September 14, 2010 9:46 World Scientific Review Volume - 9.75in x 6.5in ch16
The Evolution of HTS: T
c
-Experiment Perspectives 413
3.2.1. The first Fe-pnictide superconductor family with a T
c
up to
57 K: doped RFeAsO, where R = rare-earth [R1111]
The discovery
23
of F-doped LaFeAsO [La1111] with a T
c
= 26 K in early
January 2008 by Hideo Hosono et al. of Tokyo Institute of Technology has
inaugurated the new Fe-pnictide superconductor era, demonstrating that su-
perconductivity with a relatively high T
c
can occur in a Fe-rich environment,
contrary to conventional wisdom, providing a new opportunity to explore the
relationship between HTS and magnetism and offering a possible new avenue
for high T
c
.
Hosono and colleagues had engaged extensively in modifying the func-
tionality of transparent novel oxide semiconductors with 2D layer structures
and with two separate or loosely coupled substructures, and gained exten-
sive knowledge on the chemistry, structure and electron-band manipulation
of inorganic solids. Realizing the importance of layer structure and magnetic
interaction in HTS cuprates, they investigated LaTPO and LaTAsO, where
T is a transition metal element. They detected superconductivity in com-
pounds LaFePO and LaNiPO when the number of d-electrons in T is even,
and magnetism in LaMnPO and LaCoPO when the number of d-electrons
in T is odd. The T
c
s observed in 2006 of LaNiPO and LaFePO were 3 K and
5–12 K, respectively. Unfortunately, the results did not attract much atten-
tion by the HTS community due to the low T
c
. The situation changed when
Hosono et al. observed superconductivity up to 26 K in F-doped LaFeAsO,
or La(O
1−x
F
x
)FeAs, and the results (Fig. 13) appeared in the March 19,
2008, issue of Journal of American Chemical Society in an article entitled
“Iron-Based Layered Superconductor La[O
1−x
F
x
]FeAs (x = 0.05–0.12) with
T
c
= 26 K.”
23
The parent compound LaOFeAs [La1111] is a member of the well-known
equiatomic quaternary layered compounds ROTPn where R = La, Nd,
Sm, Gd; T = Mn, Fe, Co, Ni, Cu; and Pn = P, As, Sb. They exhibit
a tetragonal layer structure of the ZrCuSiAs type with a space group of
P4/nmm. LaOFeAs consists of (Fe
2
As
2
)-layers sandwiched by the (LaO)-
layers. Each (Fe
2
As
2
)-layer contains a squared-planar Fe-sheet sandwiched
by two As-sheets; and each (LaO)-layer comprises an O-sheet sandwiched
between two La-sheets. Similar to the cuprates, the (Fe
2
As
2
)-layers form the
active block where the charge carriers flow, while the (LaO)-layers consti-
tute the charge-reservoir block that inject charge carriers into the former
without degrading the integrity of the (Fe
2
As
2
)-layers. But different from
the cuprates: the divalent Fe is tetrahedrally coordinated with four As-ions
in LaOFeAs, whereas the divalent Cu forms the fourfold square plane in the