Well Performance by Michael Golan

By Michael Golan

"This booklet has developed from path notes ready for creation engineering classes taught on the Norwegian Institute of know-how (NTH) in Trondheim and for classes dealing particularly with the functionality of high-capacity oil and fuel wells. even supposing the aim of the e-book is to help in educating of good functionality, it's going to be priceless as a reference publication for engineers already doing a little components of good performance."
-Michael Golan and Curtis H. Whitson
Trondheim, Norway

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2 3. 003 ? 101 France Wurtemberg St. G. 015 as likely to occur within the oil rather than as a breakdown of kerogen during the maturation process. That an asphaltene-type material occurs as part of a kerogen matrix is beyond question [35]. By definition, this should be anticipated. Many kerogens contain a toluene-soluble “bitumen” and, thus, bitumen should be anticipated to contain an asphaltene fraction. But it must be remembered that asphaltenes are not a specific chemical class but are a solubility class.

SPEIGHT TABLE 2- 11 Molecular weights of petroleum asphaltenes by vapor pressure osmometry (after Moschopedis et al. [113, p. 2281) Molecular weight Sample era C6H6 Solvent temperature ("C): 37 CH2Br2 CsHsN C6HsN02 37 37 37a 100 115 130 Upper Cretaceous 2092 2010 2103 2000 1990 2050 1940 Lower Cretaceous 4850 6669 6415 5768 3977 3782 4904 6583 5886 3430 4719 4562 4952 3456 3483 4068 5512 4589 2655 422 1 2687 2736 2400 2829 255 1 3179 2439 2050 3590 1650 2040 2150 2350 2070 1300 1830 1890 2470 1550 2020 1860 2030 1790 1250 1700 1820 2220 1410 1970 1740 1900 1700 1260 1670 1825 1920 1500 2060 1660 1990 1630 1220 1650 Carboniferous 4766 6672 4174 3907 3999 3667 2721 2898 2683 2010 2500 2170 1880 2250 2090 1870 2970 2140 1830 1960 2160 Lower Devonian 4125 3864 2541 1900 1830 1890 1810 a Extrapolated value.

2-20) [111,112]. In fact, it is strongly recommended that, to negate the concentration effects and the temperature effects, the molecular weight determinations be carried out at each of three different concentrations at each of three different temperatures. G. SPEIGHT TABLE 2- 11 Molecular weights of petroleum asphaltenes by vapor pressure osmometry (after Moschopedis et al. [113, p. 2281) Molecular weight Sample era C6H6 Solvent temperature ("C): 37 CH2Br2 CsHsN C6HsN02 37 37 37a 100 115 130 Upper Cretaceous 2092 2010 2103 2000 1990 2050 1940 Lower Cretaceous 4850 6669 6415 5768 3977 3782 4904 6583 5886 3430 4719 4562 4952 3456 3483 4068 5512 4589 2655 422 1 2687 2736 2400 2829 255 1 3179 2439 2050 3590 1650 2040 2150 2350 2070 1300 1830 1890 2470 1550 2020 1860 2030 1790 1250 1700 1820 2220 1410 1970 1740 1900 1700 1260 1670 1825 1920 1500 2060 1660 1990 1630 1220 1650 Carboniferous 4766 6672 4174 3907 3999 3667 2721 2898 2683 2010 2500 2170 1880 2250 2090 1870 2970 2140 1830 1960 2160 Lower Devonian 4125 3864 2541 1900 1830 1890 1810 a Extrapolated value.

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