Surgil ESIA Report - Volume III - EKN

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Management procedure of the drilling wastes (cuttings barns) recycling, generated during production wells drilling in Surgil field Depth, m Well name direction conductor technical production Drilling interval Chisel diameter, mm String diameter, mm CL, m 150 300 450 600 750 900 1050 1200 1350 1500 1650 1800 1950 2100 2250 2400 2550 2700 2850 3000 0-50 490 426 0 50-400 393.7 298.4 0 400-1500 269.9 219.1 0 1500- 2950 190.5 139.7 0 Figure P.1.1 – Scheme of production well design of Surgil field - 30 -
“Management of Ustyurt GCC infrastructure objects and Surgil GCF construction” UE » Appendix 3 CALCULATION OF LIQUID EVAPORATION THICKNESS FROM SURFACE LAYER IN THE REGION OF SURGIL FIELD Calculation of evaporation from turbid and saline reservoirs and storages of industrial drains is carried out according to method resulted in “Instructions on calculation of evaporation from reservoirs surface”. L. Gidrometeoizdat, 1969 - by formula: E m = r х E o , (P3.1) where: E p – mud evaporation from industrial drain; E o – pure fresh water evaporation for the same period of time; r – conversion factor from evaporation with pure fresh water to evaporation from mud. Evaporation volume from reservoir E o (mm) located in the plain territory is defined by formula: E o = 0.14 х п х (е п – е 200 ) х (1 + 0.72 x v 200 ), (P3.2) where: п – number of days in design time space (month); е п – average value of maximal steam tension, mb. It is defined according to tables in Appendix 3 (“Instructions on calculation of evaporation from reservoirs surface”. L. Gidrometeoizdat, 1969); е 200 – average value of steam tension (absolute air humidity) over reservoir at the height of 200sm, mb; v 200 – average value of wind speed over reservoir at the height of 200sm, m/s. Average value of steam tension (absolute air humidity) reservoir at the height of 200sm е 200 (mb) is calculated by formula: е 200 = е’ 200 + (0.8 х е п – е’ 200 ) х М, (P3.3) where: е’ 200 – average for design time space of air humidity measured at nearby meteorological station, mb; М –transformation ratio considering average air humidity and temperature change depending on the reservoir capacity. Defined under table 4 (“Instructions on calculation of evaporation from reservoirs surface”. L. Gidrometeoizdat, 1969). In our case, transformation ratio changes depending on season of year from 0.01 to 0.003. Average value of wind speed over reservoir at the height of 200sm v 200 (m/s) is calculated by formula: v 200 = К 1 х К 2 х К 3 х v ф , (P3.4) - 31 -
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Книга 2. Часть 2. Про
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OAJ “O’ZLITINEFTGAZ” ПТЭО
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NATIONAL HOLDING COMPANY «UZBEKNEF
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