Effects of municipal solid waste compost and sewage sludge on chemical and spectroscopic properties of humic acids from a sandy Haplic Podzol and a clay loam Calcic Vertisol in Portugal

• Published in: Waste management (Elmsford) 2008-11, Vol.28 (11), p.2183-2191
• Main Authors: Pedra, Filipe, Plaza, César, Fernández, José M., García-Gil, Juan C., Polo, Alfredo
• Format: Article
• Language: English
• Subjects: Applied sciences; Elements; Exact sciences and technology; Humic Substances - analysis; Organic Chemicals - analysis; Other industrial wastes. Sewage sludge; Other wastes and particular components of wastes; Pollution; Portugal; Refuse Disposal - methods; Sewage; Soil - analysis; Spectroscopy, Fourier Transform Infrared; Urban and domestic wastes; Wastes; Water - analysis
• ISSN: 0956-053X; 1879-2456
• DOI: 10.1016/j.wasman.2007.09.031

The effects of amendment with municipal solid waste compost (MSWC) and anaerobically digested sewage sludge (SS) on the compositional and structural features of soil humic acids (HAs) were investigated. For this purpose, HAs were isolated from MSWC, SS, and two different Portuguese soils, a sandy Haplic Podzol and a clay loam Calcic Vertisol, which were either unamended or amended with MSWC or SS at a rate of 60 t ha −1. The isolated HAs were analyzed for elemental and acidic functional group composition, and by ultraviolet/visible, Fourier transform infrared (FT IR), and fluorescence spectroscopies. The application of MSWC and especially SS to soils determined an increase of C, N, H, and S contents and E 4/ E 6 ratios (i.e., ratios of absorbances at 465 and 665 nm), and a decrease of O, COOH, and phenolic OH contents and C/N, C/H, and O/C ratios of soil HAs. The FT IR and fluorescence results showed that the organic amendments, especially SS, caused an increase of the aliphatic character and a decrease of the degrees of aromatic polycondensation, polymerization, and humification of amended soil HAs. Both MSWC and SS affected more markedly the clayey soil HAs than the sandy soil HAs, possibly due to less extended mineralization processes and the protective action of clay minerals on amended soil HAs.