期刊
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL
卷 65, 期 3, 页码 787-794出版社
SOIL SCI SOC AMER
DOI: 10.2136/sssaj2001.653787x
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Different extractants have been used to determine sulfur availability in tropical soils. Due to variability in their composition, different soil S fractions are solubilized and taken up differentially by plants. We studied the dynamics of S fractions in tropical Oxisols, in the presence and absence of liming, over five consecutive harvests of sorghum [Sorghum bicolor(L.) Moench], Fourteen soil samples (0-20 cm) with differing levels of S adsorption capacity (SAC) were characterized for the following S fractions: S-s = ignition of a soil-sodium bicarbonate mixture; S-a = S available in NH4OAc (0.5 M) and HOAc (0.25 M); S-c = S available in CaCl2 (0.01 M); S-p = S available in Ca(H2PO4)(2) (500 mg P L-1 in 2.0 M HOAc); and S-r = S-s - S-a, Combined soil-root-shoot results indicate the existence of a shortterm labile organic fraction and a second more recalcitrant organic fraction, In soils with low and medium SAG, the labile organic fraction drives short-term S availability. In high-SAG soils, the mineral fractions became the main drivers of S availability, Soil SAC strongly affected the exractant predictive potential For long-term S availability. In low-SAG soils, S availability was best correlated with the S-c fraction. In medium-SAG soils, the best predictive capacity was also associated with the S-c fraction, followed by the S-a fraction, Conversely in high-SAG soils, S availability was best correlated with the S-a fraction, followed by the S-p Fraction. No single S-extraction procedure appears well suited to predicting long-term S availability across the range of soils studied.
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