2.1. Characterization of the Sediments
The samples subjected to experimental testing were analysed in terms of particle size and chemical and physical characteristics of moisture, organic matter, and ash at all stages of the study, as detailed in
Table 1. The physico–chemical analyses confirmed the different composition of the samples in terms of the percentage of volatile/organic fraction, which was found to be more prevalent in the sample designated as S1.
Sifting of S1 and S2 was carried out according to SNPA/18 2018 [
46]. Moreover, washing treatment indicated that the sediments were solid particles purely in the sand range. Specifically, 90% of samples S1–S2 were in the fine–coarse sand range (0.063–0.6 mm) and the remaining 10% in the very coarse sand range (0.6–2 mm) according to the Udden–Wentworth scale [
47,
48], with a D50 of 0.35 and 0.2 mm for samples S2 and S1, respectively (
Figure 1).
The two sediment samples (S1 and S2) are illustrated in microscopic detail in
Figure 2 and
Figure 3.
The study at the microstructural level, developed through SEM-EDX analysis, highlighted the microporous nature of the sediment particles (S1, S2) used in the experimental tests. The essential differentiating component between the samples, the presence of organic fibres in sediment S1, is illustrated in
Figure 2B, where an image of its microstructure in its natural state is shown. This is later confirmed by the product of EDX analysis (
Figure 2C), in which the organic nature of the material is highlighted due to the significant peak of C together with the presence of elements such as Na and Cl, due to the marine origin of the material used. This information corroborates the chemical and physical characterisation data for sample S1, which demonstrates a higher presence of solid volatiles intrinsically associated with organic fibre.
As illustrated in
Figure 3C, the spectrum of sediment particle S2 demonstrates a convergence of the representative peaks of the EDX analysis with the mineralogical composition of the sediments in the area under study, particularly the southern portion of the Adriatic Sea. As evidenced by Lucchini et al. 2003 [
49] and by the data of the oceanographic campaign ‘PERTRE’ (one of the European ‘PERSEUS’ project missions) carried out by the Italian Institute for Marine Biological Resources and Biotechnology (IRBM-CNR) in 2016, there is confirmation of the reduced organic content shown in the characterisation data of
Table 1.
2.2. Effect of Organic Matter on the Physical–Mechanical Performance of Cement Mortars
The chemical–physical characterisation of the non-treated, water-treated, and H2O2 pre-treated sediments is described in the following section.
The chemical–physical analysis of the samples subjected to washing and oxidation treatments indicated a progressive reduction in volatile/organic fraction (
Table 2). Indeed, samples S1 and S2, which underwent washing with H
2O, exhibited 15% and 13% reductions of the indicated fraction, respectively. Moreover, after washing with an oxidiser, the maximum reduction was observed at 40% and 31.5%, respectively. After the treatments with H
2O and H
2O
2, the grain size distribution was examined, and the data were compared to the initial condition. The most notable alteration was observed in sample S1 following the oxidation washing with H
2O
2, which indicated a slight reduction in the proportion of medium-sized sands (0.6–0.2 mm) and an increase in the finer fraction (0.2–0.063 mm) with a representative D50 of 0.28 mm. This particle size distribution is presumably correlated to the variation in organic content within the sample under study (
Figure 3). In contrast, the variations of the particle size distribution following the treatments on sample S2 are not significant (
Figure 4) because of the low organic content, so the D50 was constant following the treatments.
The mortars produced from sediment samples S1 and S2, respectively M_S1 and M_S2, showed 70% workability, slightly lower than the reference value of the normalised mortar M1 with a flow of 90%. This result is ascribed to the sediment, which is characterised by organic substances that absorb a higher quantity of water, thus reducing workability (
Figure 5).
M_S1 and M_S2 samples showed interesting flexural and compression results, comparable with the reference (M1), as shown in
Table 3. The M_S2 sample showed higher strength than the S1 sample (16%). This discrepancy can be attributed to the chemical composition of the sediments. In chemical–physical characterisation, sample S1 contained more organic particles, which were identified through optical analysis as seaweed residues (Posidonia). Experimental tests have confirmed that these particles inhibit hydration reactions and harm mechanical strength development, as shown in the study of Du et al. 2020 [
50].
It is hypothesised that the ionic substances present in seawater may affect the performance of cement-based materials, given the higher concentration of these substances in seawater compared to freshwater. Such effects may impede the development of the setting and rheological properties of the cement, consequently influencing the mechanical and durability properties of the concrete [
51,
52]. However, in contrast to these studies, other researchers have indicated that various chemicals, such as chloride ions present in seawater, can enhance the strength of concrete in the short term, in some cases with higher values than the conventional conglomerates [
53,
54]. As stated by Qu et al. (2021) [
55], saline ions within the interstitial water in marine sediments have been observed to promote compressive strength development in the early stages of the cement hydration process. Furthermore, this trend has remained constant over time, exceeding the strengths achievable in the presence of fresh water.
The chloride ions from marine sediment, present in the system in the form of NaCl, CaCl
2, MgCl
2, and KCl, can react with tri-calcium aluminate (C
3A) and/or gypsum (CaSO
4), forming Friedel’s/Kuzel salts, which can expand to fill the pores. These reactions consume calcium hydroxide (CH), a cement hydration product, and further form a new compound such as Friedel’s/Kuzel’s salts, as shown below in Equations (1) and (2) (Yadav et al., 2024) [
56].
This effect may explain the time stability of the mechanical strengths. The free
ions retained in the system, leading to an increase of pH and also alkalinity of the pose solution, means the metastable hydroxy-AFm (alumino-ferrite monosubstituted) hydrates hardly coexist with aqueous Cl
− [
57,
58], Equation (3).
Friedel’s salt is prone to instability and influenced by the alkalinity level; as alkalinity decreases due to carbonation, the salt becomes more soluble and releases chlorides into the pore solution [
55].
The aforementioned indications were consequently evaluated by using H2O as a cleaning agent in a 1:1 ratio by weight to the quantity of sample to be cleaned until ionic equilibrium was attained, as determined by a pH meter/conductance meter from PC5000 EUTECH Instruments (the average pH alteration in a heterogeneous solution was from 8.33 to 7.4).
The sediment washing treatment, which involved flowing water, reduced the salt concentration within the sedimentary material. This was achieved by removing ions present in the solution, including sodium, chlorides, magnesium, sulphate, calcium, and carbonates. Therefore, this change is associated with the enhanced workability observed in the washed sediments, which exhibited flow peaks higher than 100% for samples M_S1H20 and M_S2H20. At 28 days of curing, the hardened cement mortars subjected to sediment washing exhibited reduced flexural and compressive strength compared to the corresponding mortars that were characterised by interstitial seawater. This decline is associated with decreased salt concentration and reduced density in the hardened mortars, which leads to a more porous structure following washing with H2O.
Organic materials generally display hydrophobic behaviour, which is detrimental to developing hydration reactions. However, hydrophilic behaviour can be obtained through oxidising treatment. The oxidation process results in the formation of defects and holes on the surface of the carbon material, which can facilitate enhanced physical interactions and, consequently, a stronger anchorage and greater strength in the hardened cement mortar. Furthermore, the oxidation process can alter the chemical composition of the organic material’s surface. These chemical modifications are associated with forming oxygen-containing functional groups on the surface, which enhance the interaction with cement, thereby facilitating the interaction between silicates and aluminates with the generated groups. Because of the oxidation process, the polarity of these groups is increased, as is the wettability of the material. This results in a reduction in the workability of cement mortars due to the reduction in the availability of water to lubricate fresh mixes. Additionally, physical alterations are observed because the oxidation treatments enhance the surface texture of the organic material, thereby facilitating the incorporation of fresh cement paste into the voids created on the treated algae surface [
59].
Following oxidative washing with H2O2, the most evident results were obtained on the sample with the most significant organic component, S1. Indeed, following oxidation, S1 underwent a percentage reduction in organic compounds, which was accompanied by a correlated reduction in ∆ flow of 40%, in the corresponding mortar M_S1H2O2, due to the greater absorption of H2O by the degraded organic component. In contrast, following oxidation, S2 suffered a minimal percentage reduction in OM and a zero reduction in ∆ flow, in the corresponding mortar M_S2H2O2.
The data obtained in mortars from sediments treated with hydrogen peroxide (H
2O
2) yielded favourable results for sample S1, with a strength increase of 24% compared to the same in the as-is condition. By degrading organic particles, the reagent responsible for oxidation led to a decrease in the inhibition of mechanical strength development by organic particles. Furthermore, for sediment S2, which is less rich in organic component, oxidation with H
2O
2 did not bring any substantial changes in the mechanical behaviour of the sediment compared to the control sample (
Figure 6).
Following the SEM-EDX investigation of the mortar samples with S1 sediment and the same subjected to oxidising washing with H
2O
2 (M_S1, M_S1
H2O2), a variation in terms of the chemical composition of the organic fibres was highlighted, with a reduction in the intensity of the C peak within the spectra obtained from the analysis (
Figure 7A,B). Furthermore, an alteration in the fibre structure was observed, which, following the oxidising treatment, was found to be more degraded and amalgamated within the conglomerates.
Conversely, the Si peak became more relevant within the spectrum in mortars obtained with sediment S2, which has fewer organic fibres. Mortar is a data point that distinguishes the marine sediments under study, as defined in the literature on their chemical–mineralogical composition. The microstructural analysis correlated the increased compressive strength of M_S1_H
2O
2 mortar samples compared to M_S1 and the reduction in the organic content of the S1 sediment sample pre- and post-oxidative treatment. This, in turn, is correlated with the degradation of the organic particles’ structure, as visually evidenced in
Figure 7B. Indeed, as evidenced by
Figure 7A,B and the accompanying EDX spectra, the degradation of organic particles coupled with a reduction in available organic content facilitated the development of a positive response and increased compressive strength in the conglomerate sample produced.
A similar observation can be made for the M_S2 mortar sample, produced from untreated S2 sediment. This sample, less rich in organic components as discernible from
Figure 7C, exhibits fewer discontinuities and greater interaction between aggregate and hydration products, thereby achieving higher compressive strength values even without pre-treatments.
2.3. Influence of SAP Additive on the Rheological and Mechanical Behaviour of Mortars
The study aimed to examine the impact of a superabsorbent reagent on marine dredged sediment cement mortars. The investigation was focused on sample M_S1, which exhibited a higher organic residue and interstitial water content, to show how variations in water retention, resulting from differing mix compositions and reagent dosages, might influence the rheological and mechanical performance of cement mixes under identical operational conditions. From a technical and procedural point of view, the additive was added simultaneously during the mixing phase with cement Portland 42.5 R and wet marine sediments.
The data demonstrates a distinct response to the workability test of the mortars when the dosage of SAP is varied. The percentage of workability of the mixture consisting only of the S1 sediment sample (White) mixed with a w/c ratio of 0.8 is equivalent to the indicative value of the normalised mortar M1. Moreover, mortar samples showed a progressive reduction in spreading capacity with increasing additive concentration. Considering the aforementioned data, it can be stated that the mortar’s workability reduction is correlated with the instantaneous capacity of water absorption by the superabsorbent additive once the minimum dosage threshold is exceeded (0.5%) (
Figure 8).
A comparative analysis of the data obtained from the flexural and compressive fracture tests conducted on mortars treated with SAP revealed, in the case of a w/c ratio of 0.8, a progressive increase in strength with the quantity of additive incorporated into the mixtures.
Samples with a water/cement ratio of 0.5 showed values in the same range as the reference, but with a declining trend at increasing SAP concentration. This phenomenon can be attributed to the capture of water available in the mortar, which consequently limits the hydration reactions and, in turn, the compressive strengths after 28 days of curing. This effect was observed for a water-to-cement ratio of 0.5, in contrast to that of 0.8, due to lower water content (
Figure 9 and
Table 4).
The development of strength in mortar samples containing SAP was studied over 90 days, with samples characterised by both w/c ratios of 0.8 and 0.5. This is illustrated in
Figure 9. The analysis confirms the increasing trend in the strength development for the samples mixed with a w/c ratio of 0.8. In contrast, the decreasing development of resistance is confirmed for the samples with a reduced water content of 0.5 after 90 days. Specifically, after 90 days of curing, the samples M_S1_SAP
2 with a w/c ratio of 0.8 exhibited a 15% increase in strength compared to the white sample [0.8].
The results indicate that the additive SAP is a promising option for reducing excess water in dredged sediments. However, the dosage must be carefully calibrated to avoid compromising the post-curing strength.
2.4. Effect of Sodium Silicate Application on the Mechanical Performance of Concrete Mixes
The effects of sodium silicate in cementitious mortars were studied uniquely on sample S2, with a lower organic fraction. As observed, this tends to reduce the development of hydration reactions and, consequently, the resulting mechanical performance of conglomerates (
Table 5).
The S2 sediment sample White was considered a reference. It exhibited a lower workability compared to the normalised M1 standard. Starting from a weight percentage of 10% SS, a progressive reduction in the spreading capacity was verified. This confirms the capacity of sodium silicate to accelerate setting (
Figure 10).
The fracture test results demonstrate a gradual decline in strength. The compressive strength values were below the threshold values, with a notable decrease observed in specimens with sodium silicate dosages ≥ 10%.
At first glance, this unusual strength behaviour can be correlated to the additive’s chemical composition and its interactions with the sediments in the mixes.
Sodium silicate is regarded as an accelerating admixture in the cement field. It can increase the degree of hydration of the cement during the initial few hours, thereby reducing the setting time and accelerating the hardening process over the first 24 h. Conversely, alkaline accelerators such as sodium silicate have been found to impair mechanical performance when subjected to long curing times [
60].
The reduction in strength observed in mortars containing sodium silicate can be attributed to the chemical reaction between alkali introduced by the additive and the silica present in the sediment (reaction between silica and alkali in the moisture (4)) [
60]. The alkali-silica reaction (ASR) is a chemical phenomenon that causes the aggregate to expand due to the formation of a viscous gel, which increases its volume by water absorption , as shown in
Figure 11. This increase in volume generates expansive pressure within the silica aggregate or at the interface between cement paste and aggregate, resulting in a loss of stiffness and strength.
Microstructural analyses of sample M_S2
_SS
10, particularly relevant due to the loss of mechanical properties, revealed the presence of micrometre-scale fractures within the cementitious matrix. This discontinuity at the matrix level, developed in the mortars where the sodium silicate-based additive was added, confirms the critical issues identified in the mechanical compressive strength tests. In contrast, for the mortar sample with 5% SS (M_S2_SS
5), the negative influences in terms of mechanical strength are lower, as shown by the Rc data in
Table 5, and this is confirmed at the microscopic level (
Figure 12C) where no fractures are present within the matrix.