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Simulation of brackish karst springs operation with the MODKARST deterministic modelView Crossref metadata(active tab) <div id="edit-xml" class="form-item form-type-item"> <?xml version="1.0"?> <doi_batch version="4.4.1" xmlns="http://www.crossref.org/schema/4.4.1" xmlns:jats="http://www.ncbi.nlm.nih.gov/JATS1" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.crossref.org/schema/4.4.1 http://www.crossref.org/schemas/crossref4.4.1.xsd"><head><doi_batch_id>000695</doi_batch_id><timestamp>1714020424</timestamp><depositor><depositor_name>University of the Aegean</depositor_name><email_address>uoa@university.com</email_address></depositor><registrant>Global NEST Journal</registrant></head><body><journal><journal_metadata><full_title>Global NEST Journal</full_title><full_title>Global NEST: the international Journal</full_title><issn media_type="print">1790-7632</issn><issn media_type="electronic">2241-777X</issn></journal_metadata><journal_issue><titles><title>Issue 3</title></titles><publication_date><month>11</month><year>2024</year></publication_date><journal_volume><volume>7</volume></journal_volume><issue>3</issue></journal_issue><journal_article><titles><title>Simulation of brackish karst springs operation with the MODKARST deterministic model</title></titles><abstract xmlns="http://www.ncbi.nlm.nih.gov/JATS1"><p>A simulation is presented of the operation of brackish karst springs with the MODKARST deterministic mathematical model. Through this simulation, major issues regarding the operation mechanisms as well as the sustainable development of the springs are addressed and analyzed. The particular case analyzed is the Almiros brackish karst spring at Heraklion Crete in Greece and the Makaria brackish karst spring in Attica. Of concern are the following aspects: (a) The fractal characteristics of the Almiros karst formation, (b) the sea intrusion mechanism for the Almiros spring and the Makaria spring and (c) the choice of a suitable method for the sustainable development of the Almiros spring. It was found that the seawater intrusion in the Almiros karst-spring reservoir follows a power law, the exponent of which provides the fractal dimension of the system. Regarding sea intrusion, the spring becomes brackish due to the crossing of the tube, which carries the fresh water to the spring, with other tubes, carrying saltwater from the sea. MODKARST simulates the hydrograph along with the variation with time of the chloride concentration and correlates the discharges from the fresh water and the seawater tubes. The outcome is the relative importance of the two potential mechanisms for seawater intrusion, namely the density difference between fresh water and sea water and the venturi effect; it is found that the density difference dominates in the Almiros case while the Venturi effect dominates in the Makaria case. An important conclusion of the analysis is that raising the Almiros-spring water outlet could prevent the seawater intrusion; the location of the elevated outlet and the fresh water loss to the sea are estimated.</p></abstract><publication_date><month>04</month><day>29</day><year>2013</year></publication_date><pages><first_page>244</first_page><last_page>251</last_page></pages><publisher_item><identifier id_type="pii">340</identifier></publisher_item><doi_data><doi>10.30955/gnj.000340</doi><timestamp>1714020424</timestamp><resource>https://journal.gnest.org/publication/340</resource></doi_data></journal_article></journal></body></doi_batch> </div>
