کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
617642 | 1455002 | 2013 | 6 صفحه PDF | دانلود رایگان |

Fretting experiments with an austenitic pin on a martensitic disc were performed. X-ray diffraction revealed that a part of the austenite pin was transformed into a martensite layer. The martensite is covered by a layer of Fe–Cr–Ni oxides, detected by the Mössbauer spectroscopy. Martensite and Fe-oxide, originating from the spinel structure, were identified in the debris powder. Obtained results indicate that the crystal structures of the Fe-oxides produced during fretting are highly defected. This is the cause of the observed superparamagnetic properties, broad diffraction maxima, and differences between predicted and observed Bragg spot intensities.
► We report formation of the martensite layer on the austenitic pin.
► Spinel type oxides are formed during the fretting wear.
► Superparamagnetic behaviour of oxides was detected by Mössbauer spectroscopy.
► Highly defected crystalline phases were identified.
► Hematite is not dominating phase of debris.
Journal: Wear - Volume 300, Issues 1–2, 15 March 2013, Pages 90–95