Abstract
Field incubations of litter (01 and 02 layers) and A horizon soil utilizing S-labeled inorganic sulfate were conducted during July 1985 in an eastern white pine and a hardwood forest. Samples were assayed for the capacity to form S-labeled organic S, and in most cases these capacities were very similar to those determined in corresponding laboratory incubations. The A horizon soils from both water sheds formed approximately 3.0 nmol of organic S g-1 dry weight of sample during 2-d field or laboratory incubations. No substantial increase in this amount was observed after 7-d field incubations. Intrinsic S fractions of samples were quantified prior to and following field incubations, and organic S represented the majority of the total S in all cases. Sulfonate S and nonphosphate extractable ester sulfate were the largest organic S pools. Additional study results are discussed.
Original language | English (US) |
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Pages (from-to) | 1478-1483 |
Number of pages | 6 |
Journal | Soil Science Society of America Journal |
Volume | 52 |
Issue number | 5 |
DOIs | |
State | Published - 1988 |
ASJC Scopus subject areas
- Soil Science