The surf
ace st
ate of c
arbon n
anotubes-Fe-
alumin
a n
anocomposite powders w
as studied by tr
ansmission
andintegr
al low-energy electron Mössb
auer spectroscopy. Sever
al s
amples, prep
ared under reduction of the
ages/gifch
ars/
alph
a.gif" BORDER=0>-Al
1.8Fe
0.2O
3 precursor in
a H
2-CH
4 atmosphere
applying the s
ame he
ating
and cooling r
ate
and ch
anging only them
aximum temper
ature (800-1070
ages/entities/deg.gif">C) were investig
ated, demonstr
ating th
at integr
al low-energy electronMössb
auer spectroscopy is
a promising tool complementing tr
ansmission Mössb
auer spectroscopy for theinvestig
ation of the loc
ation of the met
al Fe
and iron-c
arbide p
articles in the different c
arbon n
anotube-n
anocomposite systems cont
aining iron. The n
ature of the iron species (Fe
3+, Fe
3C
, ages/gifch
ars/
alph
a.gif" BORDER=0>-Fe,
ages/gifch
ars/g
amm
a.gif" BORDER=0 >-Fe-C) is correl
atedto their loc
ation in the m
ateri
al. In p
articul
ar, much inform
ation w
as derived for the powders prep
ared byusing
a moder
ate reduction temper
ature (800, 850,
and 910
ages/entities/deg.gif">C), for which the tr
ansmission
and integr
allow-energy electron Mössb
auer spectr
a are m
arkedly different. Indeed,
ages/gifch
ars/
alph
a.gif" BORDER=0>-Fe
and Fe
3C were not observed
assurf
ace species, while
ages/gifch
ars/g
amm
a.gif" BORDER=0 >-Fe-C is present
at the surf
ace
and in the bulk in the s
ame proportion independentof the temper
ature of prep
ar
ation. This could show th
at most of the n
anop
articles (detected
as Fe
3C
and/or
ages/gifch
ars/g
amm
a.gif" BORDER=0 >-Fe-C) th
at contribute to the form
ation of c
arbon n
anotubes
are loc
ated in the outer porosity of the m
ateri
al,
as opposed to the topmost (c
a. 5 nm) surf
ace. For the higher reduction temper
atures
Tr of 990
ages/entities/deg.gif">C
and1070
ages/entities/deg.gif">C,
all Fe
and Fe-c
arbide p
articles formed during the reduction
are distributed evenly in the bulk
andthe surf
ace of the m
atrix gr
ains. The integr
al low-energy electron Mössb
auer spectroscopic study of
a powderoxidized in
air
at 600
ages/entities/deg.gif">C suggests th
at
all Fe
3C p
articles oxidize to
ages/gifch
ars/
alph
a.gif" BORDER=0>-Fe
2O
3, while the
ages/gifch
ars/
alph
a.gif" BORDER=0>-Fe
and/or
ages/gifch
ars/g
amm
a.gif" BORDER=0 >-Fe-C
are p
artly tr
ansformed to Fe
1-xO
and
ages/gifch
ars/
alph
a.gif" BORDER=0>-Fe
2O
3, the l
atter ph
ase forming
a protecting l
ayer th
at prevents tot
aloxid
ation.