Changes in the hydrochemistry of a karstic lake in Yucatan, Mexico
The Yucatan Peninsula is a karstic region with groundwater-dependent ecosystems and geological features such as karstic lakes. The objective of this research was to calculate the volume of water stored in this section of the aquifer and to describe the changes in the hydrochemistry of the lake Punta...
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| Veröffentlicht in: | Environmental earth sciences 2020-03, Vol.79 (5), Article 98 |
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| creator | Cejudo, Eduardo Acosta-González, Gilberto Ortega-Camacho, Daniela Tun-Rosado, Giovani Emmanuel |
| description | The Yucatan Peninsula is a karstic region with groundwater-dependent ecosystems and geological features such as karstic lakes. The objective of this research was to calculate the volume of water stored in this section of the aquifer and to describe the changes in the hydrochemistry of the lake Punta Laguna as a representative of karstic lakes in the Yucatan Peninsula. A bathymetry and calculation of the volume of water stored in the lake resulted in 5,198,505 m
3
with a maximum depth measured of 26.6 m Physicochemical measurements were completed in surface and three vertical profiles to estimate the mass of nutrients and ions and to describe the current hydrochemistry. The lake is an oligotrophic one of mixed-typed water (chloride-calcium/magnesium), saturated or supersaturated with calcite, dolomite and aragonite due to limestone dissolution. No evidence obtain regarding the saline intrusion. The conclusion that we can derive from the data is that Punta Laguna is a tropical karstic lake in good condition with low anthropogenic influence, evolving hydrochemically speaking. The changes over a 20-year period suggest that there has been reverse ion exchange, evaporation and sulfate reduction. |
| doi_str_mv | 10.1007/s12665-020-8838-3 |
| format | Article |
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3
with a maximum depth measured of 26.6 m Physicochemical measurements were completed in surface and three vertical profiles to estimate the mass of nutrients and ions and to describe the current hydrochemistry. The lake is an oligotrophic one of mixed-typed water (chloride-calcium/magnesium), saturated or supersaturated with calcite, dolomite and aragonite due to limestone dissolution. No evidence obtain regarding the saline intrusion. The conclusion that we can derive from the data is that Punta Laguna is a tropical karstic lake in good condition with low anthropogenic influence, evolving hydrochemically speaking. The changes over a 20-year period suggest that there has been reverse ion exchange, evaporation and sulfate reduction.</description><identifier>ISSN: 1866-6280</identifier><identifier>EISSN: 1866-6299</identifier><identifier>DOI: 10.1007/s12665-020-8838-3</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Anthropogenic factors ; Aquifers ; Aragonite ; Bathymeters ; Bathymetry ; Biogeosciences ; Calcite ; Calcium ; Calcium chloride ; Dolomite ; Dolostone ; Earth and Environmental Science ; Earth science ; Earth Sciences ; Environmental Science and Engineering ; Evaporation ; Fault lines ; Geochemistry ; Geology ; Groundwater ; Human influences ; Hydrochemistry ; Hydrology/Water Resources ; Intrusion ; Ion exchange ; Karst ; Lakes ; Limestone ; Magnesium ; Mathematical analysis ; Nutrients ; Original Article ; Profiles ; Saline intrusion ; Saltwater intrusion ; Sediments ; Sulfate reduction ; Sulphate reduction ; Terrestrial Pollution ; Tropical climate ; Vertical profiles ; Water depth</subject><ispartof>Environmental earth sciences, 2020-03, Vol.79 (5), Article 98</ispartof><rights>Springer-Verlag GmbH Germany, part of Springer Nature 2020</rights><rights>Environmental Earth Sciences is a copyright of Springer, (2020). All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a339t-a9ebe3eca4e05c869fdda7218f8151b99261154cce77748d438875bfc272a51b3</citedby><cites>FETCH-LOGICAL-a339t-a9ebe3eca4e05c869fdda7218f8151b99261154cce77748d438875bfc272a51b3</cites><orcidid>0000-0002-8683-7156 ; 0000-0002-5779-517X</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/s12665-020-8838-3$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s12665-020-8838-3$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Cejudo, Eduardo</creatorcontrib><creatorcontrib>Acosta-González, Gilberto</creatorcontrib><creatorcontrib>Ortega-Camacho, Daniela</creatorcontrib><creatorcontrib>Tun-Rosado, Giovani Emmanuel</creatorcontrib><title>Changes in the hydrochemistry of a karstic lake in Yucatan, Mexico</title><title>Environmental earth sciences</title><addtitle>Environ Earth Sci</addtitle><description>The Yucatan Peninsula is a karstic region with groundwater-dependent ecosystems and geological features such as karstic lakes. The objective of this research was to calculate the volume of water stored in this section of the aquifer and to describe the changes in the hydrochemistry of the lake Punta Laguna as a representative of karstic lakes in the Yucatan Peninsula. A bathymetry and calculation of the volume of water stored in the lake resulted in 5,198,505 m
3
with a maximum depth measured of 26.6 m Physicochemical measurements were completed in surface and three vertical profiles to estimate the mass of nutrients and ions and to describe the current hydrochemistry. The lake is an oligotrophic one of mixed-typed water (chloride-calcium/magnesium), saturated or supersaturated with calcite, dolomite and aragonite due to limestone dissolution. No evidence obtain regarding the saline intrusion. The conclusion that we can derive from the data is that Punta Laguna is a tropical karstic lake in good condition with low anthropogenic influence, evolving hydrochemically speaking. The changes over a 20-year period suggest that there has been reverse ion exchange, evaporation and sulfate reduction.</description><subject>Anthropogenic factors</subject><subject>Aquifers</subject><subject>Aragonite</subject><subject>Bathymeters</subject><subject>Bathymetry</subject><subject>Biogeosciences</subject><subject>Calcite</subject><subject>Calcium</subject><subject>Calcium chloride</subject><subject>Dolomite</subject><subject>Dolostone</subject><subject>Earth and Environmental Science</subject><subject>Earth science</subject><subject>Earth Sciences</subject><subject>Environmental Science and Engineering</subject><subject>Evaporation</subject><subject>Fault lines</subject><subject>Geochemistry</subject><subject>Geology</subject><subject>Groundwater</subject><subject>Human influences</subject><subject>Hydrochemistry</subject><subject>Hydrology/Water Resources</subject><subject>Intrusion</subject><subject>Ion exchange</subject><subject>Karst</subject><subject>Lakes</subject><subject>Limestone</subject><subject>Magnesium</subject><subject>Mathematical analysis</subject><subject>Nutrients</subject><subject>Original Article</subject><subject>Profiles</subject><subject>Saline intrusion</subject><subject>Saltwater intrusion</subject><subject>Sediments</subject><subject>Sulfate reduction</subject><subject>Sulphate reduction</subject><subject>Terrestrial Pollution</subject><subject>Tropical climate</subject><subject>Vertical profiles</subject><subject>Water depth</subject><issn>1866-6280</issn><issn>1866-6299</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp1kMtOwzAQRS0EElXpB7CzxBaDH_FrCRUvqYgNLFhZU8ch6SMpdiLRv8dVEKyYzczi3DvSQeic0StGqb5OjCslCeWUGCMMEUdowoxSRHFrj39vQ0_RLKUVzSOYsFRN0O28hvYjJNy0uK8Drvdl7Hwdtk3q4x53FQa8hpj6xuMNrMOBex889NBe4ufw1fjuDJ1UsElh9rOn6O3-7nX-SBYvD0_zmwUBIWxPwIZlEMFDEaj0RtmqLEFzZirDJFtayxVjsvA-aK0LUxbCGC2XleeaQwbEFF2MvbvYfQ4h9W7VDbHNLx0X0loqbcEyxUbKxy6lGCq3i80W4t4x6g623GjLZVvuYMuJnOFjJmU224h_zf-HvgESSWs3</recordid><startdate>20200301</startdate><enddate>20200301</enddate><creator>Cejudo, Eduardo</creator><creator>Acosta-González, Gilberto</creator><creator>Ortega-Camacho, Daniela</creator><creator>Tun-Rosado, Giovani Emmanuel</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>PYCSY</scope><scope>Q9U</scope><scope>SOI</scope><orcidid>https://orcid.org/0000-0002-8683-7156</orcidid><orcidid>https://orcid.org/0000-0002-5779-517X</orcidid></search><sort><creationdate>20200301</creationdate><title>Changes in the hydrochemistry of a karstic lake in Yucatan, Mexico</title><author>Cejudo, Eduardo ; Acosta-González, Gilberto ; Ortega-Camacho, Daniela ; Tun-Rosado, Giovani Emmanuel</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a339t-a9ebe3eca4e05c869fdda7218f8151b99261154cce77748d438875bfc272a51b3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Anthropogenic factors</topic><topic>Aquifers</topic><topic>Aragonite</topic><topic>Bathymeters</topic><topic>Bathymetry</topic><topic>Biogeosciences</topic><topic>Calcite</topic><topic>Calcium</topic><topic>Calcium chloride</topic><topic>Dolomite</topic><topic>Dolostone</topic><topic>Earth and Environmental Science</topic><topic>Earth science</topic><topic>Earth Sciences</topic><topic>Environmental Science and Engineering</topic><topic>Evaporation</topic><topic>Fault lines</topic><topic>Geochemistry</topic><topic>Geology</topic><topic>Groundwater</topic><topic>Human influences</topic><topic>Hydrochemistry</topic><topic>Hydrology/Water Resources</topic><topic>Intrusion</topic><topic>Ion exchange</topic><topic>Karst</topic><topic>Lakes</topic><topic>Limestone</topic><topic>Magnesium</topic><topic>Mathematical analysis</topic><topic>Nutrients</topic><topic>Original Article</topic><topic>Profiles</topic><topic>Saline intrusion</topic><topic>Saltwater intrusion</topic><topic>Sediments</topic><topic>Sulfate reduction</topic><topic>Sulphate reduction</topic><topic>Terrestrial Pollution</topic><topic>Tropical climate</topic><topic>Vertical profiles</topic><topic>Water depth</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Cejudo, Eduardo</creatorcontrib><creatorcontrib>Acosta-González, Gilberto</creatorcontrib><creatorcontrib>Ortega-Camacho, Daniela</creatorcontrib><creatorcontrib>Tun-Rosado, Giovani Emmanuel</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Environment Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Science Database</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric & Aquatic Science 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>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>Environment Abstracts</collection><jtitle>Environmental earth sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Cejudo, Eduardo</au><au>Acosta-González, Gilberto</au><au>Ortega-Camacho, Daniela</au><au>Tun-Rosado, Giovani Emmanuel</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Changes in the hydrochemistry of a karstic lake in Yucatan, Mexico</atitle><jtitle>Environmental earth sciences</jtitle><stitle>Environ Earth Sci</stitle><date>2020-03-01</date><risdate>2020</risdate><volume>79</volume><issue>5</issue><artnum>98</artnum><issn>1866-6280</issn><eissn>1866-6299</eissn><abstract>The Yucatan Peninsula is a karstic region with groundwater-dependent ecosystems and geological features such as karstic lakes. The objective of this research was to calculate the volume of water stored in this section of the aquifer and to describe the changes in the hydrochemistry of the lake Punta Laguna as a representative of karstic lakes in the Yucatan Peninsula. A bathymetry and calculation of the volume of water stored in the lake resulted in 5,198,505 m
3
with a maximum depth measured of 26.6 m Physicochemical measurements were completed in surface and three vertical profiles to estimate the mass of nutrients and ions and to describe the current hydrochemistry. The lake is an oligotrophic one of mixed-typed water (chloride-calcium/magnesium), saturated or supersaturated with calcite, dolomite and aragonite due to limestone dissolution. No evidence obtain regarding the saline intrusion. The conclusion that we can derive from the data is that Punta Laguna is a tropical karstic lake in good condition with low anthropogenic influence, evolving hydrochemically speaking. The changes over a 20-year period suggest that there has been reverse ion exchange, evaporation and sulfate reduction.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s12665-020-8838-3</doi><orcidid>https://orcid.org/0000-0002-8683-7156</orcidid><orcidid>https://orcid.org/0000-0002-5779-517X</orcidid></addata></record> |
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| identifier | ISSN: 1866-6280 |
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| subjects | Anthropogenic factors Aquifers Aragonite Bathymeters Bathymetry Biogeosciences Calcite Calcium Calcium chloride Dolomite Dolostone Earth and Environmental Science Earth science Earth Sciences Environmental Science and Engineering Evaporation Fault lines Geochemistry Geology Groundwater Human influences Hydrochemistry Hydrology/Water Resources Intrusion Ion exchange Karst Lakes Limestone Magnesium Mathematical analysis Nutrients Original Article Profiles Saline intrusion Saltwater intrusion Sediments Sulfate reduction Sulphate reduction Terrestrial Pollution Tropical climate Vertical profiles Water depth |
| title | Changes in the hydrochemistry of a karstic lake in Yucatan, Mexico |
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