Geothermal prospecting with Shallo‐Temp surveys
The Shallo‐Temp® survey is an inexpensive and rapid “first look” geophysical technique that is useful in planning the more traditional and costly reconnaissance drilling geothermal exploration programs. The technique is based on making many soil temperature measurements at 2-m depths over a given exploration area and correcting these measurements for the effects of elevation and surface geologic and meteorologic conditions. Corrections for surface conditions are made with an “annual wave correction model.” The output from the model is the normally expected 2-m temperature for the given site at the date for which input data were provided. The difference between the measured and computed 2-m temperature data represents effects of geothermal heat flow. A Shallo‐Temp residual map is compared both to a 2-m temperature map for a specific date (September, 1977) and to a mean annual 2-m temperature map for the Coso known geothermal resource area producing the same anomaly pattern in each case. Additional case history studies at Upsal Hogback in Nevada, and Animus Valley in New Mexico provide evidence to support the applicability of the Shallo‐Temp technique throughout the Basin and Range Province. The technique developed is not designed to replace reconnaissance drilling but rather help focus standard reconnaissance programs. The two potentially most reliable applications of the technique are in extending trends where standard reconnaissance holes have been drilled or filling in detail between widely spaced holes, and in surveying for near‐surface anomalies that might be developed for direct heating applications. ®Registered trademark of LeSchack Associates, Ltd.