Institut za rudarstvo i metalurgiju Bor

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Spring 2 Figure 3. Circle diagram of chemical composition, spring 2- water at the Monastery St. Sava Spring 3 Figure 4. Circle diagram of chemical composition, spring 3- water from the courtyard of R. Milosavljevic Spring 4 No 1,2010. 165 MINING ENGINEERING
Figure5. Circle diagram of chemical composition, spring 4- water from the courtyard U. Radosavljevic In the frame of the research project Hydrogeology investigation of mineral and thermo mineral waters of the northern part of Kosovo and Metohija, financed by Ministry for environmental protection and planning, the sample was taken from the Spa bath for the analyse for the investigation of the possibilities of its exploitation. These samples were analyzed in the laboratories of the <strong>Institut</strong>e for public health “dr Milan Jovanovic Batut”, Belgrade, and the results were showed in Table 2. Table 2. Physical-chemical characteristics of thermo-mineral waters of Banjska (<strong>Institut</strong>e for public health “dr Milan Jovanovic Batut”, Belgrade, 2008.) No. Basic physical-chemical prop- Content method erties 1. temperature ( 0 C) 40,5± 0,1 UP-501 2. pH 7,0± 0,1 UP-503 3. Color (degrees Pt-Co scale)
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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
Page 118 and 119: KOMITET ZA PODZEMNU EKSPLOATACIJU Y
Page 120 and 121: Tab. 1. Koordinate temena eksploata
Page 122 and 123: Eksploatacija ležišta rude bakra
Page 124 and 125: COMMITTEE OF UNDERGROUND EXPLOITATI
Page 126 and 127: Figure 3. Mutual position of open p
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Page 132 and 133: gde su: v r - brzina protoka: u r -
Page 136 and 137: z and r - cylindrical coordinates
Page 140 and 141: da zaštiti podzemne vode od kontam
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 170 and 171: 12. Lead (Pb)
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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