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2012, vol. 53, br. 2, str. 157-162
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Uticaj upotrebe komprimovanog vazduha pri bušenju, razradi i ispiranju pijezometara i bunara na rezultate ispitivanja fizičko-hemijskog sastava podzemnih voda
Influence of using compressed air for drilling, development and cleaning of the piezometers and the wells, to the results of testing physical-chemical composition of ground water
a'IPIN' Institut za primijenjenu geologiju i vodoinženjering, Bijeljina, Republika Srpska, Bosna i Hercegovina
bUniverzitet u Istočnom Sarajevu, Tehnološki fakultet, Zvornik, Republika Srpska, BiH
Sažetak
Ovim radom se ukazuje na to, da se kiseonik u podzemnim vodama, može zadržati na velikom prostoru i dugo vremena nakon izvođenja i ispiranja pijezometara i bunara, što objektivno može uticati na rezultate ispitivanja fizičko-hemijskog sastava podzemne vode u toku prvog testiranja bunara. U radu su prezentovani podaci o navedenim situacijama u akviferu neogene starosti u Stanarima kod Doboja i u aluvijalnoj izdani u Kozluku kod Zvornika. Kako bi se u budućnosti eliminisao ovaj problem u radu su date preporuke, promjene uobičajene procedure hidrogeoloških istraživanja, da se sagleda efekat aeracije vode u akviferu, tokom razrade bunara.
Abstract
The compressed air is often used for purpose of drilling or quality developing and flushing the piesometers and water wells. This paper suggests, that the oxygen in the groundwater, can keep in a large area, for a long time after the performing and cleaning of the piezometers and water wells, which objectively, might have affect to the results of physical and chemical composition of groundwater when we test water wells in the first time. The paper presents data about these situations in the Neogene aquifer in the Stanari settlement near of city of Doboj, and in the alluvial aquifer in Kozluk village, near city of Zvornik, by correlation of test results immediately after the performing of water wells and later, during their usage. In order to eliminate this problem, in this paper proposals of future works were made, different of the usual procedure of hydrogeological research. It will bi possible to examine the effect of aeration of groundwater in the aquifer, during the performing of the wells.
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