Mt. Todinov, MECHANISM FOR FORMATION OF THE RESIDUAL-STRESSES FROM QUENCHING, Modelling and simulation in materials science and engineering, 6(3), 1998, pp. 273-291
On the basis of the notion of 'strain shift induced by quenching' a co
ntinuum model is proposed to provide mechanistic insight into the form
ation of the residual stresses from quenching. An equation has been de
rived stating that for a homogeneous quenched body the residual elasti
c strain of each elemental volume is equal to the difference in the am
ount of plastic strain generated by the alternating odd and even strai
n shifts. Despite the widespread view, plastic yielding is neither nec
essary nor sufficient for the existence of residual stresses after que
nching. The proposed model successfully rationalized the results from
the computer simulations and the residual stress patterns after oil an
d water quenching of decarburized and non-decarburized cylindrical ste
el specimens. If the net plastic strain (the difference in the amount
of plastic strain during the first and second strain shift) created in
the thermal contraction region is greater than the net plastic strain
created in the transformation region the axial residual stress at the
surface of a quenched cylindrical specimen is compressive. The magnit
ude of the transformation stresses generated is inversely proportional
to the width of the transformation temperature interval. It is establ
ished that the thermal stresses during quenching raise the martensite
start temperature of the surface. An equation and a numerical model ha
ve been derived for determining the shift of the martensite start temp
erature caused by thermal stresses of large magnitude.