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IEEE TRANSACTIONS ON NUCLEAR SCIENCE 1
Red Mud Characterization Using Atomic and Nuclear
Analytical Techniques
Jasmina Obhodas, Davorin Sudac, Lidija Matjacic, and Vladivoj Valkovic
Abstract—Red mud is a toxic waste left as a byproduct in
aluminum production Bayer process. Since it contains significant
concentrations of other chemical elements interesting for industry,
including Rare Earths Elements (REEs), it is also potential sec-
ondary ore source. Recent events in some countries have shown
that red mud presents a serious environmental hazard if not
properly stored. The subject of our study is evaluation of the red
mud elemental composition, especially yttrium, scandium, gallium
and REEs, from an ex-aluminum plant in Obrovac, Croatia, left
from the processing of bauxite mined during late 70’s and early
80’s at the eastern Adriatic coast and stored in open concrete
basins for more than 30 years since then.
We have used energy dispersive x-ray fluorescence analysis
(both tube and radioactive source excitation), fast neutron ac-
tivation analysis and passive gamma spectrometry to identify a
number of elements present in the red mud, their concentration
levels and radioactivity in the red mud. The high concentrations
of Al, Si, Ca, Ti and Fe have been measured. Chemical elements
Sc, Cr, Mn, Co, Ni, Cu, Zn, Ga, As, Se, Br, Y, Rb, Sr, La, Ce, Pr,
Nd, Sm, Eu, Gd, Tb, Dy, Ho, Er, Tm, Pb, Th and U were found
in lower concentrations. No significant levels of radioactivity have
been measured.
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I. INTRODUCTION
R
ED Mud (RM) represent the poorly soluble part of the
bauxite remained after the alkaline extraction of by
the Bayer procedure. The red color is generally from iron ox-
ides, which are dominant in its composition. In addition, red
mud can contain a number of chemical elements which today
play a prominent role as strategic elements for development of
high-tech, renewable-energy, and defense-related technologies.
Today’s list of these critical elements would likely include most
of the REEs along with scandium, yttrium and gallium which
are commonly found in RM enriched 10–20 folds over normal
concentrations in the earth crust.
Manuscript received December 08, 2011; revised June 15, 2012; accepted
June 18, 2012. This work was supported in part by the EU FP7 Project No.
218148, UNCOSS—Underwater Coastal Sea Surveyor.
J. Obhodas is with the Department of Experimental Physics, Institute Ruder
Boskovic, Zagreb, Croatia (e-mail: jobhodas@irb.hr).
D. Sudac and L. Matjacic are with the Department of Experimental Physics,
Institute Ruder Boskovic, Zagreb, Croatia (e-mail: dsudac@irb.hr; Lidija.Mat-
jacic@irb.hr).
V. Valkovic is with the A.C.T.d.o.o., Prilesje 4, Zagreb, Croatia (e-mail:
vlado@act-doo.hr).
Digital Object Identifier 10.1109/TNS.2012.2206608
In this work we present the results of the measurements of
the composition of REE and other elements in the red mud left
after the closure of the aluminum processing plant in Croatia,
30 years ago. The plant was shut down in 1981 after three years
of operation owing to some political and economic factors. The
plant was producing 300,000 tons of alumina per year, resulting
in about of RM and of waste base (WB)
remained to this day in two concrete basins as it is shown in
Fig. 1.
Improperly managed red mud disposals can have serious con-
sequences for the environment and security of people. Concerns
about toxicity should be paid more to WB because of its high pH
value, although the red mud itself can physically cause a lot of
damage if it suddenly burst out of the reservoirs. Unfortunately,
such case happened in October 2010 in Kolontar red mud dis-
posal in Hungary, when 9 people died from drowning and 40
people suffered mostly from chemical burns caused by the WB
[1].
In this paper we discuss RM as a possible secondary raw
material for yttrium, scandium, gallium and REEs production
based on the results of our measurements. In addition we pro-
pose a biological remediation of WB by using Spirulina spp bac-
teria.
II. MATERIALS AND METHODS
Analysis of RM was done on samples prepared from 5 kg
of composite sample, collected from both basins in previous
survey [2]. Prior to analysis RM was dried in oven at
overnight, sieved to a fraction size of 0.7 mm, grinded and ho-
mogenized. REEs were analyzed by the energy dispersive x-ray
fluorescence technique (EDXRF) by using Bq ring-shaped
Am radioactive source for irradiation of 2 g pellets, 2.5 cm in
diameter and pressed under 9 t. Samples were placed in 99.9%
grade aluminum holder 12 mm distant from the source. The ir-
radiation time was 3000 s. X-ray spectra were collected with
a Canberra Ge(Li) detector (GL0055P, FWHM 155 eV at 5.9
keV). lines were fitted by using AXIL program from the
QXAS software package [3]. Acquisition system was made at
Ruder Boskovic Institute. Standard addition method was used
for a quantitative analysis of REEs. After addition of the dif-
ferent amounts of a standard (see Fig. 4), samples were mixed
for 15 minutes in a mixer (5100 Mixer/Mill SPEX SamplePrep
LLC) prior to each analysis and then pressed into pellets. Every
sample was analyzed two times. As the standard reference ma-
terials (SRMs) 99.9% grade REEs (La, Ce, Pr, Nd, Sm, Eu, Gd,
Tb, Dy, Ho, Er, and Tm) obtained from the Metall Rare Earth
Ltd, Shenzhen, China were used. For La, Ce, Pr, Nd, Sm, Eu,
Gd, Tb, Dy emission lines were analyzed. Elements Ho, Er
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