3.1. Carbonization Tests and Char’s Characterization
During the dry carbonization process, it was observed that the sample consisting solely of RDF pellets exhibited greater particle aggregation, which gradually decreased with the addition of biomass. Under all conditions tested, the chars showed a dark and homogeneous color. The mass yield of the chars decreased as the amount of biomass in the sample increased (
Figure 2a). The char produced by RDF pellets without biomass incorporation had a mass yield of 66%, whereas the yield decreased to 57.3% with greater biomass incorporation. The sample with 10% biomass had an average mass yield of 65.2%. Additionally, the apparent density of the chars gradually decreased as the biomass content increased. For the sample composed only of RDF pellets, the apparent density was 0.607 g/cm
3, which is an 11.5% decrease compared to the raw RDF pellets (0.686 g/cm
3). In samples with 10% and 25% biomass content, the apparent density decreased to 0.593 g/cm
3 and 0.572 g/cm
3, respectively.
The hydrochars produced from RDF pellets had a homogeneous appearance and a dark color that varied depending on the temperature applied. The samples produced at 250°C had more agglomerates and a slightly lighter brown color compared to the samples produced at 300°C, which had a smaller particle size and a black color. As the carbonization temperature rises, there was a corresponding decrease in hydrochar yield (
Figure 2b), consistent with previous research [
35]. Additionally, increasing the S/L ratio was found to have a negative impact on mass yield. The highest yield was achieved at a temperature of 250°C with an S/L ratio of 1:2.5 (69.3%). Conversely, the lowest yield was observed at a temperature of 300°C with an S/L ratio of 1:5 (59.3%).
The increase in carbonization temperature from 250°C to 300°C had a greater impact on increasing the apparent density at an S/L ratio of 1:2.5, but this behavior was not observed at 1:5. Additionally, increasing the S/L ratio seemed to have a negative effect on the value at 250°C. The hydrochars with the highest apparent density were produced at 250°C in an S/L ratio of 1:2.5 (0.564 g/cm3), while the lowest value was observed in hydrochars produced at the same temperature but in an S/L ratio of 1:5 (0.417 g/cm3). The samples produced at 300°C had values of 0.430 g/cm3 at the S/L ratio of 1:2.5 and 0.465 g/cm3 at the S/L ratio of 1:5.
The proximate composition of the raw RDF, chars and hydrochars is detailed in
Table 2. The moisture content of samples without the addition of biomass averaged 2.5%, increasing to 3.0% with the inclusion of 10% biomass. However, when the biomass content was increased to 25%, the moisture content reduced to 2.6%, indicating a non-uniform pattern in relation to the biomass addition. Carbonization led to the production of more hydrophobic chars with lower moisture content compared to the raw waste. Additionally, the process release moisture and volatile matter from the raw waste, which leads to higher fixed carbon in chars, especially in the dry carbonization process.
The volatile matter and ash contents decreased with the increase in the percentage of biomass in the samples due to the greater devolatization of this fraction at the applied carbonization temperature (400°C) and the higher ash content present in the RDF components compared to biomass [
36]. Consequently, the sample without biomass had the highest value of volatile matter in chars (63.1%), while the sample with the highest biomass content exhibited the lowest value (55.2%). Char produced with 10% biomass showed an intermediate value (60.8%). The ash content exhibited the same trend, with the highest value of 26.3% found in the RDF pellet char sample and gradually decreasing to average values of 25% and 21.6% in samples with 10% and 25% biomass incorporation, respectively. The fixed carbon content raised proportionally to the increase in biomass incorporation into the sample. Adding 10% biomass led to a 33.4% increase in fixed carbon content, from 10.6% to 14.2%. With 25% biomass incorporation, the fixed carbon content more than doubled compared to the sample without biomass, reaching 23.1%.
Regarding the hydrochars, it was observed that the moisture content is affected by both temperature and the S/L ratio. Higher temperatures and S/L ratios were seen to reduce moisture content, with the lowest value of 1.6% observed in hydrochars produced at 300°C with an S/L ratio of 1:5. Conversely, the highest moisture content at 2.7% was found in samples at 250°C with the same S/L ratio. When considering volatile matter, the S/L ratio had a more significant effect than temperature. An increase in volatile matter was noticed in samples with a 1:5 S/L ratio, with percentages of 72.8% and 71.4% for hydrochars produced at 250°C and 300°C, respectively.
The ash content did not showed a consistent pattern, with 250°C samples ranging from 21.0 to 22.5%, and the lowest percentage occurring at an S/L ratio of 1:5. At 300°C, the trend was reversed, with the lowest ash content at 17.2% in the 1:2.5 S/L ratio sample, which then increased to 20.3% at a 1:5 ratio. As the carbonization temperature rose, there was a corresponding increase in fixed carbon content, which was inversely related to the S/L ratio. For example, hydrochars produced at 300°C with a 1:2.5 S/L ratio had an average fixed carbon content of 13.6%, while those produced at 250°C with a 1:5 ratio had only 6.1%.
The elemental composition of the raw wastes, chars, and hydrochars is showed in
Table 3. Both carbonization processes increased the concentration of carbon and nitrogen compared to the raw RDF pellet sample. This rise was more noticeable in the dry carbonization tests with an increase of 21.2% of carbon content for chars produced at 400°C. Additionally, there was a significant reduction in oxygen concentration and the absence of sulfur in the chars, which is a benefit of the dry carbonization process.
For chars, the concentration of carbon and nitrogen exhibits a marginal rise upon the addition of biomass compared to the sample consisting solely of RDF pellets. Hydrogen content showed a modest increase with a 10% biomass incorporation, then declines as biomass content reaches 25%, while sulfur was absent in all samples. The increase in carbon concentration associated with the decrease in hydrogen concentration reduces the H/C ratio of char and improves its fuel properties [
37]. Oxygen content falls with a 10% biomass addition but escalates at 25%, predominantly due to the decreased hydrogen and ash quantities.
In hydrochars, the temperature increase did not affect the carbon concentration significantly, but it led to a slight increase in the nitrogen concentration. Regarding the increase in the S/L ratio, the carbon content showed an increase at 250°C, while it remained nearly constant at 300°C. However, the temperature rise caused a small reduction in the hydrogen content and an increase in the nitrogen and oxygen concentrations. Throughout all samples, the sulfur concentration accounted for 0.2% of the total.
The Van Krevelen diagram (
Figure 3) indicates that the reduction in the O/C ratio was much more pronounced in char samples, with values similar to bituminous coal, while the reduction observed in hydrochars led to values closer to lignite. The incorporation of biomass in the samples was found to lower this ratio compared to the sample consisting only of RDF pellets, although a proportional reduction to the biomass addition was not observed, where the lowest value was in the sample with 10% biomass. In the case of hydrochars, the lowest S/L ratio demonstrated to have a greater influence than the carbonization temperature. The decrease in oxygen concentration is primarily caused by the dewatering, dehydration, and decarboxylation reactions that occur during both carbonization processes. However, these reactions were more noticeable in the dry carbonization experiments, possibly due to the higher temperature severity [
38].
In terms of the H/C ratio, the reduction was more subtle compared to the raw RDF. The increase in biomass content in chars was directly related to the reduction of this ratio, while in hydrochars, the increase in the S/L ratio had a greater impact on reducing the value. For all the chars and hydrochars produced, the H/C ratio ranged from 1.23 to 1.49, while for the raw RDF it was 1.53. This demonstrates a less noticeable reduction compared to the O/C ratio as observed in other studies [
39].
The HHV of the chars is represented in
Figure 4a. It has been observed that the incorporation of biomass does not significantly affect the HHV of chars. The HHV for pellet chars without biomass incorporation is 25.0 MJ/kg, and with 25% incorporation, it is 25.1 MJ/kg. However, the sample with 10% biomass showed a lower value of 23.6 MJ/kg. On the other hand, it has been found that the washing process is associated with an increase in the HHV of chars. In all conditions, the char exhibited a higher HHV value than the chars before the washing process.
The increase in this parameter was gradual to the incorporation of biomass, where the highest value obtained was 25.9 MJ/kg in chars with 25% biomass. The sample composed only of RDF pellets presented a value of 25.4 MJ/kg, while in the sample with 10% biomass incorporation the value was 25.6 MJ/kg. The increase in HHV of chars after the washing process was also reported in previous work [
34]. The HHV of hydrochars can be seen in
Figure 4b. Increasing the temperature from 250°C to 300°C demonstrated an influence on the HHV of hydrochars produced at the S/L ratio of 1:2.5. At the lowest temperature, the HHV was 19.7 MJ/kg, while at 300°C this value was 21 MJ/kg. At the S/L ratio of 1:5, the HHV was slightly higher in the sample produced at 250°C (20.5 MJ/kg) when compared to the sample produced at 300°C (20.0 MJ/kg).
The composition of chars and hydrochars ashes is represented in
Table 3. CaO and Al
2O
3 correspond to the largest fraction in all samples. The incorporation of biomass in a greater proportion caused a reduction in these components in relation to RDF pellets, however the addition of 10% demonstrated a slight increase.
Table 3.
Ash mineral composition from the chars and hydrochars.
Table 3.
Ash mineral composition from the chars and hydrochars.
Ash mineral composition |
Dry carbonization |
Hydrothermal carbonization |
100P |
90P10B |
75P25B |
100P 250°C/1:2.5 |
100P 300°C/1:2.5 |
Oxides (%, w/w) |
Al2O3
|
13.9 |
14.1 |
12.5 |
19.6 |
13.8 |
CaO |
30.8 |
32.6 |
29.4 |
35.6 |
22.1 |
Fe2O3
|
5.4 |
4.3 |
3.7 |
4.8 |
3.1 |
K2O |
3.2 |
3.4 |
3.3 |
1.3 |
0.8 |
MgO |
9.0 |
9.5 |
9.8 |
5.3 |
4.4 |
Na2O |
1.8 |
1.9 |
1.9 |
0.8 |
0.5 |
SiO2
|
0.2 |
0.3 |
0.4 |
6.7 |
0.5 |
TiO2
|
0.6 |
0.6 |
0.7 |
0.3 |
0.2 |
Fouling and slagging index |
B/A |
3.4 h |
3.4 h |
3.5 h |
1.8 h |
2.1 h |
BAI |
1.1 l |
0.8 l |
0.7 l |
2.4 l |
2.3 l |
Fu |
7.5 h |
7.6 h |
7.6 h |
0.1 l |
0.4 l |
S/A |
0.0 l |
0.0 l |
0.0 l |
0.3 m |
0.0 l |
TA |
5.0 h |
5.3 h |
5.2 h |
2.0 h |
1.3 h |
Chlorine (%) |
0,4 |
0.4 |
0.4 |
1.0 |
1.1 |
Ash (%) |
26,3 |
25.0 |
21.6 |
17.2 |
21.0 |
Apart from Fe
2O
3, which reduced its concentration with the incorporation of biomass, and K
2O, which remained at constant levels, the other elements showed an increase in relation to char produced only by RDF pellets. This increase was most evident in MgO concentrations, characteristic of the biomass composition [
40]. In relation to hydrochars, the increase in the carbonization temperature led to the reduction of all analysed elements.
The reduction of alkaline compounds such as K, Mg, and Na in hydrochars led to a reduction in the base/acid ratio (B/A) and, more significantly, in the fouling index (Fu). This reduction meant that these samples were categorized as having a low tendency to form scale (<0.4) compared to char samples. The agglomeration index (BAI) was low in all samples, with hydrochars showing a lower trend. A lower BAI value (<0.15) indicates a higher probability of agglomerate formation in the reactor bed. The tendency for slag formation (S/A) was low in all samples (<0.3), except for the hydrochar sample at 250°C, which fell within the medium trend category. The potential for the formation of ash layers (T/A) was high (>0.3) in all samples, but there was a significant reduction in hydrochars [
32].
The chlorine content of the chars is represented in
Figure 5a. Prior to the washing process, only the sample with the highest biomass incorporation had a value lower than 1% (0.9%). However, due to the heterogeneity of the RDF composition, variation in this value does not guarantee that this composition produces chars with chlorine contents within the permitted limit for use as an alternative fuel. After washing, the samples exhibited a significant reduction in this parameter, with the final concentration at around 0.4% for all three samples. This reduction ranged from 73.4% in the sample without biomass to 61.7% in the sample with the highest percentage of this fraction.
Figure 5b shows the chlorine content of hydrochars, where increasing the carbonization temperature demonstrated a slight increase in this parameter. Conversely, increasing the S/L ratio in the HTC process led to a significant reduction in chlorine content. At a temperature of 250°C, the increase in the S/L ratio represented a 39.6% reduction in chlorine content (0.6%) compared to the S/L ratio of 1:2.5 (1.0%). Similarly, at a temperature of 300°C, the chlorine content decreased by 44% when the S/L ratio was increased from 1:2.5 to 1:5.
The thermogravimetric profile of chars and hydrochars can be seen in
Figure 6. For chars, the most significant mass loss occurred between 235-540 °C, with a gradual reduction as the temperature increased (
Figure 6a). Up to 235°C, the reduction ranged from 2.8-5.8%, with the sample composed solely of RDF pellets showing a greater reduction, likely due to the higher moisture content of the pellets compared to biomass. The temperature range where the greatest mass loss occurred represented between 65-66.4%, being proportionally higher with the increase in the incorporation of biomass, due to the high degradation of the components of this fraction (mainly hemicellulose and cellulose) in this temperature range [
41]. In the sample with greater biomass incorporation, the temperature range of greater mass reduction extends to approximately 600°C.
Regarding the hydrochars, the mass loss up to 235°C was like that observed for pellet chars (5.1-5.4%) in samples produced at the S/L ratio of 1:2.5. However, increasing the ratio to 1:5 resulted in a smaller mass reduction up to this temperature (3.8%). The chars produced by HTC exhibited greater thermal resistance, as the mass reduction was lower in the temperature range observed in the chars, and at 540°C the mass loss was 57.5-61% (
Figure 6b). Furthermore, the temperature at which mass loss stability occurred was higher when compared to chars produced from dry carbonization (~ 600°C).
The thermal differential graphs indicate that there is an initial peak of greater mass reduction up to 150°C, which is attributed to water loss. This is more noticeable in chars (see
Figure 6c) due to their higher moisture content. The highest peak of thermal degradation starts at 200°C and extends up to 440°C, being more evident in the sample with 10% biomass incorporation. Although the sample with the highest percentage of biomass exhibited a smaller peak in this temperature range, it was broader and extended over a greater temperature range. A similar behavior was observed in the second peak of maximum degradation, between 700 and 780°C, which was more noticeable at the lowest temperature in the sample with 10% biomass.
Figure 6d shows the thermal degradation rate of hydrochars. The largest peak occurred at temperatures close to that observed in chars (around 420°C). However, there is a prominent peak between 270-325°C, which may be related to the higher devolatilization of hydrochars due to their higher volatile matter content. This peak was more pronounced in the sample with the highest volatile content (250°C, S/L 1:5), being higher than the peak observed at the temperature of greatest degradation, and less noticeable in samples produced at 300°C. In contrast to chars, two other peaks of greater degradation of hydrochars were observed, one between 600-650°C and the other between 700-780°C.
The ignition and burnout temperatures were estimated according to the intercepted method, and the results are represented in
Table 4. The maximum degradation temperatures and the degradation rate in the two main peaks observed in the DTG are also presented. The addition of biomass into RDF pellets in chars demonstrated little influence on Ti and Tb, although there was a slight increase in the sample with a higher percentage of this fraction. Conversely, hydrothermal carbonization seems to influence the reduction of Ti and increase Tb, except for hydrochar at 250°C at the lowest S/L ratio. It is important to note that a decrease in Ti increases the risks of auto-ignition of chars during storage and transportation [
42], while an increase in Tb requires higher temperatures for complete degradation [
43] during admission to gasifiers, for example.
The FTIR profiles of the chars produced only from RDF pellets and with 25% biomass incorporation, in addition to the hydrochars produced at 250 and 300°C in an S/L ratio of 1:2.5 can be seen in
Figure 7.
The band between 3429-3376 cm-1, which corresponds to the stretching of O-H bonds, was more noticeable in the samples composed only of RDF pellets, while in the char sample with biomass incorporation this band was more discreet, representing the largest elimination of these elements as demonstrated in the Van Krevelen diagram.
The bands observed between 2951-2849 cm
-1, attributed to stretching vibrations of the C-H bonds, were observed in all samples, being more evident in chars, especially in those produced from 100% RDF pellets. A greater number of bands between 1600-1200 cm
-1 in the hydrochars samples, as well as a more pronounced band at 755 cm
-1, suggests a greater degree of aromaticity of these chars [
18].