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Among the radioactive wastes associated with the nuclear fuel cycle, UMT are unique in terms of their volume and their limited isolation from the surficial environment.
The study focuses on an area surrounding a pumping well penetrating the deep aquifer and impacting its piezometric level, where infiltration from the surficial aquifer can be more harmful.
Furthermore, the excessive pumping from the surficial aquifer as well as the reduced surface water inflow into BGF due to the dam constructed on Ilica Creek intensify the detrimental effects of this contamination.
Four maps, including three different flood hazard assessments of Ivanpah Valley, NV, were compared: (i) a regulatory map prepared by FEMA, (ii) a soil survey map prepared by NRCS, (iii) a surficial geologic map, and (iv) a flood hazard map derived from the surficial geologic map, both of which were prepared by NBMG.
First, Fe2+ was abruptly removed from the surficial porewaters at the onset of the tide change, before ΣH2S appeared in the sediment layers.
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This map is Plate 6 from Kerhin, R.T., "The Surficial Sediments of Chesapeake Bay, Maryland: Physical Characteristics and Sediment Budget".
This map is Plate 7 from Kerhin, R.T., "The Surficial Sediments of Chesapeake Bay, Maryland: Physical Characteristics and Sediment Budget".
This map is Plate 5 from Kerhin, R.T., "The Surficial Sediments of Chesapeake Bay, Maryland: Physical Characteristics and Sediment Budget".
The results of the study presented in this paper show that coupled analysis (considering swelling) leads to different suction (negative pore water pressure (PWP)) and FS profiles within the surficial layer from those resulting from uncoupled analysis at the same elapsed time.
From this comparison, we infer that the surficial layer strongly influences spectral acceleration values between 0.1 and 1 s.
The color of the surficial sediments varied from orange/yellow, white, and gray.
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