{"id":1297,"date":"2022-02-02T20:11:27","date_gmt":"2022-02-02T19:11:27","guid":{"rendered":"https:\/\/hydrography.boku.ac.at\/wordpress\/?page_id=1297"},"modified":"2025-04-17T12:44:58","modified_gmt":"2025-04-17T10:44:58","slug":"sediment-geology","status":"publish","type":"page","link":"https:\/\/hydrography.boku.ac.at\/wordpress\/de\/sediment-geology\/","title":{"rendered":"Sediment Geology"},"content":{"rendered":"<div data-elementor-type=\"wp-page\" data-elementor-id=\"1297\" class=\"elementor elementor-1297\" data-elementor-settings=\"{&quot;ha_cmc_init_switcher&quot;:&quot;no&quot;}\">\n\t\t\t\t\t\t<section class=\"has_eae_slider elementor-section elementor-top-section elementor-element elementor-element-43c7854 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-eae-slider=\"31108\" data-id=\"43c7854\" data-element_type=\"section\" data-e-type=\"section\" data-settings=\"{&quot;_ha_eqh_enable&quot;:false}\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"has_eae_slider elementor-column elementor-col-33 elementor-top-column elementor-element elementor-element-12fc289\" data-eae-slider=\"26423\" data-id=\"12fc289\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-9a9ad79 elementor-view-default elementor-widget elementor-widget-icon\" data-id=\"9a9ad79\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"icon.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t<div class=\"elementor-icon-wrapper\">\n\t\t\t<a class=\"elementor-icon\" href=\"https:\/\/hydrography.boku.ac.at\/wordpress\/de\/lake-altaussee\/\">\n\t\t\t<i aria-hidden=\"true\" class=\"hm hm-arrow-left\"><\/i>\t\t\t<\/a>\n\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<div class=\"has_eae_slider elementor-column elementor-col-33 elementor-top-column elementor-element elementor-element-5f73efa\" data-eae-slider=\"86747\" data-id=\"5f73efa\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-20fb57c eael-dual-header-content-align-center elementor-widget elementor-widget-eael-dual-color-header\" data-id=\"20fb57c\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"eael-dual-color-header.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t<div class=\"eael-dual-header\">\n\t\t\t\t<h2 class=\"title eael-dch-title\"><span class=\"eael-dch-title-text eael-dch-title-lead lead solid-color\">Sediment<\/span> <span class=\"eael-dch-title-text\">Geology<\/span><\/h2>\t\t\t<\/div>\n\n\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<div class=\"has_eae_slider elementor-column elementor-col-33 elementor-top-column elementor-element elementor-element-0eed9ee\" data-eae-slider=\"7638\" data-id=\"0eed9ee\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"has_eae_slider elementor-section elementor-top-section elementor-element elementor-element-dd22931 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-eae-slider=\"51656\" data-id=\"dd22931\" data-element_type=\"section\" data-e-type=\"section\" data-settings=\"{&quot;_ha_eqh_enable&quot;:false}\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"has_eae_slider elementor-column elementor-col-50 elementor-top-column elementor-element elementor-element-f43515e\" data-eae-slider=\"20424\" data-id=\"f43515e\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-58045c6 elementor-widget elementor-widget-spacer\" data-id=\"58045c6\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"spacer.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t<div class=\"elementor-spacer\">\n\t\t\t<div class=\"elementor-spacer-inner\"><\/div>\n\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-096a2e7 elementor-widget__width-initial elementor-widget elementor-widget-text-editor\" data-id=\"096a2e7\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p>The main objective of the limnogeological work is to establish a stratigraphic model of Lake Altaussee, enabling to study natural hazards and its effects on the local (Lake Altaussee), vs. regional level (i.e. in comparison to other lakes)<\/p>\n<p>Specific Objective (O-1): Establish detailed characterization of the Holocene sedimentary infill of Lake Altaussee including semi-automated sediment classification techniques<\/p>\n<p>Specific Objective (O-2): Develop lake-specific understanding of lithostratigraphic evolution and event deposition to establish event stratigraphic records and interpretations of causes and consequences of extreme events<\/p>\n<p>Investigations are focusing on the analysis of subbottom profiles and sediment cores:<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-e6ddb7a elementor-widget elementor-widget-text-editor\" data-id=\"e6ddb7a\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<ul><li>a dense network of subbottom profiles (UIBK: 3.5 kHz Geopulse Pinger; BOKU: 8 kHz Innomar SES-2000)<\/li><li>22 short cores (hammer-driven, up to 1.8 long)<\/li><li>8 surface cores (up to 49 cm)<\/li><li>7 long sediment cores (length: 3m up to 9m; hammer-piston system borrowed from ETH Z\u00fcrich)<\/li><\/ul>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-412ed60 elementor-widget elementor-widget-text-editor\" data-id=\"412ed60\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p><b><span style=\"color: #000000;\">Lab work &#8211; <a href=\"https:\/\/www.uibk.ac.at\/geologie\/corescanlab\/\">Austrian Core Facility of the University of Innsbruck (ACF)<\/a><\/span><\/b><\/p><p><span style=\"color: #000000;\"><b><em>Core images<\/em><\/b><br \/>High resolution core images of all cores have been acquired using the Smartcube Camera Image Scanner (SmartCIS) and the COX Analytical Systems ItraxXRF-CS<\/span><\/p><p><span style=\"color: #000000;\"><b><em>Multi-Sensor<\/em> <em>Core Logger<\/em> <em>(MSCL)<\/em><\/b><br \/>Whole round cores were measured with 0.5 cm resolution (bulk measurements: magnetic susceptibility, P-Wave velocity and \u03b3-density). Split cores were measured with 0.2 cm resolution (point measurements: magnetic susceptibility (Bartington MS2E sensor) and color spectrophotometer (CM-700d spectrophotometer from Konica Minolta Measuring Instruments)).<\/span><\/p><p><span style=\"color: #000000;\"><b><em>X-ray fluorescence<\/em><em> scanning (XRF)<\/em><\/b><br \/>XRF-CS was performed at ACF using COX Analytical Systems Itrax XRF core scanner on all surface and short cores at 500 \u03bcm downcore resolution. The Itrax XRF-CS was run with a Molybdenum X-ray tube (voltage 30 kV; current 45 mA; exposure time 5 s). Furthermore, radiograph of cores was collected by using Itrax XRF-CS digital continuous-strip X- radiograph (22 mm in width; at 200 \u03bcm downcore resolution).<\/span><\/p><p><span style=\"color: #000000;\"><b><em>Medical<\/em> <em>and micro<\/em><em> X-ray computed tomography ((\u03bc-)XCT)<\/em><\/b><br \/>Medical XCT scans were obtained with a voxel size of 0.2 \u00d7 0.2 \u00d7 0.3 mm3\u00a0at the Medical University of Innsbruck using a Siemens SOMATOM Definition AS.<\/span><\/p><p><span style=\"color: #000000;\"><b><em>Age<\/em> <em>constraints<\/em> <em>14<\/em><em>C-method<\/em><\/b><br \/>Constraints on the depositional age of the sedimentary sequence of the last ~ 150 years as covered by the surface cores will be available from gamma spectrometric measurements (short-lived radionuclide 137Cs and 210Pb dating); radiocarbon AMS 14C dating was obtained on cores to extend the existing age model.<\/span><\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<div class=\"has_eae_slider elementor-column elementor-col-50 elementor-top-column elementor-element elementor-element-86f3c66\" data-eae-slider=\"18910\" data-id=\"86f3c66\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<section class=\"has_eae_slider elementor-section elementor-inner-section elementor-element elementor-element-5b301e4 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-eae-slider=\"25917\" data-id=\"5b301e4\" data-element_type=\"section\" data-e-type=\"section\" data-settings=\"{&quot;_ha_eqh_enable&quot;:false}\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"has_eae_slider elementor-column elementor-col-50 elementor-inner-column elementor-element elementor-element-57cf1f0\" data-eae-slider=\"14748\" data-id=\"57cf1f0\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-b8d453f elementor-widget elementor-widget-text-editor\" data-id=\"b8d453f\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p><span style=\"color: #000000;\">Contact:\u00a0 <a href=\"https:\/\/www.uibk.ac.at\/geologie\/moernaut\/\">Jasper Moernaut<\/a><br \/><\/span><span style=\"color: #000000;\">\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0 Department of Geology<br \/>\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0 University of Innsbruck (UIBK)<br \/><\/span><\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<div class=\"has_eae_slider elementor-column elementor-col-50 elementor-inner-column elementor-element elementor-element-b27bed3\" data-eae-slider=\"29371\" data-id=\"b27bed3\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-db80ae8 elementor-widget elementor-widget-image\" data-id=\"db80ae8\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<a href=\"https:\/\/www.uibk.ac.at\/\">\n\t\t\t\t\t\t\t<img decoding=\"async\" src=\"https:\/\/hydrography.boku.ac.at\/wordpress\/wp-content\/uploads\/elementor\/thumbs\/UIBK_Logo_150x44-pjrve5rmzr3ts3osc5zkvpimiqbgj5b2yu1cj3njug.jpg\" title=\"UIBK\" alt=\"Universit\u00e4t Innsbruck\" loading=\"lazy\" \/>\t\t\t\t\t\t\t\t<\/a>\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<div class=\"elementor-element elementor-element-cc681bd elementor-widget elementor-widget-spacer\" data-id=\"cc681bd\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"spacer.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t<div class=\"elementor-spacer\">\n\t\t\t<div class=\"elementor-spacer-inner\"><\/div>\n\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-dfc5075 elementor-arrows-position-inside elementor-pagination-position-outside elementor-widget elementor-widget-image-carousel\" data-id=\"dfc5075\" data-element_type=\"widget\" data-e-type=\"widget\" data-settings=\"{&quot;slides_to_show&quot;:&quot;1&quot;,&quot;autoplay_speed&quot;:3000,&quot;navigation&quot;:&quot;both&quot;,&quot;autoplay&quot;:&quot;yes&quot;,&quot;pause_on_hover&quot;:&quot;yes&quot;,&quot;pause_on_interaction&quot;:&quot;yes&quot;,&quot;infinite&quot;:&quot;yes&quot;,&quot;effect&quot;:&quot;slide&quot;,&quot;speed&quot;:500}\" data-widget_type=\"image-carousel.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t<div class=\"elementor-image-carousel-wrapper swiper\" role=\"region\" aria-roledescription=\"carousel\" aria-label=\"Image Carousel\" dir=\"ltr\">\n\t\t\t<div class=\"elementor-image-carousel swiper-wrapper\" aria-live=\"off\">\n\t\t\t\t\t\t\t\t<div class=\"swiper-slide\" role=\"group\" aria-roledescription=\"slide\" aria-label=\"1 of 9\"><figure class=\"swiper-slide-inner\"><img decoding=\"async\" class=\"swiper-slide-image\" 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class=\"swiper-pagination\"><\/div>\n\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-7f28cf0 elementor-widget elementor-widget-image\" data-id=\"7f28cf0\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<img decoding=\"async\" src=\"https:\/\/hydrography.boku.ac.at\/wordpress\/wp-content\/uploads\/elementor\/thumbs\/analysis_101-pjvp4eji3dsxwsa4nhxmdnh4mjrqzj4g1ngil59mo0.jpg\" title=\"analysis_101\" alt=\"analysis_101\" loading=\"lazy\" \/>\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-20330d6 elementor-widget elementor-widget-text-editor\" data-id=\"20330d6\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p><span style=\"color: #000000;\">Analysis 101 of the sediment core delivered\u00a0 &#8230;..<\/span> <\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<\/div>","protected":false},"excerpt":{"rendered":"<p>Sediment Geology The main objective of the limnogeological work is to establish a stratigraphic model of Lake Altaussee, enabling to study natural hazards and its effects on the local (Lake Altaussee), vs. regional level (i.e. in comparison to other lakes) Specific Objective (O-1): Establish detailed characterization of the Holocene sedimentary infill of Lake Altaussee including 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