Geothermal potential, chemical characteristics, and utilization of groundwater in Serbia
To collect and unify data about all geothermal resources in Serbia, a database was formed. The database allows us to perceive the geothermal resources of Serbia and their potential for utilization. Based on the data available in the geothermal database, the estimated temperatures of reservoirs, heat...
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| Veröffentlicht in: | Environmental earth sciences 2021-11, Vol.80 (22), p.736-736, Article 736 |
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| creator | Petrović Pantić, Tanja Atanasković Samolov, Katarina Štrbački, Jana Tomić, Milan |
| description | To collect and unify data about all geothermal resources in Serbia, a database was formed. The database allows us to perceive the geothermal resources of Serbia and their potential for utilization. Based on the data available in the geothermal database, the estimated temperatures of reservoirs, heat power, and geothermal energy utilization were calculated. The database contains 293 geothermal records (springs, boreholes) registered at 160 locations, with groundwater temperatures in the range between 20 and 111 °C. The maximum expected temperature of the reservoir is 146 °C according to the use of a SiO
2
geothermometer. Some thermal water is cooled due to mixing with cold, shallow water. Geothermal resources are mostly used for balneology and recreation, and less for heating, water supply, bottling, fish and animal farms, agriculture, and industrial. 26% of all geothermal resources is used by the local population or has not been used at all. The annual utilization of geothermal energy for direct heat is 1507 TJ/yr, and the estimated capacity of geothermal energy in Serbia is 111 MWt. The results of analytical work were presented in the form of maps with a geological and hydrogeological background. Thermal waters are mostly located within an area of Tertiary magmatism. Three geothermal potential areas are identified in Serbia: Pannonian basin-Vojvodina Province, the Mačva-Srem area and area from Jošanička Banja to Vranjska Banja (southern Serbia). Based on chemical analyses, four hydrochemical facies are distinguished. Thermal water mainly belongs to the NaHCO
3
or CaMgHCO
3
hydrochemical facies, usually depending on the primary aquifer type: karst, karst-fissured, intergranular or fissured. |
| doi_str_mv | 10.1007/s12665-021-09985-w |
| format | Article |
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2
geothermometer. Some thermal water is cooled due to mixing with cold, shallow water. Geothermal resources are mostly used for balneology and recreation, and less for heating, water supply, bottling, fish and animal farms, agriculture, and industrial. 26% of all geothermal resources is used by the local population or has not been used at all. The annual utilization of geothermal energy for direct heat is 1507 TJ/yr, and the estimated capacity of geothermal energy in Serbia is 111 MWt. The results of analytical work were presented in the form of maps with a geological and hydrogeological background. Thermal waters are mostly located within an area of Tertiary magmatism. Three geothermal potential areas are identified in Serbia: Pannonian basin-Vojvodina Province, the Mačva-Srem area and area from Jošanička Banja to Vranjska Banja (southern Serbia). Based on chemical analyses, four hydrochemical facies are distinguished. Thermal water mainly belongs to the NaHCO
3
or CaMgHCO
3
hydrochemical facies, usually depending on the primary aquifer type: karst, karst-fissured, intergranular or fissured.</description><identifier>ISSN: 1866-6280</identifier><identifier>EISSN: 1866-6299</identifier><identifier>DOI: 10.1007/s12665-021-09985-w</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Agriculture ; Aquifers ; Biogeosciences ; Boreholes ; Bottling ; Chemical analysis ; cold ; Earth and Environmental Science ; Earth Sciences ; Energy utilization ; Environmental Science and Engineering ; Farms ; Fish ; Fish farms ; Geochemistry ; Geological mapping ; Geology ; Geothermal energy ; Geothermal energy utilization ; Geothermal power ; Geothermal resources ; Groundwater ; Groundwater temperatures ; heat ; Hydrochemicals ; hydrochemistry ; Hydrogeology ; Hydrology/Water Resources ; Karst ; karsts ; Local population ; Magma ; Original Article ; recreation ; Reservoirs ; Resources ; Serbia ; Shallow water ; Silica ; Silicon dioxide ; Sodium bicarbonate ; temperature ; Terrestrial Pollution ; Tertiary ; Thermal water ; Water springs ; Water supply</subject><ispartof>Environmental earth sciences, 2021-11, Vol.80 (22), p.736-736, Article 736</ispartof><rights>The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2021</rights><rights>The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2021.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a375t-9f3dbc453661d913af02db182ae89dd7aa27b4d593e4505adc90b0e0b6e158a13</citedby><cites>FETCH-LOGICAL-a375t-9f3dbc453661d913af02db182ae89dd7aa27b4d593e4505adc90b0e0b6e158a13</cites><orcidid>0000-0003-1456-6913</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s12665-021-09985-w$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s12665-021-09985-w$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27903,27904,41467,42536,51298</link.rule.ids></links><search><creatorcontrib>Petrović Pantić, Tanja</creatorcontrib><creatorcontrib>Atanasković Samolov, Katarina</creatorcontrib><creatorcontrib>Štrbački, Jana</creatorcontrib><creatorcontrib>Tomić, Milan</creatorcontrib><title>Geothermal potential, chemical characteristics, and utilization of groundwater in Serbia</title><title>Environmental earth sciences</title><addtitle>Environ Earth Sci</addtitle><description>To collect and unify data about all geothermal resources in Serbia, a database was formed. The database allows us to perceive the geothermal resources of Serbia and their potential for utilization. Based on the data available in the geothermal database, the estimated temperatures of reservoirs, heat power, and geothermal energy utilization were calculated. The database contains 293 geothermal records (springs, boreholes) registered at 160 locations, with groundwater temperatures in the range between 20 and 111 °C. The maximum expected temperature of the reservoir is 146 °C according to the use of a SiO
2
geothermometer. Some thermal water is cooled due to mixing with cold, shallow water. Geothermal resources are mostly used for balneology and recreation, and less for heating, water supply, bottling, fish and animal farms, agriculture, and industrial. 26% of all geothermal resources is used by the local population or has not been used at all. The annual utilization of geothermal energy for direct heat is 1507 TJ/yr, and the estimated capacity of geothermal energy in Serbia is 111 MWt. The results of analytical work were presented in the form of maps with a geological and hydrogeological background. Thermal waters are mostly located within an area of Tertiary magmatism. Three geothermal potential areas are identified in Serbia: Pannonian basin-Vojvodina Province, the Mačva-Srem area and area from Jošanička Banja to Vranjska Banja (southern Serbia). Based on chemical analyses, four hydrochemical facies are distinguished. Thermal water mainly belongs to the NaHCO
3
or CaMgHCO
3
hydrochemical facies, usually depending on the primary aquifer type: karst, karst-fissured, intergranular or fissured.</description><subject>Agriculture</subject><subject>Aquifers</subject><subject>Biogeosciences</subject><subject>Boreholes</subject><subject>Bottling</subject><subject>Chemical analysis</subject><subject>cold</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Energy utilization</subject><subject>Environmental Science and Engineering</subject><subject>Farms</subject><subject>Fish</subject><subject>Fish farms</subject><subject>Geochemistry</subject><subject>Geological mapping</subject><subject>Geology</subject><subject>Geothermal energy</subject><subject>Geothermal energy utilization</subject><subject>Geothermal power</subject><subject>Geothermal resources</subject><subject>Groundwater</subject><subject>Groundwater temperatures</subject><subject>heat</subject><subject>Hydrochemicals</subject><subject>hydrochemistry</subject><subject>Hydrogeology</subject><subject>Hydrology/Water Resources</subject><subject>Karst</subject><subject>karsts</subject><subject>Local population</subject><subject>Magma</subject><subject>Original Article</subject><subject>recreation</subject><subject>Reservoirs</subject><subject>Resources</subject><subject>Serbia</subject><subject>Shallow water</subject><subject>Silica</subject><subject>Silicon dioxide</subject><subject>Sodium bicarbonate</subject><subject>temperature</subject><subject>Terrestrial Pollution</subject><subject>Tertiary</subject><subject>Thermal water</subject><subject>Water springs</subject><subject>Water supply</subject><issn>1866-6280</issn><issn>1866-6299</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp9kE9LwzAYh4soOHRfwFPBi4dV86dJm6MMncLAgwrewtsk3TK6ZiYpQz-90YqCB99LXsLz-_HyZNkZRpcYoeoqYMI5KxDBBRKiZsX-IJvgmvOCEyEOf_YaHWfTEDYoDcVUID7JXhbGxbXxW-jynYumjxa6Wa7WZmtV-lNr8KCi8TZEq8Ish17nQ7SdfYdoXZ-7Nl95N_R6D4nKbZ8_Gt9YOM2OWuiCmX6_J9nz7c3T_K5YPizu59fLAmjFYiFaqhtVMso51gJTaBHRDa4JmFpoXQGQqik1E9SUDDHQSqAGGdRwg1kNmJ5kF2PvzrvXwYQotzYo03XQGzcESXiqJrgqSULP_6AbN_g-XScJq6uyZpzQRJGRUt6F4E0rd95uwb9JjOSnbzn6lsm3_PIt9ylEx1BIcL8y_rf6n9QHNg-EBg</recordid><startdate>20211101</startdate><enddate>20211101</enddate><creator>Petrović Pantić, Tanja</creator><creator>Atanasković Samolov, Katarina</creator><creator>Štrbački, Jana</creator><creator>Tomić, Milan</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7ST</scope><scope>7TG</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>M2P</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>SOI</scope><scope>7S9</scope><scope>L.6</scope><orcidid>https://orcid.org/0000-0003-1456-6913</orcidid></search><sort><creationdate>20211101</creationdate><title>Geothermal potential, chemical characteristics, and utilization of groundwater in Serbia</title><author>Petrović Pantić, Tanja ; 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The database allows us to perceive the geothermal resources of Serbia and their potential for utilization. Based on the data available in the geothermal database, the estimated temperatures of reservoirs, heat power, and geothermal energy utilization were calculated. The database contains 293 geothermal records (springs, boreholes) registered at 160 locations, with groundwater temperatures in the range between 20 and 111 °C. The maximum expected temperature of the reservoir is 146 °C according to the use of a SiO
2
geothermometer. Some thermal water is cooled due to mixing with cold, shallow water. Geothermal resources are mostly used for balneology and recreation, and less for heating, water supply, bottling, fish and animal farms, agriculture, and industrial. 26% of all geothermal resources is used by the local population or has not been used at all. The annual utilization of geothermal energy for direct heat is 1507 TJ/yr, and the estimated capacity of geothermal energy in Serbia is 111 MWt. The results of analytical work were presented in the form of maps with a geological and hydrogeological background. Thermal waters are mostly located within an area of Tertiary magmatism. Three geothermal potential areas are identified in Serbia: Pannonian basin-Vojvodina Province, the Mačva-Srem area and area from Jošanička Banja to Vranjska Banja (southern Serbia). Based on chemical analyses, four hydrochemical facies are distinguished. Thermal water mainly belongs to the NaHCO
3
or CaMgHCO
3
hydrochemical facies, usually depending on the primary aquifer type: karst, karst-fissured, intergranular or fissured.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s12665-021-09985-w</doi><tpages>1</tpages><orcidid>https://orcid.org/0000-0003-1456-6913</orcidid></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 1866-6280 |
| ispartof | Environmental earth sciences, 2021-11, Vol.80 (22), p.736-736, Article 736 |
| issn | 1866-6280 1866-6299 |
| language | eng |
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| source | Springer Nature - Complete Springer Journals |
| subjects | Agriculture Aquifers Biogeosciences Boreholes Bottling Chemical analysis cold Earth and Environmental Science Earth Sciences Energy utilization Environmental Science and Engineering Farms Fish Fish farms Geochemistry Geological mapping Geology Geothermal energy Geothermal energy utilization Geothermal power Geothermal resources Groundwater Groundwater temperatures heat Hydrochemicals hydrochemistry Hydrogeology Hydrology/Water Resources Karst karsts Local population Magma Original Article recreation Reservoirs Resources Serbia Shallow water Silica Silicon dioxide Sodium bicarbonate temperature Terrestrial Pollution Tertiary Thermal water Water springs Water supply |
| title | Geothermal potential, chemical characteristics, and utilization of groundwater in Serbia |
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