Loading…
Hydrogeochemical characterization and identification of a system of regional flow. Case study: the aquifer on the Gulf of Urabá, Colombia
Hydrogeochemistry is an essential tool for the verification of conceptual models, especially of groundwater flow models. This is even more relevant when dealing with complex hydrogeological models that have intercalating layers with different degrees of permeability, and regional flows contributing...
Saved in:
Published in: | Revista Facultad de Ingeniería 2018-03 (86), p.9-18 |
---|---|
Main Authors: | , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that cite this one |
Online Access: | Get full text |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
cited_by | cdi_FETCH-LOGICAL-c424t-d5dd0823cccd471406aba8cba24c76477ab325bd460359424b598023fc1dad3b3 |
---|---|
cites | |
container_end_page | 18 |
container_issue | 86 |
container_start_page | 9 |
container_title | Revista Facultad de Ingeniería |
container_volume | |
creator | Ossa-Valencia, Juliana Betancur-Vargas, Teresita |
description | Hydrogeochemistry is an essential tool for the verification of conceptual models, especially of groundwater flow models. This is even more relevant when dealing with complex hydrogeological models that have intercalating layers with different degrees of permeability, and regional flows contributing to the system. The hydrogeochemical characteristics of the Urabá-Colombia Aquifer and geological cross-sections were studied to establish possible processes that explain the groundwater flow evolution and the recharge zones. 4 flow lines were considered to show the groundwater evolution from Ca2+-HCO3facies and a TDS concentration of approximately 400 mg/L, trough Ca2+-Mg2+-HCO3and Na+-Mg2+-HCO3- facies, ending with Na+-HCO3- facies close to discharge area, with TDS=1,550 mg/L. Data on stable isotopes confirmed the groundwater flow directions. It is also clear that evolution orders correspond to the possible flow rates in areas with a homogeneous gradient, but with higher hydraulic conductivity conditions to the south and center, compared to the north. |
doi_str_mv | 10.17533/udea.redin.n86a02 |
format | article |
fullrecord | <record><control><sourceid>proquest_doaj_</sourceid><recordid>TN_cdi_doaj_primary_oai_doaj_org_article_3f080a66dfd843d2b41ec6c6704e6c9c</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><doaj_id>oai_doaj_org_article_3f080a66dfd843d2b41ec6c6704e6c9c</doaj_id><sourcerecordid>2037412729</sourcerecordid><originalsourceid>FETCH-LOGICAL-c424t-d5dd0823cccd471406aba8cba24c76477ab325bd460359424b598023fc1dad3b3</originalsourceid><addsrcrecordid>eNo9kc1qGzEUhUVpoW7aF-hKkG3H1VxpNHJ2xTQ_EMimWYurP1tmPEokDcV9hLxFnyUvlrFdurq6h_OdCzqEfG3Zsu07zr9PzuMyexfH5agkMnhHFiAAGlBCvCcL1gJrJHD2kXwqZcdYpyRTC_Jye3A5bXyyW7-PFgdqt5jRVp_jH6wxjRRHR6PzY41hNpykFCjScijV74_v7DezOrNhSL-XdI3F01Ind7iidespPk8x-Exn8LjeTEM4Uo8Zzevfb3SdhrQ3ET-TDwGH4r_8mxfk8frnr_Vtc_9wc7f-cd9YAaI2rnOOKeDWWif6VjCJBpU1CML2UvQ9Gg6dcUIy3q1mxHQrxYAH2zp03PALcnfOdQl3-inHPeaDThj1SUh5ozHXaAeveWCKoZQuOCW4AyNab6WVPRNe2pWdsy7PWU85PU--VL1LU56_omhgvBct9LCaXXB22ZxKyT78v9oyfepPH_vTp_70uT_-BkIHk4Y</addsrcrecordid><sourcetype>Open Website</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2037412729</pqid></control><display><type>article</type><title>Hydrogeochemical characterization and identification of a system of regional flow. Case study: the aquifer on the Gulf of Urabá, Colombia</title><source>Publicly Available Content Database</source><creator>Ossa-Valencia, Juliana ; Betancur-Vargas, Teresita</creator><creatorcontrib>Ossa-Valencia, Juliana ; Betancur-Vargas, Teresita ; Universidad de Antioquia</creatorcontrib><description>Hydrogeochemistry is an essential tool for the verification of conceptual models, especially of groundwater flow models. This is even more relevant when dealing with complex hydrogeological models that have intercalating layers with different degrees of permeability, and regional flows contributing to the system. The hydrogeochemical characteristics of the Urabá-Colombia Aquifer and geological cross-sections were studied to establish possible processes that explain the groundwater flow evolution and the recharge zones. 4 flow lines were considered to show the groundwater evolution from Ca2+-HCO3facies and a TDS concentration of approximately 400 mg/L, trough Ca2+-Mg2+-HCO3and Na+-Mg2+-HCO3- facies, ending with Na+-HCO3- facies close to discharge area, with TDS=1,550 mg/L. Data on stable isotopes confirmed the groundwater flow directions. It is also clear that evolution orders correspond to the possible flow rates in areas with a homogeneous gradient, but with higher hydraulic conductivity conditions to the south and center, compared to the north.</description><identifier>ISSN: 0120-6230</identifier><identifier>EISSN: 2422-2844</identifier><identifier>DOI: 10.17533/udea.redin.n86a02</identifier><language>eng</language><publisher>Medellín: Universidad de Antioquía</publisher><subject>Aquifers ; Calcium ions ; conceptual hydrogeological model ; Evolution ; Geochemistry ; Geology ; groundwater ; Groundwater flow ; Groundwater recharge ; Hydrogeochemistry ; Hydrogeology ; Hydrology ; Multivariate analysis ; Permeability ; Principal components analysis ; water quality</subject><ispartof>Revista Facultad de Ingeniería, 2018-03 (86), p.9-18</ispartof><rights>Copyright Universidad de Antioquía Mar 2018</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c424t-d5dd0823cccd471406aba8cba24c76477ab325bd460359424b598023fc1dad3b3</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.proquest.com/docview/2037412729/fulltextPDF?pq-origsite=primo$$EPDF$$P50$$Gproquest$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/2037412729?pq-origsite=primo$$EHTML$$P50$$Gproquest$$Hfree_for_read</linktohtml><link.rule.ids>314,780,784,25753,27924,27925,37012,44590,74998</link.rule.ids></links><search><creatorcontrib>Ossa-Valencia, Juliana</creatorcontrib><creatorcontrib>Betancur-Vargas, Teresita</creatorcontrib><creatorcontrib>Universidad de Antioquia</creatorcontrib><title>Hydrogeochemical characterization and identification of a system of regional flow. Case study: the aquifer on the Gulf of Urabá, Colombia</title><title>Revista Facultad de Ingeniería</title><description>Hydrogeochemistry is an essential tool for the verification of conceptual models, especially of groundwater flow models. This is even more relevant when dealing with complex hydrogeological models that have intercalating layers with different degrees of permeability, and regional flows contributing to the system. The hydrogeochemical characteristics of the Urabá-Colombia Aquifer and geological cross-sections were studied to establish possible processes that explain the groundwater flow evolution and the recharge zones. 4 flow lines were considered to show the groundwater evolution from Ca2+-HCO3facies and a TDS concentration of approximately 400 mg/L, trough Ca2+-Mg2+-HCO3and Na+-Mg2+-HCO3- facies, ending with Na+-HCO3- facies close to discharge area, with TDS=1,550 mg/L. Data on stable isotopes confirmed the groundwater flow directions. It is also clear that evolution orders correspond to the possible flow rates in areas with a homogeneous gradient, but with higher hydraulic conductivity conditions to the south and center, compared to the north.</description><subject>Aquifers</subject><subject>Calcium ions</subject><subject>conceptual hydrogeological model</subject><subject>Evolution</subject><subject>Geochemistry</subject><subject>Geology</subject><subject>groundwater</subject><subject>Groundwater flow</subject><subject>Groundwater recharge</subject><subject>Hydrogeochemistry</subject><subject>Hydrogeology</subject><subject>Hydrology</subject><subject>Multivariate analysis</subject><subject>Permeability</subject><subject>Principal components analysis</subject><subject>water quality</subject><issn>0120-6230</issn><issn>2422-2844</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2018</creationdate><recordtype>article</recordtype><sourceid>PIMPY</sourceid><sourceid>DOA</sourceid><recordid>eNo9kc1qGzEUhUVpoW7aF-hKkG3H1VxpNHJ2xTQ_EMimWYurP1tmPEokDcV9hLxFnyUvlrFdurq6h_OdCzqEfG3Zsu07zr9PzuMyexfH5agkMnhHFiAAGlBCvCcL1gJrJHD2kXwqZcdYpyRTC_Jye3A5bXyyW7-PFgdqt5jRVp_jH6wxjRRHR6PzY41hNpykFCjScijV74_v7DezOrNhSL-XdI3F01Ind7iidespPk8x-Exn8LjeTEM4Uo8Zzevfb3SdhrQ3ET-TDwGH4r_8mxfk8frnr_Vtc_9wc7f-cd9YAaI2rnOOKeDWWif6VjCJBpU1CML2UvQ9Gg6dcUIy3q1mxHQrxYAH2zp03PALcnfOdQl3-inHPeaDThj1SUh5ozHXaAeveWCKoZQuOCW4AyNab6WVPRNe2pWdsy7PWU85PU--VL1LU56_omhgvBct9LCaXXB22ZxKyT78v9oyfepPH_vTp_70uT_-BkIHk4Y</recordid><startdate>20180301</startdate><enddate>20180301</enddate><creator>Ossa-Valencia, Juliana</creator><creator>Betancur-Vargas, Teresita</creator><general>Universidad de Antioquía</general><general>Universidad de Antioquia</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TB</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>CCPQU</scope><scope>CLZPN</scope><scope>DWQXO</scope><scope>FR3</scope><scope>HCIFZ</scope><scope>KR7</scope><scope>L6V</scope><scope>M7S</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>PTHSS</scope><scope>DOA</scope></search><sort><creationdate>20180301</creationdate><title>Hydrogeochemical characterization and identification of a system of regional flow. Case study: the aquifer on the Gulf of Urabá, Colombia</title><author>Ossa-Valencia, Juliana ; Betancur-Vargas, Teresita</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c424t-d5dd0823cccd471406aba8cba24c76477ab325bd460359424b598023fc1dad3b3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2018</creationdate><topic>Aquifers</topic><topic>Calcium ions</topic><topic>conceptual hydrogeological model</topic><topic>Evolution</topic><topic>Geochemistry</topic><topic>Geology</topic><topic>groundwater</topic><topic>Groundwater flow</topic><topic>Groundwater recharge</topic><topic>Hydrogeochemistry</topic><topic>Hydrogeology</topic><topic>Hydrology</topic><topic>Multivariate analysis</topic><topic>Permeability</topic><topic>Principal components analysis</topic><topic>water quality</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Ossa-Valencia, Juliana</creatorcontrib><creatorcontrib>Betancur-Vargas, Teresita</creatorcontrib><creatorcontrib>Universidad de Antioquia</creatorcontrib><collection>CrossRef</collection><collection>Mechanical & Transportation Engineering Abstracts</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>AUTh Library subscriptions: ProQuest Central</collection><collection>Technology Collection</collection><collection>ProQuest One Community College</collection><collection>Latin America & Iberia Database</collection><collection>ProQuest Central</collection><collection>Engineering Research Database</collection><collection>SciTech Premium Collection</collection><collection>Civil Engineering Abstracts</collection><collection>ProQuest Engineering Collection</collection><collection>ProQuest Engineering Database</collection><collection>Publicly Available Content Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><collection>Engineering Collection</collection><collection>DOAJ Directory of Open Access Journals</collection><jtitle>Revista Facultad de Ingeniería</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Ossa-Valencia, Juliana</au><au>Betancur-Vargas, Teresita</au><aucorp>Universidad de Antioquia</aucorp><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Hydrogeochemical characterization and identification of a system of regional flow. Case study: the aquifer on the Gulf of Urabá, Colombia</atitle><jtitle>Revista Facultad de Ingeniería</jtitle><date>2018-03-01</date><risdate>2018</risdate><issue>86</issue><spage>9</spage><epage>18</epage><pages>9-18</pages><issn>0120-6230</issn><eissn>2422-2844</eissn><abstract>Hydrogeochemistry is an essential tool for the verification of conceptual models, especially of groundwater flow models. This is even more relevant when dealing with complex hydrogeological models that have intercalating layers with different degrees of permeability, and regional flows contributing to the system. The hydrogeochemical characteristics of the Urabá-Colombia Aquifer and geological cross-sections were studied to establish possible processes that explain the groundwater flow evolution and the recharge zones. 4 flow lines were considered to show the groundwater evolution from Ca2+-HCO3facies and a TDS concentration of approximately 400 mg/L, trough Ca2+-Mg2+-HCO3and Na+-Mg2+-HCO3- facies, ending with Na+-HCO3- facies close to discharge area, with TDS=1,550 mg/L. Data on stable isotopes confirmed the groundwater flow directions. It is also clear that evolution orders correspond to the possible flow rates in areas with a homogeneous gradient, but with higher hydraulic conductivity conditions to the south and center, compared to the north.</abstract><cop>Medellín</cop><pub>Universidad de Antioquía</pub><doi>10.17533/udea.redin.n86a02</doi><tpages>10</tpages><oa>free_for_read</oa></addata></record> |
fulltext | fulltext |
identifier | ISSN: 0120-6230 |
ispartof | Revista Facultad de Ingeniería, 2018-03 (86), p.9-18 |
issn | 0120-6230 2422-2844 |
language | eng |
recordid | cdi_doaj_primary_oai_doaj_org_article_3f080a66dfd843d2b41ec6c6704e6c9c |
source | Publicly Available Content Database |
subjects | Aquifers Calcium ions conceptual hydrogeological model Evolution Geochemistry Geology groundwater Groundwater flow Groundwater recharge Hydrogeochemistry Hydrogeology Hydrology Multivariate analysis Permeability Principal components analysis water quality |
title | Hydrogeochemical characterization and identification of a system of regional flow. Case study: the aquifer on the Gulf of Urabá, Colombia |
url | http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-07T23%3A37%3A09IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_doaj_&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Hydrogeochemical%20characterization%20and%20identification%20of%20a%20system%20of%20regional%20flow.%20Case%20study:%20the%20aquifer%20on%20the%20Gulf%20of%20Urab%C3%A1,%20Colombia&rft.jtitle=Revista%20Facultad%20de%20Ingenier%C3%ADa&rft.au=Ossa-Valencia,%20Juliana&rft.aucorp=Universidad%20de%20Antioquia&rft.date=2018-03-01&rft.issue=86&rft.spage=9&rft.epage=18&rft.pages=9-18&rft.issn=0120-6230&rft.eissn=2422-2844&rft_id=info:doi/10.17533/udea.redin.n86a02&rft_dat=%3Cproquest_doaj_%3E2037412729%3C/proquest_doaj_%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-c424t-d5dd0823cccd471406aba8cba24c76477ab325bd460359424b598023fc1dad3b3%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=2037412729&rft_id=info:pmid/&rfr_iscdi=true |