Abstract
The present study develops a previously suggested physico-chemical theory, according to which the regular structure of planetary and satellite systems is explained on the basis of notions regarding periodic condensation of gaseous matter in space and time during formation of the centre body. The author examines specific chemical transformation models that may have been determinative factors in the formation of primary rings of planetary systems. A simplified model is based on the concept that condensed iron compounds, which formed as a result of reactions between the protocloud (protodisk) matter and iron carbonyl hydrides diffusing from the neighbourhood of the centre body, were essentially the primary ring embryos. A concept has been suggested according to which optically active substances (stereoisomers) can form in protoplanetary clouds in the magnetic and gravitational fields of centre bodies.
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