Post-drilling destabilization of temperature profile in borehole Yaxcopoil-1, Mexico |
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| Authors: | Jan ?afanda Philipp Heidinger Helmut Wilhelm Vladimír ?ermák |
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| Institution: | (1) Geophysical Institute, Boční II/1401, 14131 Prague, Czech Republic;(2) Geophysical Institute, University Karlsruhe, Hertzstrasse 16, 76187 Karlsruhe, Germany |
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| Abstract: | As part of the International Continental Scientific Drilling Program (ICDP), the 1.5-km-deep borehole Yaxcopoil-1, located in the Chixculub meteor impact structure in Mexico, has undergone further study after drilling operations ceased. Temperature logs were repeated ten times at intervals 0.3–0.8, 15, 24 and 34 months after borehole shut-in. The logs bear a distinct signature of transient heat transfer by groundwater flow manifested by a gradual distortion of the linear temperature profile when a cold wave of 0.8–1.6°C amplitude was detected propagating downward from 145 to 312 m at a rate of 4–6 m/month. To understand the nature of this moving anomaly, a 20-day monitoring of the cold wave was carried out at a depth of 307 m that showed further cooling of 0.6°C during the first 16 days of the passage followed by temperature stabilisation. As an explanation of this unusual phenomenon, a theory is proposed, whereby the drilling mud has accumulated within the overlying and cooler highly porous and permeable karstic rocks during the drilling and migrates downward. The observed migration rate suggests a permeability higher than 10?11 m2. This indicates a high vulnerability to contamination of the only freshwater aquifer in the Yucatan region. |
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| Keywords: | Karst Yucatan Peninsula Thermal conditions Groundwater flow Hydraulic properties |
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