Open Access Article
This Open Access Article is licensed under a Creative Commons Attribution-Non Commercial 3.0 Unported Licence

Enhancement of biogas production using nanostructured magnetite (Fe3O4) in a biodigester fed with Peruvian guinea pig manure

Rosa Flores Vargas, William Eduardo Gómez Hernández, Karenina Ela Macazana López, Clemente Alfredo Luyo Caycho, Yelstin Adrian Muñoz Baca, Harry Anderson Rivera Tito and María Esther Quintana Cáceda*
Center for the Development of Advanced Materials and Nanotechnology, National University of Engineering, Av. Tupac Amaru 210, Lima 25, Peru. E-mail: mquintana@uni.edu

Received 6th January 2025 , Accepted 11th March 2025

First published on 9th May 2025


Abstract

Magnetite nanoparticles were used to increase biogas production in a biodigester fed with Peruvian guinea pig (Cavia porcellus) manure (PGPM). The nanoparticles were synthesized via two different methods—coprecipitation and polyol—and thus showed different sizes of 410.7 nm and 34.03 nm, respectively. Likewise, various configurations were tested using three distinct Fe3O4 proportions, with each configuration tested in triplicate biodigesters. The coprecipitation trial with Fe3O4 was tested with an initial substrate of 5.57 g of chemical oxygen demand (COD) and 0.96 g of volatile solids (VSs) as inoculum. This ferrous additive led to a methane production increase of up to 9.61%, with a biodegradability of 57.91%. At the same time, the polyol trial with Fe3O4 was tested with an initial substrate of 34.47 g of COD and 0.80 g VS as inoculum, increasing methane production by up to 64.5% with a biodegradability of up to 8.56%. Moreover, the inhibitory effect of the synthesized Fe3O4, which was inconsequential for bacterial growth, was analyzed. Therefore, these nanoparticles have been shown to support methanogenic bacteria in enhancing methane production.


Introduction

Biogas is a gaseous mixture primarily composed of methane (CH4) and carbon dioxide (CO2); it also contains traces of other gases such as hydrogen (H2) and hydrogen sulfide (H2S) and is formed through the decomposition of natural organic matter (OM) in an anaerobic environment.1,2 Among these gases, CH4 stands out for its calorific value of around 7.0 kWh m−3 (considering an average 65% CH4 and 35% CO2 biogas composition).3 Furthermore, among the trace gases, H2S is noteworthy as it is responsible for the strong and unpleasant odor associated with biogas.4

As its name suggests, biogas is naturally formed through a biological pathway and is therefore widely present in nature.1 It can be found in swamps, ruminants' stomachs,5 and sanitary landfills.6 In the latter, when there are high OM levels, such as in landfill leachate, its decomposition produces biogas due to the low solubility of oxygen (O2) in water. This gas is chemically similar to the natural gas found in fossil fuel deposits.4 In terms of energy content, 1 m3 of biogas is equivalent to 0.6–0.65 L of petroleum.3

Moreover, the European Union retrieves methane (CH4) from sanitary landfills. For example, Germany leads in biogas production owing to its positive legal framework established in 2000 for renewable energy sources, which has promoted the development of biogas facilities throughout the country.1 Currently, there are over 10[thin space (1/6-em)]000 facilities across Germany.7 Similarly, in Asia, thanks to programs that fomented the construction of digesters,3 China has over 100[thin space (1/6-em)]000 biogas plants.7 This overview stands in stark contrast to Peru's efforts, as Peru is still far from reaching the renewable energy production goal set for 2030, which is 20%.8 As of 2022, Peru has converted only 5.9% of its energy matrix to unconventional renewable energy,9 of which only 0.1% is derived from biomass,10 despite the country's potential for renewable energy production (solar, wind, and biomass).11 Likewise, Peru generates a large volume of agricultural and commercial fishing waste, which is discarded,12 although it could be used for biogas production and thus tackle three major national needs: (1) improve organic waste disposal sanitation; (2) generate renewable energy and (2) supply stabilized materials, such as biofertilizer, that can be used in agriculture.3 Farm animal waste has already been used in biogas and energy production, with an array of different applications according to Monteros et al.13

Biogas production occurs through a complex biotechnological process of anaerobic digestion, where a consortium of bacteria degrades the OM in a coordinated manner.4 The essential condition to ensure the success of the process is the absence of O2. Biochemical and microbiological studies have thus far divided the process into four phases: hydrolysis, acidogenesis, acetogenesis, and methanogenesis.3 Anaerobic digestion has been extensively studied. However, despite being a promising method for treating large quantities of waste, it remains a low-efficiency process, which limits its ability to compete in the current fuel market.14 Since hydrolysis is the rate-limiting step of the process, several studies have focused on this phase to make the digestion process more efficient using chemical or physical pretreatments, such as the one reported by Hu et al.14 where oxidative methods were applied to enhance the degradation rate of sludge from a water treatment plant. Other studies evaluated the effect of component addition during digestion, as reported by Casals et al.15 who investigated the effect of adding magnetite (Fe3O4) nanoparticles of 7 nm into an anaerobic reactor for waste treatment.

Their results showed that biogas production per gram of OM increased by up to 180% when working with 100 ppm of Fe3O4, approximately 2.8 times the typical output. Huamán et al.16 also evaluated the effect of adding Fe3O4 particles sized 0.5–1.0 mm during anaerobic digestion. They used pig manure and evaluated the effect of two Fe3O4 dosages: 8 g and 12 g. The best results were obtained with 8 g of Fe3O4, yielding 3.82 × 10−2 N m3 of CH4 kg−1 of volatile solids (VSs). It is important to note that each OM source possesses different biogas production potentials. Generally, manure from polygastric animals generates less biogas than that from monogastric animals.17 According to the Food and Agriculture Organization (FAO),3 carbon (C) and nitrogen (N) are the main nutrients for methanogenic bacteria, both of which are present in larger quantities in PGPM compared with horse, cow, bird or pig manure.18

Villargaray et al.19,20 maintain that the average amount of guinea pig manure produced by females is 28.15 g per day and 31.03 g per day for males, which implies an average daily production of 801.19 tons of guinea pig excrement per day (considering the number of guinea pigs in 2021 reported by MIDAGRI: approximately 25820[thin space (1/6-em)]000 guinea pigs).21

Therefore, this study focuses on the effect of Fe3O4 particles on biogas production using PGPM under standard conditions, taking into account the geography and the diet of the animals in situ. The effect of the nanostructured particles was evaluated using a laboratory-scale biogas prototype reactor consisting of 500 mL bottles with hermetically sealed caps adapted for this purpose. They were used to directly quantify the amount of CH4 via volumetric displacement, produced through the synergy between the OM, microorganisms, and Fe3O4 nanoparticles. Finally, this study aims to contribute to the enhancement of biogas production in sectors dedicated to the use of guinea pig manure.

Materials and methods

Chemical reagents

The materials used for the synthesis and methanogenic activity tests are listed below: Iron nitrate (III) nonahydrate (Fe(NO3)3·9H2O, ≥98%), Sigma-Aldrich. Triethylene glycol (HO(CH2CH2O)3H, ≥98%), Merck. Ethyl acetate (CH3COOC2H5, ≥98), Merck. Ethanol (C2H6O, 99.5%), Spectrum Chemical. Iron chloride (II) (FeCl2, 99%), J. T. Baker. Iron chloride (III) (FeCl3, 97%), Central Drug House (CDH). Hydrochloric acid (HCl, 37%), Spectrum Chemical. Ammonium hydroxide (NH4OH, 30%), Merck. Sodium hydroxide (NaOH, ≥97%), Merck. Bromothymol blue (C27H28Br2O5S), Merck.

Inoculum

The bacterial consortium (Fig. 1a) was collected from a biodigester of Universidad Nacional Agraria La Molina (UNALM). Moreover, the analyses of total solids (TS) and volatile suspended solids (VSS) were carried out at the SLab Peru testing and research laboratory (Table 1). The VSS/TS ratio was 0.38. This means that the amount of bacterial biomass in the inoculum was approximately 38% by mass.
image file: d5ra00102a-f1.tif
Fig. 1 (a) Bacterial inoculum and (b) dry Cavia porcellus manure.
Table 1 Values of variables analysed in the inoculum
Analysis Results
TS 48[thin space (1/6-em)]200 mg L−1
VSS 18[thin space (1/6-em)]200 mg L−1


Raw material

Dried guinea pig manure collected (Fig. 1b) from the UNALM cages was used as a feedstock bio-substrate providing MO to each experiment. Its physicochemical characteristics, such as TS, were analysed at the SLab Peru testing and research laboratory. At the same time, the percentages of carbon (C%), nitrogen (N%), carbon-to-nitrogen ratio (C/N), and moisture (H%) were determined at the Soil Laboratory of the Faculty of Agricultural Engineering of the UNALM (Table 2).
Table 2 Analysed parameters of guinea pig manure
Analysis Results (%)
TS 79.42
C 44.95
N 2.04
C/N 22.03
H 25.04


Microbial growth support

The salts necessary for bacterial growth were prepared following the guidelines of Chernicharo et al.22,23 and the amounts reported by Cendales et al.24 using a Balch-type and reducing solution.

Magnetite (Fe3O4) synthesis

Coprecipitation method. This is the simplest and most efficient chemical route to produce magnetic particles.25–28 Fe3O4 was prepared using a stoichiometric mixture of ferric and ferrous salts (eqn (1)). Thermodynamically, Fe3O4 precipitation is expected when a stoichiometric ratio of 2[thin space (1/6-em)]:[thin space (1/6-em)]1 (Fe3+/Fe2+) is maintained in an alkaline medium (pH between 8 and 14) and an inert environment since Fe3O4 is unstable and sensitive to oxidation, which would lead to the formation of maghemite (γ-Fe2O3). However, oxygen is not the only oxidizing agent for Fe3O4, as shown in eqn (2); oxidation can also occur via electron or ion transfer, depending on the pH of the suspension.29
 
Fe2+ + 2Fe3+ + 8OH → Fe3O4 + 4H2O (1)
 
Fe3O4 + 2H+ → γ-Fe2O3 + Fe2+ + H2O (2)

The main advantage of this method is that a large number of particles can be synthesized albeit at the cost of a limited size distribution. In this study, Fe3O4 was synthesized following the method described by Puca et al.,29 with slight modifications. The experimental setup is shown in Fig. 2a. FeCl3 and FeCl2 were used as precursor salts, and 50 mL solutions were prepared, with each salt dissolved in HCl. Both solutions were poured into a three-necked flask equipped with a magnetic stirring bar. The reaction was conducted in an inert environment, with N2(g) bubbled into the system for over 5 min. The flask was then heated to about 80 °C, and synthesis started by dropwise adding 50 mL of NH4OH (1[thin space (1/6-em)]:[thin space (1/6-em)]4). Thereafter, Fe3O4 was washed with distilled water until the supernatant reached a pH of ≈7. Finally, the precipitate was poured into a Petri dish and stored in a desiccator for further use.


image file: d5ra00102a-f2.tif
Fig. 2 Schematic representation of the apparatus for Fe3O4 synthesis using the coprecipitation (a) and polyol (b) methods.
Polyol method. This is a chemical reduction method to synthesize nanoparticles by reducing a portion of a salt.30 The method involves suspending the precursor (iron salt Fe(NO3)3·9H2O) in a liquid polyol (e.g. triethylene glycol (TEG)).31,32 Vega et al.33 has described in detail the reaction pathways involved in each step of nanoparticle formation. The resulting suspension is heated to approximately the boiling point of the polyol, during which a solvolysis process occurs in the initial stage (eqn (3)).

In parallel, the precursor metal dissolves in the diol, thereby reducing the salt into iron complexes, which subsequently decompose and produce intermediate species (denoted as FeAx) (eqn (4)). These species act as nanoparticle cores in the subsequent step (eqn (5)) and serve as building blocks for their self-assembly and growth.

 
Fe(NO3)3 + TEG ↔ Fe(NO3)2TEG + NO3 (3)
 
Fe(NO3)2TEG → FeAx (4)
 
FeAx ↔ Fe3O4 (5)
In this regard, Fe3O4 nanoparticles were prepared using the precursor salt Fe(NO3)3·9H2O and TEG as the surfactant-reducing agent. First, the system shown in Fig. 2b was brought to optimum conditions. Second, the precursor salt, TEG, and a magnetic stir bar were added to the three-necked flask. The reaction was carried out at three different temperatures under an inert N2(g) atmosphere: (1) 30 minutes at 120 °C, (2) 30 minutes at 180 °C, and (3) 60 minutes at 280 °C. Once the reaction was complete, the resulting product was poured into a beaker, and flocculation of Fe3O4 was carried out using ethyl acetate and ethanol. The process was repeated until the entire product had flocculated and the supernatant became colorless. Finally, the precipitate obtained was dispersed in ethanol and stored in a desiccator.

Specific methanogenic activity (SMA)

There are different methods for testing SMA. The one used as a basis for this work is described in the book Anaerobic Reactors23 and recommendations from the experiments developed by Córdova et al.34 and Cendales et al.24 To perform the tests, two glass bottles of 500 mL and 1000 mL were used. These were joined using a snap connector in the cap, through which a small hose allowed the biogas to flow from one container to the other. The digestion process was carried out inside the 500 mL bottle. In addition, 53 mL of inoculum, 32 mL of dissolved manure and 395 mL of mineral salt solution were added to each reactor.

To measure gas production during the digestion process, the volumetric displacement method was used (Fig. 3). Each 1 L bottle was prepared with a 5% NaOH solution and a few drops of bromothymol blue. Additionally, the bottle cap contained a hose extended to the bottom of the bottle so that the displaced soda could flow due to the pressure of the generated biogas, while the other end of the hose rested on a glass collector. The tests were repeated three times under mesophilic conditions (35 °C). A total of five reactors were evaluated per run (the composition of each one is shown in Fig. 4). The first reactor was the target, the second was the pattern, and the rest were evaluated to assess the effect of different F3O4 quantities. Group 1 evaluated the performance of cop-Fe3O4 (magnetite synthesized via the coprecipitation method) with an initial organic loading of 5.57 g COD. Group 2 used pol-Fe3O4 (magnetite synthesized via the polyol method) and had an organic loading of 34.47 g COD, where higher performance was achieved when working up to 100 ppm16 (100 mg per litre of mixture).


image file: d5ra00102a-f3.tif
Fig. 3 Schematic representation of the MAT system mounted.

image file: d5ra00102a-f4.tif
Fig. 4 Schematic of the whole system assembly for nanoparticle evaluation and biogas production.

Characterization equipment

Light dynamic dispersion (LDS). The 90 Plus Particle Size Analyser from Brookhaven Instruments was used. It operated using a refraction index (n) of 2.36 for Fe3O4. The LDS samples were prepared by dispersing a small amount of Fe3O4 powder in TEG. The suspension was sonicated with an amplitude of 40% per minute. Thereafter, the sample was poured on disposable cuvettes with 4 optical windows from BRAND.
X-ray diffraction. The D8 ADVANCE model from Bruker brand diffractometer was used to assess the crystal properties of Fe3O4. This was operated under a current of 30 mA, 40 kV, (2θ) range of 10°–90° and 2.5° per min and a wavelength of 1.5418 Å (λCuα).
Scanning electron microscopy. Model EVO-MA10 of brand ZEISS instruments was used to explore the Fe3O4 morphology. This was operated under 20 kV and an 8.5 mm working distance between the objective lens and the sample camera.

Results and discussion

The quantities of Fe3O4 obtained from the synthesis routes are reported in Table 3. These measurements represent averages and do not account for the weight of small particles lost during the washing process.
Table 3 Quantities of powder Fe3O4 obtained through synthesis
Method Quantity
Coprecipitation 1.34 g
Polyol 0.48 g


Therefore, the average crystallite size was calculated from the analysis of the most intense diffraction peaks using the Debye–Scherrer equation (eqn (6)):

 
image file: d5ra00102a-t1.tif(6)
where D represents the crystallite grain size (Å), k is a constant with a value of 0.9, λ is the incident radiation wavelength (Å) (in this case the incident radiation was CuKα, λ = 1.54 Å), β is the width of the peak at half its strongest intensity (rad) and θ represents the diffraction angle.35 The cop-Fe3O4 showed characteristic Fe3O4 signals at 2θ angles with intensities at 30.16°, 35.60°, 43.22°, 53.72°, 57.14° and 62.83° (Fig. 5) and an average grain size of 8.92 nm (Table 4). Pol-Fe3O4, displayed similar intense peaks at 30.24°, 35.57°, 42.71°, 53.92°, 57.18° and 62.49° (Fig. 5), achieving medium crystallite sizes, as depicted in Table 5, corresponding to an average Fe3O4 crystal size of 6.78 nm. Both samples were compared with the maghemite diffraction pattern from the XRD software library, showing analogous intensities at 28.57°, 34.34° and 48.25°, suggesting that the prepared samples are isostructural ferromagnetic iron oxides and Fe3O4.36,37


image file: d5ra00102a-f5.tif
Fig. 5 Fe3O4 pattern, cop-Fe3O4 and pol-Fe3O4 X-ray diffractograms.
Table 4 Lattice parameter regarding each cop-Fe3O4 crystallographic plane
Miller index 2θ (°) d a (Å)
(220) 30.16 2.96 8.38
(311) 35.60 2.52 8.36
(400) 43.22 2.09 8.37
(422) 53.72 1.71 8.36
(511) 57.14 1.61 8.38
(440) 62.83 1.48 8.37
Average 8.37


Table 5 Lattice parameter regarding each pol-Fe3O4 crystallographic plane
Miller index 2θ (°) d a (Å)
(220) 30.24 2.96 8.36
(311) 35.57 2.52 8.37
(400) 42.71 2.12 8.47
(422) 53.92 1.70 8.33
(511) 57.18 1.61 8.37
(440) 62.49 1.49 8.41
Average 8.38


K factor depends on the geometry, although a commonly used value is 0.89. This approximation is based on the assumption of perfectly spherical particles and is applicable to crystals with sizes up to 100 or 200 nm,38 as peak broadening decreases with an increasing particle size. In this regard, Bragg's law allows the determination of the lattice parameters of a crystal structure. cop-Fe3O4 and pol-Fe3O4 results are shown in Tables S1 and S2, respectively. In addition, the Fe3O4 structure is a characteristic FCC of the inverse spinel type, featuring 8 tetrahedral sites occupied by Fe2+ and 16 octahedral sites equally occupied by Fe2+ and Fe3+.39 As an FCC structure, it has only one lattice parameter, which can be calculated from each crystallographic plane using Eq. (7) and (8).

 
λCuKα = 2 × d × sin(θ) (7)
 
image file: d5ra00102a-t2.tif(8)

Moreover, it is well known in crystallography that h, k, and l are the Miller indices of a crystallographic plane. The calculated values for cop-Fe3O4 and pol-Fe3O4 are shown in Tables 4 and 5, respectively.

Both materials have a similar average lattice parameter of ≈8.39 Å, which was also reported by G. Peña et al.40

Measuring CH4 production content in biogas through the volumetric displacement method demonstrated daily biogas production by applying nanoparticles (Fig. 6a and b). In Group 2, the Fe3O4 effect is highly remarkable. Using 48 mg of pol-Fe3O4 (100 ppm) with a smaller particle size (according to DLS,41 Fig. S1 and eqn (S1)–(S3)), CH4 production increased by up to 64.5% compared with the sample without Fe3O4. Nonetheless, the use of larger cop-Fe3O4 (100 ppm) (0.4 μm particle size) resulted in only a 9.61% increase. Therefore, both tests confirm that the optimal amount of Fe3O4 is around 100 ppm. Although, particle size also affects biogas production, when particles are too large (800 nm to 4.5 μm), they become inefficient.42 Thus, the increase in biogas is attributed to magnetite's role as a mediator between the donors and acceptors of chemical species involved in methanogenesis.42–44 According to the results, this suggests that increased biogas production was due to the symbiotic association between bacteria and iron nanoparticles, according to Baek et al.45 and Wang et al.,46 whose studies focused on investigating the role of iron compounds such as Fe3O4 in the performance of anaerobic digestion. Biogas production modelling can follow a sigmoid function.42,47 The most commonly used function is the modified Gompertz function (eqn (9)). Using this equation, the average daily gas production rate, the lag time, and the mass production estimate were obtained:

 
image file: d5ra00102a-t3.tif(9)
where a corresponds to maximum CH4 production (mL), b is the average production rate (mL per day) and λ is the lag time.


image file: d5ra00102a-f6.tif
Fig. 6 Total CH4 production using (a) cop-Fe3O4 (mg) and (b) pol-Fe3O4 (mg) groups.

Furthermore, Gompertz’s correlation in CH4 production (as shown in Fig. 7) from the corresponding reactors is shown in Fig. 6a. It is possible to determine the theoretical maximum CH4 that could be produced from a specific organic load. Theoretically, 2.61 g of COD can be converted into 1 L of CH4 under standard conditions if the organic matter is fully converted to methane.22 In the case of the trials with pol-Fe3O4, an additional amount of PGPM corresponding to 34.47 g COD was used, whereas the trials with cop-Fe3O4 used a corresponding amount of 5.57 g COD. The results for these trials are shown in Table 6.


image file: d5ra00102a-f7.tif
Fig. 7 Gompertz model to reactors 2 and 4 of enhanced CH4 production with cop-Fe3O4.
Table 6 Biodegradability (Bd) percentage of each trial
Analysis Results
Bd target (%) Bd 100 ppm (%)
Coprecipitation trial 52.88% 57.91%
Polyols trial 5.30% 8.56%


Additionally, Table 8 provides a summary of various sources regarding the CH4 vol. Produced relative to volatile solids in the feed and the COD of the substrate.

The models are experimental extrapolation since most studies on biogas have test periods of 30 or 60 days. For this reason, the Gompertz mathematical model, commonly applied in such cases, was used for approximation (eqn (9) (S4) and (S5)).

In the assays with pol-Fe3O4, an average increase of up to 64.5% in biogas production over 7 days was observed when 100 ppm of Fe3O4 nanoparticles were added, compared with a bioreactor without them. According to the Gompertz model, this increase would reach 45.81% after 40 days, indicating the point of maximum biogas production. In contrast, for the cop-Fe3O4 assays, an average increase of 9.61% was observed over 14 days with the addition of 100 ppm of Fe3O4 nanoparticles. Based on the Gompertz model, this increase would reach only 6.13% after 40 days.

Bacterial inoculum samples were taken and analyzed to determine the types of bacteria and to assess the potential inhibitory effect of Fe3O4 (Fig. 8). As shown in Table 7 and Fig. 9, the bacteria exhibited no inhibition in the presence of Fe3O4. These findings are corroborated by other studies, which confirm that Fe3O4 is not inhibitory but rather highly biocompatible with methanogenic bacteria.43


image file: d5ra00102a-f8.tif
Fig. 8 SEM image of Fe3O4 used to evaluate biological inhibition.
Table 7 Biological study results
Analysis 108 UFC mL−1
0 h 24 h 48 h 96 h 120 h
Inoculum (control) 9.7 9.5 9.0 8.0 7.0
Inoculum plus Fe3O4 9.7 9.3 8.9 8.1 6.9


Table 8 Comparison in biogas productiona
Substrate mL CH4/g VSs* mL CH4/g COD** Time (days) Temperature (°C)
a *VSs: volatile solids, ** COD: chemical oxygen demand.
Guinea pig manure (blank- pol-Fe3O4) - modeling 1386 32 40 37.5 ± 0.5
Guinea pig manure (blank- cop-Fe3O4) - modeling 1583 274 40 37.5 ± 0.5
Guinea pig manure (pol-Fe3O4) - modeling 2021 47 40 37.5 ± 0.5
Guinea pig manure (cop-Fe3O4) - modeling 1680 291 40 37.5 ± 0.5
Guinea pig manure (blank- pol-Fe3O4) 869 20 7 37.5 ± 0.5
Guinea pig manure (blank- cop-Fe3O4) 1166 202 14 37.5 ± 0.5
Guinea pig manure (pol-Fe3O4) 1402 33 7 37.5 ± 0.5
Guinea pig manure (cop-Fe3O4) 1277 221 14 37.5 ± 0.5
Cow manure48 168   90 to 180 37 ± 1
Mink manure48 512   90 to 180 37 ± 1
Cattle excrement49 300 7.3 Mesophilic (30 to 38)
Domestic solid waste50 882 (mL biogas) Continuous 35 ± 1
Municipal solid waste51 360   Continuous 35 ± 2
Rice straw52 178 356 40 37
Corn straw53 217   35 37 ± 1
Wheat straw in co-digestion with fungi54 269 269 62 37
Fallen leaves55 82 21 30 37
Garden waste56 45 11 40 37 ± 1
Pig manure57 127 212 30 32
Pig manure58 247 412 60 32



image file: d5ra00102a-f9.tif
Fig. 9 Benchmark of Methanosarcina bacteria in culture. (a) Bacteria Methanosarcina barkeri reported in the literature.58 (b) Methanosarcina colonies found in the experiment.

Two main bacterial strains were identified, corresponding to methanogenic bacteria. Methanosarcina species were found, which are characteristic of ruminants. They primarily metabolize CH3COO, C2H5OH and NH2CH3, converting these into CH4. They thrived at temperatures between 30 °C and 45 °C and at a pH between 5.0 and 7.4. They were observed to be immobile and grouped in cell aggregates, as shown in Fig. 9.58

The other strain identified was Methanothrix (Fig. 10). These are Gram-negative bacteria, filamentous in shape and measuring several micrometres in length. They are characterized by their ability to degrade CH3COO into CH4 and CO2 and are incapable of degrading other substrates.44,59


image file: d5ra00102a-f10.tif
Fig. 10 Benchmark of Methanothrix bacteria in culture. (a) Methanothrix sp. As reported in the literature.58 (b) Methanothrix colonies found in the experiment.

Conclusions

To conclude, the trials clearly demonstrate the effect of adding Fe3O4 in 100 ppm on CH4 production. Smaller Fe3O4 particles (34 nm) showed an increase of up to 64.5% in total CH4 production compared with the Group 2 control reactor. Regarding cop-Fe3O4 (average size 0.4 μm), a slight increase of up to 9.61% was observed in the total CH4 production compared with the Group 1 control reactor. Notably, Fe3O4 also significantly affects lag time by reducing it. Although with cop-Fe3O4, the effect is negligible (a reduction of 0.13 days or 3 hours). When comparing trials with a smaller initial organic load over 7 days (Group 1 = 5.57 g COD initial), a higher biodegradability percentage was achieved compared with Group 2, which had a greater initial load (34.47 g). This highlights the importance of avoiding biodigester overloading with excessive substrate to ensure a more efficient COD removal process. Furthermore, nanoscale magnetite enhances biogas production regardless of the organic load, although its effects are best seen at higher loads (pol-Fe3O4). Finally, in the three regions of Peru (coast, Andes and Amazonia) household biogas production is feasible owing to abundant guinea pig farms, and the addition of Fe3O4 to guinea pig manure could help address energy needs in these remote areas.

Data availability

https://www.drive.google.com/drive/folders/1k9sdaxQYGRHHUZfbE6r2ipNFfTMsWlto?usp=drive_link.

Author contributions

Rosa Flores Vargas: formal analysis, investigation, methodology, validation, writing-original draft, and visualization; William Eduardo Gómez Hernández: investigation and methodology; Karenina Ela Macazana López: investigation, methodology, and manuscript correction; Clemente Alfredo Luyo Caycho: resources and investigation; Yelstin Adrian Muñoz Baca: resources and investigation; Harry Anderson Rivera Tito: investigation and manuscript correction and María Esther Quintana Cáceda: conceptualization, formal analysis, funding, and writing–review & editing.

Conflicts of interest

The authors declare that they have no competing interests.

Acknowledgements

This research has been financed by PROCIENCIA, CONCYTEC and SENCICO through project 123-2018-FONDECYT. We extend our gratitude to the professors and researchers of the Science Faculty—Ronny Huamani, Bryan Córdova, Iván Luyo, Pilar García and Henry Huanca—for their contributions as well as Carmen Felipe-Morales and Jaime Villa for their guidance and expertise in biodigester development. Finally, we thank the Thin Films Lab, URPUNANO group and CEMAT for the facilities provided.

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Footnote

Electronic supplementary information (ESI) available. See DOI: https://doi.org/10.1039/d5ra00102a

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