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Therefore, the groundwater temperature will affect the COP value.
Groundwater temperature is a direct indicator of geothermal influence.
The groundwater temperature ranges from 26 to 30 °C.
There is inherent uncertainty in groundwater temperature measurements.
This study evaluated groundwater temperature data obtained from 266 Korean national groundwater monitoring stations.
It was employed to estimate the sub-surface groundwater temperature and the corresponding depth of groundwater.
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Sensitivity analyses showed that input groundwater temperatures ≤ 17 °C produced meromictic conditions, whereas groundwater temperatures ≥ 17 °C produced holomictic conditions.
This study was based on natural groundwater temperatures.
Figure 7 Measured and computed underground and groundwater temperatures.
Groundwater temperatures vary from 26 to 29 °C (average of 27.5 °C).
The distribution pattern for the groundwater temperatures is most similar to that of the air temperature.
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