PHYSICAL REVIEW B 84, 184422 (2011)
Ferromagnetic transition and specific heat of Pr
0.6
Sr
0.4
MnO
3
S. R¨ oßler,
1,*
Harikrishnan S. Nair,
2
U. K. R ¨ oßler,
3
C. M. N. Kumar,
2
Suja Elizabeth,
4
and S. Wirth
1
1
Max Planck Institute for Chemical Physics of Solids, N¨ othnitzer Straße 40, D-01187 Dresden, Germany
2
J¨ ulich Centre for Neutron Sciences-2, Peter Gr¨ unberg Institute-4, Forschungszentrum J¨ ulich GmbH, D-52425 J¨ ulich, Germany
3
IFW Dresden, Postfach 270016, D-01171 Dresden, Germany
4
Department of Physics, C.V. Raman Avenue, Indian Institute of Science, Bangalore-560012, India
(Received 30 June 2011; revised manuscript received 20 October 2011; published 16 November 2011)
The critical properties of orthorhombic Pr
0.6
Sr
0.4
MnO
3
single crystals were investigated by a series of
static magnetization measurements along the three different crystallographic axes as well as by specific heat
measurements. A careful range-of-fitting-analysis of the magnetization and susceptibility data obtained from
the modified Arrott plots shows that Pr
0.6
Sr
0.4
MnO
3
has a very narrow critical regime. Nevertheless, the
system belongs to the three-dimensional (3D) Heisenberg universality class with short-range exchange. The
critical exponents obey Widom scaling and are in excellent agreement with the single scaling equation of state
M(H, ) =| |
β
f
±
(H/| |
(β+γ )
; with f
+
for T>T
c
and f
−
for T<T
c
. A detailed analysis of the specific heat
that account for all relevant contributions allows us to extract and analyze the contribution related to the magnetic
phase transition. The specific heat indicates the presence of a linear electronic term at low temperatures and a
prominent contribution from crystal field excitations of Pr. A comparison with data from literature for PrMnO
3
shows that a Pr-Mn magnetic exchange is responsible for a sizable shift in the lowest lying excitation.
DOI: 10.1103/PhysRevB.84.184422 PACS number(s): 75.47.Lx, 75.40.Cx
I. INTRODUCTION
Colossal magnetoresistive (CMR) oxides of the manganite
family with the generic formula R
1−x
A
x
MnO
3
(R = rare earth
ion, A = alkaline earth or equivalent ion) possess a complex
phase diagram that often includes charge order (CO)/orbital
order (OO), metal-insulator (MI) transitions, and various mag-
netic phases tunable as a function of composition, magnetic
field and/or temperature.
1–3
The physical properties of these
materials strongly depend on subtle structural distortions. The
composition Pr
0.6
Sr
0.4
MnO
3
, which forms the subject of this
paper, has been reported to constitute a ferromagnet with a
Curie temperature T
C
∼ 297 K.
4
Pr
0.6
Sr
0.4
MnO
3
also under-
goes a structural phase transition from a high-temperature
orthorhombic P nma to a low-temperature monoclinic I 2/a
space group which was reported to take place at T
str
∼ 100 K.
5
Powder neutron diffraction studies report structural phase
separation below T
str
.
5
Furthermore, the magnetization curves
(M-H ) measured below the structural transition temperature
are found to be anomalous: The virgin curve stays outside
the subsequent M-H hysteresis loops
6
thereby suggesting
that the structural phase separation has a profound influence
on the magnetic properties. Optical conductivity data
7
on
Pr
0.6
Sr
0.4
MnO
3
in applied magnetic field deviate from the
expected universal scaling. In particular, a nearly linear |M|
dependence of the magneto-optical conductivity in the critical
regime indicates strong ferromagnetic spin fluctuations of
Mn above T
C
.
7
The irreversible magnetization processes
related to the structural phase separation and the anomalous
behavior of the magneto-optical conductivity motivated us to
investigate some basic physical properties of Pr
0.6
Sr
0.4
MnO
3
single crystals in order to unambiguously distinguish between
conventional and unconventional properties of this essentially
metallic and ferromagnetic mixed-valent manganite. The main
focus is the nature of the paramagnetic (PM)-ferromagnetic
(FM) transition. Hence we present a scaling analysis of static
magnetization data supplemented by a detailed analysis of
the specific heat C
p
within the temperature range 2–350 K,
that covers both the PM-FM transition and the structural
transitions.
The critical nature of manganites near a PM-FM phase
transition have been the subject of many studies.
8–25
Different
experimental techniques have been used in these investigations
to obtain the critical exponent β of the spontaneous magne-
tization. The values of the exponent from these reports were
found in a range from 0.3 to 0.5 which covers the mean-field
value (β = 0.5) as well as the values corresponding to the
three-dimensional (3D) isotropic Heisenberg (β = 0.365) and
the 3D Ising (β = 0.325) universality classes. In addition to
the above variety of continuous phase transitions, first-order
nature of the PM-FM transition was found in in the case
of LaMnO
3.14
13
and La
0.7
Ca
0.3
MnO
3
.
26
The first-order phase
transition has been recently found in the phase diagrams
generated by large-scale Monte Carlo simulations within
the two-orbital model Hamiltonian.
27
This suggests that the
PM-FM transitions in manganites display different properties
varying from continuous transitions due to short-range ex-
change to first-order transitions.
Although our preliminary investigations
6
of the resistivity
at the paramagnetic-ferromagnetic (PM-FM) transition in
Pr
0.6
Sr
0.4
MnO
3
already suggested that the critical exponents
most probably belong to the class of conventional isotropic
ferromagnets, a clear-cut evidence from the magnetization
data was missing. Therefore, we here report a detailed analysis
of magnetization. The results reveal that the modified Arrott
plots provide straight lines for a range of exponents β and
γ (see definition below), including those belonging to both
the three-dimensional (3D) Heisenberg as well as 3D Ising
universality classes. These observations suggested a possible
role of anisotropy affecting the asymptotic critical properties.
Furthermore, a very recent investigation
28
of critical behavior
in polycrystalline Pr
0.55
Sr
0.45
MnO
3
by Fan et al. using the
field dependence of magnetic entropy change reports expo-
nents close to the mean-field values. In their method, only two
184422-1 1098-0121/2011/84(18)/184422(10) ©2011 American Physical Society