06\/7-tvyordyj.pdf\" style=\"border-color:#5b1919;border-style:solid;border-width:2px;border-radius:8px;color:#5b1919;padding-top:0.4rem;padding-right:var(--wp--preset--spacing--40);padding-bottom:0.4rem;padding-left:var(--wp--preset--spacing--40);font-size:12px\">PDF<\/a><\/div>\n<\/div>\n\n\n\n<div style=\"height:0px;width:0px\" aria-hidden=\"true\" class=\"wp-block-spacer wp-container-content-273e683f\"><\/div>\n\n\n\n<div class=\"wp-block-buttons is-layout-flex wp-block-buttons-is-layout-flex\">\n<div class=\"wp-block-button has-custom-width wp-block-button__width-100 is-style-outline is-style-outline--2\"><a class=\"wp-block-button__link has-background-background-color has-text-color has-background has-link-color has-border-color has-text-align-center has-custom-font-size wp-element-button\" href=\"https:\/\/journals.rcsi.science\/1991-6639\/article\/xml\/378616\" style=\"border-color:#5b1919;border-width:2px;border-top-left-radius:8px;border-top-right-radius:8px;border-bottom-left-radius:8px;border-bottom-right-radius:8px;color:#5b1919;padding-top:0.4rem;padding-right:var(--wp--preset--spacing--40);padding-bottom:0.4rem;padding-left:var(--wp--preset--spacing--40);font-size:12px\">JATS XML<\/a><\/div>\n<\/div>\n<\/div>\n\n\n\n<p class=\"has-text-color has-link-color has-lora-font-family has-extra-small-font-size wp-elements-41ee428b6a5740c7f514a7432ff786a3 wp-block-paragraph\" style=\"border-style:none;border-width:0px;border-top-left-radius:0px;border-top-right-radius:0px;border-bottom-left-radius:0px;border-bottom-right-radius:0px;color:#5b1919;margin-top:0;margin-right:0;margin-bottom:0;margin-left:0;padding-top:0;padding-right:0;padding-bottom:0;padding-left:0\"><\/p>\n<\/div>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity is-style-wide\" style=\"margin-top:var(--wp--preset--spacing--20);margin-bottom:var(--wp--preset--spacing--20)\"\/>\n\n\n\n<p class=\"has-foreground-color has-text-color has-link-color has-lora-font-family has-extra-small-font-size wp-elements-6507531cdc0310145c06d4d73cf7ab61 wp-block-paragraph\" style=\"line-height:1.4\"><em><strong><strong>Abstract<\/strong><\/strong>. <\/em>The seismicity issue in the Kamchatka region highlights the importance of fundamental research to understand the processes occurring in the Earth&#8217;s crust. Anomalous changes in the concentration of radioactive radon gas (222Rn) have been observed to be precursor to earthquakes. Monitoring involves collecting data on the volume activity of 222Rn in the recording chamber over time and detecting any unusual patterns or anomalies. However, the mechanisms behind these irregularities are still not well understood. Therefore, the authors have previously proposed new mathematical hereditary VAR models to describe the unusual migration capacity of 222Rn, taking into account the time-dependent transport<br>process in a heterogeneous fractal geoenvironment. The key parameter of the models is the variable order of the Gerasimov-Caputo fractional derivative, related to the intensity of the 222Rn transport process with changes in the permeability of the geoenvironment.<br><strong>\u0410im<\/strong>. The study is to solve the coefficient inverse problem of identifying values in the mathematical hereditary model of anomalous variations of the OAR.<br><strong>Research methods<\/strong>. Methods of mathematical modeling of processes occurring in the geological environment are used, as well as solving coefficient inverse problems for these models using an algorithm based on the Levenberg-Marquardt method (IP-LM).<br><strong>Results<\/strong>. A series of results are obtained for solving the inverse problem with various parameters controlling the IP-LM motion. The results are divided into two types: implausible \u2013 due to going beyond the range of acceptable values and the initial approximation of identified values close to the reference point, similar to manually selected values; plausible \u2013 due to the initial approximation close to 0, good agreement between the results and the OAR data, where the increase in values from 0 to 1 is maintained despite the loss of the reference point&#8217;s apparent periodicity.<br><strong>Conclusions<\/strong>. The results suggest that it is possible to solve the formulated two-parameter inverse problem based on the experimental data of the OAR. The obtained results are plausible; however, the outcome of the inverse problem solution depends on the initial approximation of the identified values.<\/p>\n\n\n\n<p class=\"has-foreground-color has-text-color has-link-color has-lora-font-family has-extra-small-font-size wp-elements-df03325adc83c022634de6b79d43432f wp-block-paragraph\" style=\"line-height:1.4\"><\/p>\n\n\n\n<p class=\"has-foreground-color has-text-color has-link-color has-lora-font-family has-extra-small-font-size wp-elements-e955820d5785c3c190330d8528e7227d wp-block-paragraph\" style=\"line-height:1.4\"><strong><em><strong>Keywords<\/strong><\/em><\/strong><em>:<\/em> mathematical modeling, radon volumetric activity, fractional derivative of variable order, inverse problems<\/p>\n\n\n\n<p class=\"has-foreground-color has-text-color has-link-color has-lora-font-family has-extra-small-font-size wp-elements-df03325adc83c022634de6b79d43432f wp-block-paragraph\" style=\"line-height:1.4\"><\/p>\n\n\n\n<p class=\"has-foreground-color has-text-color has-link-color has-lora-font-family wp-elements-f2eb6b8fe613b87937ff450290fd4fee wp-block-paragraph\" style=\"font-size:12px;line-height:1.4\"><strong><strong>For citation<\/strong>.<\/strong> Tverdyi D.A., Parovik R.I. Inverse problem on determining variable-order fractional derivative in mathematical model of anomalous variations in radon volumetric activity. News of the Kabardino-Balkarian Scientific Center of RAS. 2025. Vol. 27. No. 6. Pp. 77\u201388. DOI: 10.35330\/1991-6639-2025-27-6-77-88<\/p>\n\n\n\n<p class=\"has-foreground-color has-text-color has-link-color has-lora-font-family wp-elements-17c3333a0b1db39b7fa4a3e1a1572bc4 wp-block-paragraph\" style=\"font-size:12px;line-height:1.4\"><\/p>\n\n\n\n<details class=\"wp-block-details has-foreground-color has-text-color has-link-color has-lora-font-family has-extra-small-font-size wp-elements-ec2549c97d58248882a0645dd72a5f4c is-layout-flow wp-container-core-details-is-layout-f488f964 wp-block-details-is-layout-flow\" style=\"font-style:normal;font-weight:700;line-height:1.5\"><summary><strong>R<\/strong>eferences<\/summary>\n<ol style=\"margin-top:0;margin-bottom:0\" class=\"wp-block-list\">\n<li style=\"font-style:normal;font-weight:400\">Firstov P.P., Makarov E.O. Dynamics of subsurface radon in Kamchatka and strong earthquakes. Petropavlovsk-Kamchatsky: Vitus Bering Kamchatka State University. 2018. 148 p. EDN: VXTMDH (In Russian)<\/li>\n\n\n\n<li style=\"font-style:normal;font-weight:400\">Nikolopoulos D., Cantzos D., Alam A. et al. Electromagnetic and radon earthquake precursors. Geosciences. 2024. Vol. 14. No. 10. P. 271. EDN: YDMFHA<\/li>\n\n\n\n<li style=\"font-style:normal;font-weight:400\">Biryulin S.V., Kozlova I.A., Yurkov A.K. Investigation of informative value of volume radon activity in soil during both the stress build up and tectonic earthquakes in the South Kuril region. Bulliten of KRASEC. Earth Sci. 2019. Vol. 44. No. 4. Pp. 73\u201383. EDN: IMOXJB. (In Russian)<\/li>\n\n\n\n<li style=\"font-style:normal;font-weight:400\">Zubkov S.I. Radon precursors of earthquakes. Volcanology and Seismology. 1981. No. 6. Pp. 74\u2013105. (In Russian)<\/li>\n\n\n\n<li style=\"font-style:normal;font-weight:400\">Dubinchuk V.T. Radon as a precursor of earthquakes. 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Hereditary mathematical model of the dynamics of radon accumulation in the accumulation chamber. Mathematics. 2023. Vol. 11. No. 4:850. DOI: 10.3390\/math11040850<\/li>\n\n\n\n<li style=\"font-style:normal;font-weight:400\">Tverdyi D.A., Makarov E.O., Parovik R.I. Research of stress-strain state of geo-environment by emanation methods on the example of alpha(t)-model of radon transport. Bulletin KRASEC. Physical and Mathematical Sciences. 2023. Vol. 44. No. 3. Pp. 86\u2013104. EDN: AOBZGA (In Russian)<\/li>\n\n\n\n<li style=\"font-style:normal;font-weight:400\">Uchaikin V.V. Fractional derivatives for physicists and engineers. Vol. I. Background and Theory. Berlin\/Heidelberg: Springer. 2013. 373 p. DOI: 10.1007\/978-3-642-33911-0<\/li>\n\n\n\n<li style=\"font-style:normal;font-weight:400\">Parovik R.I., Shevtsov B.M. Radon transfer processes in fractional structure medium. Mathematical Models and Computer Simulations. 2010. Vol. 2. Pp. 180\u2013185. 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DOI: 10.1515\/fca-2017-0040<\/li>\n\n\n\n<li style=\"font-style:normal;font-weight:400\">Kabanikhin S.I. Obratnye i nekorrektnye zadachi [Inverse and Ill-Posed Problems]: 4th ed. Novosibirsk: Izdatel&#8217;stvo Sibirskogo otdeleniya RAN, 2018. 508 p. EDN: UQAVAO. (In Russian)<\/li>\n\n\n\n<li style=\"font-style:normal;font-weight:400\">Mueller J.L., Siltanen S. Linear and nonlinear inverse problems with practical applications. Philadelphia: Society for Industrial and Applied Mathematics, 2012. 351 p.<br>DOI: 10.1137\/1.9781611972344<\/li>\n\n\n\n<li style=\"font-style:normal;font-weight:400\">Tverdyi D.A., Parovik R.I., Makarov E.O. Estimation of radon flux density changes in temporal vicinity of the Shipunskoe earthquake with MW = 7.0, 17 August 2024 with the use of<br>the hereditary mathematical model. Geosciences. 2025. Vol. 15. No. 1:30. EDN: WJIKNS<\/li>\n\n\n\n<li style=\"font-style:normal;font-weight:400\">Tverdyi D.A. Refinement of variable order fractional derivative of Gerasimov-Caputo type by multidimensional Levenberg-Marquardt optimization method. In: Computing Technologies and Applied Mathematics. CTAM 2024. Springer Proceedings in Mathematics &amp; Statistics. 2025. Vol. 500. Pp. 159\u2013173. EDN: IRBPFF<\/li>\n\n\n\n<li style=\"font-style:normal;font-weight:400\">More J.J. The Levenberg-Marquardt algorithm: implementation and theory. In: Numerical Analysis. Lecture Notes in Mathematics. 1978. Vol. 630. Pp. 105\u2013116. DOI: 10.1007\/BFb0067700<\/li>\n\n\n\n<li style=\"font-style:normal;font-weight:400\">Vasilyev A.V., Zhukovsky M.V. Determination of mechanisms and parameters which affect radon entry into a room. Journal of Environmental Radioactivity. 2013. Vol. 124. Pp. 185\u2013190. EDN: RFGXPN<\/li>\n\n\n\n<li style=\"font-style:normal;font-weight:400\">Tverdyi D.A., Parovik R.I. Investigation of finite-difference schemes for the numerical solution of a fractional nonlinear equation. Fractal and Fractional. 2022. Vol. 6. No. 1:23.<br>EDN: XPPXOV<\/li>\n\n\n\n<li style=\"font-style:normal;font-weight:400\">Tverdyi D.A. Matematicheskoe modelirovanie variaciy ob&#8217;emnoy aktivnosti radona s uchetom nasledstvennosti: model&#8217;, metody resheniya, programma [Mathematical modeling of variations in radon volumetric activity taking into account heredity: model, solution methods, program]. Moscow: Akademiya Estestvoznaniya, 2025. 186 p. EDN: QUCYFP. (In Russian)<\/li>\n\n\n\n<li style=\"font-style:normal;font-weight:400\">Tikhonov A.N., Samarskii A.A. Equations of Mathematical Physics. London: Macmillan, 1963, 765 p.<\/li>\n\n\n\n<li style=\"font-style:normal;font-weight:400\">Dennis J.E., Robert Jr., Schnabel B. Numerical methods for unconstrained optimization and nonlinear equations. Philadelphia: SIAM, 394 p.<\/li>\n<\/ol>\n<\/details>\n\n\n\n<details class=\"wp-block-details has-foreground-color has-text-color has-link-color has-lora-font-family has-extra-small-font-size wp-elements-7bc2a551d61522c475d436e38fd2c1b1 is-layout-flow wp-container-core-details-is-layout-9ff6af70 wp-block-details-is-layout-flow\" style=\"font-style:normal;font-weight:700;line-height:1.5\"><summary><strong>Information about the author<\/strong>s<\/summary>\n<div class=\"wp-block-group is-vertical is-layout-flex wp-container-core-group-is-layout-1c18c512 wp-block-group-is-layout-flex\" style=\"min-height:0px;margin-top:0;margin-bottom:0;padding-top:var(--wp--preset--spacing--20);padding-right:var(--wp--preset--spacing--40);padding-bottom:var(--wp--preset--spacing--20);padding-left:var(--wp--preset--spacing--40)\">\n<p class=\"wp-block-paragraph\" style=\"font-style:normal;font-weight:400\"><strong>Dmitrii A. Tverdyi<\/strong>, Candidate of Physics and Mathematics, Researcher, Institute of Cosmophysical Research and Radio Wave Propagation Far Eastern Branch of the Russian Academy of Sciences;<br>7, Mirnaya street, Paratunka village, 684034, Russia;<br>dimsolid95@gmail.com, ORCID: https:\/\/orcid.org\/0000-0001-6983-5258, SPIN-code: 2849-4814<br><strong>Roman I. Parovik<\/strong>, Doctor of Physics and Mathematics, Professor of the Far Eastern Branch of the Russian Academy of Sciences, Leading Researcher, Institute of Cosmophysical Research and Radio Wave Propagation Far Eastern Branch of the Russian Academy of Sciences;<br>7, Mirnaya street, Paratunka village, 684034, Russia;<br>parovik@ikir.ru, ORCID: https:\/\/orcid.org\/0000-0002-1576-1860, SPIN-code: 4295-6894<\/p>\n\n\n\n<p class=\"wp-block-paragraph\" style=\"font-style:normal;font-weight:400\"><\/p>\n\n\n\n<p class=\"wp-block-paragraph\" style=\"font-style:normal;font-weight:400\"><\/p>\n\n\n\n<p class=\"wp-block-paragraph\" style=\"font-style:normal;font-weight:400\"><\/p>\n<\/div>\n<\/details>\n\n\n\n<p class=\"wp-block-paragraph\"><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Inverse problem on determining variable-order fractional derivative in mathematical model of anomalous variations in radon volumetric activity D.A. Tverdyi, R.I. Parovik Abstract. The seismicity issue in the Kamchatka region highlights the importance of fundamental research to understand the processes occurring in the Earth&#8217;s crust. Anomalous changes in the concentration of radioactive radon gas (222Rn) have [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"wp-custom-template-home","meta":{"footnotes":""},"class_list":["post-6045","page","type-page","status-publish","hentry"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.8 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>27.6.7 En - \u0418\u0417\u0412\u0415\u0421\u0422\u0418\u042f \u041a\u0410\u0411\u0410\u0420\u0414\u0418\u041d\u041e-\u0411\u0410\u041b\u041a\u0410\u0420\u0421\u041a\u041e\u0413\u041e \u041d\u0410\u0423\u0427\u041d\u041e\u0413\u041e \u0426\u0415\u041d\u0422\u0420\u0410 \u0420\u0410\u041d\u00bb<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/izvestiyakbncran.ru\/index.php\/en\/27-6-7-en\/\" \/>\n<meta property=\"og:locale\" content=\"ru_RU\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"27.6.7 En - \u0418\u0417\u0412\u0415\u0421\u0422\u0418\u042f \u041a\u0410\u0411\u0410\u0420\u0414\u0418\u041d\u041e-\u0411\u0410\u041b\u041a\u0410\u0420\u0421\u041a\u041e\u0413\u041e \u041d\u0410\u0423\u0427\u041d\u041e\u0413\u041e \u0426\u0415\u041d\u0422\u0420\u0410 \u0420\u0410\u041d\u00bb\" \/>\n<meta property=\"og:description\" content=\"Inverse problem on determining variable-order fractional derivative in mathematical model of anomalous variations in radon volumetric activity D.A. Tverdyi, R.I. Parovik Abstract. The seismicity issue in the Kamchatka region highlights the importance of fundamental research to understand the processes occurring in the Earth&#8217;s crust. 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Tverdyi, R.I. Parovik Abstract. The seismicity issue in the Kamchatka region highlights the importance of fundamental research to understand the processes occurring in the Earth&#8217;s crust. 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