TY - JOUR
T1 - Mössbauer study of contaminated soils by industrial activity in Paramonga city, Region Lima Provinces, Peru
AU - Bustamante, Angel
AU - Fabián, Julio
AU - De Los Santos, Luis
AU - Barnes, C. H.W.
AU - Majima, Yutaka
N1 - Copyright:
Copyright 2012 Elsevier B.V., All rights reserved.
PY - 2012/5
Y1 - 2012/5
N2 - In this work we characterize soils from the Paramonga city, Region Lima Provinces in Peru, which are contaminated by residual chemicals (Br, As and Sr) from sugar and paper industry in the city. Four samples were collected, labelled as S1, S2, S3 and S4 and analized by X-ray diffraction (XRD), energy-dispersive X-ray fluorescence (EDXRF) and Mössbauer spectroscopy. For all the samples, the chemical analysis by EDXRF revealed the presence of Fe, Mn, Cu, Zn, K, Br, Sr. The XRD detected the presence of quartz as principal phase and copper sulfide and potassium magnesium as secondary phases. The Mössbauer spectra at room temperature (RT) for all the samples exhibit sextets which reveal the presence of an iron oxide or hydroxide. The fitting Mössbauer for both samples S1 and S4 have three doublets corresponding to iron in paramagnetic phases and a magnetic component of around 35.50 T corresponding to goethite, α-FeOOH. Sample S2 have two magnetic phases with internal fields of 37 T and 34.6 T which correspond to the goethite and other incorporated element in the structure. The sample S3 have three magnetic fields of H1 = 36.8 T, H2 = 33.6 T and H3 = 34.8 T which correspond to hydroxide iron, pyrrhotite and goethite respectively.
AB - In this work we characterize soils from the Paramonga city, Region Lima Provinces in Peru, which are contaminated by residual chemicals (Br, As and Sr) from sugar and paper industry in the city. Four samples were collected, labelled as S1, S2, S3 and S4 and analized by X-ray diffraction (XRD), energy-dispersive X-ray fluorescence (EDXRF) and Mössbauer spectroscopy. For all the samples, the chemical analysis by EDXRF revealed the presence of Fe, Mn, Cu, Zn, K, Br, Sr. The XRD detected the presence of quartz as principal phase and copper sulfide and potassium magnesium as secondary phases. The Mössbauer spectra at room temperature (RT) for all the samples exhibit sextets which reveal the presence of an iron oxide or hydroxide. The fitting Mössbauer for both samples S1 and S4 have three doublets corresponding to iron in paramagnetic phases and a magnetic component of around 35.50 T corresponding to goethite, α-FeOOH. Sample S2 have two magnetic phases with internal fields of 37 T and 34.6 T which correspond to the goethite and other incorporated element in the structure. The sample S3 have three magnetic fields of H1 = 36.8 T, H2 = 33.6 T and H3 = 34.8 T which correspond to hydroxide iron, pyrrhotite and goethite respectively.
KW - Field emission-scanning electron microscope
KW - Mössbauer spectroscopy
KW - XRF
UR - http://www.scopus.com/inward/record.url?scp=84860889729&partnerID=8YFLogxK
U2 - 10.1007/s10751-012-0591-x
DO - 10.1007/s10751-012-0591-x
M3 - Artículo
AN - SCOPUS:84860889729
SN - 0304-3843
VL - 211
SP - 147
EP - 152
JO - Hyperfine Interactions
JF - Hyperfine Interactions
IS - 1-3
ER -