2011
DOI: 10.1088/1742-2132/8/2/010
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A new look at the statistical assessment of approximate and rigorous methods for the estimation of stabilized formation temperatures in geothermal and petroleum wells

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Cited by 22 publications
(14 citation statements)
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“…As for the regression models, results showed that SFT values estimated by using an ordinary linear regression model were less than those by the quadratic regression model in Figure 5. This observation was also reported in other literature [16,17].…”
Section: Applications In the Case Of A Small Number Of Data Pointssupporting
confidence: 91%
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“…As for the regression models, results showed that SFT values estimated by using an ordinary linear regression model were less than those by the quadratic regression model in Figure 5. This observation was also reported in other literature [16,17].…”
Section: Applications In the Case Of A Small Number Of Data Pointssupporting
confidence: 91%
“…The general equation of the OLD model is: y = a + bx , where a and b are the intercept and the slope of the fitted straight line [16], while that for the QR model is given by: y = a + bx + cx 2 , where a, b, and c represent the polynomial coefficients [16].…”
Section: Selection Of the Regression Modelsmentioning
confidence: 99%
“…This well had a depth of 50 m, with purely conductive thermal behavior ( Figure 5). For an estimation of the natural geothermal gradient, the bottom-hole temperature (BHT) versus time measurements to different depths was registered after a borehole drilling operation [18,19], and the Horner-plot method (Equation (1)) was used to estimate the static formation temperature (SFT) to a 50-m depth. This method suggests a linear relationship between BHT measurements and the dimensionless Horner time that corresponds to the logarithmic function of the following equation: For the present study, W1 (Figures 4 and 5) was used as a low-enthalpy geothermal energy source for heating water up to 55 °C in a U-tube heat exchanger (HE).…”
Section: Geothermal Source Modelingmentioning
confidence: 99%
“…For an estimation of the natural geothermal gradient, the bottom-hole temperature (BHT) versus time measurements to different depths was registered after a borehole drilling operation [18,19], and the Horner-plot method (Equation (1)) was used to estimate the static formation temperature (SFT) to a 50-m depth. This method suggests a linear relationship between BHT measurements and the dimensionless Horner time that corresponds to the logarithmic function of the following equation: For an estimation of the natural geothermal gradient, the bottom-hole temperature (BHT) versus time measurements to different depths was registered after a borehole drilling operation [18,19], and the Horner-plot method (Equation (1)) was used to estimate the static formation temperature (SFT) to a 50-m depth. This method suggests a linear relationship between BHT measurements and the dimensionless Horner time that corresponds to the logarithmic function of the following equation:…”
Section: Geothermal Source Modelingmentioning
confidence: 99%
“…Andaverde et al (2005) and Espinoza‐Ojeda et al (2011) estimate equilibrium formation temperatures from measured BHTs by linear and quadratic regression modelling. Both studies find that in a majority of the analysed cases, the relationship between the BHT data and the formation temperature is non‐linear.…”
Section: Theorymentioning
confidence: 99%