{"id":28129,"date":"2022-03-07T18:40:39","date_gmt":"2022-03-07T17:40:39","guid":{"rendered":"https:\/\/www.ig.cas.cz\/?page_id=28129"},"modified":"2026-02-18T11:43:44","modified_gmt":"2026-02-18T10:43:44","slug":"environmental-and-applied-geophysics","status":"publish","type":"page","link":"https:\/\/www.ig.cas.cz\/en\/research\/teams\/environmental-and-applied-geophysics\/","title":{"rendered":"Environmental and applied geophysics"},"content":{"rendered":"<p>[et_pb_section fb_built=&#8221;1&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; custom_padding=&#8221;40px|||||&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_row column_structure=&#8221;1_2,1_2&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_column type=&#8221;1_2&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_text _builder_version=&#8221;4.24.2&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;]<\/p>\n<h4>Team leader: Hana Grison<\/h4>\n<p>&nbsp;<\/p>\n<p>The priority of our research is to understand the mechanisms at work in our environment and thus contribute to its sustainability. To do this, we use geophysical methods to investigate not only shallow layers of geology\/volcanology\/archaeology, but also deeper structures for geothermal energy exploitation. Specifically, we address the following topics:<\/p>\n<p>[\/et_pb_text][et_pb_toggle title=&#8221;Environmental research on soils and rocks&#8221; _builder_version=&#8221;4.24.2&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;]<\/p>\n<p>As part of our environmental studies, we measure the magnetic properties of soils and rocks to study, e.g., pollution and\/or to more accurately determine soil characteristics. In this area, we cooperate in particular with colleagues from Poland and Belgium.<\/p>\n<p>[\/et_pb_toggle][et_pb_toggle title=&#8221;Geothermal research&#8221; _builder_version=&#8221;4.24.2&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;]<\/p>\n<p>In geothermal research we measure the thermophysical properties of rocks from boreholes to determine and refine the values of the Earth&#8217;s&nbsp;heat flux and calculate the temperature in the Earth&#8217;s&nbsp;crust.<br \/>We investigate the potential for exploiting geothermal energy, and in interdisciplinary studies we look at the links between air, soil and bedrock temperature. Temperature data are also used for palaeoclimate reconstructions, including the occurrence and dynamics of permafrost.<\/p>\n<p>[\/et_pb_toggle][et_pb_toggle title=&#8221;Non-destructive archaeological research&#8221; _builder_version=&#8221;4.24.2&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;]<\/p>\n<p>The aim is to streamline archaeological research by measuring magnetic susceptibility, magnetic field strength, electrical resistivity tomography (ERT) and microgravimetry. In addition to identifying hidden archaeologically significant remains, another goal is to obtain information from the magnetic and geochemical record of past human activity in the soil.<\/p>\n<p>[\/et_pb_toggle][et_pb_toggle title=&#8221;Research on shallow geological structures&#8221; _builder_version=&#8221;4.24.2&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;]<\/p>\n<p>We contribute to studies of salt bodies and to search for unknown volcanic structures by gravimetry and magnetometry, supplemented by ERT measurements. This research also includes 3D gravimetric and magnetic modelling.<br \/>Since 2007, we have been cooperating with German geological organisations to search for volcanic structures in Bavaria, the Czech Republic and Saxony.<\/p>\n<p>[\/et_pb_toggle][et_pb_toggle title=&#8221;Hydrogeological research &#8221; _builder_version=&#8221;4.24.2&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;]<\/p>\n<p>We investigate the hydrogeological regime in a&nbsp;coal mine based on microgravimetric monitoring. In the CSA quarry, we monitor the stability of the risky slope of the Jeze\u0159\u00ed Castle mine using inclinometer stations.<\/p>\n<p>[\/et_pb_toggle][et_pb_toggle title=&#8221;Laboratory equipment&#8221; _builder_version=&#8221;4.24.2&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;]<\/p>\n<p>Bartington MS2B (dual frequency), probe for soil cores MS2C (https:\/\/www.bartington.com)<br \/>Agico instruments: MFK1, KLY5 with 3D Rotator, CS4\/ CS-L High\/Low Temperature Furnace Apparatus (https:\/\/www.agico.com)<br \/>ADE EV9 vibrating sample magnetometer (DSM Magnetics, ADE Corporation; Lowell, MA, USA):Hysteresis loops (induced magnetization) magnetic fields from -2 to +2 T.<\/p>\n<p>[\/et_pb_toggle][et_pb_toggle title=&#8221;Instruments for the in-situ measurements&#8221; _builder_version=&#8221;4.24.2&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;]<\/p>\n<p>Batrington MS2\/MS3 System for surface magnetic mapping: MS2D and MS2F (https:\/\/www.bartington.com)<br \/>Susceptibility meter SM400 (http:\/\/www.zhinstruments.com)<br \/>Shirt Pocket zise magnetic susceptibility meter SM30 (http:\/\/www.zhinstruments.com)<br \/>Potrable magnetic susceptibility meters with adjustable frequency and field intensity SM 150L and SM150H (http:\/\/www.zhinstruments.com)<br \/>Gravimeter Scintrex CG-6 (https:\/\/scintrexltd.com)<br \/>Gravimeter LaCoste&amp;Romberg model D (http:\/\/microglacoste.com)<br \/>Automatic resistivitity system ARESII in 5-channel configuration with 10 cable sections (http:\/\/www.gfinstruments.cz\/)<\/p>\n<p>[\/et_pb_toggle][et_pb_text _builder_version=&#8221;4.24.2&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;]<\/p>\n<p><strong>Topic of Bacelors\/Master\/PhD thesis<\/strong><\/p>\n<p>Development of 3D gravity modelling of salt diapirs (PrF UK, R. Ber\u00e1nek, PhD theses)<\/p>\n<p>[\/et_pb_text][\/et_pb_column][et_pb_column type=&#8221;1_2&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_text _builder_version=&#8221;4.24.2&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;]<\/p>\n<h4>Running projects<\/h4>\n<p>&nbsp;<\/p>\n<ul>\n<li>Czech Science Foundation \u2013 National Science Centre Poland 23-09559L, 2024-2026<\/li>\n<li>The origin of iron minerals in soils with high permeability and determination of soil diagnostic horizons using magnetic proxies \u2013 E. Petrovsk\u00fd (PI), team members Grison, Stejskalov\u00e1<br \/>Mobility Plus (MPP) between CAS and FNRS (Belgium), 2023\u20132025<\/li>\n<li>Geophysical survey as a&nbsp;tool for assessing magnetomineralogical changes in soils at archaeological sites endangered by erosion \u2013 H. Grison (PI), team members \u0160. Stejskalov\u00e1, R. Klanica, R. Ber\u00e1nek, E. Petrovsk\u00fd<\/li>\n<li>Mobility project CAS, 2022-2024. Comparison of geophysical and geological structures of the Western Carpathian lithosphere with other orogenic areas in Europe (mainly Bohemian Massif and Norwegian Caledonides) \u2013 R. Klanica (PI), S. Kov\u00e1\u010dikov\u00e1<\/li>\n<li>Grant GACR, 2024-2026. Structure and dynamics of shallow salt sheet extrusion investigated by means of magnetotellurics, gravity and analog &amp; numerical modelling \u2013 R. Klanica. J. Mrlina team members, G.Hill (PI)<\/li>\n<li>Grant GACR 2022-2024, Geodynamic controls on continental rifting in Cenozoic central Europe: Insight from the Eger Rift, Bohemia] \u2013 J. Mrlina team member, D. Uli\u010dn\u00fd (PI)<\/li>\n<li>Since 2016 International collaboration project <a href=\"http:\/\/www.alparray.ethz.ch\/en\/research\/research-groups\/gravity-rg\/\" target=\"_blank\" rel=\"noopener\">AlpArrayGravityGroup<\/a> (AAGG) \u2013 Mrlina<\/li>\n<li>Cooperation with industry support: Tilt and groundwater monitoring in Jeze\u0159\u00ed gallery, North Bohemia &#8211; Severn\u00ed energetick\u00e1, a.s., project SE 2023\/34 &#8211; observatory program since 1982 \u2013 J. Mrlina (PI), Pol\u00e1k, Skalsk\u00fd, Seidl<\/li>\n<li>Since 2007 partnership projects with Bavarian and Saxonian Geological Surveys on research of volcanic structures in the Czechia, Bavaria and Saxony \u2013 Mrlina (PI), Ber\u00e1nek, Pol\u00e1k, Klanica<\/li>\n<li><a href=\"https:\/\/opst.cz\/projekt\/synergys\/\">SYNERGYS<\/a> \u2013 Borehole Thermal Energy Storage, BTES<\/li>\n<\/ul>\n<p>[\/et_pb_text][et_pb_toggle title=&#8221;Completed research projects&#8221; _builder_version=&#8221;4.24.2&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;]<\/p>\n<p><a href=\"https:\/\/www.saga-cost.eu\/\" target=\"_blank\" rel=\"noopener\">COST Action SAGA<\/a> (The Soil Science &amp; Archaeo-Geophysics Alliance) from 10\/2018 until 4\/2023 (H. Grison)<br \/>Inter COST Project \u201cApplication of Geophysical Approach in Archaeological Research and Prospection\u201c is supported by the program INTER-EXCELLENCE of the Ministry of Education, Youth and Sports of the Czech Republic (MEYS), grant No. LTC19029, 2019-2022. (H. Grison (PI), R. Klanica, J. Mrlina, \u0160. Stejskalov\u00e1)<br \/>Mobility project ASCR 2021-2022 &#8211; Comparison of geophysical and geological structures of the Western Carpathian lithosphere with other orogenic areas in Europe (mainly Bohemian Massif and Norwegian Caledonides) (R. Klanica(PI), S. Kov\u00e1\u010dikov\u00e1)<br \/>Cooperation with industry support: Hydrological regime in coal mine indicated by gravity monitoring &#8211; Severo\u010desk\u00e9 doly, a.s. \u2013 project 2023 (Mrlina)<\/p>\n<p>[\/et_pb_toggle][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_text _builder_version=&#8221;4.27.4&#8243; _module_preset=&#8221;default&#8221; hover_enabled=&#8221;0&#8243; global_colors_info=&#8221;{}&#8221; sticky_enabled=&#8221;0&#8243;]<\/p>\n<p><strong>People<\/strong><\/p>\n<table style=\"width: 1114px;\">\n<tbody>\n<tr>\n<td style=\"width: 140.4px;\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-21828 alignnone size-full\" src=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-obr-grison-1.jpg\" alt=\"\" width=\"286\" height=\"286\" srcset=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-obr-grison-1.jpg 286w, https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-obr-grison-1-150x150.jpg 150w\" sizes=\"(max-width: 286px) 100vw, 286px\" \/><\/td>\n<td style=\"width: 234.65px;\">\n<p><a href=\"https:\/\/www.ig.cas.cz\/en\/contact\/staff\/hana-grison\/\">Hana Grison<\/a><\/p>\n<p>ORCID:\u00a0<a href=\"https:\/\/orcid.org\/0000-0002-0402-2026\">0000-0002-0402-2026<\/a><\/p>\n<\/td>\n<td style=\"width: 117.333px;\">Ing, PhD<\/td>\n<td style=\"width: 205.567px;\">\n<p>Researcher<\/p>\n<p>(team leader)<\/p>\n<\/td>\n<td style=\"width: 382.05px;\">Environmental magnetism, soil science, archaeomagnetic dating<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 140.4px;\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-21824 alignnone size-full\" src=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-obr-beranek.jpg\" alt=\"\" width=\"244\" height=\"244\" srcset=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-obr-beranek.jpg 244w, https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-obr-beranek-150x150.jpg 150w\" sizes=\"(max-width: 244px) 100vw, 244px\" \/><\/td>\n<td style=\"width: 234.65px;\">\n<p>Roman Ber\u00e1nek<\/p>\n<p>ORCID:\u00a0<a href=\"https:\/\/orcid.org\/0000-0002-7273-8472\">0000-0002-7273-8472<\/a><\/p>\n<\/td>\n<td style=\"width: 117.333px;\">\u00a0<\/td>\n<td style=\"width: 205.567px;\">PhD student<\/td>\n<td style=\"width: 382.05px;\">Microgravimetry, \u00a0magnetometry, 3D gravity-magnetic modeling and inversion of geophysical data, archaeogeophysics, volcanology, and geodynamics<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 140.4px;\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-20676 alignnone size-full\" src=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/dedecek.jpg\" alt=\"\" width=\"300\" height=\"299\" srcset=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/dedecek.jpg 300w, https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/dedecek-150x150.jpg 150w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><\/td>\n<td style=\"width: 234.65px;\"><a href=\"https:\/\/www.ig.cas.cz\/en\/contact\/staff\/petr-dedecek\/\">Petr D\u011bde\u010dek<\/a><\/td>\n<td style=\"width: 117.333px;\">PhD<\/td>\n<td style=\"width: 205.567px;\">Researcher<\/td>\n<td style=\"width: 382.05px;\">\u00a0<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 140.4px;\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-21831 alignnone size-medium\" src=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-obr-klanica-300x300.jpg\" alt=\"\" width=\"300\" height=\"300\" srcset=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-obr-klanica-300x300.jpg 300w, https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-obr-klanica-150x150.jpg 150w, https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-obr-klanica.jpg 408w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><\/td>\n<td style=\"width: 234.65px;\">\n<p><a href=\"https:\/\/www.ig.cas.cz\/en\/contact\/staff\/radek-klanica\/\">Radek Klanica<\/a><\/p>\n<p>ORCID:\u00a0<a href=\"https:\/\/orcid.org\/0000-0002-8302-7537\">0000-0002-8302-7537<\/a><\/p>\n<\/td>\n<td style=\"width: 117.333px;\">Mgr, PhD<\/td>\n<td style=\"width: 205.567px;\">Researcher<\/td>\n<td style=\"width: 382.05px;\">\n<p>Geoelectrical methos, magnetometry, magnetotellurics<\/p>\n<p>&nbsp;<\/p>\n<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 140.4px;\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-21835 alignnone size-medium\" src=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-obr-mrlina-300x300.jpg\" alt=\"\" width=\"300\" height=\"300\" srcset=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-obr-mrlina-300x300.jpg 300w, https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-obr-mrlina-150x150.jpg 150w, https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-obr-mrlina.jpg 450w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><\/td>\n<td style=\"width: 234.65px;\">\n<p><a href=\"https:\/\/www.ig.cas.cz\/en\/contact\/staff\/jan-mrlina\/\">Jan Mrlina<\/a><\/p>\n<p>ORCID:\u00a0<a href=\"https:\/\/orcid.org\/0000-0002-4224-1609\">0000-0002-4224-1609<\/a><\/p>\n<\/td>\n<td style=\"width: 117.333px;\">RNDr, PhD<\/td>\n<td style=\"width: 205.567px;\">Senior researcher<\/td>\n<td style=\"width: 382.05px;\">Gravimetry, applied geophysics, geodynamics, volcanology, reservoirs,gravity\/magnetic exploration, archaeogeophysics<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 140.4px;\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-21837 alignnone size-medium\" src=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-obr-petrovsky-300x300.jpg\" alt=\"\" width=\"300\" height=\"300\" \/><\/td>\n<td style=\"width: 234.65px;\">\n<p><a href=\"https:\/\/www.ig.cas.cz\/en\/contact\/staff\/eduard-petrovsky\/\">Eduard Petrovsk\u00fd<\/a><\/p>\n<p>ORCID: <a href=\"https:\/\/orcid.org\/0000-0001-7792-9123\">0000-0001-7792-9123<\/a><\/p>\n<\/td>\n<td style=\"width: 117.333px;\">RNDr, CSc<\/td>\n<td style=\"width: 205.567px;\">Senior researcher<\/td>\n<td style=\"width: 382.05px;\">Environmental magnetism<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 140.4px;\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-20672 alignnone size-full\" src=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/safanda.jpg\" alt=\"\" width=\"273\" height=\"274\" srcset=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/safanda.jpg 273w, https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/safanda-150x150.jpg 150w\" sizes=\"(max-width: 273px) 100vw, 273px\" \/><\/td>\n<td style=\"width: 234.65px;\">\n<p><a href=\"https:\/\/www.ig.cas.cz\/en\/contact\/staff\/jan-safanda\/\">Jan \u0160afanda<\/a><\/p>\n<p>ORCID: <a href=\"https:\/\/orcid.org\/0000-0002-0300-7545\">0000-0002-0300-7545<\/a><\/p>\n<\/td>\n<td style=\"width: 117.333px;\">RNDr, CSc<\/td>\n<td style=\"width: 205.567px;\">Researcher<\/td>\n<td style=\"width: 382.05px;\">Geothermics, permafrost dynamics, paleoclimate reconstructions, utilization of geothermal energy<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 140.4px;\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-21820 alignnone size-medium\" src=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-obr-stejskalova-300x300.jpg\" alt=\"\" width=\"300\" height=\"300\" srcset=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-obr-stejskalova-300x300.jpg 300w, https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-obr-stejskalova-150x150.jpg 150w, https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-obr-stejskalova.jpg 463w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><\/td>\n<td style=\"width: 234.65px;\">\n<p>\u0160\u00e1rka Stejskalov\u00e1<\/p>\n<p>ORCID: <a href=\"https:\/\/orcid.org\/0000-0002-0722-0466\">0000-0002-0722-0466<\/a><\/p>\n<\/td>\n<td style=\"width: 117.333px;\">Ing, PhD<\/td>\n<td style=\"width: 205.567px;\">Researcher<\/td>\n<td style=\"width: 382.05px;\">Environmental magnetism, soil science<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 140.4px;\">\u00a0<\/td>\n<td style=\"width: 234.65px;\"><a href=\"https:\/\/www.ig.cas.cz\/en\/contact\/staff\/contact-staff-anna-plackova\/\">Anna Pla\u010dkov\u00e1<\/a><\/td>\n<td style=\"width: 117.333px;\">Ing.<\/td>\n<td style=\"width: 205.567px;\">PhD student<\/td>\n<td style=\"width: 382.05px;\">Environmental and applied geomagnetism with a&nbsp;focus on magnetic properties of soils, interpretation of magnetic data, and their application in the assessment of soil profiles, soil processes, and soil contamination.<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<p>[\/et_pb_text][et_pb_text _builder_version=&#8221;4.27.4&#8243; _module_preset=&#8221;default&#8221; hover_enabled=&#8221;0&#8243; global_colors_info=&#8221;{}&#8221; sticky_enabled=&#8221;0&#8243;]<\/p>\n<p><strong>Collaborating members<\/strong><\/p>\n<p><a href=\"https:\/\/www.ig.cas.cz\/en\/contact\/staff\/svetlana-kovacikova\/\">Svetlana Kov\u00e1\u010dikov\u00e1<\/a><br \/><a href=\"https:\/\/www.ig.cas.cz\/en\/contact\/staff\/tomas-bayer\/\">Tom\u00e1\u0161 Bayer<\/a><br \/><a href=\"https:\/\/www.ig.cas.cz\/en\/contact\/staff\/michal-seidl\/\">Michal Seidl<\/a><\/p>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=&#8221;1_3,1_3,1_3&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_column type=&#8221;1_3&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_image src=&#8221;https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-grison-obr3.jpg&#8221; title_text=&#8221;web grison obr3&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][\/et_pb_image][\/et_pb_column][et_pb_column type=&#8221;1_3&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_image src=&#8221;https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-grison-obr4.jpg&#8221; title_text=&#8221;web grison obr4&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][\/et_pb_image][\/et_pb_column][et_pb_column type=&#8221;1_3&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_image src=&#8221;https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2022\/03\/app6.png&#8221; title_text=&#8221;App6&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][\/et_pb_image][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=&#8221;1_3,1_3,1_3&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_column type=&#8221;1_3&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_text _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;]<\/p>\n<p style=\"text-align: center;\"><em>Soil sampling at the Hillfort \u0160t\u011bp\u00e1nov, Czechia, Inter-COST project. Magnetic soil properties with ERT measurements are employed for description of Late Bronze Age water reservoirs (photo \u2013 E. Garcia, 2\/2020<\/em>)<\/p>\n<p>[\/et_pb_text][\/et_pb_column][et_pb_column type=&#8221;1_3&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_text _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;]<\/p>\n<p style=\"text-align: center;\"><em>R. Klanica p\u0159i&nbsp;ERT m\u011b\u0159en\u00ed na hradi\u0161ti Hradi\u0161\u0165any (star\u0161\u00ed doba bronzov\u00e1), projekt Inter-COST. Detekce mo\u017en\u00e9ho zanikl\u00e9ho vodn\u00edho zdroje na hradi\u0161ti (foto \u2013 T. Junek, 5\/2020)<\/em><\/p>\n<p>[\/et_pb_text][\/et_pb_column][et_pb_column type=&#8221;1_3&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_text _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;]<\/p>\n<p style=\"text-align: center;\"><em>Gravity monitoring in Stefanos crater (with enough H2S to respire), Greece \u2013 observatory project CzechGeo (photo &#8211; J.Mrlina, 2019)<\/em><\/p>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=&#8221;1_3,1_3,1_3&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_column type=&#8221;1_3&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_image src=&#8221;https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2022\/03\/app4.png&#8221; title_text=&#8221;App4&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][\/et_pb_image][\/et_pb_column][et_pb_column type=&#8221;1_3&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_image src=&#8221;https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2022\/03\/app5.png&#8221; title_text=&#8221;App5&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][\/et_pb_image][\/et_pb_column][et_pb_column type=&#8221;1_3&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_image src=&#8221;https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-grison-obr7.jpg&#8221; title_text=&#8221;web grison obr7&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][\/et_pb_image][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=&#8221;1_3,1_3,1_3&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_column type=&#8221;1_3&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_text _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;]<\/p>\n<p style=\"text-align: center;\"><em>Sampling for paleomagnetic dating, cellar V&nbsp;Kolkovn\u011b street, Inter-Cost project, (Photo &#8211; P.&nbsp;Schnabl, 2\/2022)<\/em><\/p>\n<p>[\/et_pb_text][\/et_pb_column][et_pb_column type=&#8221;1_3&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_text _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;]<\/p>\n<p style=\"text-align: center;\"><em>Magnetic survey in Ba\u017eina maar, scientific cooperation with GFZ Potsdam (photo \u2013 V.Pol\u00e1k, 2021<\/em><em>)<\/em><\/p>\n<p>[\/et_pb_text][\/et_pb_column][et_pb_column type=&#8221;1_3&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_text _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;]<\/p>\n<p style=\"text-align: center;\"><em>Drill-coring at the Roman site of Zaldua, the Basque province of Navare. Short term scientific mission project in scope of SAGA Action (photo H. Grison, 1\/2020)<\/em><\/p>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section]<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Team leader: Hana Grison &nbsp; The priority of our research is to understand the mechanisms at work in our environment and thus contribute to its sustainability. To do this, we use geophysical methods to investigate not only shallow layers of geology\/volcanology\/archaeology, but also deeper structures for geothermal energy exploitation. 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