Permafrost, heat flow, and the geothermal regime at Prudhoe Bay, Alaska
| Autor: | John H. Sass, Arthur H. Lachenbruch, B.V. Marshall, T. H. Moses |
|---|---|
| Rok vydání: | 1982 |
| Předmět: |
Atmospheric Science
Soil Science Aquatic Science Oceanography Permafrost Geochemistry and Petrology Earth and Planetary Sciences (miscellaneous) Geomorphology Geothermal gradient Sea level Earth-Surface Processes Water Science and Technology geography geography.geographical_feature_category Ecology Continental shelf business.industry Geothermal energy Paleontology Forestry Thermal conduction Geophysics Arctic Heat flux Space and Planetary Science business Geology |
| Zdroj: | Journal of Geophysical Research. 87:9301 |
| ISSN: | 0148-0227 |
| DOI: | 10.1029/jb087ib11p09301 |
| Popis: | Temperature measurements through permafrost in the oil field at Prudhoe Bay, Alaska, combined with laboratory measurements of the thermal conductivity of drill cuttings permit an evaluation of in situ thermal properties and an understanding of the general factors that control the geothermal regime.A sharp contrast in temperature gradient at approx.600 m represents a contrast in thermal conductivity caused by the downward change from interstitial ice to interstitial water at the base of permafrost under near steady state conditions. Interpretation of the gradient contrast in terms of a simple mode for the conductivity of an aggregate yields the mean ice content (approx.39%), and thermal conductivities for the frozen and thawed section (8.1 and 4.7 mcal/cm s /sup 0/C, respectively). These results yield a heat flow of approx.1.3 HFU, which is similar to other values on the Alaskan Arctic Coast; the anomalously deep permafrost is a result of the anomalously high conductivity of the siliceous ice-rich sediments. Curvature in the upper 160 m of the temperature profiles represents a warming of approx.1.8 /sup 0/C of the mean surface temperature and a net accumulation of 5--6 kcal/cm/sup 2/ by the solid earth surface during the last 100 years or so. Rising sea levelmore » and thawing of ice-rich sea cliffs probably caused the shoreline to advance tens of kilometers in the last 20,000 years, inundating a portion of the continental shelf that is presently the target of intensive oil exploration. A simple conduction model suggests that this recently inundated region is underlain by near-melting ice-rich permafrost to depths of 300--500 m; its presence is important to seismic interpretations in oil exploration and to engineering considerations in oil production. With confirmation of the permafrost configuration by offshore drilling, heat conduction models can yield reliable new information on the chronology of arctic shorelines.« less |
| Databáze: | OpenAIRE |
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