RMZ â MATERIALI IN GEOOKOLJE

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420 Adewale, A., Olawale, O. O., Martins, O. M.ble made from thick filter papersloaded in the main chamber of theapparatus and placed on a flask containingthe extraction solvent. Thesolvent is heated to reflux, releasingits vapour to travel up the distillationarm. A condenser ensures thatthe solvent vapour cools and dripsback into the chamber housing thetar materials. The chamber containingthe solid material is slowly filledwith the warm solvent. When theSoxhlet chamber is almost filled, it isautomatically emptied by siphon sidearm with the solvent running downinto the distillation flask. This cycleis allowed to repeat many times, overhours or days.Results and discussionElectrical resistivity method has foundwide and successful application both insurface and borehole measurements todifferentiate hydrocarbon saturated regionfrom saline water saturated sandon the account of very high resistivitysignature of hydrocarbon pore fluidsthat are incapable of ionic conduction(Winsauer et al, 1952). Representativeresistivity VES curves obtained after1-d inversion of the field data are presentedin figure 3 (a–c). The interpretationof the resistivity layered parameterswas constrained by core and drillcuttings information from a drilledborehole from where samples werea)<strong>RMZ</strong>-M&G 2012, 59
Geophysical and sedimentological studies for reservoir characterization of ...421b)c)Figure 3. VES Curves obtained from the Study Area<strong>RMZ</strong>-M&G 2012, 59
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IVTable of Contents - KazaloProfess
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Calculation of stress-strain depend
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() = (, )() () ()Calculation
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, ) (, )(, ) 1 () + = (, ) =
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RMZ - Materials and Geoenvironment,
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Petrochemical characteristics and g
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360 Akinola, O. O., Talabi, A. O.A
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362 Akinola, O. O., Talabi, A. O.of
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364 Sunmonu, L. A., Adagunodo, T. A
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Page 66 and 67: 392 Shemetov, P. A., Bibik, I. P.in
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Page 70 and 71: k =1.05+Dλ = 1+k =( s )396 Shemeto
Page 72 and 73: 398 Shemetov, P. A., Bibik, I. P.si
Page 74 and 75: у 3 b400 D = f eShemetov, P. A., B
Page 76 and 77: V4BEK Q σBEad = ,commQрσV 01 +
Page 78 and 79: 404 Shemetov, P. A., Bibik, I. P.wh
Page 80 and 81: thrмR iλ = 2 λ= 100⋅exp[ −(
Page 82 and 83: qLevel of average technical (theore
Page 84 and 85: .6670.05=0.35k1,05+D avet( s3≥ Kt
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Page 88 and 89: 414 Adewale, A., Olawale, O. O., Ma
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Page 104 and 105: 430 Kos, A., Dervarič, E.novega ve
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Page 108 and 109: 434 Kos, A., Dervarič, E.chines to
Page 110 and 111: 436 Kos, A., Dervarič, E.the best
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Page 114 and 115: 440 Kos, A., Dervarič, E.nally to
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Page 118 and 119: 444 Lajovic, A.disc brakes, further
Page 120 and 121: 446 Lajovic, A.Slika 2. Izrez iz Si
Page 122 and 123: 448 Lajovic, A.Livne lonce smo na n
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Page 136 and 137: 462 Lajovic, A.Sredi osemdesetih le
Page 138 and 139: 464 Lajovic, A.njem delu forme. Na
Page 140 and 141: 466 Lajovic, A.Enourni film je mars
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470 Medved, J., Rosina, A., Vončin
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472 Author’s IndexAuthor`s Index,
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RMZ-M&G 2012, 59
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Contents476Phase contrast method fo
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Contents47859/4Calculation of stres
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Instructions to authors481Compositi
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Instructions to authors483NAVODILA
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Instructions to authors485Knjige:Ro
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Template487TEMPLATEThe title of the
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Template489References (Times New Ro
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Template491Obstajata dve sprejemlji
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RMZ â MATERIALI IN GEOOKOLJE