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Chemical Properties and Mineralogical Characteristics of Selected Dredged Material
Author(s) -
Combs S. M.,
Dowdy R. H.,
Gupta S. C.,
Larson W. E.,
Gast R. G.
Publication year - 1982
Publication title -
journal of environmental quality
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.888
H-Index - 171
eISSN - 1537-2537
pISSN - 0047-2425
DOI - 10.2134/jeq1982.00472425001100020022x
Subject(s) - cation exchange capacity , environmental chemistry , soil water , illite , leaching (pedology) , organic matter , kaolinite , sediment , manganese , lessivage , cadmium , clay minerals , chemistry , environmental science , soil ph , entisol , mineralogy , geology , soil science , paleontology , organic chemistry
Transporting dredged spoils inland for use in reconditioning adjacent lands marginally suited for agricultural production may be an attractive alternative to other disposal practices. The objective of this study was to evaluate dredged materials (DM) by determining the elemental content and mineralogical characteristics of 10 freshwater and estuarine DM from eastern and central U.S. waterways. Dredged materials ranged from very acidic (pH ≤ 4.7) to alkaline (pH ≥ 7.4) in reaction. Acidity was attributed to S 2− and/or Fe 2+ oxidation resulting when initially reduced sediments were exposed to aerobic conditions. Dredged materials had cation exchange capacity values that ranged from 1.0 to 33.5 meq/100 g. Organic matter contents (5.9–22.5%) accounted for approximately 60% of the variation in the exchange capacity of fine‐textured DM. Total N was mainly in organic forms and C/N ratios ranged from 13:1 to 22:1. Dredged materials exhibited variable accumulations of nutrients and metals reflecting varying degrees of waterway contamination. The levels of Al, Ca, K, Mg, P, and S were generally higher in DM than in reference Minnesota soils. Cadmium, Cr, Ni, Pb, and Zn concentrations in DM were 2 to 6 times, and Cu 20 times, those observed in the reference soils. Manganese concentrations were substantially less in DM than in the soils. Mineralogy varied with geographical location, contributing watershed, and environmental conditions. All DM contained kaolinite and illite. Amounts of montmorillonite varied because of some conversion to pedogenic chlorite during rapid leaching conditions of sediment drainage. Crystalline Fe 2 O 3 was associated with DM clay fractions, indicating precipitation of colloidal‐sized hydrous oxide particles and/or surface coatings on clay complexes.