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Soil cation leaching by acid rain with varying nitrate-to-sulfate ratios

Journal Article · · J. Environ. Qual.; (United States)
OSTI ID:6004260
The influence of the anion composition of simulated acid rain on cation leaching of three soils with different surface-charge properties was examined. Four acid mixtures of H/sub 2/SO/sub 4/ and HNO/sub 3/, all with pH 3.5, but with varying NO/sub 3//sup -//SO/sub 4//sup 2 -/ mole ratios of 1.00:0.00, 0.75:0.25, 0.55:0.45, and 0.00:1.00, were used to leach an Ultic-Alfisol, and Oxisol, and an Entisol. The taxonomic names of these three soils are (i) Cornutt series: fine, mixed, mesic Ultic Haploxeralfs, (ii) unnamed Rhodustox, and (iii) Hanford series: coarse-loamy, mixed, nonacid, thermic Typic Xerorthents. The Alfisol had a high SO/sub 4//sup 2 -/ adsorption capacity because of its high Fe/sub 2/O/sub 3/ content of 12 g kg/sup -1/ and high point-of-zero charge (PZC) of 6.0. The Oxisol, although strongly weathered, had a lower Fe/sub 2/O/sub 3/ content of 5 g kg/sup -1/ and PZC of 4.5. The Entisol was a relatively unweathered soil derived from silicaceous alluvium, with even less Fe/sub 2/O/sub 3/ of 3 g kg/sup -1/ and a lower PZC of 3.5, and represented a soil of fixed charge. Cation leaching of the Alfisol varied directly with the NO/sub 3//sup -/ content of the leaching input due to the higher mobility of NO/sub 3//sup -/ compared with SO/sub 4//sup 2 -/ that was adsorbed. The relative NO/sub 3//sup -//SO/sub 4//sup 2 -/ contents of inputs had no effects on cation leaching of the Entisol. Effects on leaching of the Oxisol were intermediate between those of the Alfisol and Entisol.
Research Organization:
Univ. of California, Berkeley
OSTI ID:
6004260
Journal Information:
J. Environ. Qual.; (United States), Journal Name: J. Environ. Qual.; (United States) Vol. 13:3; ISSN JEVQA
Country of Publication:
United States
Language:
English