RMZ â MATERIALI IN GEOOKOLJE

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384 Sunmonu, L. A., Adagunodo, T. A., Olafisoye, E. R., Oladejo, O. P.the bedrock increases, there wouldbe a reduction in the influence ofweathering, with a correspondinglowering of the aquifer potential(Olayinka et al, 1997). Table 7gives a summary of the variation ofaquifer potential with bedrock resistivity.Final Groundwater Potential Map ofthe Study AreaFinal groundwater potential map of thestudy area was produced in order todraw the final conclusion from the evaluatedmaps. The weights that have beenassigned in Table 1 – Table 7 were usedto get the weights of Overburden Thick-Figure 9. Bedrock relief map.Table 7. Aquifer potential as a function of bedrock resistivity.Bedrock Resistivity (Ω m)Range Aquifer Characteristics Weighting3000 Little or no weathering of the bedrock; negligible potential 2.5<strong>RMZ</strong>-M&G 2012, 59
The groundwater potential evaluation at industrial estate Ogbomoso, ...385ness, Anisotropy Coefficient, WeatheredLayer Resistivity, Transverse Resistanceand Bedrock Resistivity of thestudy area.A single weighted average is then determinedfrom the geometric mean of thefive weights to produce the 2-Dimensionalgroundwater potential map of theinvestigated area (figure 10). The mappresents local groundwater prospects ofthe study area which is zoned in to high,medium and low groundwater potentials.Area with colour brown on the map constitutethe low groundwater potentialzone (i. e. VES 1, VES 3, VES 4, VES 5,VES 7 and VES 10) while area with colourblue constitute the high groundwaterpotential zone (i. e. VES 2 and VES6). Medium groundwater potential zoneshare its colour between brown and blue,this is noted at the Northeastern side ofthe study area (I .e. VES 8 and VES 9).The Southern (VES 6) and the Eastern(VES 2) part of the study area are seento have relatively higher groundwaterpotential than the Northeastern (VES8 and VES 9) region of the study area.Southwestern, Southeastern, Western,Northern and Northwestern (i. e. VES 1,VES 3, VES 4, VES 5, VES 7 and VES10) regions are seen to have low groundwaterpotential in the study area. Thesezones with low groundwater potentialwill be good for engineering purposes(i.e. construction of factories).Figure 10. Final groundwater potential map of the study area<strong>RMZ</strong>-M&G 2012, 59
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IVTable of Contents - KazaloProfess
Page 7 and 8: Calculation of stress-strain depend
Page 11 and 12: () = (, )() () ()Calculation
Page 13 and 14: , ) (, )(, ) 1 () + = (, ) =
Page 21 and 22: RMZ - Materials and Geoenvironment,
Page 23 and 24: Petrochemical characteristics and g
Page 34 and 35: 360 Akinola, O. O., Talabi, A. O.A
Page 36 and 37: 362 Akinola, O. O., Talabi, A. O.of
Page 38 and 39: 364 Sunmonu, L. A., Adagunodo, T. A
Page 66 and 67: 392 Shemetov, P. A., Bibik, I. P.in
Page 68 and 69: 394 Shemetov, P. A., Bibik, I. P.
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 106 and 107: 432 Kos, A., Dervarič, E.diamond w
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434 Kos, A., Dervarič, E.chines to
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436 Kos, A., Dervarič, E.the best
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438 Kos, A., Dervarič, E.Before th
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440 Kos, A., Dervarič, E.nally to
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RMZ-M&G 2012, 59
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444 Lajovic, A.disc brakes, further
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446 Lajovic, A.Slika 2. Izrez iz Si
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448 Lajovic, A.Livne lonce smo na n
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450 Lajovic, A.Ingersol pa je bil z
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452 Lajovic, A.Med delavci, ki so b
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454 Lajovic, A.imel vsak delavec na
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456 Lajovic, A.Slika 5. Izdelki Že
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458 Lajovic, A.pa se ni najbolje iz
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460 Lajovic, A.za delo. Promet na z
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462 Lajovic, A.Sredi osemdesetih le
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464 Lajovic, A.njem delu forme. Na
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466 Lajovic, A.Enourni film je mars
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RMZ-M&G 2012, 59
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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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