“…As we know today there are four different crystalline polymorphs of iron(III) oxide [1,2]: a-Fe203, naturally occurring as hematite, showing a rhombohedrally centered hexagonal structure of a corundum type (space group R3c); /3-Fe203 having a body-centered cubic "bixbyite" structure (space group Ia3); 7-Fe203, known as maghemite, with a cubic spinel structure; and r exhibiting an orthorhombic structure (space group Pna21). Maghemite, a red-brown magnetic material that is structurally similar with magnetite and has the same chemical composition as hematite, is the most important and prosperous phase out of the above mentioned polymorphs because it is widely used in a plenty of applications such as magnetic pigments in recording and information-storage media [3,4], in catalysis [5], *) Presented at International Colloquium "M6ssbauer Spectroscopy in Materials Science", V~emina, Czech Republic, June 1-4, 2004. magnetic fluids [6], anticorrosion protective paints [7], gas sensors [8], magnetooptical devices [9] and in studies of macroscopic quantum tunneling effect [10]. It is also worthwhile to mention that maghemite has been found effective as an imageintensifying agent for nuclear magnetic resonance imaging [11], in bioprocessing [12], magnetic separations [13], magneto-caloric refrigeration [14], medical diagnosis [15], controlled drug delivery [16] and magnetic-induced cancer therapy [17].…”