DISTRIBUTION OF RADIOACTIVITY AND RADIOGENIC HEAT PRODUCTION ACROSS THE SEDIMENTARY BASIN IN NEBRASKA, CENTRAL UNITED STATES
Drill cuttings were collected from 18 heat flow holes in Nebraska in the 1980's for thermal conductivity measurements. The locations were largely of the Northern, Northwestern and Eastern edges of Nebraska. Recently, these cuttings were combined stratigraphically, based on their radioactivity and depth. The cuttings were poured into pint sized containers, averaging 8-9 600 to 700 g containers per test hole. A total of 173 containers were created, all undergoing a gamma ray spectrometry analysis using a Ge-Li GRS. The eU and eTh were determined in ppm and the K in pct. This data was then used to calculate the heat production and heat flow present. Stratigraphic columns were created for each test hole, comparing the radioactive concentrations, heat production, as well as heat flow per depth, in order to show the variation and distribution across the state of Nebraska.
A total of 5 containers were of Paleozoic carbonate origin, averaging a heat production of 1.0 mW m-2. 35 were of a siliciclastic Mesozoic origin, yielding an average of 1.4 mW m-2. Lastly, 28 were of a Cenozoic siliciclastic origin, with an average heat production of 1.4 mW m-2, respectively. The abundance and variation was largely influenced by the age and sequence of deposition, however, they do not correlate to any geophysical anomalies in Nebraska. This variability shows that further research is needed in accordance to radioactivity in sedimentary basins.