{"id":24,"date":"2024-04-04T01:55:40","date_gmt":"2024-04-03T22:55:40","guid":{"rendered":"https:\/\/sisu.ut.ee\/marek\/geofuusikalised-uuringud\/"},"modified":"2024-04-29T13:15:11","modified_gmt":"2024-04-29T10:15:11","slug":"geofuusikalised-uuringud","status":"publish","type":"page","link":"https:\/\/sisu.ut.ee\/marek\/geofuusikalised-uuringud\/","title":{"rendered":"Geof\u00fc\u00fcsikalised uuringud"},"content":{"rendered":"<p>Geof\u00fc\u00fcsikaliste meetoditega on v\u00f5imalik tuvastada maap\u00f5ue ehitust ilma puurimist\u00f6\u00f6deta. Teostatakse georadariga profileerimist ja elektromeetrilisi, seismilisi ja magnetomeetrilisi uuringuid. Samuti tehakse kivimite-setendite f\u00fc\u00fcsikaliste omaduste (tihedus, poorsus, P- ja S-lainete kiirus, magnetiline vastuv\u00f5tlikkus) m\u00f5\u00f5tmisi.<\/p>\n<p>Kontakt:\u00a0<a href=\"https:\/\/sisu.ut.ee\/marek\/inimesed\">Argo J\u00f5eleht<\/a> argo.joeleht(\u00e4t)ut.ee, <a href=\"https:\/\/sisu.ut.ee\/marek\/inimesed\">J\u00fcri Plado<\/a> juri.plado(\u00e4t)ut.ee<\/p>\n<h3>Kasutatavad aparatuurid ja nende v\u00f5imalused:<\/h3>\n<p><strong>Georadar Radsys ZOND12e\u00a0<\/strong><\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"alignnone  wp-image-152\" src=\"https:\/\/sisu.ut.ee\/wp-content\/uploads\/sites\/147\/georadar.jpg\" alt=\"\" width=\"360\" height=\"217\" srcset=\"https:\/\/sisu.ut.ee\/wp-content\/uploads\/sites\/147\/georadar.jpg 1200w, https:\/\/sisu.ut.ee\/wp-content\/uploads\/sites\/147\/georadar-300x181.jpg 300w, https:\/\/sisu.ut.ee\/wp-content\/uploads\/sites\/147\/georadar-1024x617.jpg 1024w, https:\/\/sisu.ut.ee\/wp-content\/uploads\/sites\/147\/georadar-768x463.jpg 768w\" sizes=\"auto, (max-width: 360px) 100vw, 360px\"><\/p>\n<p>V\u00f5imaldab k\u00f5rge lahutusv\u00f5imega uuringuid kuni 10 m s\u00fcgavusele. Uuringu s\u00fcgavus ja detailsus s\u00f5ltuvad kasutatavast sagedusest (olemas varjestatud antennid 100, 300, 500 ja 900 MHz). Eduka kasutuse kogemused on liivakate-kruusakate setete aladelt, turba aladelt ja v\u00e4hesavikate karbonaatkivimite aladelt.<\/p>\n<p><strong>Elektrilise tomograafia seade P.A.S.I. Polares\u00a0<\/strong><\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"alignnone  wp-image-158\" src=\"https:\/\/sisu.ut.ee\/wp-content\/uploads\/sites\/147\/elektromeetria-2.jpg\" alt=\"\" width=\"361\" height=\"239\" srcset=\"https:\/\/sisu.ut.ee\/wp-content\/uploads\/sites\/147\/elektromeetria-2.jpg 1200w, https:\/\/sisu.ut.ee\/wp-content\/uploads\/sites\/147\/elektromeetria-2-300x199.jpg 300w, https:\/\/sisu.ut.ee\/wp-content\/uploads\/sites\/147\/elektromeetria-2-1024x678.jpg 1024w, https:\/\/sisu.ut.ee\/wp-content\/uploads\/sites\/147\/elektromeetria-2-768x509.jpg 768w\" sizes=\"auto, (max-width: 361px) 100vw, 361px\"><\/p>\n<p>V\u00f5imaldab geoloogilise ehituse tuvastamist kuni 40 m s\u00fcgavuseni. Multi-elektroodiline s\u00fcsteem (kuni 64 elektroodi) v\u00f5imaldab koostada detailseid eritakistuse l\u00e4bil\u00f5ikeid. P\u00f5hilised kasutusvaldkonnad on seotud erineva elektrilise takistusega kihtide paksuse ja leviku selgitamine ning l\u00f5helisusv\u00f6\u00f6ndite piiritlemine.<\/p>\n<p><strong>Seismomeetrid DMT Summit II\u00a0<\/strong><\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"alignnone  wp-image-172\" src=\"https:\/\/sisu.ut.ee\/wp-content\/uploads\/sites\/147\/seismika_img_0521.jpg\" alt=\"\" width=\"361\" height=\"203\" srcset=\"https:\/\/sisu.ut.ee\/wp-content\/uploads\/sites\/147\/seismika_img_0521.jpg 1140w, https:\/\/sisu.ut.ee\/wp-content\/uploads\/sites\/147\/seismika_img_0521-300x169.jpg 300w, https:\/\/sisu.ut.ee\/wp-content\/uploads\/sites\/147\/seismika_img_0521-1024x576.jpg 1024w, https:\/\/sisu.ut.ee\/wp-content\/uploads\/sites\/147\/seismika_img_0521-768x432.jpg 768w\" sizes=\"auto, (max-width: 361px) 100vw, 361px\"><\/p>\n<p>Peegeldunud lainete meetod v\u00f5imaldab sette- ja kivimikihtide ehituse tuvastamist m\u00f5nek\u00fcmne kuni mitmesaja meetri s\u00fcgavuseni. Murdunud lainete meetodil saab hinnata n\u00e4iteks pinnakatte paksust. Pinnalainete dispersiooni anal\u00fc\u00fcs (MASW meetod) v\u00f5imaldab hinnata maapinnal\u00e4hedaste setendite ja kivimite tugevusomadusi.<\/p>\n<p><strong>Magnetomeetrid Geometrics G-856AX\u00a0<\/strong><\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"alignnone  wp-image-154\" src=\"https:\/\/sisu.ut.ee\/wp-content\/uploads\/sites\/147\/magnetomeetria.jpg\" alt=\"\" width=\"360\" height=\"522\" srcset=\"https:\/\/sisu.ut.ee\/wp-content\/uploads\/sites\/147\/magnetomeetria.jpg 525w, https:\/\/sisu.ut.ee\/wp-content\/uploads\/sites\/147\/magnetomeetria-207x300.jpg 207w\" sizes=\"auto, (max-width: 360px) 100vw, 360px\"><\/p>\n<p>Magnetv\u00e4lja uuringud annavad valdavalt infot kristalse aluskorra ehituse kohta. Samas detailsete t\u00f6\u00f6dega on v\u00f5imalik uurida maapinnal\u00e4hedasi objekte (geoarheoloogia).<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Geof\u00fc\u00fcsikaliste meetoditega on v\u00f5imalik tuvastada maap\u00f5ue ehitust ilma puurimist\u00f6\u00f6deta. Teostatakse georadariga profileerimist ja elektromeetrilisi, seismilisi ja magnetomeetrilisi uuringuid. Samuti tehakse kivimite-setendite f\u00fc\u00fcsikaliste omaduste (tihedus, poorsus, P- ja S-lainete kiirus, magnetiline vastuv\u00f5tlikkus) m\u00f5\u00f5tmisi. Kontakt:\u00a0Argo J\u00f5eleht argo.joeleht(\u00e4t)ut.ee, J\u00fcri Plado juri.plado(\u00e4t)ut.ee Kasutatavad aparatuurid &#8230;<\/p>\n","protected":false},"author":69,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_acf_changed":false,"inline_featured_image":false,"footnotes":""},"class_list":["post-24","page","type-page","status-publish","hentry"],"acf":[],"_links":{"self":[{"href":"https:\/\/sisu.ut.ee\/marek\/wp-json\/wp\/v2\/pages\/24","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/sisu.ut.ee\/marek\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/sisu.ut.ee\/marek\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/sisu.ut.ee\/marek\/wp-json\/wp\/v2\/users\/69"}],"replies":[{"embeddable":true,"href":"https:\/\/sisu.ut.ee\/marek\/wp-json\/wp\/v2\/comments?post=24"}],"version-history":[{"count":2,"href":"https:\/\/sisu.ut.ee\/marek\/wp-json\/wp\/v2\/pages\/24\/revisions"}],"predecessor-version":[{"id":410,"href":"https:\/\/sisu.ut.ee\/marek\/wp-json\/wp\/v2\/pages\/24\/revisions\/410"}],"wp:attachment":[{"href":"https:\/\/sisu.ut.ee\/marek\/wp-json\/wp\/v2\/media?parent=24"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}