GEOLOGIC AND GEOCHEMICAL ASPECTS OF GROUND SOURCE HEAT PUMP WELL DESIGN, BOSTON, MA
Three test wells were drilled in the Cambridge Argillite. The first two deviated considerably from vertical, and were not considered acceptable for thermal load testing or full scale operation.
The third test well, drilled using a different method, was advanced to approximately 1,200 feet and was sufficiently vertical to be used in subsequent testing. Groundwater temperature ranged from 55o F near the ground surface, to 62o F at 1,150 feet. Geophysical logging did not indicate significant fractures, consistent with the observed 5 to 10 gpm well yield.
Geophysical logging and drill cuttings indicated thin sandstone and diabase intervals throughout the borehole. Drilling behavior indicated softer rock at 1,160 to 1,180 feet, which resulted in an unstable collapsing borehole. The softer rock was identified as altered volcanic ash based on observation of the cuttings and a review of the USGS description of the Cambridge Argillite.
Groundwater samples from 300, 600, 900 and 1,100 feet indicated concentrations of chloride, sulfate, sodium, calcium and magnesium increased significantly from 900 and 1,100 feet, consistent with geophysical data. Iron concentrations are high enough to cause significant precipitation problems if the water is aerated.
The well’s thermal properties, thermal conductivity (keff) and thermal diffusivity (αeff), were estimated using the data from the thermal load test and the Line-Source Approximation method. The estimated values were somewhat lower than expected based on values in the literature.