714 XXXI International Mineral Processing Congress 2024 Proceedings/Washington, DC/Sep 29–Oct 3
and P2O5. The presence of Fe2O3, Al2O3, and MgO fur-
ther validates the existence of clay minerals in the tailings.
Mineralogical analysis using XRD, coupled with
chemical characterization, reveals the presence of calcite,
dolomite, fluorapatite, quartz, montmorillonite, palygor-
skite, and kaolinite. The elevated percentages of CaO and
MgO suggest a significant abundance of carbonate min-
erals in the sample. Approximately 19% of the sample’s
composition is constituted by clay minerals, specifically
palygorskite, montmorillonite, and kaolinite, as outlined in
Table 3. Notably, the sample exhibits a substantial residual
quantity of fluorapatite (29%) alongside carbonate miner-
als (41%) and quartz (12%).
The zeta potential study, conducted with a dilute sus-
pension containing 0.1 wt.% solids in a background of
distilled 10–3 M KCl electrolyte, is depicted in Figure 2.
Notably, the tailings consistently demonstrate a negative
charge at the slipping g plane of the particles across the
pH range investigated, spanning from 4 to 10. The magni-
tude of the charge intensifies with rising pH and reaches its
minimum value at pH 10. Beyond a pH value of 11, the
zeta potential remains relatively constant, maintaining its
lowest values.
As the tailings contain varying proportions of min-
eral phases, with a predominance of phases exhibiting a
negative charge across the studied pH range (A. Kaya &
Yukselen, 2005 Y. Y. A. Kaya, 2011 Moulin &Roques,
2003 Owens et al., 2019 Saka &Gu, 2006 White, 1986),
the overall slipping plane charge of the sample is negative.
The isoelectric point of the sample is prominently evident
at pH levels lower than 2.
Figure 2. Particle size distribution of the FPTs sample
Table 3. Chemical and mineralogical analyses of the FPTS sample
Chemical
Composition
Oxide CaO SiO
2 Al
2 O
3 Fe
2 O
3 MgO K
2 O Na
2 O P
2 O
5 Other LOI Total LOD*
%wt 38.77 20.22 2.72 1.06 3.07 0.49 0.61 13.2 1.21 18.65 100 0.01
Mineralogical
Composition
Mineral Fluorapatite Calcite Dolomite Quartz Palygorskite Palygorskite Montmorillonite Kaolinite
%wt 28 29 12 12 6 6 8 5
*Limit of detection.
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Extracted Text (may have errors)

714 XXXI International Mineral Processing Congress 2024 Proceedings/Washington, DC/Sep 29–Oct 3
and P2O5. The presence of Fe2O3, Al2O3, and MgO fur-
ther validates the existence of clay minerals in the tailings.
Mineralogical analysis using XRD, coupled with
chemical characterization, reveals the presence of calcite,
dolomite, fluorapatite, quartz, montmorillonite, palygor-
skite, and kaolinite. The elevated percentages of CaO and
MgO suggest a significant abundance of carbonate min-
erals in the sample. Approximately 19% of the sample’s
composition is constituted by clay minerals, specifically
palygorskite, montmorillonite, and kaolinite, as outlined in
Table 3. Notably, the sample exhibits a substantial residual
quantity of fluorapatite (29%) alongside carbonate miner-
als (41%) and quartz (12%).
The zeta potential study, conducted with a dilute sus-
pension containing 0.1 wt.% solids in a background of
distilled 10–3 M KCl electrolyte, is depicted in Figure 2.
Notably, the tailings consistently demonstrate a negative
charge at the slipping g plane of the particles across the
pH range investigated, spanning from 4 to 10. The magni-
tude of the charge intensifies with rising pH and reaches its
minimum value at pH 10. Beyond a pH value of 11, the
zeta potential remains relatively constant, maintaining its
lowest values.
As the tailings contain varying proportions of min-
eral phases, with a predominance of phases exhibiting a
negative charge across the studied pH range (A. Kaya &
Yukselen, 2005 Y. Y. A. Kaya, 2011 Moulin &Roques,
2003 Owens et al., 2019 Saka &Gu, 2006 White, 1986),
the overall slipping plane charge of the sample is negative.
The isoelectric point of the sample is prominently evident
at pH levels lower than 2.
Figure 2. Particle size distribution of the FPTs sample
Table 3. Chemical and mineralogical analyses of the FPTS sample
Chemical
Composition
Oxide CaO SiO
2 Al
2 O
3 Fe
2 O
3 MgO K
2 O Na
2 O P
2 O
5 Other LOI Total LOD*
%wt 38.77 20.22 2.72 1.06 3.07 0.49 0.61 13.2 1.21 18.65 100 0.01
Mineralogical
Composition
Mineral Fluorapatite Calcite Dolomite Quartz Palygorskite Palygorskite Montmorillonite Kaolinite
%wt 28 29 12 12 6 6 8 5
*Limit of detection.

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