B. Chen et al., NATURE OF THE HCL-SOLUBLE SULFATE IN THE SEQUENTIAL EXTRACTION FOR SULFUR SPECIATION IN SOILS, Fresenius' journal of analytical chemistry, 357(7), 1997, pp. 941-945
Thirty soils collected from different regions of China were used to in
vestigate the nature of HCl-soluble sulfate (HCl-S) and to evaluate th
e importance of HCl-S for sulfur speciation in soils. The soils were f
irst extracted with NaH2PO4 solution to remove water-soluble and adsor
bed sulfate, followed by extraction in 1 mol/l HCl at room temperature
, minimizing the hydrolysis of organic sulfur into sulfate. Excellent
linear correlations (r = 0.986) were found between the HCl-S and the c
arbonate contents in these soils, indicating HCl-S was mainly the carb
onate-occluded inorganic sulfate in calcareous soils, averaging for 39
% of total sulfur. However, the traditionally recog nized major form o
f soil sulfate (water-soluble and adsorbed sulfate) only account for 7
.5% of total sulfur. The non-calcareous soils were also found to conta
in some of HCl-S (6.9% of total sulfur). Large errors will occur in th
e determination of ester sulfur if HCl-S is not subtracted from the HI
-reducible sulfur, especially in calcareous soils and soils containing
little organic matter, which was the common practice in sulfur specia
tion studies. The reasonableness of including HCl-S in the subtraction
method to determine ester sulfur was further verified by the good cor
relations between ester sulfur and organic carbon content in the soils
.