Pith. sign in

REVIEW

Crystal and magnetic structure of La$_{1-x}$Ca$_{x}$MnO$_{3}$ compound $(0.11\leq x\leq 0.175

Not yet reviewed by Pith; the record is open.

This paper has not been read by Pith yet. Machine review is queued; the pith claim, tier, and objections will appear here once it completes.

SPECIMEN: schema-true, not a live event

T0 review · schema-true

One-sentence machine reading of the paper's core claim.

pith:XXXXXXXX · record.json · timestamp

arxiv cond-mat/0503253 v2 pith:L4XHJSOA submitted 2005-03-10 cond-mat.str-el cond-mat.mtrl-sci

classification cond-mat.str-elcond-mat.mtrl-sci
keywords structurecrystalsamplesferromagneticinsulatingmagneticmonoclinicbelow
verification ladder T0 review T1 audit T2 compute T3 formal
0 comments
abstract

We studied the crystal and magnetic structure of the La$_{1-x}$Ca$_{x}$MnO$_{3}$ compound for $(0.11\leq x\leq 0.175)$ using stoichiometric samples. For $x<0.13$ the system's ground state is insulating canted antiferromagnetic. For $0.13\le x \le 0.175$ e below the Jahn Teller transition temperature ($T_{\rm JT}$) the crystal structure undergoes a monoclinic distortion. The crystal structure can be described with $P 2_1/c$ space group which permits two Mn sites. The unit cell strain parameter $s=2(a-c)/(a+c)$ increases for $T<T_{\rm JT}$, taking the maximum value at the Curie point, and then decreases. Below $T_{\rm M^/M^{//}}\approx 60 $ K $s$ abruptly changes slope and finally approaches T=0 K with nearly zero slope. The change of $s$ at $T_{\rm M^/M^{//}}$ is connected to a characteristic feature in the magnetic measurements. As $x$ increases towards the ferromagnetic metallic boundary, although $s$ is reduced appreciably, the monoclinic structure is preserved. The monoclinic structure is discussed with relation to the orbital ordering, which can produce the ferromagnetic insulating ground state. We also studied samples that were prepared in air atmosphere. This category of samples shows ferromagnetic insulating behavior without following the particular variation of the $s$ parameter. The crystal structure of these samples is related to the so-called O$^{*}$ ($c>a>b/\sqrt{2}$) structure.

Discussion (0). Continue with ORCID to comment.

Pith tools