Institut za rudarstvo i metalurgiju Bor

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12. Lead (Pb)
Figure 6. Circle chart of the chemical composition of thermo mineral waters of Banjska, sample taken from the Spa pool Based on the results of physicalchemical characteristics of thermo-mineral waters of Banjska (Table 1 and Table 2) and based on the graphic presentation of their chemical composition (Figures 2,3,4,5 and 6) it can be concluded that those belong to the same water type. Based on the obtained results it can be said that in the group of cathions the sodium is dominating, but there is also high content of magnesium and calcium. From the group of anions hydro-carbonate is mostly present, than chlorides and the total anions content is three times higher than cathions content. The investigated waters are in the group of sodium, calcium, magnesium hydro carbonated carbon hydro carbonated hypothermal waters [6]. Referring to physical-chemical analyze of the thermo-mineral waters of Banjska, the balneology estimation of their medicinal properties was made. The radioactivity testing in the sample of thermo mineral water was made in the institute for professional medicine and radiology protection “Dr Dragomir Karajovic” in Belgrade, whose results were presented in Table 3. Table 3. Results of gama spectrometry analysis (institute for professional medicine and radiology protection “ dr Dragomir Karajovic” in Belgrade, 2008): Sample type 137 Cs (Bq/l) 134 Cs (Bq/l) 40 K (Bq/l) 232 Th (Bq/l) 238 U (Bq/l) 226 Ra (Bq/l) Banjska Spa < 0.007 < 0.003 0.60 ± 0.04 < 0.02 < 0.10 < 0.03 The results of gama spectrometry analysis of water ( specific activity) point on the fact that the analyzed waters are adequate by the regulation of drinking water quality ( according to the regulative S.L.SRJ No.9/1999) USAGE OF THERMO MINERAL WATERS OF BANJSKA The possibilities of using thermal water Banjska are: balneo therapy, sport and recreation, heating fluid, fuel et al. Mineral water Banjska provide numerous opportunities for development and improvement balneotherapy sports and No 1,2010. 168 MINING ENGINEERING
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INSTITUT ZA RUDARSTVO I METALURGIJU
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KOMITET ZA PODZEMNU EKSPLOATACIJU Y
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Analizirajući ovaj način uzorkova
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SADRŽINA UPROŠĆENOG RUDARSKOG PR
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COMMITTEE OF UNDERGROUND EXPLOITATI
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area is constantly increased. Figur
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CONTENT OF THE SIMPLIFIED MINING PR
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U morfološkom smislu, teren predst
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Rezultati terenski istraživanja i
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In morphological terms, the terrain
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GEO-MECHANICAL FEATURES OF THE TERR
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Sl. 3. Smičući naponi u konstrukc
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Na modelu bojom su razgraničeni od
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Figure 3. Shear stresses in collect
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Dumped material and collector eleme
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PODRUČJE ISTRAŽIVANJA Aleksinačk
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Da bi se izbor otkopne mehanizacije
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lansnih rezervi uglja, a druga za g
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veličina i takođe zahteva neophod
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exploitation, two variants of this
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esses, require the use of modern sy
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• method without underground room
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directly used to drive power plants
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gde je: Δ - nasipna masa uzorka; m
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D (%) 100 90 80 70 60 50 40 30 20 1
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Where is: Δ - volumetric density o
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D (%) 100 90 80 70 60 50 40 30 20 1
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PRORAČUN STABILNOSTI SOFTVEROM GEO
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Sl. 6. Izgled klizne ravni i koefic
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CALCULATION OF STABILITY BY THE SOF
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Figure 6. View of sliding plane and
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kon sulfatizacije, postignut je sle
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Table 2. Degrees of metal leaching
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70%. Dreniranje izdani vrši se po
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do kote K+656 m gde su postavljene
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is very abundant feeding aquifers.
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Start-minute maximum intensity of d
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Figure 3. Operation diagram of pump
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Zlato u koncentratu kg - 27,988 12,
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Na samlevenim uzorcima topioničke
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Dry concentrate t 5,226 10.563 5.82
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Sadržaj klase -75μm , % 100 80 60
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Page 120 and 121: Tab. 1. Koordinate temena eksploata
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Page 124 and 125: COMMITTEE OF UNDERGROUND EXPLOITATI
Page 126 and 127: Figure 3. Mutual position of open p
Page 128 and 129: underground water in the first wate
Page 130 and 131: KOMITET ZA PODZEMNU EKSPLOATACIJU Y
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Page 136 and 137: z and r - cylindrical coordinates
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Page 142 and 143: • Otpadne vode od samog postrojen
Page 146 and 147: Practically, the “in-situ” expl
Page 148 and 149: • Waste water created during the
Page 152 and 153: geotektonska zona prema severoistok
Page 154 and 155: Osmatrani režim izdašnosti i temp
Page 156 and 157: Sl. 4. Kružni dijagram hemijskog s
Page 158 and 159: 15. Nikl (Ni) 0,012±0,00500 UP-919
Page 160 and 161: alneoterapijskih i sportsko-rekreat
Page 164 and 165: phase are presented by andesite bas
Page 166 and 167: Figure 1. Hydro-geology maps of the
Page 168 and 169: Spring 2 Figure 3. Circle diagram o
Page 172 and 173: ecreational activities. The beginni
Page 174 and 175: UTICAJ GRANULOMETRIJSKOG SASTAVA ML
Page 176 and 177: SADR@AJ CONTENS D. Sokolović, D. E
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Institut za rudarstvo i metalurgiju Bor

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