Metadata
Author: WikiMatrix
Data
English[en]
The ferromagnetism which is widely observed in pyrrhotite is therefore attributed to the presence of relatively large concentrations of iron vacancies (up to 20%) in the crystal structure.
Spanish[es]
El ferromagnetismo que se observa ampliamente en la pirrotina se atribuye por tanto a la presencia de concentraciones relativamente grandes de vacantes de hierro (hasta un 20%) en la estructura cristalina.