1. Introduction
The constantly growing problems related to the existing excessive use of raw materials and fossil fuels by humans, combined with excessive consumerism and waste generation, have resulted in an urgent need to find new ways to produce goods. An important role in this challenge is played by the use of secondary raw materials, rich in still useful compounds and substances, but—directed imprudently to landfills or incineration plants. In this way, approaches that fit into the ideas of the circular economy and bioeconomy, based on constantly maintaining a high value of materials and products through their turnover in closed loops, are becoming more and more important. Continuously developed solutions together with a well-established system approach and the involvement of all relevant entities can result in even more efficient use of valuable raw materials.
The area of interest of the bioeconomy includes organic materials, such as bio-waste, and green or agricultural waste. As substrates rich in organic carbon, they are currently mainly subjected to composting or anaerobic digestion processes; however, their potential is constantly recognized also in other areas, such as biorefinery processes [
1]. Despite the development of this branch in recent years, so far it does not take into account the possibility of coupling “conventional” waste processing processes with the production of valuable biochemicals or biofuels by converting generated process gases [
2]. However, the bio-waste composting process, during which net carbon monoxide (CO) production has been observed, has the such potential [
3,
4,
5,
6,
7,
8].
So far, research on CO production from aerobic bio-waste processing is characterized by a high degree of uncertainty, largely based on sometimes contradictory reports on the optimal conditions for the formation of this gas. However, analyses conducted by a few researchers in the 1990s and early 2000s identified two main variables influencing CO formation—oxygen concentration and temperature [
7,
8,
9,
10,
11]. Further studies conducted at the beginning of the second decade of the 21
st century defined the production of CO from waste composting as a combination of a dual nature—abiotic and biotic processes [
5,
6,
12,
13].
CO production is stimulated by the increased availability of O
2; higher concentrations of CO were recorded after turning the material into a compost pile due to the aeration of areas where anaerobic conditions had previously developed [
7]. In addition to the positive correlation to O
2 availability, CO generation is also temperature dependent. Based on studies conducted for soils, during which these produced CO during the day at a temperature of 30–40 °C and became a net CO sink at night (temperature <30 °C), the researchers built a hypothesis about the physicochemical sources of CO generation [
14]. This observation was confirmed by later analyses by Phillip et al. [
6], where higher CO levels were found in sterilized samples of composts. An unambiguous indication of the nature of CO formation was, however, impossible due to the observed fluctuations in the concentration of this gas during waste composting. A high level of CO is characteristic for the initial phase of the process (a few hours [
7,
11] or even 10 minutes after starting the process, temperature 35 °C [
7]); then the concentration of CO decreases and increases again after approx. 5–8 days (50 °C [
3,
7,
11]). A similar trend was also observed during analyzes of CO production from wetlands [
15]. Due to the increasing concentration of CO
2 occurring in parallel with the lowering of CO concentration, the gradual depletion of CO is associated with it’s microbial oxidation [
7]. Although the first rapid increase of CO concentration is explained by the thermochemical processes of its generation, e.g. abiotic degradation of fatty acids, polyphenols, and aromatic acids, the next peak was defined as the biotic [
8]. As reported by Haarstad et al. [
8] and Rich and King [
15] CO production during composting is linked to methanogenesis and the activity of methanogens since the strong peak of CO concentration reached even 2,022 ppm (0.2%) at a very low level of O
2.
Since it is known that a combination of abiotic and biotic processes (that can occur in parallel) are happening to stimulate or compete with each other, the issue of CO production during the bio-waste composting process should be treated holistically and the process conditions that are most conducive to its generation. The study aimed to investigate the CO production potential during bio-waste composting under controlled laboratory conditions depending on different aeration rates and temperatures. For this purpose, a series of composting processes were carried out in conditions ranging from ~psychrophilic to thermophilic (T = 35, 45, 55, and 65 °C) and aeration rate in the range of 2.7 to 7.8 L·h−1. Daily measurements of CO concentration were used to determine the kinetic parameters of the decrease in CO concentration, to find optimal conditions for its generation.
4. Discussion
The conducted research proved that CO concentration varies depending on the temperature of the process and the level of aeration. Observations made for individual composting variants, however, pay particular attention to two CO production environments: at 35 °C and 65 °C, with simultaneous oxygen deficit.
Despite the forced, constant temperature level throughout the composting process, the phase of CO production reported earlier by the researchers was also noted during the these experiment. For each of the analyzed thermal variants, the CO level was high at the beginning of the process, and then gradually decreased after about 7 days. This finding is consistent with the trend observed for composting various fractions of organic waste, including animal dung, leaves, grass, sewage sludge with bio-waste, green waste, and livestock waste [
3,
7,
11]. The stimulation of CO production through low aeration of composted waste was also consistent for all temperature variants, as it was also associated with the highest C
COmax. Oxygen deficits was favorable for CO release at lower than optimal aeration (variant 2.7 L·h
−1) and therefore indicating to anaerobic processes as a probable source of CO production for each temperature variant. As mentioned earlier, Haarstad et al. [
8] and Rich and King [
15] came to similar conclusions in their research. During aerobic processing of municipal solid waste, the CO concentration exceeded even 2,000 ppm, which the authors explained by the activity of methanogens at intermittent O
2 loading [
8]. In turn, a closer association with anaerobic biotic H
2 generation was observed for the production of CO by wetland peats [
15].
The intensification of net CO production associated with the presence of anaerobic conditions is also confirmed by the highest CO concentrations obtained during composting at 65 °C. This suggests a connection with the biological nature of CO formation, based on the activity of anaerobic microorganisms capable of producing the enzyme carbon monoxide dehydrogenase (CODH). This enzyme catalyzes the reversible oxidation of CO to CO
2 in the water-gas shift reaction [
28] and thus it is responsible for both the production and conversion of CO. Potential microorganisms inhabiting the compost that produce oxygen tolerant CODH are e.g.,
Desulfovibrio vulgaris or
Carboxydothermus hydrogenoformans [
29]. In addition, this enzyme can be reactivated after a temporary occurrence of conditions with increased oxygen concentration [
28,
30]. Thus, turning the material after 7 days of the process could interrupt, the biological production of CO, but would restart when O
2 is depleted again.
The association of the high CO concentrations in the 65 °C thermal variant observed in this experiment with the activity of CODH-producing bacteria is based on the characteristics of the bacterial species capable of converting CO. The thermophilic CODH-producing strains discovered so far are more numerous than the mesophilic species [
31]. The conditions prevailing in the temperature variant of 65 °C in the experiment carried out here, were therefore optimal for a number of anaerobic bacterial strains for which the production of CODH was proven [
32]. Oxygen deficit (2.7 L·h
−1 aeration) together with high temperature in the climatic chamber could lead to the development of such bacterial groups as methanogenic, carboxydotrophic, hydrogenogenic, and acetogenic microorganisms, with potential representatives for which the optimum temperature is 65 °C—among others
Methanothermobacter thermautotrophicus,
Thermoanaerobacter kivui,
Carboxydothermus pertinax,
Carboxydothermus islandicus,
Calderihabitans maritimus KKC1 [
32]. It has also been proven that with increasing temperature, CODH activity increases and is associated with a greater yield of CO
2 to CO conversion [
33] and thus, in the high-temperature variant of this experiment, the expression of the CODH gene in the bacteria colonizing the composted waste could occur.
The biological production in this temperature variant may also be the reason why it was characterized by the greatest randomness, and the measured CO concentrations differed significantly from each other (high standard deviation for samples at 65 °C). Different bacterial strains, characterized by different efficiency of CO production, could have appeared in individual reactors [
34]. In turn, the analysis of the kinetics of the decrease in CO concentration during composting showed that although C
COmax was the highest for aeration of 2.7 L·h
−1 in each temperature variant, the reaction rate constant k for this level of aeration was highest at 55 °C, not 65 °C. This can be explained by the doubling time of CODH-producing bacteria; for example, for the
Methanothermobacter thermautotrophicus strain, developing optimally at 65 °C, it is reported as extremely slow, reaching up to 200 h [
32].
However, it is not only the thermophilic conditions in the experiment that indicate the biological production of CO during composting in oxygen-deficient areas. As proved by the analysis of variance, the lowest of the analyzed temperatures (35 °C) had a significant impact on the concentration of CO. Additionally, the correlation analysis showed that both for the 35 °C and 65 °C variants, the CO concentration was negatively correlated with the availability of oxygen, which also can be explained by the activity of CODH-producing anaerobes. In addition to species developing at temperatures >65 °C, this group also includes mesophiles, and the optimum of their activity is the thermal range of 30–37 °C. Among the strains known so far that function in the environment with CO, these include e.g.:
Methanosarcina barkeri,
Methanosarcina acetivorans,
Alkalibaculum bacchi,
Butyribacterium methylotrophicum (optimum reached at 37 °C) or
Acetobacterium woodii,
Rhodospirillum rubrum and
Clostridium drakei (optimum is 30 °C) [
32]. It should be emphasized that although the bacterial strains discussed above have been analyzed for CO conversion by using CODH, there are no studies that analyze the ability of the same bacteria to carry out the reverse process—net CO production using the same enzyme. The release of a small amount of CO during laboratory analyses at the end of the 20
th century, noted in the case of
Moorella thermoacetica and
Methanothermobacter thermautotrophicus, did not lead to the continuation of research [
35].
Although the composting process in individual temperature conditions (35, 45, 55, 65 °C) was carried out separately, each of the analyzed variants takes place in a real, traditional composting process. Starting from the mesophilic phase, when the temperature of the material increases through 35 °C to 45 °C, the decomposition of organic matter in the composted waste generates heat and the pile or bioreactor becomes thermophilic (55–65 °C and above) [
36]. Combining this information with the results obtained in this study, it can therefore be assumed that CO production under oxygen deficit conditions follows changes in the microbial community in the waste, which are caused by process temperature phases. In this way CO can be produced by CODH-producing bacteria; first by mesophilic species growing at 35 °C, and then by thermophiles as the process temperature increases (65 °C). Such a trend is consistent with the observations of other researchers who noted the second peak of CO production, when the temperature of the material after previous cooling increased again to thermophilic conditions [
7,
11].
As mentioned earlier, waste composting is currently not seen as a technology with the potential to be coupled with biorefinery processes. However, the observations made during this research may lead to the formulation of recommendations for the composting process focused on CO production. According to the results obtained, CO production is significantly affected by low aeration (<3.4 L·h−1) and low temperature (<45 °C). From a practical point of view, composting aimed at generating net CO could therefore be carried out in economically effective conditions, based on low efficiency of aeration systems. The composting process system would change; when controlling the thermal conditions in the pile or bioreactor, it would be advantageous to extend the mesophilic phase with temperatures close to 35 °C and not exceeding 45 °C. Then, in order to hygienize the material and simultaneously generate CO in thermophilic conditions, the material would be exposed to high temperature (65 °C). Such an artificially imposed system, however, requires prior analysis in controlled laboratory conditions, and then during pilot composting processes on a semi-technical or technical scale, so as to also assess the quality of the final product of the process. Additional requirements to a plant that utilizes bio-waste for production of CO are of course strict safety considerations due to the toxicity of the gas and developments towards, capturing and purification of CO.
Figure 1.
Bioreactors for laboratory scale composting: (
a) scheme of the bioreactor (based on [
16]), 1—closed valve, 2—covers screw cup, 3—cover edge, 4—perforated plastic screen, 5—aeration hose, 6—exhaust air outlet, 7—screw cup for temperature measurements; (
b) bioreactors in the climate chamber.
Figure 1.
Bioreactors for laboratory scale composting: (
a) scheme of the bioreactor (based on [
16]), 1—closed valve, 2—covers screw cup, 3—cover edge, 4—perforated plastic screen, 5—aeration hose, 6—exhaust air outlet, 7—screw cup for temperature measurements; (
b) bioreactors in the climate chamber.
Figure 2.
Laboratory scale composting system (based on [
16]): 1—air supply, 2—flowmeter, 3—climate chamber, 4—thermocouple, 5—bioreactor, 6—cooling system, 7—puffer bag, 8—IR gas analyzer (CO
2, % v/v), 9—gas concentration analyzer (CO, ppm; O
2, % v/v).
Figure 2.
Laboratory scale composting system (based on [
16]): 1—air supply, 2—flowmeter, 3—climate chamber, 4—thermocouple, 5—bioreactor, 6—cooling system, 7—puffer bag, 8—IR gas analyzer (CO
2, % v/v), 9—gas concentration analyzer (CO, ppm; O
2, % v/v).
Figure 3.
Properties of substrate and composts after 14 days of composting process in different temperature variants: (a) pH; (b) EC, mS·cm−1; (c) AT4, mg O2·g d.m.−1; (d) TOC, % d.m.; (e) TN, % d.m.; (f) C/N; (g) Water content, %; (h) LOI, % d.m.; (i) NH4-N, mg·kg d.m.−1; (j) NO3-N, mg·kg d.m.−1; letters (a, b, c) indicate homogeneity group according to Tukey’s test at the significance level p < 0.05
Figure 3.
Properties of substrate and composts after 14 days of composting process in different temperature variants: (a) pH; (b) EC, mS·cm−1; (c) AT4, mg O2·g d.m.−1; (d) TOC, % d.m.; (e) TN, % d.m.; (f) C/N; (g) Water content, %; (h) LOI, % d.m.; (i) NH4-N, mg·kg d.m.−1; (j) NO3-N, mg·kg d.m.−1; letters (a, b, c) indicate homogeneity group according to Tukey’s test at the significance level p < 0.05
Figure 4.
Properties of substrate and composts after 14 days of composting process in different aeration rates variants: (a) pH; (b) EC, mS·cm−1; (c) AT4, mg O2·g d.m.−1; (d) TOC, % d.m.; (e) TN, % d.m.; (f) C/N; (g) Water content, %; (h) LOI, % d.m.; (i) NH4-N, mg·kg d.m.−1; (j) NO3-N, mg·kg d.m.−1; letters (a, b, c) indicate homogeneity group according to Tukey’s test at the significance level p < 0.05
Figure 4.
Properties of substrate and composts after 14 days of composting process in different aeration rates variants: (a) pH; (b) EC, mS·cm−1; (c) AT4, mg O2·g d.m.−1; (d) TOC, % d.m.; (e) TN, % d.m.; (f) C/N; (g) Water content, %; (h) LOI, % d.m.; (i) NH4-N, mg·kg d.m.−1; (j) NO3-N, mg·kg d.m.−1; letters (a, b, c) indicate homogeneity group according to Tukey’s test at the significance level p < 0.05
Figure 6.
Average CO concentration (± standard deviation) during 14 days of composting process in (a) different temperature variants, and (b) different aeration variants; letters (a, b) indicate homogeneity group according to Tukey’s test at the significance level p < 0.05.
Figure 6.
Average CO concentration (± standard deviation) during 14 days of composting process in (a) different temperature variants, and (b) different aeration variants; letters (a, b) indicate homogeneity group according to Tukey’s test at the significance level p < 0.05.
Table 1.
Experimental design for laboratory composting.
Table 1.
Experimental design for laboratory composting.
Composting series # |
Compost substrates |
Duration of the process, days |
Temperature, °C |
Aeration rate, L·h−1
|
1 |
Bio-waste (green waste and vegetables) mixed with chopped branches |
14 |
35 |
2.7 |
3.4 |
4.8 |
7.8 |
2 |
45 |
2.7 |
3.4 |
4.8 |
7.8 |
3 |
55 |
2.7 |
3.4 |
4.8 |
7.8 |
4 |
65 |
2.7 |
3.4 |
4.8 |
7.8 |
Table 2.
Properties of substrates for composting process in different temperature variants (average ± st. dev.); d.m.—dry matter
Table 2.
Properties of substrates for composting process in different temperature variants (average ± st. dev.); d.m.—dry matter
|
Substrates for the composting process |
Properties ± st. dev. |
35 °C |
45 °C |
55 °C |
65 °C |
pH |
7.48 ± 0.07 |
5.60 ± 0.01 |
6.51 ± 0.11 |
6.75 ± 0.09 |
EC, mS·cm−1
|
3.53 ± 0.03 |
4.06 ± 0.05 |
3.09 ± 0.06 |
3.51 ± 0.04 |
TOC, % d.m. |
35.66 ± 0.07 |
33.81 ± 0.47 |
33.03 ± 0.12 |
36.94 ± 0.83 |
TN, % d.m. |
1.26 ± 0.02 |
1.50 ± 0.01 |
1.44 ± 0.03 |
1.62 ± 0.03 |
C/N |
28 |
24 |
23 |
23 |
Water content, % |
54.40 ± 0.30 |
55.70 ± 0.89 |
54.28 ± 0.32 |
61.00 ± 0.23 |
LOI, % d.m. |
69.19 ± 0.26 |
67.48 ± 0.44 |
64.15 ± 0.30 |
71.01 ± 0.37 |
AT4, mg O2·g d.m.−1
|
37.6 ± 0.2 |
64.0 ± 2.8 |
61.7 ± 1.2 |
71.1 ± 10.0 |
NH4-N, mg·kg d.m.−1
|
140.46 ± 3.02 |
850.40 ± 13.76 |
689.28 ± 44.56 |
248.08 ± 1.63 |
NO3-N, mg·kg d.m.−1
|
58.22 ± 6.10 |
82.90 ± 6.36 |
30.42 ± 12.69 |
169.62 ± 26.65 |
Table 3.
Relative process efficiency in different temperature variants (%).
Table 3.
Relative process efficiency in different temperature variants (%).
Process temperature, °C |
Aeration rate, L·h−1
|
pH |
EC |
AT4
|
TOC |
TN |
C/N |
Water content |
LOI |
NH4-N |
NO3-N |
35 |
2.7 |
12.47 |
-24.54 |
-65.38 |
-6.17 |
38.93 |
-32.14 |
3.27 |
-8.21 |
-90.94 |
-51.23 |
3.4 |
12.47 |
-25.25 |
-65.65 |
-6.87 |
43.77 |
-35.71 |
1.65 |
-8.89 |
-89.95 |
-33.10 |
4.8 |
13.87 |
-24.54 |
-65.65 |
-8.56 |
39.05 |
-32.14 |
-5.27 |
-9.83 |
-92.11 |
-55.96 |
7.2 |
15.08 |
-23.40 |
-66.18 |
-8.70 |
46.42 |
-35.71 |
-0.73 |
-11.70 |
-93.21 |
-66.07 |
45 |
2.7 |
-6.59 |
21.20 |
-78.99 |
-6.02 |
9.92 |
-16.67 |
1.01 |
-6.37 |
74.25 |
-12.06 |
3.4 |
31.17 |
11.64 |
-51.58 |
-4.22 |
17.24 |
-20.83 |
0.59 |
-7.68 |
-2.08 |
-32.01 |
4.8 |
32.06 |
-0.49 |
-27.23 |
-9.66 |
22.50 |
-29.17 |
-7.49 |
-10.22 |
-22.49 |
-4.45 |
7.2 |
32.50 |
-13.60 |
-32.91 |
-8.29 |
18.12 |
-25.00 |
-10.23 |
-9.39 |
-45.47 |
-44.19 |
55 |
2.7 |
27.59 |
-19.68 |
-46.19 |
-3.02 |
19.07 |
-17.39 |
-12.36 |
-5.15 |
-43.29 |
-7.94 |
3.4 |
27.44 |
-22.90 |
-76.23 |
-4.06 |
28.45 |
-26.09 |
-23.68 |
-8.93 |
-80.02 |
184.66 |
4.8 |
26.83 |
-26.45 |
-85.02 |
-5.16 |
20.02 |
-21.74 |
-28.44 |
-6.15 |
-79.62 |
-21.03 |
7.2 |
27.36 |
-22.90 |
-80.00 |
-8.54 |
29.52 |
-30.43 |
-28.84 |
-7.18 |
-89.53 |
-30.12 |
65 |
2.7 |
11.64 |
-18.97 |
-63.33 |
-2.55 |
20.23 |
-17.39 |
-9.44 |
-5.87 |
6.97 |
-94.06 |
3.4 |
11.56 |
-17.83 |
-69.03 |
-2.71 |
25.04 |
-21.74 |
-8.80 |
-4.67 |
-21.63 |
-98.09 |
4.8 |
14.68 |
-26.96 |
-75.93 |
-3.06 |
15.45 |
-17.39 |
-15.98 |
-4.84 |
-61.60 |
-85.16 |
7.2 |
15.72 |
-27.25 |
-52.55 |
-4.80 |
24.82 |
-26.09 |
-16.96 |
-6.18 |
-53.74 |
-89.25 |
Table 4.
The bio-waste weight loss during composting under different process conditions
Table 4.
The bio-waste weight loss during composting under different process conditions
Aeration rate, L·h−1
|
Weight loss, % |
35 °C |
45 °C |
55 °C |
65 °C |
2.7 |
Total |
11.44 ± 1.05 |
4.90 ± 2.50 |
7.48 ± 0.82 |
9.94 ± 0.96 |
As leachate |
5.95 ± 1.03 |
0.99 ± 1.71 |
16.47 ± 1.65 |
9.20 ± 2.98 |
3.4 |
Total |
11.66 ± 1.16 |
8.09 ± 3.87 |
12.51 ± 0.85 |
12.04 ± 2.02 |
As leachate |
6.18 ± 0.35 |
2.88 ± 2.50 |
18.84 ± 2.47 |
5.41 ± 4.69 |
4.8 |
Total |
13.64 ± 0.41 |
15.83 ± 9.10 |
16.15 ± 0.09 |
16.20 ± 0.37 |
As leachate |
5.32 ± 0.83 |
7.43 ± 7.21 |
20.03 ± 0.82 |
12.31 ± 1.18 |
7.8 |
Total |
13.59 ± 0.76 |
12.88 ± 8.07 |
13.26 ± 1.27 |
16.14 ± 2.94 |
As leachate |
5.80 ± 1.86 |
4.71 ± 4.93 |
20.10 ± 2.88 |
14.61 ± 4.09 |
Table 5.
CO production kinetics during composting under different temperatures and aeration.
Table 5.
CO production kinetics during composting under different temperatures and aeration.
Process T, °C |
Aeration, L·h−1
|
Reaction order |
CCOmax, ppm |
k, d−1
|
a=k·CCOmax, ppm·d−1
|
35 |
2.7 |
1st-order |
185.3 ± 21.4 |
0.846 ± 0.025 |
156.5 ± 15.6 |
3.4 |
1st-order |
109.5 ± 52.5 |
0.822 ± 0.185 |
90.4 ± 43.1 |
4.8 |
1st-order |
101.0 ± 19.0 |
0.834 ± 0.160 |
86.2 ± 32.5 |
7.8 |
1st-order |
120.1 ± 77.7 |
0.850 ± 0.335 |
119.4 ± 120.5 |
45 |
2.7 |
1st-order |
103.1 ± 44.0 |
0.185 ± 0.053 |
18.5 ± 8.8 |
3.4 |
1st-order |
214.6 ± 84.7 |
0.453 ± 0.301 |
114.2 ± 116.2 |
4.8 |
1st-order |
95.6 ± 12.4 |
0.218 ± 0.041 |
21.1 ± 6.5 |
7.8 |
1st-order |
80.2 ± 18.2 |
0.179 ± 0.092 |
14.9 ± 10.2 |
55 |
2.7 |
1st-order |
471.9 ± 283.4 |
0.816 ± 0.496 |
478.8 ± 530.0 |
3.4 |
1st-order |
168.8 ± 84.4 |
0.338 ± 0.088 |
61.9 ± 46.1 |
4.8 |
1st-order |
153.0 ± 19.3 |
0.410 ± 0.051 |
62.2 ± 5.0 |
7.8 |
1st-order |
183.9 ± 87.3 |
0.434 ± 0.157 |
89.0 ± 61.6 |
65 |
2.7 |
1st-order |
403.6 ± 43.1 |
0.422 ± 0.090 |
172.8 ± 56.2 |
3.4 |
1st-order |
127.5 ± 89.1 |
0.183 ± 0.111 |
29.9 ± 27.6 |
4.8 |
0-order |
– |
– |
0.09 ± 0.1 |
7.8 |
1st-order |
161.9 ± 152.2 |
0.670 ± 0.620 |
92.0 ± 73.2 |