
588
In the paper (Hassan et al. 2013), sodium nitrite
was studied as an inhibitor for the protection of
reinforcing steel in concrete from corrosion. The
purposeofthisstudywasanattempttounderstand
the mechanism by which sodium nitrite contributes
to reducing the rate of corrosion on the surface of
carbon steel, depending on pH and the presence of
chlorideinthesystem.Inthelit
erature(Rosenberg&
Gaidis1979)ithavesuggestedthatnitriteundergoes
achemicalreactionwiththedivalentiron:
OHOFeNONOOHFe
2322
2
2222
(1)
ThisreactionformsthebarrierfilmofoxideFe
2O3
on the metal surface. The film protects from
corrosion.Thecorrosionratelargelydependsonthe
pH of the solution. The presence of chlorides
increasesthereactionrateofcorrosionbyactingasa
catalyst. Nitrite ions act as inhibitors by increasing
the rate of the barrier iron oxide film formation.
Increasing temperature leads to the desorption of
adsorb
ed sodium nitrite on the surface of the steel
andreducestheeffectivenessoftheinhibitor.
Theaimofthisworkwastostudychangesinthe
relaxation times distribution of nuclear quadrupole
resonance (NQR) in microscopic inhibitor after its
contactwiththesurfaceofinhibitedbla
ckmetal. This
approach is original since the change of the metal
surfacestatebycorrosioninthepresenceofinhibitor
isusuallyinvestigated.
2 EXPERIMENTALSTUDY
We have used nuclear quadrupole resonance as a
researchmethodbeca use relaxationtimes,spectrum
and shape of the NQR lines are very sensit
ive to
small changes in the environment of the nuclei.
Unlike nuclear magnetic resonance (NMR), nuclear
quadrupoleresonancefrequenciesaredeterminedby
the electric interactions, so the method allows not
indirectly, but directly to study the electric field at
the nuclei of atoms. NQR spectroscopy data are of
fundamental importance for understanding the
changesintheelectronicdistribution,theobservation
of physica
l phenomena occurring in crystals at the
microlevel.
Relaxationtimes express molecular dynamics, as
wellasprovideinformationaboutthemicrostructure
of matter. For homogeneous samples the signals of
nuclear quadrupole resonance recedes by the same
exponent.Inthi
scase,onlytherelaxationtimecanbe
preciselydeterminedbya linearapproximation.The
relaxation time distribution is continuous for more
complexsamples,molecularcrystalswithimpurities
micropowders, porous media due to various
intermolecular and many exponential inversion is
required for definition of the relaxation times
distribution.
LongitudinalNQRrelaxationti
mesaredefinedby
spin‐lattice interaction with the transfer of energy
fromthenuclearspinstomobilelattice,relaxationof
thetransversenuclearmagnetizationdependsonthe
spin‐spin interactions and due to the
inhomogeneities of crystallite lattice. Magnetization
of the nuclei in the different materials differing in
density, molecular structure and mobilit
y in
dependence on the environment is restored to the
individual time constant. NQR signals relaxation in
solidsareverydependentonthedegreeofordering
in the sample. Amorphous samples generally relax
fasterthancrystallinesamples.
Itwasfoundpreviouslythatthelongitudinaland
transverse relaxation ti
mes of nuclei in the fine
particles are reduced in comparison with the
corresponding samples in large samples. It is
assumed that this is caused by magnetization
diffusionfromthebulktothecrystallitesurface.Itis
known that the phonon spectrum of atoms at the
crystalsurfacediffersfromatomsinthebulk,dueto
thehighconcentrationofl
atticedefects,dislocations,
amorphouscharacter,causedbyplasticdeformation
during the milling process, or the influence of the
environmentsurroundingthecrystal.Theresultisa
strongconnectionofthesurfacespinswiththelattice
duetofluctuationscausedby theincreased number
ofdegreesoffreedom.
Experimental measurements were performed on
the NQR spectrometer Tecmag Apollo with TNMR
software (Fig. 1). The pulse sequence recovery
inversion 180° –τ
– 90° was used to measure the
spin‐latticerelaxationtime.Carr‐Purcell‐Meiboom
‐ Gill (CPMG) sequence was used to measure the
spin‐spinrelaxationti
meT
2.T2
*
relaxation timewas
measured from the shape of the Hahn echo signal.
Finally, the sequences with spin‐locking pulse of
variable duration was used to measure the spin‐
lattice relaxation in the rotating coordinate system
T
1
.Allpulsesequencesarewellknownandrequire
nospecialdescription.
The program RILT (Regularized Inverse Laplace
Transform)wasusedfortheinversionoftheLaplace
transformdescribedintheIari‐GabrielMarinowork
(Marino 2004). The desired array of relaxation time
distribution f(T) is the inverse Laplace transform of
the ti
me signal exponential decays measured by an
arrayofS(t).Arrayiscalculatedbytheregularization
using the least squares method. In the process of
calculation was used from 50 to 200 iterations.
Inversion of the Laplace transform have been used
effectively by us previously (Sinyavsky et al. 2014,
Dolinenkov et al. 2014) in the study of micro‐
composite and porous ma
terials and phase
transitions.
Figure1.Tecmag‐ApolloNQRspectrometerandinterface
ofTNMRsoftware.