269 D9. Recent Advances in Quaternary Geology and Geomorphology (Posters)
Wednesday, 12 October 2022
2:00 PM - 6:00 PM
Exhibit Hall F
FALLOUT RADIONUCLIDE CONCENTRATIONS IN CENTRAL AND WESTERN CUBAN RIVER SEDIMENT
Paper number: 269-18
Program: Technical Sessions
Time: 2:00 PM – 6:00 PM
Authors
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Rita Y. Sibello HernándezCienfuegos
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Alejandro García MoyaCienfuegos
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Hector A. Cartas AguilaCienfuegos
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Aniel Guillén ArruebarrenaCienfuegos
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Amanda H. SchmidtOberlin College, Oberlin, OH
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Paul R. BiermanUniversity of Vermont, Burlington, VT
Abstract
Western Cuba sediments show a marked difference between the nuclide concentration of fine and coarse grained sediments. While fine grained sediments from western Cuba had the highest mean activities for the samples studied, none of the coarse-grained samples had any detectable Be-7, and few of the coarse grained samples (2 out of 18) had detectable Cs-137. Fine-grained samples from western Cuba had excess Pb-210 activities ranging from 3.3 to 167.1 Bq/kg (mean 43.6+/-37.6, 1 SD) and Cs-137 activities ranging from 2.3 to 7.7 Bq/kg (mean 4.3+/-1.5, 1 SD). Coarse grained sediment from western Cuba had excess Pb-210 activities ranging from 0.2 to 37.8 Bq/kg (mean, 6.8+/-8.4, 1SD). Cs-137 activities ranged from 1.1 to 1.5 Bq/kg (mean 1.3+/-0.3, 1 SD). Thus far, we find no correlation (R2 < 0.45) between the activities of the fallout radionuclides and factors such as slope, average rainfall, elevation, and land use type.
It appears that erosion over the past decades, the time frame for which excess Pb-210 and Cs-137 are most sensitive, is more rapid and/or deeper in central than western Cuba. Higher frequency of detectable excess Pb-210 may indicate slowing of erosion over the past decades. Furthermore, low to undetectable concentrations of Cs-137 may suggest channel bank erosion. Our ongoing research investigates which, if any, environmental factors are related to this difference.
Geological Society of America Abstracts with Programs. Vol. 54, No. 6
doi: 10.1130/abs/2022AM-383895
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