Reports by Jürgen Thieme

	Relationships between the speciation of sulfur and iron in oxic and anoxic soils and soil aggregates as revealed by synchrotron-based X-ray spectromicroscopy.
	The Colloidal Structure of Soils--Characterized by X-ray Spectromicroscropy.
	The speciation of sulfur in bulk soil differs from the S speciation in humic acid, fulvic acid, and most particle size fractions.