{"id":34029,"date":"2020-09-21T08:51:53","date_gmt":"2020-09-21T08:51:53","guid":{"rendered":"http:\/\/www.hgi-cgs.hr\/?page_id=34029"},"modified":"2024-03-14T05:57:32","modified_gmt":"2024-03-14T05:57:32","slug":"hotlime","status":"publish","type":"page","link":"https:\/\/www.hgi-cgs.hr\/en\/hotlime\/","title":{"rendered":"HotLime"},"content":{"rendered":"

[et_pb_section fb_built=”1″ fullwidth=”on” _builder_version=”4.16″ custom_padding=”0px||0px|||” global_colors_info=”{}”][et_pb_fullwidth_slider _builder_version=”4.16″ min_height=”112px” height=”400px” custom_margin=”0px||||false|false” custom_padding=”0px||18px||false|false” auto=”on” auto_ignore_hover=”on” locked=”off” global_colors_info=”{}”][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.16″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/Br\u010di\u0107_Drvenik02-scaled.jpg” background_enable_image=”on” locked=”off” global_colors_info=”{}” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.16″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban2-scaled.jpg” background_enable_image=”on” locked=”off” global_colors_info=”{}” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.16″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/20190228_094232-scaled.jpg” background_enable_image=”on” locked=”off” global_colors_info=”{}” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.16″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban3-scaled.jpg” background_enable_image=”on” locked=”off” global_colors_info=”{}” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.16″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/Bijele_stijene-Gorski_kotar-scaled.jpg” background_enable_image=”on” locked=”off” global_colors_info=”{}” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.16″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban4-scaled.jpg” background_enable_image=”on” locked=”off” global_colors_info=”{}” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.16″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban5-scaled.jpg” background_enable_image=”on” locked=”off” global_colors_info=”{}” sticky_transition=”on”][\/et_pb_slide][\/et_pb_fullwidth_slider][\/et_pb_section][et_pb_section fb_built=”1″ _builder_version=”4.16″ custom_padding=”20px||41px|||” global_colors_info=”{}”][et_pb_row _builder_version=”4.16″ global_colors_info=”{}”][et_pb_column type=”4_4″ _builder_version=”4.16″ global_colors_info=”{}”][et_pb_text _builder_version=”4.16″ text_font_size=”32px” header_2_text_color=”#1e5096″ global_colors_info=”{}”]<\/p>\n

ZAVOD ZA HIDROGEOLOGIJU I IN\u017dENJERSKU GEOLOGIJU<\/strong><\/h2>\n

[\/et_pb_text][et_pb_text _builder_version=”4.16″ text_font_size=”32px” header_2_text_color=”#1e5096″ header_2_line_height=”1.3em” global_colors_info=”{}”]<\/p>\n

GeoERA – <\/strong>HotLime: Mapping and Assessment of Geothermal Plays in Deep Carbonate Rocks \u2013 Cross-domain Implications and Impacts <\/strong><\/h2>\n

[\/et_pb_text][et_pb_text _builder_version=”4.16″ header_4_line_height=”1.3em” custom_margin=”-22px|||||” global_colors_info=”{}”]<\/p>\n

Voditelj projekta: dr.sc. Sta\u0161a Borovi\u0107
<\/em><\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=”4.24.2″ custom_padding=”0px|||||” hover_enabled=”0″ global_colors_info=”{}” column_structure=”1_4,1_4,1_4,1_4″ height=”200px” sticky_enabled=”0″ custom_margin=”21px|auto||auto||”][et_pb_column type=”1_4″ _builder_version=”4.16″ global_colors_info=”{}”][\/et_pb_column][et_pb_column type=”1_4″ _builder_version=”4.16″ global_colors_info=”{}”][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/09\/HotLime-logo.png” title_text=”HotLime-logo” align=”center” align_tablet=”center” align_phone=”” align_last_edited=”on|desktop” _builder_version=”4.24.2″ width=”100%” max_width=”85%” module_alignment=”center” custom_margin=”||-15px|||” custom_padding=”0px|||||” hover_enabled=”0″ global_colors_info=”{}” sticky_enabled=”0″][\/et_pb_image][\/et_pb_column][et_pb_column type=”1_4″ _builder_version=”4.16″ global_colors_info=”{}”][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2024\/03\/gseu.png” _builder_version=”4.24.2″ _module_preset=”default” title_text=”gseu” custom_margin=”50px||||false|false” hover_enabled=”0″ sticky_enabled=”0″][\/et_pb_image][\/et_pb_column][et_pb_column type=”1_4″ _builder_version=”4.16″ global_colors_info=”{}”][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=”4.16″ min_height=”192px” custom_margin=”-5px|auto||auto||” custom_padding=”0px|||||” global_colors_info=”{}”][et_pb_column type=”4_4″ _builder_version=”4.16″ global_colors_info=”{}”][et_pb_text _builder_version=”4.16″ text_font=”||||||||” link_font=”||||||||” link_text_color=”#e09900″ custom_margin=”18px|||||” custom_padding=”|10px||10px|false|true” global_colors_info=”{}”]<\/p>\n

Hidrotermalni sustavi u razlomljenim i okr\u0161enim karbonatnim stijenama spadaju u najperspektivnije geotermalne vodonosnike u Europi. Osim nekoliko podru\u010dja u kojima je odr\u017eivost hidrotermalne proizvodnje topline i elektri\u010dne energije dokazana, ve\u0107ina dubokih karbonatnih vodonosnika privla\u010di relativno malo pozornosti, jer se takve stijene do\u017eivljavaju kao slabo propusne. Istra\u017eivanja i razvoj dubokog podzemlja poznati su kao visokorizi\u010dno ulaganje, osobito u niskoentalpijske sustave, gdje je potrebno bu\u0161enje na dubinama ve\u0107im od 3 km kako bi se pridobile vode pogodne temperature za kori\u0161tenje geotermalne energije. Da bismo smanjili rizik tih zahtjevnih geotermalnih operacija, klju\u010dno je pobolj\u0161ati razumijevanje geolo\u0161kih uvjeta koji odre\u0111uju raspodjelu i obnovljivost potencijalnih resursa. U\u010dinkovitost geotermalnih operacija u dubokim karbonatnim vodonosnicima ovisi o pridobivom protoku podzemne vode koji je odre\u0111en rasjednim strukturama i okr\u0161avanjem. Ovaj \u0107e projekt identificirati generi\u010dke strukturne \u010dimbenike u dubokim karbonatnim formacijama usporedbom geolo\u0161kih situacija i njihovog strukturnog inventara, kao i usporedbom podataka dubokih bu\u0161otina i njihovih petro- i hidrofizi\u010dkih karakteristika. Dosljedna procjena i razmjena znanja koja sve partnere vodi na vi\u0161u razinu poznavanja ove problematike rezultirat \u0107e univerzalno primjenjivim listama najboljih praksi za procjenu, usporedbu i rangiranje perspektivnih hidrotermalnih resursa u dubokim karbonatnim vodonosnicima. Primijenjene u specifi\u010dnim pokusnim podru\u010djima podru\u010djima pomo\u0107u 2D ili 3D kartiranja i karakterizacije, ove \u0107e prostorne procjene pomo\u0107i u smanjenju rizika pri investiranju u ovakve projekte, otkrit \u0107e mogu\u0107e implikacije na vi\u0161e domena i podr\u017eati odr\u017eivo upravljanje povr\u0161inom.<\/p>\n

POKUSNA PODRU\u010cJA<\/strong><\/p>\n