A certified Sm standard (1000 mg∙L⁻¹ in 2% HNO₃; CPI International, S4400-1000471) was diluted to obtain 1.0 × 10⁻³, 1.0 × 10⁻⁶, and 1.0 × 10⁻⁸ mol∙L⁻¹ Sm(III) solutions. Eosin (H.E. Daniel Ltd.) and o-phenanthroline (Merck) stock solutions were prepared at 1.0 × 10⁻³ mol∙L⁻¹. Working solutions of both reagents at 1.0 × 10⁻⁷ mol∙L⁻¹ were subsequently prepared by serial dilution with ultrapure water. Under the optimized conditions, 250 µL of the eosin working solution and 1000 µL of the o-phenanthroline working solution were added to a final assay volume of 10.0 mL, corresponding to final concentrations of 2.5 × 10⁻⁹ and 1.0 × 10⁻⁸ mol∙L⁻¹, respectively. HTAB (Sigma-Aldrich) was prepared at 1.0 × 10⁻² mol∙L⁻¹ and diluted to a 1.0 × 10⁻³ mol∙L⁻¹ working solution. Potassium phosphate buffer (1.0 × 10⁻² mol∙L⁻¹) was adjusted with HCl or NaOH; optimized conditions were pH 6.5 and 2.0 × 10⁻⁴ mol∙L⁻¹ final phosphate. Blue-ribbon Whatman filter paper (2 - 5 μm, 4.5 cm diameter) was used as the SSF substrate. All reagents were analytical grade, and ultrapure water was used throughout.

Fluorescence measurements were performed with a Shimadzu RF-5301 PC spectrofluorometer equipped with a 150 W xenon lamp and a solid-sample holder. Emission spectra were recorded from 500 to 750 nm at λexc = 525 nm; excitation/emission slit widths were 1.5/3.0 nm, and intensity at 645 nm was used for quantification. pH was measured with an Orion EA 940 analyzer.

Calibration standards were prepared at 1.31, 15.04, 37.59, 75.18, 112.77, 150.36, 300.72, and 375.90 ng∙L⁻¹ Sm(III). A reagent blank was prepared separately and included as the zero-concentration level in the least-squares regression. Six independently prepared assay solutions were analyzed at each calibration level. Each solution was filtered through a separate cellulose paper substrate, air-dried, independently placed in the solid-sample holder, and measured under the selected instrumental conditions.

Intra-day precision was evaluated at 50 ng∙L⁻¹ using six independently prepared solutions analyzed on the same day. Inter-day precision was evaluated at the same concentration by repeating six independent complete determinations on each of seven different days. Each determination included solution preparation, filtration through a separate cellulose substrate, drying, independent paper placement, and fluorescence measurement. Therefore, the reported precision represents the variability of the complete analytical procedure rather than repeated instrumental readings of the same substrate.

The complete solution was filtered through blue-ribbon cellulose paper, air-dried for 15 - 20 min until completely dry, and placed directly in the solid-sample holder. Emission was recorded at λexc = 525 nm, and the 645 nm signal was used as the analytical response. Samples followed the same procedure after the introduction of the water or sediment-extract aliquot.

Calibration standards were prepared at 1.31, 15.04, 37.59, 75.18, 112.77, 150.36, 300.72, and 375.90 ng∙L⁻¹ Sm(III). A reagent blank was prepared separately. The lowest calibration level, corresponding to the calculated LOQ of 1.31 ng∙L⁻¹, was experimentally prepared and analyzed to verify its quantification performance.

In April 2026, paired water and sediment samples were collected upstream and downstream of five reservoirs in San Luis, Argentina: Dique Chico (M1-M2), Cruz de Piedra (M3-M4), Potrero de los Funes (M5-M6), La Estrechura (M7-M8), and Berta Vidal de Battini (M9-M10). Water was stored frozen in aliquots, and sediments were transported in resealable bags. Sampling coordinates were 33.300961˚S, 66.292621˚W (M1); 33.303872˚S, 66.316481˚W (M2); 33.256296˚S, 66.212217˚W (M3); 33.276033˚S, 66.228927˚W (M4); 33.220925˚S, 66.229500˚W (M5); 33.237842˚S, 66.239929˚W (M6); 33.208380˚S, 66.178012˚W (M7); 33.240606˚S, 66.179168˚W (M8); 33.163477˚S, 66.152481˚W (M9); and 33.171985˚S, 66.154498˚W (M10).

The closed Las Águilas East and West Ni-Cu-Co deposit is located approximately 4.8 - 5.7 km from M9-M10 and was considered only as a regional geological context, not evidence of direct mining input [14].

Water samples were filtered through 0.45 µm syringe membranes. A 1.00 mL aliquot was transferred to a 10 mL flask and analyzed by the general SSF procedure. Accuracy and matrix effects were assessed by two-level spike-recovery experiments; native and spiked samples were measured six times (n = 6).

Sediments were air-dried, ground, and sieved through a 2 mm mesh. Portions of 1.00 g of dry sediment were placed in digestion vessels and treated with 7.0 mL of concentrated HNO₃ (70%, v/v) and 3.0 mL of 10-volume H₂O₂. For the pre-digestion spike-recovery experiments, known amounts of Sm(III) standard solution were added directly to the digestion vessels after the addition of HNO₃ and H₂O₂ but before the heating step. Both spiked and unspiked samples were subsequently digested at 75˚C - 80˚C for 2 h.

After cooling, the extracts were quantitatively adjusted to 10.0 mL with ultrapure water, allowed to settle, and decanted. A 1.00 mL aliquot of each extract was diluted to 10.0 mL with ultrapure water and carefully neutralized with 0.10 mol∙L⁻¹ NaOH until a pH of approximately 6.0 was reached. Subsequently, 250 µL of the neutralized dilution was introduced into the 10.0 mL SSF assay. After the addition of all reagents and phosphate buffer, the pH of the complete assay solution was measured and confirmed to be approximately 6.0.

Samples whose concentrations exceeded the upper calibration limit of 375.9 ng∙L⁻¹ were further diluted, and the results were corrected using the corresponding dilution factor. The reported sediment concentrations represent the acid-extractable Sm fraction rather than the total Sm content. For each native and spiked extract, six independently prepared SSF assay solutions were analyzed on separate cellulose paper substrates, with independent paper placements.

The retained Sm(III)-Eo-o-phen-HTAB system showed a concentration-dependent fluorescence increase at 645 nm (λexc = 525 nm), consistent with the characteristic ⁴G₅/₂ → ⁶H₉/₂ transition of Sm³⁺. The blank intensity was 23 a.u., increasing to 981 a.u. at the highest calibration level (Figure 1(A)).

Regression of fluorescence intensity versus Sm(III) concentration gave IF = 378.85 CSm + 47.52 (CSm in 10⁻⁹ mol∙L⁻¹), R² = 0.9967, over 1.31 - 375.9 ng∙L⁻¹ (Figure 1(B)).

Figure 1.(A) Reconstructed solid-surface fluorescence emission profiles of the Sm(III)-Eo-o-phen-HTAB system at increasing Sm(III) concentrations. The profiles were generated using a common band shape centered at 645 nm and scaled to the experimental fluorescence intensity recorded at this wavelength. (B) Calibration plot obtained at λ_exc = 525 nm and λ_em = 645 nm.

Effect of pH

Fluorescence increased from pH 4.0 to a maximum at pH 6.5 (640 a.u.), remained high between pH 6.0 and 7.5, and decreased at higher pH (Figure 2Figure 2). Thus, pH 6.5 was selected. The trend may reflect changes in ligand protonation, Sm(III) hydrolysis, and retention of the fluorescent assembly; these mechanistic interpretations remain provisional because speciation was not independently evaluated.

Although pH 6.5 was selected as the optimum condition, the final sediment-assay solutions exhibited a pH of approximately 6.0 after neutralization and reagent addition. This value remained within the high-response interval observed between pH 6.0 and 7.5.

Figure 2.Effect of pH on the solid-surface fluorescence intensity of the Sm(III)-Eo-o-phen-HTAB system. Fluorescence measurements were performed at λexc = 525 nm and λem = 645 nm. Other experimental conditions were as described in Section 2.3.

Optimization ofLigand Volumes

Eosin and o-phenanthroline both enhanced the response (Figure 3Figure 3). Eosin reached a plateau at 250 - 300 µL; 250 µL was selected as the minimum volume that provided maximum response. For o-phenanthroline, the maximum was obtained at 1000 µL, with no benefit at 1250 µL. These trends are consistent with ligand participation in the formation and sensitization of the retained fluorescent assembly, although stoichiometry was not independently established.

Effect of HTABVolume

HTAB markedly enhanced fluorescence (Figure 4Figure 4), increasing the signal from 254 a.u. without surfactant to 661 a.u. at 100 µL, an approximately 2.6-fold enhancement. Higher volumes produced no further improvement; therefore, 100 µL was selected. The effect is consistent with favorable eosin-HTAB ion association and improved retention on cellulose, although aggregation/speciation was not independently studied.

Figure 3.Influence of the added volumes of (A) eosin and (B) o-phenanthroline on the solid-surface fluorescence intensity of the Sm(III)-Eo-o-phen-HTAB system. Measurements were performed at λ_exc = 525 nm and λ_em = 645 nm. Other experimental conditions were as described in Section 2.3.

Figure 4.Effect of HTAB volume on the solid-surface fluorescence intensity of the Sm(III)-Eo-o-phen-HTAB system. Measurements were performed at λ_exc = 525 nm and λ_em = 645 nm. Other experimental conditions were as described in Section 2.3.

Effect ofPhosphate Buffer Volume

Phosphate buffer volume affected the response (Figure 5Figure 5): fluorescence increased from 347 a.u. at 100 µL to a maximum of 674 a.u. at 200 µL and then remained near a plateau. Accordingly, 200 µL was selected as the lowest volume providing maximum signal and adequate pH control.

Figure 5.Effect of phosphate buffer volume on the solid-surface fluorescence intensity of the Sm(III)-Eo-o-phen-HTAB system. Measurements were performed at λ_exc = 525 nm and λ_em = 645 nm. Other experimental conditions were as described in Section 2.3.

Effect ofReagent Addition Order

The addition order strongly influenced fluorescence (Figure 6Figure 6). The highest response (687 a.u.) was obtained for O1: Eo → o-phen → Sm(III) → HTAB → phosphate buffer. Alternative sequences gave lower signals, supporting ligand-metal association before surfactant organization and final pH adjustment. Because no kinetic or speciation study was performed, this interpretation remains provisional; O1 was adopted for subsequent measurements.

Figure 6.Effect of reagent addition order on the solid-surface fluorescence intensity of the Sm(III)-Eo-o-phen-HTAB system. PB: phosphate buffer. Measurements were performed at λ_exc = 525 nm and λ_em = 645 nm. Other experimental conditions were as described in Section 2.3.

Under the optimized conditions, the reagent blank and all Sm(III) calibration standards were included in the least-squares regression. The resulting calibration equation was (I_F = 378.85C_{Sm} + 47.52), where (C_{Sm}) is expressed in (10^{−9}) mol∙L⁻¹, with (R^2 = 0.9967) over the range of 1.31 - 375.90 ng∙L⁻¹. Six independently prepared assay solutions were analyzed at each calibration level. The RSD values obtained for the non-zero calibration levels ranged from 0.010 to 0.175%, while the standard deviation of the reagent blank was 0.33 a.u.

The LOD and LOQ, calculated as (3\sigma/slope) and (10\sigma/slope), were 0.39 and 1.31 ng∙L⁻¹, respectively. The calculated LOQ was subsequently verified experimentally by preparing and analyzing Sm(III) solutions at 1.31 ng∙L⁻¹ under the complete SSF procedure. At this concentration, a mean recovery of 99.89% and an RSD of 0.21% were obtained, confirming that 1.31 ng∙L⁻¹ could be reliably quantified. Therefore, the experimentally verified linear range was 1.31 - 375.90 ng∙L⁻¹.

Precision was evaluated at 50 ng∙L⁻¹ considering the complete analytical procedure. For intra-day precision, six independent solutions were prepared and individually filtered through six different cellulose substrates on the same day. Inter-day precision was assessed at the same concentration by performing six independent complete determinations on each of seven different days. Each substrate was independently dried, positioned in the solid-sample holder, and measured. The intra-day and inter-day RSD values were 0.33% and 0.36%, respectively. These results demonstrate satisfactory repeatability and intermediate precision, including variability associated with solution preparation, filtration, cellulose substrate heterogeneity, drying, paper placement, and instrumental measurement (See Table 1).

Table 1.Analytical performance of the proposed SSF method for Sm(III).

The potential effects of selected cations, anions, and rare earth elements on the determination of Sm(III) were evaluated at a Sm(III) concentration of 1.0 × 10⁻⁹ mol∙L⁻¹. The investigated species included Na⁺, K⁺, Ca²⁺, Mg²⁺, Al³⁺, Fe³⁺, Mn²⁺, Co²⁺, Ni²⁺, Cu²⁺, Zn²⁺, Cd²⁺, Pb²⁺, Cr³⁺, La³⁺, Ce³⁺, Nd³⁺, Eu³⁺, Gd³⁺, Tb³⁺, Cl⁻, NO 3 − , SO 4 2 − , CO 3 2 − , HCO 3 − , and PO 4 3 − . Each experimental condition was evaluated using six independently prepared solutions and separate cellulose paper substrates (n = 6). The results are reported as mean fluorescence intensity ± standard deviation and mean signal variation ± standard deviation (Table 2).

A signal variation of ±5% relative to the Sm(III) solution without interferent was adopted as the acceptance criterion. The evaluated species were tested at an interferent-to-Sm(III) molar ratio of 1000:1, except Cr(III), which was evaluated at 500:1. Mean signal variations ranged from −1.22% for Mg²⁺ to −0.15% for K⁺ and Al³⁺, while the associated standard deviations ranged from 0.09% to 0.21%. The standard deviations of the measured fluorescence intensities ranged from 2.04 to 2.34 a.u. None of the investigated species produced a signal variation exceeding the ±5% acceptance criterion under the tested conditions.

These results demonstrate satisfactory tolerance toward the specific ions and concentration ratios evaluated in this study. Because yttrium and the remaining lanthanides were not investigated, the results should not be interpreted as evidence of general selectivity against all rare earth elements.

Table 2.Effect of the evaluated potentially interfering species on the fluorescence determination of Sm(III). Results are expressed as mean ± SD based on six independent determinations.

SedimentSamples

Acid-extractable Sm(III) was quantified in all ten sediments (Table 3). Final analytical concentrations of 127.44 - 304.67 ng∙L⁻¹ corresponded to 509.76 - 1218.68 µg∙kg⁻¹ dry sediment after correction for extraction and dilution. M5 showed the lowest and M8 the highest value. These concentrations represent the acid-extractable fraction, not the absolute total Sm.

Pre-digestion spike recoveries ranged from 99.50% to 100.43%. Because the Sm(III) standard was added directly to the digestion vessels before heating, the spiked samples underwent the complete digestion and analytical procedure. These results therefore support satisfactory procedural recovery and limited matrix effects under the selected conditions.

Table 3.Determination of acid-extractable Sm(III) and pre-digestion spike-recovery results in sediment samples.

NaturalWater Samples

Sm(III) was detected in six of ten natural waters; M3, M5, M6, and M9 were below the detection limit (Table 4). Detectable final-solution concentrations were 16.33 - 21.44 ng∙L⁻¹, corresponding to 163.3 - 214.4 ng∙L⁻¹ in the original samples after the tenfold dilution correction. M4 had the lowest detectable concentration, and M8 the highest.

Spike recoveries in waters ranged from 92.71% to 105.42%, supporting satisfactory accuracy and limited matrix effects under the selected conditions.

Table 4.Determination of Sm(III) and spike-recovery results in natural water samples.

Accuracy Assessment and Validation Limitations

The accuracy of the proposed procedure was evaluated through two-level standard-addition and recovery experiments in all investigated water and sediment samples. For water samples, recoveries ranged from 92.71% to 105.42%, indicating satisfactory analyte recovery and limited matrix effects. For sediment samples, the Sm(III) standard was added directly to the digestion vessels before the heating step; therefore, the spiked samples underwent the complete digestion, dilution, neutralization, filtration, drying, and SSF measurement procedure. The corresponding pre-digestion recoveries ranged from 99.50% to 100.43%.

Additional evidence of method performance was provided by the experimentally verified LOQ, with a recovery of 99.89% and an RSD of 0.21%, as well as by intra-day and inter-day precision values of 0.33% and 0.36%, respectively. All calibration and spiking solutions were prepared from a certified 1000 mg∙L⁻¹ Sm standard solution.

Independent confirmation by ICP-MS or analysis of an appropriate certified reference material could not be performed during the present study. Therefore, the reported environmental concentrations should be interpreted as method-dependent estimates of the filtered Sm fraction in water and the acid-extractable Sm fraction in sediment. Although the standard-addition recoveries support the applicability of the procedure to the investigated matrices, future comparison with an independent reference technique or a suitable certified reference material would provide further confirmation of the method’s accuracy.