The paper assesses the vulnerability of 27 groundwater bodies in the basin of the river Bosna, ie Spreča, then the river basin of the Drina river (Drinjača), as well as parts of the immediate Sava river basin (Čelić area - Gnjica river and Turija basin) by the GLA method. For each water body, the determination of the effective soil capacity, degree of infiltration and rock type was made, as well as the final assessment of the protective efficiency of the unsaturated zones soil covering.
Foster S, Hirata R. Groundwater Pollution Risk Assessment – A Methodology Using Available Data. 1988.
2.
Hrvatović H. Geological guide through BiH, Institute of Geology of FBiH, Sarajevo. Geological guide through B&H. 2006.
3.
Čičić S. Geological map of Bosnia and Herzegovina. 2002.
4.
Babajić E. Petrološko – geohemijska i geotektonska obilježja mafitnih magmatskih stijena Krivajsko-konjuškog ofiolitnog kompleksa. 2009.
5.
Pamić J. Magmatske formacije Dinarida-Vardarske zone i južnih dijelova Panonskog bazena, Časopis Nafta Zagreb. [Croatian language] Magmatic formations of the Dinarides-Vardar zone and the southern parts of the Pannonian Basin. Magazine Nafta Zagreb. 1996;
6.
Pamić J. Magmatske i tektonske strukture u ultramafitima bosanske serpentinske zone, Geološki Zavod u Sarajevu. In: Magmatic and tectonic structures in ultramafics of the Bosnian serpentine zone, Geological Institute in. 1964.
7.
Pamić J, Olujić J. Hidrotermalne metasomatske stijene sa sjeverne granice ozrenskog ultramafitnog masiva. Jugoslovenska akademija znanosti i umjetnosti, Beograd. Hydrothermal metasomatic rocks from the northern border of Ozren ultramafic massif. 1974.
8.
Đurić N, Radovanović S. Energetska potencijalnost geotermalnih resursa i mogućnost njihovog korištenja za toplifikaciju grada Bijeljine, Tehnički institut, Bijeljina. [Serbian language] Energy potential of geothermal resources and possibility their use for heating the city of Bijeljina. 2012.
9.
Lepirica A. Reljef geomorfoloških makroregija Bosne i Hercegovine, 2013. Bosnian language] Geomorphological macroregion relief of Bosnia and Herzegovina. 2015;
10.
Žigić I, Pašić-Škripić D, Srkalović D. Studija karakterizacije podzemnih voda sliva rijeke Save. 2011.
11.
Kudumović Dostović F, Ahmetbegović S, Stjepić Srkalović Ž. Klima kao faktor razvoja rekreativnog turizma Sjeveroistočne Bosne, Acta geographica Bosniae et Herzegovinae, Sarajevo.[Bosnian language] Climate as a factor of recreational tourism development of Northeast Bosnia. 2019.
12.
Žigić I, Pašić-Škripić D, Srkalović D i saradnici. Studija ranjivosti Tuzlanskog kantona, Bosna SOil. 2008.
13.
Žigić I, Pašić-Škripić D i S, D. Studija karakterizacije podzemnih voda podsliva rijeke Drine. 2009.
14.
Srkalović D. Ranjivost vodnih tijela podzemnih voda područja sjeveroistočne Bosne – magistarski rad, RGGF, Tuzla[Bosnian language] Vulnerability of groundwater bodies in the area of northeastern Bosnia. 2011.
15.
Srkalović ŽS. Pedogeografske karakteristike područja općine Tuzla (Magistarski rad, str. 6) [Bosnian language] Pedogeographical characteristics of the municipality of Tuzla. 2015. p. 6.
16.
Hölting B, Wilhelm G. Hydrogeologie. Einführung in die Allgemeine und Angewandte Hydrogeologie, Auflage 6, pp 326[German language. Introduction to the general and applied Hydrogeology. 2005;(ue 6):326.
Citation
Copyright
This is an open access article distributed under the Creative Commons Attribution License which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
The statements, opinions and data contained in the journal are solely those of the individual authors and contributors and not of the publisher and the editor(s). We stay neutral with regard to jurisdictional claims in published maps and institutional affiliations.