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Table 9 Statistical metrics used for evaluating the prediction efficiency of gas geothermometers (new and existing)

From: GaS_GeoT: A computer program for an effective use of newly improved gas geothermometers in predicting reliable geothermal reservoir temperatures

Statistical metric

Calculation equation

Equation number

Reference

Percent difference (DIFF%)

\(DIFF\% = \left[ {\left( {\frac{{BHT_{CALC\left( i \right)} - BHT_{m\left( i \right)} }}{{BHT_{m\left( i \right)} }}} \right) \times 100} \right]\)

(6)

García-López et al. (2014)

Root mean square error (RMSE)

\(RMSE = \sqrt{{\frac{1}{n}\mathop \sum \limits_{i = 1}^{n} \left( {BHT_{m\left( i \right)} - BHT_{CALC\left( i \right)} } \right)^{2} }}\)

(7)

Willmott et al. (2009)

Mean absolute error (MAE)

\(MAE = \frac{1}{n}\mathop \sum \limits_{i = 1}^{n} \left| {BHT_{m\left( i \right)} - BHT_{CALC\left( i \right)} } \right|\)

(8)

Wang and Lu (2018)

Mean absolute percentage error (MAPE)

\(MAPE = \left( {\frac{1}{n}\mathop \sum \limits_{i = 1}^{n} \left| {\frac{{BHT_{m\left( i \right)} - BHT_{CALC\left( i \right)} }}{{BHT_{m\left( i \right)} }}} \right|} \right) \times 100\)

(9)

Li and Shi (2010)

Difference coefficient (Theil's U)

\(Theil^{\prime}s U = \frac{{\sqrt{{\mathop \sum \nolimits_{i = 1}^{n} \left( {BHT_{m\left( i \right) - } BHT_{GaS\_GeoT\left( i \right) } } \right)^{2} }}}}{{\sqrt{{\mathop \sum \nolimits_{i = 1}^{n} \left( {BHT_{m\left( i \right) - } BHT_{GasGeo\_Lit\left( i \right) } } \right)^{2} }}}}\)

(10)

Álvarez del Castillo et al. (2012)

  1. BHTm(i) is the bottom-hole temperature measured in a geothermal well; BHTCALC(i) is the temperature calculated by any gas geothermometer; BHTGaS_GeoT(i) is the temperature calculated by the new gas geothermometers (GasG1 to GasG8); BHTGasGeo_Lit(i) is the temperature calculated by the existing gas geothermometers (Table 3), and n is the total number of gas samples