Hydrogeological protection of the buchak-kaniv aquifer complex in the central part of Dnipro-Donetsk artesian basin from possible technological contamination
DOI:
https://doi.org/10.26565/2410-7360-2017-47-25Keywords:
hydrogeological protection, Buchak-Kaniv aquifer complex, contaminated water, surface pollution, water intake, water table regime, separation layer, ascending stream zonesAbstract
Formulation of the problem. Every year, the problem of studying the ecological state of drinking groundwater becomes more and more acute, as the reserves of ecologically clean groundwater is becoming more and more depleted. At the same time, at the time of significant influence of technogenic factors on the quality of drinking groundwater, there is an urgent need for a more detailed assessment of the protection index of aquifer complexes promising for water use purposes.
The purpose of the article. The main purpose of the research is to show the degree of modern hydrogeological protection of one of the strategic reserves of drinking underground water in the region – Buchak-Kaniv aquifer complex – in the area of its greatest distribution and use – the central part of Dnipro-Donetsk artesian basin from possible contamination of water that lie above. Corresponding trends in protection changes during the long period of time (55 years) within the territory of work were also traced.
Methods. Taking into account the hydrogeological and lithological features of aquifer complexes and waterproof rocks in the interior of the subsoil, as well as on the basis of previous research by scientists, a multi-factor, adapted to these conditions, methodology for carrying out the research was developed. The methodology includes the definition of both static and dynamic components of the protection index. Calculations and graphic constructions were made for 2 periods of time – 1960 and 2015.
Results. The peculiarities of the hydrogeological protection of the aquifer complex within the territory of works during these periods were analyzed and relevant trends in changes in the indicator over the 55-year period have been traced. It has been determined that the territories of areas with unprotected and conditionally protected underground water expanded, and protected areas – on the contrary, decreased. The largest changes occurred in the areas affected by water intakes of large cities in the region. The reasons for these processes are presented, the main of which is an anthropogenic factor.
Scientific novelty and practical significance. This methodology in assessing the protection in this region has been used for the first time. The obtained results of the research should be used to develop recommendations for the ecological protection of drinking groundwater in the region. This method of work can be used to determine a hydrogeological protection index of other pressure aquifer complexes in similar conditions.
References
Levonyuk, S. M. (2017). Zminy pokaznyku zahyshenosti pidzemnykh vod buchats’ko-kanivs’koho vodonosnoho kompleksu tsentral’noyi chastyny DDAB / Tezy dopovidi na IV Naukoviy konferentsiyi z mizhnarodnoyu uchastyu «Hidroheolohiya: nauka, osvita, praktyka». Kharkiv, 54-57.
Gol’dberg, V. M. (1987). Vzaimosviaz’ zagrjaznenija podzemnyh vod i prirodnoj sredy. Leningrad, 248.
Shestopalov, V. M., Boguslavskij, A. S., Bubljas’, V. N. (2007). Otsenka zashishennosti i uiazvimosti podzemnyh vod s uchetom zon bystroi migratsii. Kyiv, 120.
Mikitchuk, L. A. otv. isp. Karta estestvennoj zashhishhennosti podzemnyh vod Poltavskoj oblasti m-ba 1:200 000 (otchet o rabotah, vypolnennyh Kremenchugskoj GRJe v 1980-1982 gg.) (1982). Dnipropetrovsk: Kremenchugskja GRJe tresta «Ukrjuzhgeologija», 169.
Mikitchuk, L. A., Terentieva, A. E. otv. isp. (1987). Karta estestvennoj zashishennosti podzemnyh vod Ukrainy, m-b 1:200000, 1987 g. Poltavskaja oblast’. Novaia Galeshhina: Kremenchugskaja GRJe tresta «Ukrjuzhgeologija», 28.
Kamenskaia, I. N., Chopyk, B. N. (1983). Otchet o rezultatah rabot po sostavleniyu karty usloviy zashishennosti podzemnyh vod po Har’kovskoj i Sumskoj oblastjam USSR za 1979-1982 gg. Kharkov: Harkovskaja GRJe tresta «Ukrjuzhgeologija», 242.
Chopyk, B. N. (1988). Karta estestvennoj zashishhennosti podzemnyh vod USSR m-ba 1:200000. Har’kovskaja oblast’. Kharkov: Har’kovskaja GRJe tresta «Ukrjuzhgeologija», 35.
Ostroukh, O. A. (2016). Zakonomirnosti zmin khimichnoho skladu gruntovyh vod Chop-Mukachivs’koho baseynu. HNU im. V.N. Karazina. Kharkiv, 20.
Marchenko, G. P., Kutashenko, L. E., Aleinikova, L. N. edc. (1965). Podzemnye vody SSSR. Obzor podzemnyh vod Poltavskoj oblasti. V 3-eh tomah. Moscow, 950.
Kostjuchenko-Pavlova, M. M., Jandola, S. P., Belogorskaja Je. G. edc. (1968). Podzemnye vody SSSR. Obzor podzemnyh vod Har’kovskoj oblasti. V 3-eh tomah. Moscow, 900.
Pedan, V. V. (2002). Vedennya AIS DVK, derzhoblik ta vyvchennya rezhymu pidzemnykh vod u zonakh vplyvu vodozaboriv na terytoriyi Sums’koi, Kharkivs’koyi ta Poltavs’koyi oblasti, 1996-2000 rr. Kharkiv: Kharkivs’ka KHP KP «Pivdenukrheolohiya», 150.
Lega, V. I. (2003). Zvit pro rezul’taty robit po otsintsi stanu prohnoznykh resursiv ta ekspluatatsiynyh zapasiv pytnykh ta tekhnichnykh pidzemnykh vod na terytoriyi Poltavs’koyi oblasti v 2000-2003 rr. Dnipropetrovs’k: Kremenchuts’ka HRE KP «Pivdenukrheolohiya», 140.
Berezhna, K. I. (2006). Vedennya AIS DVK, derzhavnoho obliku vykorystannya pidzemnykh vod, monitorynhu resursiv ta zapasiv pidzemnykh vod na terytoriyi Sums'koyi, Kharkivs'koyi ta Poltavs'koyi oblastey, 2001-2005 rr. Kharkiv: Kharkivs'ka K·HP KP «Pivdenukrheolohiya», 135.
Barabanova, N. V. (2007). Otsinka stanu prognoznykh resursiv ta ekspluatatsiynikh zapasiv pytnykh ta tehnichnykh pidzemnykh vod na terytoriyi Sums’koyi, Kharkivs’koyi ta Poltavs’koyi oblastey. Kharkiv: Kharkivska KHP KP «Pivdenukrheolohiya», 145.
Panikars’ka, I. S. (2016). Uzahal'nennya materialiv AIS DVK, derzhavnoho obliku vykorystannya pidzemnykh vod ta kadastru poshukovo-rozviduval'nykh i ekspluatatsiynykh sverdlovyn na vodu v mezhakh terytoriyi diyal'nosti pidpryyemstva: zvit z NDR (zakl.) Dnipropetrovs’k: KP «Pivdenukrheolohiya», 170.
Maksimov, V. M. ed. (1979). Spravochnoe rukovodstvo gidrogeologa. Leningrad, 1, 512.
Shvyd, N. T., Terentiev, Ju. A. (1983). Detal’naja razvedka podzemnyh vod uchastkov vodozaborov № 6 i № 7 dlia vodosnabzheniia g. Poltavy v 1980-1983 gg. Dnepropetrovsk: Kremenchugskaja GRJe tresta «Ukrjuzhgeologija», 250.
Kamzist, Zh. S. (2009). Hidroheolohiya Ukrainy: navch. posibnyk. Kyiv: INKOS, 614.
Rudenko, F. A. (1971). Gidrogeologia SSSR, 614.
Klimentov, P., Kononov, V. (1985). Dinamika podzemnyh vod. Moscow: Vysshaja shkola, 200.
Downloads
Published
Issue
Section
License
Copyright (c) 2018 С. М. Левонюк
This work is licensed under a Creative Commons Attribution 4.0 International License.
Authors who publish with this journal agree to the following terms:- Authors retain copyright and grant the journal right of first publication with the work simultaneously licensed under a Creative Commons Attribution License that allows others to share the work with an acknowledgement of the work's authorship and initial publication in this journal.
- Authors are able to enter into separate, additional contractual arrangements for the non-exclusive distribution of the journal's published version of the work (e.g., post it to an institutional repository or publish it in a book), with an acknowledgement of its initial publication in this journal.
- Authors are permitted and encouraged to post their work online (e.g., in institutional repositories or on their website) prior to and during the submission process, as it can lead to productive exchanges, as well as earlier and greater citation of published work (See The Effect of Open Access).
