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- W2186805216 abstract "A thermal evolution study of the LV-3 geothermal well (depth: 2150 m) is presented. Such a study is based on wellbore temperature logs, transient temperature profiles (obtained from numerical modeling of the heat transfer processes during well drilling and shut-in) and fluid inclusion logging. Drilling and shut-in temperature profiles were predicted by use of a transient wellbore thermal simulator which considers conductive and convective heat transfer processes. Such a numerical simulation considered the LV-3 well geometry in the presence of fluid losses into the formation. Thus, numerical simulation enabled the drilling and shut-in thermal history of well LV-3 to be closely reproduced. Precision temperature logs from LV-3 well (at 402-m and 2000-m) provided information on the location of permeable zones intersecting the wellbore. Such permeable zones were partially identified at a wellbore depth of 400-m and more significantly between 1300-m and 1600-m. Microthermometric determinations on well cuttings and core samples containing veins filled with secondary minerals (epidote, quartz and calcite) were also carried out. Minimum homogenization temperatures ranging from 109 °C to 125 °C were measured in the first 920 m deep. Between 1830 m and 2150 m deep, the minimum homogenization temperatures ranged from 256 °C to 268 °C. Likewise salinity concentration ranges from 3.4 to 18.5 wt% as NaCl equivalent were found. Static formation temperatures were also computed by five analytical methods which are the most commonly used in the geothermal industry: the classical Horner plot, the improved Horner, the two-point method and the spherical-radial and cylindrical-radial heat flow models. A comparison among the wellbore temperature logs, the homogenization temperatures, and the transient temperature profiles is also presented." @default.
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- W2186805216 date "2000-01-01" @default.
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- W2186805216 title "THERMAL EVOLUTION STUDY OF THE LV-3 WELL IN THE TRES VIRGENES GEOTHERMAL FIELD, MEXICO" @default.
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