Interpretation of Ground Temperature Anomalies in Hydrothermal Discharge Areas
Autor: | Jerry P. Fairley, Cary R. Lindsey, A. N. Price |
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Rok vydání: | 2017 |
Předmět: |
Convection
010504 meteorology & atmospheric sciences Biot number Mineralogy Flux 010502 geochemistry & geophysics Thermal conduction 01 natural sciences Overburden Heat flux Heat transfer Geotechnical engineering Subsurface flow Geology 0105 earth and related environmental sciences Water Science and Technology |
Zdroj: | Water Resources Research. 53:10173-10187 |
ISSN: | 1944-7973 0043-1397 |
DOI: | 10.1002/2017wr021077 |
Popis: | Researchers have long noted the potential for shallow hydrothermal fluids to perturb near-surface temperatures. Several investigators have made qualitative or semi-quantitative use of elevated surface temperatures; for example, in snowfall calorimetry, or for tracing subsurface flow paths. However, a quantitative framework connecting surface temperature observations with conditions in the subsurface is currently lacking. Here, we model an area of shallow subsurface flow at Burgdorf Hot Springs, a rustic commercial resort in the Payette National Forest, north of McCall, Idaho USA. We calibrate the model using shallow (0.2 m depth) ground temperature measurements and overburden thickness estimates from seismic refraction studies. The calibrated model predicts negligible loss of heat energy from the laterally-migrating fluids at the Burgdorf site, in spite of the fact that thermal anomalies are observed in the unconsolidated near-surface alluvium. Although elevated near-surface ground temperatures are commonly assumed to result from locally high heat flux, this conflicts with the small apparent heat loss during lateral flow inferred at the Burgdorf site. We hypothesize an alternative explanation for near-surface temperature anomalies that is only weakly dependent on heat flux, and more strongly controlled by the Biot number, a dimensionless parameter that compares the rate at which convection carries heat away from the land surface to the rate at which it is supplied by conduction to the interface. |
Databáze: | OpenAIRE |
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