Szczegóły publikacji
Opis bibliograficzny
Evaluation of exploitable resources of water intakes located between rivers, based on numerical modeling, on the example of Tarnów region in Poland / Andrzej HAŁADUS, Robert ZDECHLIK, Andrzej SZCZEPAŃSKI, Przemysław Bukowski, Grzegorz Wojtal // W: SGEM 2017 : 17th international multidisciplinary scientific geoconference : science and technologies in geology, exploration and mining : 29 June–5 July, 2017, Albena, Bulgaria : conference proceedings. Vol. 17 iss. 12, Hydrogeology, engineering geology and geotechnics. — Sofia : STEF92 Technology Ltd., cop. 2017. — (International Multidisciplinary Scientific GeoConference SGEM ; ISSN 1314-2704). — ISBN: 978-619-7105-99-5. — S. 297–304. — Bibliogr. s. 304, Abstr.
Autorzy (5)
- AGHHaładus Andrzej
- AGHZdechlik Robert
- AGHSzczepański Andrzej
- Bukowski Przemysław
- Wojtal Grzegorz
Słowa kluczowe
Dane bibliometryczne
| ID BaDAP | 107093 |
|---|---|
| Data dodania do BaDAP | 2017-07-20 |
| DOI | 10.5593/sgem2017/12/S02.038 |
| Rok publikacji | 2017 |
| Typ publikacji | materiały konferencyjne (aut.) |
| Otwarty dostęp |  |
| Konferencja | 17th international multidisciplinary scientific geoconference |
| Czasopismo/seria | International Multidisciplinary Scientific GeoConference SGEM |
Abstract
Tarnow region is supplied with water from intensively exploited groundwater and surface water intakes located in the small area between Dunajec and Biała rivers. Three groundwater intakes are a part of the Tarnow Municipal Water Service, i.e. Świerczków, Kępa Bogumiłowicka and newly constructed Zbylitowska Góra intake, as well as the intake of surface water in Zbylitowska Góra. The chemical company Zakłady Azotowe in Tarnów has groundwater intake located in Tarnów-Mościce, and one of surface water located nearby. Groundwater intakes draw water of the Quaternary aquifer (sandy and gravel deposits, mixed with pebbles, with hydraulic conductivity from a dozen to more than 100 m/d), recharged directly with rainfall and infiltrating river water, and locally with water from irrigation ditches. Exploitation of water takes place in the conditions involving several major sources of contamination. The magnitude evaluation of exploitable resources of subject intakes involved calibrated numerical model of the aquifer’s hydrogeological structure, developed on the basis of the actual size of groundwater withdrawal and depth to groundwater table. The model was modified and updated on the basis of the existing single-layer numerical model, that maps the hydrogeological conditions occurring in the Quaternary aquifer. As a part of predictive tests, the research team used the model to map average low water levels in surface flows, and then simulated the operation of individual intakes in order to obtain the greatest possible efficiency. Possible withdrawal can be estimated at around 81.5% of the resources. © SGEM2017. All Rights Reserved.
