{"id":36636,"date":"2020-11-12T10:41:22","date_gmt":"2020-11-12T10:41:22","guid":{"rendered":"https:\/\/www.hgi-cgs.hr\/?page_id=36636"},"modified":"2020-11-12T11:07:46","modified_gmt":"2020-11-12T11:07:46","slug":"geochemical-processes-of-karst-and-karst-paleoenvironments","status":"publish","type":"page","link":"https:\/\/www.hgi-cgs.hr\/en\/geochemical-processes-of-karst-and-karst-paleoenvironments\/","title":{"rendered":"Geochemical Processes of Karst and Karst Paleoenvironments"},"content":{"rendered":"<p>[et_pb_section fb_built=&#8221;1&#8243; fullwidth=&#8221;on&#8221; _builder_version=&#8221;4.4.1&#8243; custom_padding=&#8221;0px||0px|||&#8221;][et_pb_fullwidth_slider _builder_version=&#8221;4.4.2&#8243; min_height=&#8221;112px&#8221; height=&#8221;400px&#8221; custom_margin=&#8221;0px||||false|false&#8221; custom_padding=&#8221;0px||18px||false|false&#8221; auto=&#8221;on&#8221; auto_ignore_hover=&#8221;on&#8221; locked=&#8221;off&#8221;][et_pb_slide heading=&#8221;Hrvatski geolo\u0161ki institut&#8221; _builder_version=&#8221;4.4.1&#8243; header_font=&#8221;|||on|||||&#8221; background_image=&#8221;https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/Br\u010di\u0107_Drvenik02-scaled.jpg&#8221; background_enable_image=&#8221;on&#8221; locked=&#8221;off&#8221; sticky_transition=&#8221;on&#8221;][\/et_pb_slide][et_pb_slide heading=&#8221;Hrvatski geolo\u0161ki institut&#8221; _builder_version=&#8221;4.4.1&#8243; header_font=&#8221;|||on|||||&#8221; background_image=&#8221;https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban2-scaled.jpg&#8221; background_enable_image=&#8221;on&#8221; locked=&#8221;off&#8221; sticky_transition=&#8221;on&#8221;][\/et_pb_slide][et_pb_slide heading=&#8221;Hrvatski geolo\u0161ki institut&#8221; _builder_version=&#8221;4.4.1&#8243; header_font=&#8221;|||on|||||&#8221; background_image=&#8221;https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/20190228_094232-scaled.jpg&#8221; background_enable_image=&#8221;on&#8221; locked=&#8221;off&#8221; sticky_transition=&#8221;on&#8221;][\/et_pb_slide][et_pb_slide heading=&#8221;Hrvatski geolo\u0161ki institut&#8221; _builder_version=&#8221;4.4.1&#8243; header_font=&#8221;|||on|||||&#8221; background_image=&#8221;https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban3-scaled.jpg&#8221; background_enable_image=&#8221;on&#8221; locked=&#8221;off&#8221; sticky_transition=&#8221;on&#8221;][\/et_pb_slide][et_pb_slide heading=&#8221;Hrvatski geolo\u0161ki institut&#8221; _builder_version=&#8221;4.4.1&#8243; header_font=&#8221;|||on|||||&#8221; background_image=&#8221;https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/Bijele_stijene-Gorski_kotar-scaled.jpg&#8221; background_enable_image=&#8221;on&#8221; locked=&#8221;off&#8221; sticky_transition=&#8221;on&#8221;][\/et_pb_slide][et_pb_slide heading=&#8221;Hrvatski geolo\u0161ki institut&#8221; _builder_version=&#8221;4.4.1&#8243; header_font=&#8221;|||on|||||&#8221; background_image=&#8221;https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban4-scaled.jpg&#8221; background_enable_image=&#8221;on&#8221; locked=&#8221;off&#8221; sticky_transition=&#8221;on&#8221;][\/et_pb_slide][et_pb_slide heading=&#8221;Hrvatski geolo\u0161ki institut&#8221; _builder_version=&#8221;4.4.1&#8243; header_font=&#8221;|||on|||||&#8221; background_image=&#8221;https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban5-scaled.jpg&#8221; background_enable_image=&#8221;on&#8221; locked=&#8221;off&#8221; sticky_transition=&#8221;on&#8221;][\/et_pb_slide][\/et_pb_fullwidth_slider][\/et_pb_section][et_pb_section fb_built=&#8221;1&#8243; _builder_version=&#8221;4.4.2&#8243;][et_pb_row _builder_version=&#8221;4.4.2&#8243;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;4.4.2&#8243;][et_pb_text _builder_version=&#8221;4.6.1&#8243; text_font_size=&#8221;32px&#8221; header_2_text_color=&#8221;#1e5096&#8243;]<\/p>\n<h2 style=\"text-align: center; color: #1e5096;\"><strong>NOVOSTI<\/strong><\/h2>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=&#8221;4.4.2&#8243; custom_margin=&#8221;|auto|15px|auto||&#8221; custom_padding=&#8221;||0px|||&#8221;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;4.4.2&#8243;][et_pb_text _builder_version=&#8221;4.6.6&#8243; text_font_size=&#8221;32px&#8221; header_2_text_color=&#8221;#1e5096&#8243; header_2_line_height=&#8221;1.3em&#8221; custom_margin=&#8221;||23px|||&#8221;]<\/p>\n<h2 style=\"text-align: center; color: #1e5096;\">Geochemical Processes of Karst and Karst Paleoenvironments<\/h2>\n<p>[\/et_pb_text][et_pb_image src=&#8221;https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/11\/Banner-Geochemical_Processes_of_Karst_Paleoenvironments_horizontal_dark.png&#8221; title_text=&#8221;Banner-Geochemical_Processes_of_Karst_Paleoenvironments_horizontal_dark&#8221; align=&#8221;center&#8221; _builder_version=&#8221;4.6.6&#8243; _module_preset=&#8221;default&#8221; width=&#8221;100%&#8221; max_width=&#8221;100%&#8221; border_radii=&#8221;on|5px|5px|5px|5px&#8221; box_shadow_style=&#8221;preset1&#8243; box_shadow_blur=&#8221;15px&#8221;][\/et_pb_image][\/et_pb_column][\/et_pb_row][\/et_pb_section][et_pb_section fb_built=&#8221;1&#8243; _builder_version=&#8221;4.4.2&#8243; custom_padding=&#8221;20px||41px|||&#8221;][et_pb_row _builder_version=&#8221;4.0.3&#8243; min_height=&#8221;192px&#8221; custom_margin=&#8221;-4px|auto||auto||&#8221; custom_padding=&#8221;0px|||||&#8221;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;4.0.3&#8243;][et_pb_text _builder_version=&#8221;4.6.6&#8243; text_font=&#8221;||||||||&#8221; link_font=&#8221;||||||||&#8221; link_text_color=&#8221;#e09900&#8243; custom_margin=&#8221;9px|||||&#8221; custom_padding=&#8221;|10px||10px|false|true&#8221;]<\/p>\n<p><strong>Guest Editors:<\/strong><br \/>Dr. Slobodan Miko, Croatian Geological Survey, Zagreb, Croatia (<em><a href=\"mailto:smiko@hgi-cgs.hr\">slobodan.miko@hgi-cgs.hr<\/a>\u00a0)<\/em><\/p>\n<p>Dr. Nikolina Ilijani\u0107,\u00a0 Croatian Geological Survey, Zagreb, Croatia (<em><a href=\"mailto:nilijanic@hgi-cgs.hr\">nikolina.ilijanic@hgi-cgs.hr<\/a> )<\/em><\/p>\n<p><em>Deadline for manuscript submissions:<\/em> 30 September 2021<\/p>\n<p>[\/et_pb_text][et_pb_text _builder_version=&#8221;4.6.6&#8243; _module_preset=&#8221;default&#8221; custom_margin=&#8221;||50px|||&#8221;]<\/p>\n<p><strong>Message from the Guest Editors<\/strong><\/p>\n<p>Dear Colleagues, Karst landscapes and karst aquifers, which are composed of a variety of soluble rocks, comprise 20\u201325% of the icefree land surface, and nearly 20% of society worldwide relies on karst aquifers for economic, urban, and environmental fresh water. The dissolution of a carbonate rock and the influence on water chemistry are a combination of various geochemical processes of major significance to the origin and evolution of the karst environment. Today, the main driver influencing environmental changes in the karst environment is anthropogenic chemical contamination and climate change. In order to evaluate the impact of these changes on karst systems it is necessary to determine geochemical background levels for delineating between natural and anthropogenic impacts[&#8230;].<\/p>\n<p>For further reading, please follow the link to the Special Issue Website at: <em><a href=\"https:\/\/www.mdpi.com\/journal\/water\/special_issues\/Geochemical_Processes_of_Karst_Paleoenvironments\">https:\/\/www.mdpi.com\/journal\/water\/special_issues\/Geochemical_Processes_of_Karst_Paleoenvironments<\/a><\/em><\/p>\n<p><em>Dr. Slobodan Miko<\/em><\/p>\n<p><em>Dr. Nikolina Ilijani\u0107<\/em><\/p>\n<p><em>Guest Editors<\/em><\/p>\n<p>[\/et_pb_text][et_pb_text _builder_version=&#8221;4.6.6&#8243; _module_preset=&#8221;default&#8221; custom_margin=&#8221;3px|||||&#8221;]<\/p>\n<p><strong>Editor-in-Chief<\/strong><br \/>Dr. Jean-Luc PROBST ECOLAB, Centre National de la Recherche Scientifique (CNRS), University of Toulouse, campus ENSAT, Auzeville Tolosane, France<\/p>\n<p>[\/et_pb_text][et_pb_text _builder_version=&#8221;4.6.6&#8243; _module_preset=&#8221;default&#8221; custom_margin=&#8221;-19px|||||&#8221;]<\/p>\n<p><strong>Message from the Editor-in-Chief<\/strong><\/p>\n<p>In the context of global changes, the sustainable management of water cycles, going from global and regional water cycles to urban, industrial and agricultural water cycles, plays a very important role on the water resources and on their relationships with food, energy, biodiversity, ecosystem functioning and human health. W a t e r invites authors to provide innovative original full articles, critical reviews and timely short communications and to propose special issues devoted to new technological and scientific domains and to interdisciplinary approaches of the water cycles. We ensure a critical review process and a quick turnaround between submission and final decision.<\/p>\n<p>[\/et_pb_text][et_pb_text _builder_version=&#8221;4.6.6&#8243; _module_preset=&#8221;default&#8221;]<\/p>\n<p><strong>Author Benefits<\/strong><\/p>\n<p><em><strong>Open Access:<\/strong><\/em>\u2014free for readers, with <em><a href=\"https:\/\/www.mdpi.com\/journal\/water\/apc\">article processing charges (APC)<\/a><\/em> paid by authors or their institutions.<\/p>\n<p><strong>High Visibility:<\/strong> indexed by the <strong><a href=\"https:\/\/mjl.clarivate.com\/search-results\">Science Citation Index Expanded<\/a><\/strong> (Web of Science), <em><a href=\"https:\/\/www.engineeringvillage.com\/home.url\">Ei Compendex<\/a> <\/em>and <em><a href=\"https:\/\/www.mdpi.com\/journal\/water\/indexing\">other databases<\/a><\/em>.<\/p>\n<p><strong>CiteScore<\/strong> (2019 Scopus data): <strong><a href=\"https:\/\/www.scopus.com\/sourceid\/21100255400\">3.0<\/a><\/strong>, which equals rank 82\/217 (Q2) in &#8216;Water Science and Technology&#8217;, rank 88\/219 (Q2) in &#8216;Aquatic Science&#8217; and rank 147\/679 (Q1) in &#8216;Geography, Planning and Development&#8217;.<\/p>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section]<\/p>\n","protected":false},"excerpt":{"rendered":"<p>NOVOSTIGeochemical Processes of Karst and Karst PaleoenvironmentsGuest Editors:Dr. Slobodan Miko, Croatian Geological Survey, Zagreb, Croatia (slobodan.miko@hgi-cgs.hr\u00a0) Dr. Nikolina Ilijani\u0107,\u00a0 Croatian Geological Survey, Zagreb, Croatia (nikolina.ilijanic@hgi-cgs.hr ) Deadline for manuscript submissions: 30 September 2021Message from the Guest Editors Dear Colleagues, Karst landscapes and karst aquifers, which are composed of a variety of soluble rocks, comprise 20\u201325% [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_et_pb_use_builder":"on","_et_pb_old_content":"","_et_gb_content_width":"","footnotes":""},"class_list":["post-36636","page","type-page","status-publish","hentry"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/36636","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/comments?post=36636"}],"version-history":[{"count":5,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/36636\/revisions"}],"predecessor-version":[{"id":36648,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/36636\/revisions\/36648"}],"wp:attachment":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/media?parent=36636"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}