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Table 1 The fitting equations of each curve in Fig. 4

From: Optimized geothermal energy extraction from hot dry rocks using a horizontal well with different exploitation schemes

IPS

[Model A, water]

[Model A, SCCO]

[Model B, water]

[Model B, SCCO]

Tb (°C)

    

74

ηs = 0.1832 Tin + 65.375 (R2 = 0.987)

ηs = 0.1470 Tin + 69.375 (R2 = 0.999)

ηs = 0.2771 Tin + 44.066 (R2 = 0.999)

ηs = 0.1714 Tin + 61.205 (R2 = 0.999)

92

ηs = 0.1371 Tin + 68.576 (R2 = 0.997)

ηs = 0.0913 Tin + 73.948 (R2 = 0.999)

ηs = 0.1771 Tin + 50.580 (R2 = 0.999)

ηs = 0.1040 Tin + 65.787 (R2 = 0.998)

104

ηs = 0.1001 Tin + 71.502 (R2 = 0.992)

ηs = 0.0530 Tin + 77.576 (R2 = 0.983)

ηs = 0.1300 Tin + 54.421 (R2 = 0.999)

ηs = 0.0804 Tin + 68.681 (R2 = 0.999)

116

ηs = 0.0830 Tin + 73.167 (R2 = 0.988)

ηs = 0.0502 Tin + 79.456 (R2 = 0.998)

ηs = 0.1056 Tin + 57.013 (R2 = 0.999)

ηs = 0.0591 Tin + 70.839 (R2 = 0.999)

146

ηs = 0.0390 Tin + 77.263 (R2 = 0.989)

ηs = 0.0328 Tin + 81.646 (R2 = 0.995)

ηs = 0.0473 Tin + 60.900 (R2 = 0.999)

ηs = 0.0364 Tin + 73.328 (R2 = 0.997)

200

ηs = 0.0335 Tin + 79.173 (R2 = 0.952)

ηs = 0.0259 Tin + 84.373 (R2 = 0.939)

ηs = 0.0424 Tin + 64.508 (R2 = 0.999)

ηs = 0.0316 Tin + 74.385 (R2 = 0.980)