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Distribution and provenance of trace elements in Gulf of Mexico sediments

Conference · · Am. Assoc. Pet. Geol., Bull.; (United States)
OSTI ID:6533907

By knowing the dispersion patterns of river-borne sediments in marine environments, one can predict the spatial distribution of selected minerals, elements, and particle-bound pollutants. One potentially useful method for determining sediment pathways is by contouring selected trace metals in the sediment seaward of the river outflow. Using computer techniques involving trend surface analysis and a massive data set, the authors have contoured the regional distribution of chromium, copper, iron, nickel, and lead in surficial sediments from the Gulf of Mexico. Spatially, these metals range from very low concentrations in the sediments of the west Florida shelf to highest values on the Mississippi delta and along portions of the south Texas shelf. Intermediate concentrations are interspersed between these areas. Observed contour patterns are referenced to suspended matter trace metal data for the Apalachicola, Mobile, Mississippi, Brazos, and Rio Grande Rivers to determine sediment-metal provenance and thus infer river dispersal patterns. Statistical treatment of the trace metal and sediment data was also carried out to identify the important geochemical variables (grain-size, carbonate content, and clay mineralogy) that control the observed sediment trace metal patterns.

Research Organization:
Florida Inst. of Technology, Melbourne
OSTI ID:
6533907
Report Number(s):
CONF-8310301-
Journal Information:
Am. Assoc. Pet. Geol., Bull.; (United States), Journal Name: Am. Assoc. Pet. Geol., Bull.; (United States) Vol. 67:9; ISSN AAPGB
Country of Publication:
United States
Language:
English