HAL Id: jpa-00214066
https://hal.archives-ouvertes.fr/jpa-00214066
Submitted on 1 Jan 1971
HAL is a multi-disciplinary open access archive for the deposit and dissemination of sci- entific research documents, whether they are pub- lished or not. The documents may come from teaching and research institutions in France or abroad, or from public or private research centers.
L’archive ouverte pluridisciplinaire HAL, est destinée au dépôt et à la diffusion de documents scientifiques de niveau recherche, publiés ou non, émanant des établissements d’enseignement et de recherche français ou étrangers, des laboratoires publics ou privés.
STRESS-INDUCED MAGNETIZATION
D. Craik, R. Fairholme
To cite this version:
D. Craik, R. Fairholme. STRESS-INDUCED MAGNETIZATION. Journal de Physique Colloques,
1971, 32 (C1), pp.C1-681-C1-683. �10.1051/jphyscol:19711238�. �jpa-00214066�
JOURNAL DE PHYSIQUE Colloque C 1, supplbment au no 2-3, Tome 32, Fbvrier-Mars 1971, page C 1 - 681
STRE S S-INDUCED MAGNETIZATION
D. J. CRAIK and R. J. FAIRHOLME (*)
University, Nottingham (*) Novo a t Plessey Research Laboratories, Caswell, England
RbsumB. - Les courbes d'aimantation de forme complexe sont obtenues en appliquant des contraintes des ferro- magnktiques soumis a de faibles champs de pulsation. Un ensemble consbquent de donnkes est dkcrit en termes de para- metres-empiriques et de courbes caractkristiques rendant compte des rotations des mouvements irrkversibles de parois et de transformations compl~tes des domaines. L'observation des domaines et des cycles de contraintes permettent les interprktations.
Abstract. - M-a curves of complex form are obtained on applying stresses to ferromagnetics in small bias fields.
A large amount of data is described in terms of empirical parameters and characteristic curves, the explanations of which involve rotations, irreversible wall motion and complete transformations of the domains. Domain observations and stress cycling aid the interpretations.
1. Introduction. - The application of tensile or compressive stresses to ferromagnetic materials in small bias fields can cause large changes in magnetiza- tion. The bias fields referred to are generally such as t o induce only a low level of magnetization compared with that induced by the subsequent application of the stress, but no consistent stress-induced changes are observed in the complete absence of a bias field. The coupling between the stress and magnetization is magnetostrictive and the stresses can be equated to effective fields using the magnetostriction coefficients of the materials concerned. Craik and Wood [l]
illustrated the complexity of the magnetization-stress (M-o) curves for substantial stresses still below the elastic limit, and gave references to earlier work. In the present paper an attempt is made to classify the types of M-o curve which may be obtained for a wide range of materials, and empirical parameters are introduced to aid comparison of the response of different materials.
The effects of repeated stress cycling also help to elucidate the underlying mechanisms.
2. Method of measurement. - The important fea- tures of the measurements are that they are made on thin strips, with low demagnetizing factors, fitting into
Material - Ni
85/15 NiFe 8211 8 NiFe 80120 NiFe 70130 NiFe 50150 NiFe Mild steel
Random 3 % SiFe Cube 3 % SiFe Single 3 % SiFe Mumetal Hard steel Cobalt
M-0 sequence
-
? (9 (iii) (iv) (iv) - (iv) (iv) (iv) (iv) -
?
a yoke and with compensation for residual demagne- tizing fields. This avoids variable demagnetizing effects but involves the necessity for high sensitivity measure- ments of the magnetization changes. A voltage-to- frequency converter with effective microvolt sensitivity was used to integrate the voltages induced in a coil around the specimen, giving AB = 1 gauss or AM = 0.08 e. m. u. detectable for an iron specimen with 0.05 cm2 section. Specimens were ac demagne- tized before applying the bias field and stresses. The earth's field was annulled.
3. Classification of M-o curves. - On applying a stress the magnetization rises and may approach a steady value or even pass through a maximum and fall once more. On removing the stress M may rise further or fall.
Behaviour of the two most extreme types can be conveniently specified in terms of the magnetization induced by the bias field alone, M,, the stress-induced remanent magnetization Mtr or Mc, for tension and compression respectively, the maximum induced magnetization with o increasing, Mtm or Mcm, and the stress otm or o,, at which this occurs. This data is outlined in table 1 for all the specimens measured.
Compression
M-0 sequence
-
(iv) (iv) (iv)
?
(9 (i) (iii) (iii) (iii) (iii) (i) ?
Tension
Article published online by EDP Sciences and available at http://dx.doi.org/10.1051/jphyscol:19711238
C 1 - 682 D. J. CRAIK, R. J. FAIRHOLME Description is complicated by the dependence of the
form of the results on the peak value of the total effec- tive field (bias field and equivalent stress field) attai- ned. Four sequences appear t o arise for various mate- rials, in terms of increasing fields (Fig. 1). All thevarious
FIG. 1. - Characteristic sequences of M-s curves for differing peak stresses. The origin in these is the magnetization induced by the bias field alone. Table 1 shows which materials exhibit
each type or sequence of curves.
types of M - o curves are incorporated in these sequences and the sequence applicable to each material shown in table 1. The first two sequences are characterised by an approach to a limiting value of M, and indeed (i) is very similar to a family of magnetization-field curves. (iii) and (iv) are jointly distinguished by the onset of a peak value of M at high values of o and distinguished from each other by the shape of the curves with decreasing a and the magnitude of the dip in (iv) which may extend to the demagnetized state.
(ii) might be considered as a special case of (iv) : for materials giving this type of result no value of o will produce a maximum M with subsequent decrease, at low bias fields, but increasing the bias field may give results characterised by (iv).
Sequence (i) applies to materials where simple considerations of the magneto-elastic and anisotropy torques suggest that the results can be regarded as indicating large rotations in an effective field H, = 3 Aa/2 Ms. This corresponds well with the general appearance of the curves, with irreversibility due to rotational hysteresis.
Sequences (iii) and (iv) apply to materials with negli- gible rotation (lo 4 K,). It was natural to associate this behaviour with movement of domain walls.
Sequence (iii) may be explained using an extended form of Brown's theory [l, 21 with the smoothing effect of 1800 walls. In sequence (iv) the initial increase in the magnetization is followed by a complete break- down in the domain structure as observed by Bates and Carey 13, 41. Using the longitudinal Kerr effect it
was possible to confirm (Fig. 2)Xthat domains magne- tized normal to the strip axis (i. e. the direction in which the bias field and stress were applied) gradually replaced those parallel to the field axistas the turnover and decrease in M occurred. Clearly, with all 1800 domains normal to the strip axis the measured magne- tization must be zero.
It is of considerable interest to note that while our observations of the domain rearrangement, and those of Bates and Carey, were made on singly-oriented and
FIG. 2. -Domains in SiFe (Kerr effect) related to the M-a curve.
cube-textured silicon iron respectively this rearrange- ment must now be considered a very common pheno- menon (in mild steel, nickel and some NiFe alloys) unless an alternative explanation of the type (iv) sequence can be put forward.
4. Stress cycling. - A basic feature of the mecha- nism, which leads to the stress-induced remanence,
Q 4 t . P 40
a o r
complete cycles
b)
S t r e s s c y c l e s ottersnhys t e r e t i r d e m ~ ~ n e t i s a t i o n
6 (%/mme'