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Volume 3, Issue 2

ISSN: 2470-9905

Crystallography 2017

October 16-17, 2017

2

nd

International Conference on

October 16-17, 2017 | Chicago, USA

Applied Crystallography

Interplay between H-bonding and charge ordering in Fe

3

(PO

4

)

2

(OH)

2

barbosalite

J Rouquette

1

, J Haines

1

, V Ranieri

1

, M Poienar

2

, A Guesdon

3

and

C Martin

3

1

Université Montpellier, France

2

CRISMAT, France

3

Laboratoire Léon Brillouin, France

C

harge Ordering (CO) in transition metal oxides is an important parameter for obtaining original magnetic and/or electric

properties. That was largely shown within the framework of the studies on colossal magneto-resistance in manganese perovskites

and it again seems to be at the origin of the ferroelectricity in CaMn

7

O

12

or LuFe

2

O

4

. The mixed valence of iron in the system is a

particularmotivation in viewof the long lasting research on the understanding of the effects of pressure on charge order/magnetic order

in iron compounds such as the LuFe

2

O

4

new charge ordered state and the pressure dependence of its magnetic order. Here we focus

on Fe

2+

Fe

3+

2

(PO

4

)

2

(OH)

2

barbosalite single crystal, an hydroxyphosphate of iron which exhibits a mixed valence state. High pressure

behavior of barbosalite was successfully characterized based on single crystal X-ray diffraction, Raman and infrared spectroscopies.

Fe

2+

Fe

3+

2

(PO

4

)

2

(OH)

2

presents two phase transition at close to 3 and 8 GPa respectively which are clearly governed by an interplay

between H-bonding and electron delocalization. Moreover the temperature reaction Fe

2+

Fe

3+

2

(PO

4

)

2

(OH)

2+

Fe

3+

3

(PO

4

)

2

(OOH).

Figure 1:

h0l

reconstruction of the reciprocal space of incommensurate Fe

3+

3

(PO

4

)

2

(OOH).

Biography

J Rouquette has obtained his PhD in Julien Haines’ group in Materials Science (Condensed Matter) from University of Montpellier, France in 2004 and was a Postdoctoral

Fellow in Leonid Dubrovinsky’s group at the Bayerisches Geoinstitut in Bayreuth University, Germany for two years. He has joined the CNRS as a Researcher in 2004 in

the field of ferroelectrics/multiferroics and he defended his Habilitation in 2012 entitled “

insitu

structural studies of ferroic materials as a function of P,T,E,B. He has published

more than 50 research papers in these areas.

jerome.rouquette@umontpalllier.fr

J Rouquette et al., Struct Chem Crystallogr Commun, 3:2

DOI: 10.21767/2470-9905-C1-002