{"id":20,"date":"2012-05-30T16:04:11","date_gmt":"2012-05-30T16:04:11","guid":{"rendered":"http:\/\/hgc.lt\/?p=20"},"modified":"2022-08-12T16:00:53","modified_gmt":"2022-08-12T14:00:53","slug":"nr3","status":"publish","type":"post","link":"http:\/\/hgc.lt\/?p=20","title":{"rendered":"Vandening\u0173 sluoksni\u0173 nustatymas \u010dia ir dabar."},"content":{"rendered":"\r\n<p>Eksploatacinio vandens gr\u0119\u017einio gylis tiesiogiai\u00a0priklauso nuo vandeningo sluoksnio sl\u016bgsojimo gylio. Eksploatacinio\u00a0vandens gr\u0119\u017einio kolonos montavimas\u00a0yra tik dalis darb\u0173. Svarbiausia &#8211;\u00a0atsi\u017evelgiant \u012f poreikius ir perspektyv\u0105 parinkti vadnening\u0105 sluoksn\u012f ir j\u012f atpa\u017einti dar mechaninio \u017dem\u0117s gr\u0119\u017eimo metu.\u00a0Tai n\u0117ra paprasta ir kiekvienu atveju reikalauja speciali\u0173 \u017eini\u0173,\u00a0\u012frangos ir i\u0161asnkstinio pasiruo\u0161imo, kam, gr\u0119\u017eim\u0105 vykdan\u010diam personalui,\u00a0 paprastai tr\u016bksta laiko ar kompetencijos.<\/p>\r\n<p>Atliekame uolien\u0173\u00a0ir gr\u0119\u017eimo \u0161lamo s\u0105vybi\u0173 \u012fvertinim\u0105 mechaninio \u017dem\u0117s gr\u0119\u017eimo metu.<\/p>\r\n<p>Kompleksi\u0161kai, tuo pa\u010diu metu,\u00a0atliekant\u00a0kelis skirtingus geologinius tyrimus galime \u010dia ir dabar interpretuoti storym\u0117s geologin\u0119 s\u0105rang\u0105 ir hidrogeologini\u0173 s\u0105lyg\u0173\u00a0kait\u0105.\u00a0 Tam reikia:<\/p>\r\n<span class=\"collapseomatic \" id=\"id6af4f9c88ea4a\"  tabindex=\"0\" title=\"&lt;strong&gt;Paruo\u0161iamieji darbai.&lt;\/strong&gt;\"    ><strong>Paruo\u0161iamieji darbai.<\/strong><\/span><div id=\"target-id6af4f9c88ea4a\" class=\"collapseomatic_content \"> J\u0173 metu pagal U\u017esakovo pateikt\u0105 u\u017eduot\u012f atliekamas pirminis geologin\u0117s informacijos apie konkret\u0173 objekt\u0105 rinkimas, sisteminimas ir pradinis vertinimas. Pateikiamas prognozinis vandeningo sluoksnio sl\u016bgsojomo gylis, sudaromas preliminarus geologini\u0173 s\u0105lyg\u0173 pj\u016bvis pagal Lietuvos Geologijos Tarnybos fonde esan\u010di\u0105 informacij\u0105.Content goes here<\/div>\r\n<p>&nbsp;<\/p>\r\n<span class=\"collapseomatic \" id=\"id6af4f9c88eaac\"  tabindex=\"0\" title=\"&lt;strong&gt;Vizualinis uolien\u0173 vertinimas.&lt;\/strong&gt;\"    ><strong>Vizualinis uolien\u0173 vertinimas.<\/strong><\/span><div id=\"target-id6af4f9c88eaac\" class=\"collapseomatic_content \"> Turint atitinkamas \u017einias, pagal i\u0161 gr\u0119\u017eskyl\u0117s i\u0161ne\u0161amo grunto vizualin\u012f \u012fvertinim\u0105 galima atlikti pradin\u012f geologini\u0173 s\u0105lyg\u0173 \u012fvertinim\u0105. Nustatyti grunto litologin\u0119 sud\u0117t\u012f, spalv\u0105, m\u0117ginio pa\u0117mimo gyl\u012f. \u0160ie duomenys yra pirminiai ir naudojami, kaip papildoma informacija vykdant tolimesnius po\u017eeminio vandens paie\u0161kos darbus. D\u0117je, bet \u0161iuo metodu galima \u201epasitik\u0117ti\u201c tik dalinai, nes did\u0117jant gr\u0119\u017einio gyliui did\u0117ja ir paklaidos. Su kiekvienu pragr\u0119\u017etu metru d\u0117l nuolat, u\u017edaru ciklu, cirkuliuojan\u010dio gr\u0119\u017eimo skiedinio, daug\u0117ja priemai\u0161\u0173, did\u0117ja pragr\u0119\u017etos uolienos pak\u0117limo \u012f pavir\u0161i\u0173 laikas, o pasiekus 30 ir daugiau metr\u0173 gyl\u012f atpa\u017einti smulk\u0173 sm\u0117l\u012f pasidaro ypa\u010d sud\u0117tinga ir, kaip beb\u016bt\u0173 apmaudu, b\u016btent sm\u0117liuose ir yra susikaup\u0119s po\u017eeminis vanduo, kurio mes ir ie\u0161kome.<\/div>\r\n<p>&nbsp;<\/p>\r\n<span class=\"collapseomatic \" id=\"id6af4f9c88eadd\"  tabindex=\"0\" title=\"&lt;strong&gt;Gr\u0119\u017eimo skiedinio fizini\u0173 s\u0105vybi\u0173 kitimo steb\u0117jimas mechaninio gr\u0119\u017eimo metu.&lt;\/strong&gt;\"    ><strong>Gr\u0119\u017eimo skiedinio fizini\u0173 s\u0105vybi\u0173 kitimo steb\u0117jimas mechaninio gr\u0119\u017eimo metu.<\/strong><\/span><div id=\"target-id6af4f9c88eadd\" class=\"collapseomatic_content \"> \u012edealaus gr\u0119\u017eimo per vandensparines uolienas (molis, priemolis, priesm\u0117lis) metu gr\u0119\u017eimo skiedinio temperat\u016bra nesikeist\u0173. Laimei \u012fdeali\u0173 s\u0105lyg\u0173 n\u0117ra ir gr\u0119\u017eimo skiedinio temperat\u016bra nuolat kinta gr\u0119\u017eimo metu, o jos svyravimo steb\u0117jimas leid\u017eia daug tiksliau interpretuoti hidrogeologin\u0119 situacij\u0105. Vandening\u0173 sluoksni\u0173 temperat\u016bra paprastai yra \u017eemesn\u0117, nei gr\u0119\u017eimo skiedinio. Prad\u0117jus gr\u0119\u017eti vandningas uolienas tuoj pat kei\u010diasi ir skiedinio temperat\u016bra. B\u016btent tai ir leid\u017eia i\u0161kart pasteb\u0117ti hidrogeologini\u0173 s\u0105lyg\u0173 kait\u0105. <\/div>\r\n<p>&nbsp;<\/p>\r\n<p>Kaip vien\u0105 visum\u0105 vertinant\u00a0vis\u0105 mechaninio gr\u0119\u017eimo proces\u0105, paimtus uolien\u0173 m\u0117ginius ir\u00a0gr\u0119\u017eimo skiedinio savybi\u0173 kitimo duomenis galima interpretuoti\u00a0hidrogeologines s\u0105lygas, pagr\u012fsti sluoksnio vandeningum\u0105, patikslinti\u00a0vandening\u0173 darini\u0173\u00a0sl\u016bgsojimo gyl\u012f ir stor\u012f \u010dia ir dabar.\u00a0<\/p>\r\n","protected":false},"excerpt":{"rendered":"<p>Eksploatacinio vandens gr\u0119\u017einio gylis tiesiogiai\u00a0priklauso nuo vandeningo sluoksnio sl\u016bgsojimo gylio. Eksploatacinio\u00a0vandens gr\u0119\u017einio kolonos montavimas\u00a0yra tik dalis darb\u0173. Svarbiausia &#8211;\u00a0atsi\u017evelgiant \u012f poreikius ir perspektyv\u0105 parinkti vadnening\u0105 sluoksn\u012f ir j\u012f atpa\u017einti dar mechaninio \u017dem\u0117s gr\u0119\u017eimo metu.\u00a0Tai n\u0117ra paprasta ir kiekvienu atveju reikalauja speciali\u0173 \u017eini\u0173,\u00a0\u012frangos ir i\u0161asnkstinio pasiruo\u0161imo, kam, gr\u0119\u017eim\u0105 vykdan\u010diam personalui,\u00a0 paprastai tr\u016bksta laiko ar kompetencijos. Atliekame [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":528,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":[],"categories":[1,35],"tags":[],"_links":{"self":[{"href":"http:\/\/hgc.lt\/index.php?rest_route=\/wp\/v2\/posts\/20"}],"collection":[{"href":"http:\/\/hgc.lt\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"http:\/\/hgc.lt\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"http:\/\/hgc.lt\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"http:\/\/hgc.lt\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=20"}],"version-history":[{"count":39,"href":"http:\/\/hgc.lt\/index.php?rest_route=\/wp\/v2\/posts\/20\/revisions"}],"predecessor-version":[{"id":615,"href":"http:\/\/hgc.lt\/index.php?rest_route=\/wp\/v2\/posts\/20\/revisions\/615"}],"wp:featuredmedia":[{"embeddable":true,"href":"http:\/\/hgc.lt\/index.php?rest_route=\/wp\/v2\/media\/528"}],"wp:attachment":[{"href":"http:\/\/hgc.lt\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=20"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"http:\/\/hgc.lt\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=20"},{"taxonomy":"post_tag","embeddable":true,"href":"http:\/\/hgc.lt\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=20"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}