The use of biomass pellets as a source of renewable energy has increased in recent times. However, pellet storage during transportation can compromise their properties, due to fluctuating temperature and humid environments. Here, we show that extended storage of one month at 40 °C and 85% relative humidity causes significant biomass pellet degradation. This was evidenced by higher pellet porosity, weight gain, increased inclusion body formation and creation of an internal network of cracks. We quantify the inclusion and pore growth processes at the surface and within the pellets, which has implications for subsequent thermochemical conversion. The global bioenergy transition may depend upon biomass pellets, and this study shows that storage conditions are critical in the supply chain, so to maintain their quality. Without the development of stronger policies to avoid premature degradation of biomass pellets, they may not realize their full potential as a bioenergy source.
The use of biomass as a renewable fuel has increased sharply during the last decade as a result of the concern of high anthropogenic emissions1. However, due to the challenges in establishing sustainable supply chains for biomass, its heterogeneity, and the inherent physicochemical properties of biomass feedstock, such as low bulk density and high moisture content, biomass implementation has not grown as originally anticipated2,3. To overcome these challenges and to make raw biomass easier to handle, pretreatment processes and pelletization are used to improve its quality for later use in residential heating, large-scale electricity generation and as renewable carbon feedstock for the chemical industry4. However, many countries do not have a large potential of biomass resources or have only marginal land available for biomass production, which has rocked the global biomass pellet market and trade (Fig. 1).
A considerable amount of the overall global consumption of pellets are traded from the Americas to Europe and Asia, around one third in 20185. In 2018 the global demand of pellets for heating and industrial purposes totalled 34 million tonnes and it is expected to increase to around 69 million tonnes, by 20256. Depending on the transportation type, transport distance and storage conditions, biomass pellets are being stored for a period from up to one week or to three months in a fluctuating temperature and humidity environment7. Storage during extended periods of time, especially at high temperatures8,9,10,11, accelerates the degradation of pellets, reducing the quality of the fuel and consequently the fuel conversion behavior12. Recently, coupling advanced pretreatment processes4, such as torrefaction with pelletization, have opened new frontiers to enhance the physicochemical properties of raw biomass to stand the current environmental conditions during transport and storage4,13. However, similar problems as those observed in untreated biomass pellets, such as particle breakage and moisture-induced damage, are still present during logistics of torrefied pellets, leading to structural degradation13. Biomass degradation, especially when dealing with large volume of pellets, can lead to self-heating, spontaneous combustion, pellet attrition, equipment fouling, and numerous health threats to workers exposed to dust particles9,14,15,16,17.
To the best of our knowledge, limited studies have focused on studying qualitatively the morphological modifications at the surface of biomass pellets18,19 and quasi in situ quantification of changes in their physicochemical properties resulting from storage8,20. Typical investigated properties are density, chemical content (proximate and ultimate analysis), moisture sorption, mechanical strength and heating value. In the present work we provide insights on pellets degradation during storage at relatively high but possible temperature. To this end, we studied two untreated and one type of torrefied wood pellets stored in a climate chamber, during a period of one month at a constant condition of 40 °C and 85% relative humidity (RH). By the use of digital microscopy, scanning electron microscopy equipped with energy dispersive X-ray spectroscopy (SEM-EDS) and high-resolution micro-computed tomography (micro-CT), we study surface, structural and chemical changes in biomass pellets, resulting from storage. We demonstrate the expansion of pre-existing fractures and the growth mechanism of inclusions at the surface and inside the cracks of biomass pellets as a result of storage conditions. Ensuring the quality parameters of biomass pellets and avoiding premature degradation are crucial for increasing the adoption of biomass and to avoid costly modifications to the existing infrastructure, especially in large-scale power generation.
Results and discussion
The effect of storage conditions on the development of biomass pellet surface damage
Optical images of the three types of pellets studied before and after storage are presented in Fig. 2. Pellet surface damage is typically present in the form of cracks and damage (e.g., regions with different surface texture and color), from now on referred to as damage. The damage analysis for all nine samples is provided in Supplementary Note 3, Supplementary Fig. 1 and Supplementary Table 3.
Figure 2 illustrates that all fresh pellets already exhibit large areas of damage at the surface before being exposed to the storage conditions. Results show that after storage at 40 °C and 85% RH, all biomass pellets are heavily damaged at the surface. Surface degradation due to the storage is attributed to breakage of bonds, expansion of pre-existing cracks into networks of cracks (creep damage) and de-cohesion of fibers21. After storage, the damaged area with respect to the total area of the front surface of all pellets (area ratio), increased in average by 5%. Of all samples, wood pellets type II were the most affected at the surface level (Fig. 2f).
The presence of large longitudinal cracks at the pellet surface is not necessarily predictive for strength reduction as it also depends on their in-depth growth. Cracks related to pellet breakage are more likely to occur in radial direction due to the high length-to-cross-section ratio of pellets9. Thus, to monitor the expansion of cracks, we performed a three-dimensional (3D) surface profile analysis of pellets at different storage times using digital microscopy. The mean apparent crack depth at the pellet surface before storage, 2 weeks after storage and one month after storage is provided in Fig. 3. The apparent crack depth for all evaluated samples is provided in Supplementary Fig. 2.
We found that before storage, torrefied pellets and wood pellets type II have deeper cracks compared to wood pellets type I. For example, in some torrefied samples, cracks almost reached 1 mm depth (Supplementary Fig. 2). Cracks start to form at the surface and the mean apparent depth of their penetration with respect to the diameter of the pellet is 9% for torrefied pellets, 7% for wood pellets type I and 9% for wood pellets type II (Fig. 3), before storage. We found that the mean apparent crack depth decreased gradually after storage, 65% for torrefied pellets, 43% for wood pellets type I and 71% for wood pellets type II, due to pellet swelling. Results from the profile analysis do not necessarily indicate that the apparent crack depth decreased after storage, but rather imply less space between the wall fibers at the surface. The surrounding moisture fills the interstitial volume within the biomass fibers at the surface of all pellets and expands them due to moisture build-up, resulting in a mean increase of 0.4 mm in pellet diameter (Supplementary Table 2). Swelling of pellets is confirmed by an average pellet diameter increase of 2% for torrefied pellets, 9% for wood pellet type I and 7% for wood pellet type II, after one month of storage. A relatively small radial strain is noticed for the torrefied pellets, due to the crystalline structure of the torrefied biomass microfibrils4, which hold back the swelling. A decrease in the apparent crack depth after storage might also be attributed to increased inclusion body formation as a result of chemical reactions (e.g., oxidation) on the edge of the cracks and agglomeration within the cavities and fibre walls.
Inclusion formation at the surface and inside the cavities/cracks of biomass pellets
We next describe the changes in morphology and elemental composition at the pellet surface, as a result of storage conditions. For simplicity, we refer to the microstructure of the pellets as “solid matrix” and all bright discernible amorphous particles as “inclusions”. Inclusions comprise original inorganic-forming elements in biomass such as Ca, K, Si, Mg, Al, Fe, P, Cl, Na, Mn, and Ti22. Hence, inclusions also include the new minerals or phases formed during storage. Fig. 4 presents the scanning electron microscopy (SEM) imaging conducted on pellets before storage (a, c, e) and after one month of storage (b, d, f). Searching for an optimal way to quantify inclusions at the pellet surface after storage, we performed image analysis of each SEM image (Fig. 5). In SEM images using backscattered electron detector, elements with higher atomic number appear brighter than those with a small atomic number23. Supplementary Note 4 provide SEM images and corresponding image analysis for all six samples, at two different surface regions, before and after storage.
SEM images confirm that at micro level, untreated or torrefied biomass pellets, have pre-existing cracks at the surface, which is in accordance with previous studies18. Pre-existing cracks are an indication of poor adhesion between adjacent fibers resulting from pelletization conditions12. After 1 month of storage, we observed changes in surface morphology and texture in all pellets due to moisture sorption (Fig. 4b, d, f). This could lead to pellet abrasion9 during handling as a result of fracture of uneven regions or detachment of small particles from pellet’s surface. For wood pellet type II in particular, the ash content was relatively low (Supplementary Note 1). However, sufficient minerals existed in this type of pellet to produce a significant difference in surface morphology and texture after one month, the biggest compared to all other samples (Fig. 4f).
Increased inclusion formation has been reported in biomass harvest24, drying22, devolatilization25, and ash storage26. Nevertheless, as far as the authors are concerned, no previous studies have quantified the formation or enlargement of inclusions neither at microscale during storage nor in any of the aforementioned stages. Inclusions are mainly observed between fibers or at the cracks located at the pellet surface (Fig. 4). Image analysis confirms inclusion growth on the pellet surface after one month of storage (Fig. 5). The mean number of inclusions in torrefied pellets increases by 80%; in wood pellets type I and II by 650% and 700%, respectively. Detailed analysis is provided in Supplementary Table 4–6. Despite thermal pretreatment, SEM images of torrefied pellets show similar structural pattern as untreated biomass pellets. Nevertheless, the number of inclusions detected at their surface before storage is higher than that for wood pellets due to the pretreatment method itself (Fig. 5a). Torrefaction converts a certain part of the original organic structures into new formed polymeric structures and ashes that later bind to the fiber wall4. In general, a higher number of inclusions could limit diffusion into and from the biomass pellet, affecting the transfer of the surrounding medium (e.g., oxidant) to the pellet and reducing char conversion. Similar phenomena has already been reported in combustion of poplar wood and wheat straw25.
There are four mechanisms that can explain increased inclusion formation due to storage: (M1) mineral precipitation; (M2) solid-gas chemical reactions; (M3) mineral transport through moist-softened polysaccharides; and (M4) agglomeration of inclusions. These mechanisms are further elaborated throughout the manuscript. Earlier studies on the chemical composition of biomass indicate that there is intensive mineral precipitation (M1) due to moisture evaporation after biomass harvesting22. Such mineral formations result of natural degradation could explain the increase in the number of inclusions detected at the surface of all pellets, after 1 month of storage. These minerals are in the form of in water-soluble phosphates, carbonates, sulphates, chlorides, and nitrates22. When biomass is left in the field for a prolonged time and combined with rainfall, these water-soluble salts tend to contribute to enhanced leaching of Ca, Cl, K, Mg, Na, P, and S22,24. Other mechanisms involved in inclusion growth (M2–M4) are linked to the inherent chemical composition of biomass and will be further explained using SEM-EDS analysis and micro-computed tomography.
Biomass is generally composed of organic (cellulose, hemicellulose, and lignin), inorganic constituents (e.g., amorphous components and minerals), and fluid matter (e.g., moisture)22. The concentrations of each constituent depend on the type of biomass, harvest practices, and environmental conditions. Furthermore, when biomass is subjected to thermochemical processes (>200 °C4), new minerals or inorganic phases are created, commonly referred as ash22. Ash contains forming elements such as Si, K, Na, S, Cl, P, Ca, Mg, and Fe responsible for toxic particulate matter emissions, fouling and slagging14,27. To complement morphological changes observed in pellets, we performed EDS analysis on our samples. Fig. 6 presents the percentage change of mean elemental concentrations of region 1 and region 2, for all analyzed pellets, before storage and after one month of storage. Values presented in Fig. 6 can be interpreted as enrichment/depletion of elements with respect to the conditions before storage. The results are separated by the mean elemental composition (at. %) of matrix (Fig. 6a, c, e) and of the inclusions (Fig. 6b, d, f) detected at the surface of the sample pellets. Detailed elemental analysis is provided in Supplementary Note 5.
Energy dispersive X-ray spectroscopy (EDS) analysis of the skeletal matrix of pellets
EDS results show that C > O are the major elements (>1% at.) in pellets (Supplementary Figs. 9a, c; 10a, c; 11a, c). Meanwhile, the minor elements (1–0.1% at.) found on average at the skeletal matrix include Si > N > Ca > Mn > Fe > K > S for torrefied pellets, Mn > Fe > N for wood pellets type I, and N > Fe > Ca for wood pellets type II. After 1 month, EDS measurements report on average an increase of trace elements such as K, Si, and Mg in the solid matrix of wood pellets type I and type II (Fig. 6c, e). In the solid matrix of torrefied pellets, concentration of Si, K, and Mg decreased after 1 month. Also, it is observed that Ca increased in the solid matrix of torrefied pellets and wood pellets type I. This could be attributed to the formation of Ca(OH)2 from CaO and moisture uptake, as has been observed in studies of biomass ash storage26. Ca(OH)2 could further react with CO2 from air or from pellet off-gassing to produce crystalline CaCO326 (M2). During thermochemical conversion, Ca carbonates can contribute to enhanced leaching and emission volatile elements during combustion27. CaCO3 is known as a brittle material28, which could compromise the integrity of the pelletʼs microstructure and lead to changes in surface morphology such as decreased particle size. This observation is backed by the decrease in the average area of the inclusions in torrefied pellets and wood pellets type I, as shown in Fig. 5b, f, Supplementary Tables 4, 5. In wood pellets type II, the mean concentration of Ca decreased 10% in the matrix and 88% in the inclusions, after one month of storage. It is plausible that other inorganic-forming elements play a more active role in reacting with the surrounding moisture/gases than Ca. After 1 month of storage, wood pellets type II inclusions got enriched in Si, Mg, and K. As expected, torrefied pellets were the most resistant to chemical changes due to the nature of its hydrophobic structure29. We also observe a decrease of 10% in the oxygen content in the organic matrix of all pellets after 1 month of storage. This suggests that pellets suffer oxygen-induced degradation, leading to an increase of oxygen-based inclusions, which is consistent with results presented in Fig. 5.
EDS analysis of inclusions at the surface of biomass pellets
Before storage, inclusions at the surface of all samples are, in average, consisting of major elements such as C > O > Fe > Si > Ca for torrefied pellets, C > O > Si > Ca > N for wood pellets type I, and C > O > Ni for wood pellets type II. Minor elements found in the inclusions of torrefied pellets, wood pellets type I and II are Zn > K > N > Mg > Cu, Cu > Cl > Zn > K > Fe > S, and Fe > Ca > Si > Mg > S, respectively.
After 1 month of storage, inclusions in wood pellets type I and II (Fig. 6d, f) got mainly enriched in Fe (1453%) and Si (296%). Si is mostly found in biomass as amorphous silica (SiO2)22, while in ash, Si and Fe are mostly found as glass, silicates, and oxyhydroxides30. We ascribe this large increase in concentrations to the untreated fibers of wood pellets, which are more prone to moisture sorption (M2) than the reacted organic material of torrefied pellets, which have a lower pore size29. Enrichment of Si and Fe is also consistent with increased size of inclusions observed from SEM images (Fig. 5d, f). Image analysis of these SEM images indicates an increase in the average maximum area of the inclusions in wood pellets type I and II (Supplementary Tables 5, 6). During thermochemical conversion, Si- and Fe-bearing glass, silicates and oxyhydroxides can increase ash yield, enhance abrasion-erosion, decrease combustion efficiency and increase operation costs for handling of ashes27. The enrichment of SiO2 at the surface of the pellets can also lead to a decrease of thermochemical fuel conversion rates, due to the low melting temperature of silicates, which might encapsulate the remaining char25. Additionally, when moisture is adsorbed by the pellets, free hydroxyl ions (OH−) coupled with alkali cations (K+ and Ca2+) might react with siliceous phases31. The reaction products are water-insoluble compounds based on calcium, alkalis and dissolved silica, leading to inclusion growth due to a concentration gradient through biomass pores31. A similar phenomenon has already been observed in concrete32.
Regarding minor inorganic-forming elements, after 1 month of storage, inclusions in all pellets got enriched in Mg, followed by K, except in wood pellets type I. These elements are known to be present in the organic structure as Mg-K oxalates33 and carbonates22, while in ash in the form of glass, silicates, carbonates, oxyhydroxides, sulphates, and phosphates27. Either at the solid matrix or at the inclusions, increases in the concentration of Mg and K are associated with increased inclusion body formation. This is the result of the mobile nature30 of these elements, agglomeration, and moisture sorption. Enrichment of K after storage could be attributed to the formation/enlargement of K-silicates27. In the case of torrefied pellets, K-silicates could already have been formed during thermal pretreatment34. Low melting temperature of K-silicates leads to increased ash deposition and fouling35. Furthermore, in biomass combustion processes, K can be released as vapor species, which can further react with other gas components to form slag36. On the other hand, Mg after storage can be present as dolomite (CaMg(CO3)2)26 or MgO37, which can cause heat exchanger fouling through increased alkali devolatilization36.
After 1 month of storage, EDS indicates a decrease in Ca content from major to minor constituent for torrefied samples and wood pellets type I. Meanwhile, in wood pellets type II, Ca decreases from minor to trace element. As explained above, a carbonatation from Ca(OH)2 could have diluted the average concentration of Ca in the inclusions of all samples26.
Lastly, each of the EDS detected elements in inclusions have different surface energy that could lead to agglomeration (M4). Inclusions with lower surface area tend to agglomerate into larger inclusions to reduce their surface energy38. This rearrangement also leads to creation or expansion of cracks.
Micro-CT scans of biomass pellets: porosity and inclusion growth mechanism
Given the tortuous nature of the cracks within the pellets, we used micro-CT to gain insight into the porosity, development of inclusions, cavities and crack formation and growth during storage. Micro-CT provides advantages compared to conventional microscopy, which is not effective at quantifying buried crack formation away from the pellet surface (Fig. 3). Figs. 7, 8 show the 3D images of the porosity and inclusions along the sample of 4-mm length from the top to the bottom of the pellets. Values of the porosity and inclusion-to-pellet volume ratio for each of the pellets are given in Supplementary Table 7. Detailed 3D representation of porosity evolution and inclusion formation, growth, and agglomeration, as a function of storage time, is provided in Supplementary Note 6 and Supplementary Movies 1–3.
Results of the CT scans confirm our hypothesis regarding the reduction in the apparent crack depth after storage (Fig. 3). Due to the tortuous nature of the cracks within the pellets and the increased inclusions at the surface and within the pellets after 1 month of storage, the light from the microscope does not penetrate deep (enough) into the biomass fibres, restricting the application of digital microscopy in crack imaging seriously. CT scans show that although wall fibres expand within the pellets, the void space is higher after one month of storage.
Storage at 40 °C and 85% RH produces changes in the internal porous structure of the pellets. The porosity of the torrefied pellets, wood pellets type I and type II increased by 35%, 66%, and 59%, respectively, after 1 month of storage. Our findings confirm previous experiments and support the suggestion9 that the volume of the pellet expands as a result of moisture sorption (M2) during high humidity storage (85% RH). This phenomenon could lead to decreased bulk density and reduced pellet strength9. Furthermore, the void space within the pellets can be filled by entrapped air, water molecules and gaseous compounds (CO2, CO, CH4, and volatile organic compounds)8,15 released from decomposition of biomass during storage. All these compounds fill the pre-existing cracks and expand them, producing a tortuous 3D network of cracks. The findings presented in Figs. 7, 8 add to observations made by Strandberg et al.25, who reported enlargement of cracks and internal cavities during devolatilization of biomass pellets. Internal cavities and cracks can affect the conversion rates by increasing active char oxidation surface25. Thus, storage degradation could enhance char oxidation by further increasing gas transport to and from the pellet.
Although we did not monitor off-gassing from stored pellets, there is a large difference between the weight change estimated from porosity calculations and the weight change estimated from weight measurements (Supplementary Note 7 and Supplementary Table 9). This difference in weight implies that pellets are not only absorbing moisture but there are also off-gassing emissions. Gases denser (aldehydes and ketones)8 than moist air are known to be present in the off-gassing of biomass pellets during storage. For example, volatile organic compounds, such as acetaldehyde and propanal, which have densities two orders of magnitude higher than moist air.
Furthermore, the resulting highly porous structure exposes a higher surface area of pellet fibers to interact with the surrounding medium during storage. This phenomenon leads to increased oxidation8,15,39 accelerating pellet degradation. Examples of the consequences are reduced mechanical durability18, decreased calorific value40, increased microbial activity41, increased risk of self-ignition8,42, and gas concentrations that can exceed occupational standards for worker exposure43. Potential solutions to reduce oxidation, moisture sorption and off-gassing during storage are the use of antioxidants42 or hydrophobic coatings44 during pellet production.
Changes in porosity are in agreement with weight measurements, which report that after one month of storage, torrefied samples, wood pellet type I and type II, increased in average 2.8%, 2.7%, and 2.8%, respectively, compared to their initial weight (Supplementary Note 2). Weight change is also in agreement with measurements of pellet diameter (Supplementary Table 2). Results of the statistical analysis indicate that the two pairs of variables, weight-diameter and porosity-diameter, have a strong positive correlation with a p value less than 0.01 (Supplementary Note 8).
A volume increase of the inclusions within the internal cavities also leads to expansion of cracks (Fig. 8 and Supplementary Movie 3). After 1 month of storage, the inclusion-to-pellet volume ratio increased in torrefied pellets by 38%, in wood pellets type I by 800% and in wood pellets type II by 310%, with respect to the ratio calculated for pellets before storage. Increased inclusion growth can also be attributed to the presence of rubbery amorphous polysaccharides which are responsible for mineral ion transport (M4). Especially at high humidity, such as the one used in this work; amorphous polysaccharides pass through a moisture-induced glass transition inside the wood cell wall layers which facilitates the diffusion of chemicals45. Thus, our findings support this hypothesis that moisture-softened polysaccharides facilitated the growth of inclusions at 40 °C and 85%. To complement the results presented on Figs. 7, 8, Supplementary Movies 1–3 show how the enlargement of inclusions affect the structure of the pellet and increased cracks.
Our results suggest that significant degradation of biomass pellets was proven due to storage conditions at 40 °C and 85% RH. We show that the creation and expansion of cracks in pellets is tightly linked to the increased porosity, regained moisture content, higher inclusion body formation and inclusion agglomeration as a result of extended storage of 1 month. After 1 month of storage, the damaged area with respect to the total area of the front surface of all pellets (area ratio) increased in average by 5%.
To the best of our knowledge, no other authors have quantified the microstructural changes occurring in pellets during storage. Quantification of crack formation and inclusion body formation at the surface and within the pellets is obtained with the use of micro-CT. Results indicate that the increase in the inclusion-to-pellet volume ratio can be as high as 800% in wood pellets after one month of storage. As described in previous sections, inclusion growth is the result of multiple mechanisms (M1–M5). Although mechanical properties, such as durability are important to understand the behavior of pellets as a bulk, inclusion formation and agglomeration within the pellets should be studied to optimize fine particulate emissions, thermochemical conversion and fuel particle modeling. Inclusion agglomeration may affect large-scale thermochemical conversion processes, such as centralized district heating and biomass co-firing. On the other hand, pellets with a higher number of cracks at the surface and within the structure are more sensitive to degradation during storage, possibly resulting in revenue loss to companies and consumers as part of the material could be lost. To the extent of discouraging the use of biomass pellets and slowing down the bioenergy transition. Our results challenge existing local and international certifications to develop new standards for handling, transport and storage of biomass pellets. Creation of stronger policies to avoid degradation of pellets could help to reduce breakage, reduce off-gassing and increase pellet conversion efficiency.
In the present work the following techniques were used to characterize the degradation of biomass pellets before and after storage: weight and diameter change, digital microscopy, scanning electron microscopy equipped with energy dispersive X-ray spectroscopy (SEM-EDS), and X-ray micro-computed tomography (micro-CT). Morphological changes at the pellet surface were monitored using digital microscopy. SEM-EDS analysis was carried out at the surface and at the cross section of the pellets for better understanding of the changes in morphology and elemental composition of pellets, due to storage. Then, micro-CT was used to characterize the pellet structure using high lateral resolution 3D images.
In this work, we monitored two types of untreated commercial white wood pellets, wood pellet type I (wp1) and wood pellet type II (wp2), and one type of torrefied wood pellets (tor). Wood pellets were made from sawdust and purchased from local stores in the Netherlands. No information regarding the manufacturing process was provided. The torrefied pellets were obtained from a pilot-scale production facility in the UK and no information about the origin of the pellets and production process was disclosed. The main characteristics of the studied pellets based on ultimate and proximate analysis are provided in Supplementary Note 1. Samples were stored in a climate chamber (C + 10/600 Climate Test Chamber) with a volume of 600 L for a period of one month at a constant condition of 40 °C and 85% RH. These conditions were selected since they represent typical conditions of transatlantic transportation (from North America to Europe)8,46. Furthermore, at and above this temperature and RH value, deterioration9,11 and off-gassing8 have proven to be significant in the degradation of biomass pellets. The temperature and relative humidity inside the chamber were kept constant all the time and monitored continuously. We did not investigate higher storage temperatures because, at industrial level, temperatures above 60 °C are already a concern and then cooling is needed through mechanical ventilation16. During the storage period, pellets were examined at 3 sample dates: 0 days, 2 weeks, and 1 month. A detailed description of the characterization and analytical techniques used to carry out this study are described in the following sections. The as-received properties such as proximate and ultimate analysis, weight, diameter, surface morphology, and microstructure of the pellets before storage are given as the benchmark for assessment and comparison. Therefore, any changes in the pellet properties after storage can be compared to the as-received properties.
Weight and diameter of pellets
An electronic balance (Sartorius Practum 124-1 S analytical) was used to measure the mass of each pellet at three sampling dates: 0 days, 2 weeks, and 1 month. At the same time, the diameter of each pellet was measured with a Kunzer 7EMS01 digital caliper 150 mm with an accuracy of 0.01 mm. Data on weight change for all samples are reported in Supplementary Note 2.
Physical changes at the pellet surface
Pre-existing cracks, expansion of pre-existing cracks and formation of new ones were quantified using a digital microscope, Keyence VHX- 5000 series, ocular VH-Z100R/W/T. A total of nine samples were examined: three samples per each type of pellet. The notation of these samples is the following: wp1_sample1-3, wp2_sample1-3 and tor_sample1-3. A mark was placed on one side of each sample to ensure that the observation area remained the same during the three sample dates. The damaged surface area at the front face of the pellets was measured using the area measurement built-in function in the digital microscope that allows detection of cracks based on brightness and contrast variations. The front surface of the pellet is defined as the surface facing the lens of the microscope. Besides the pre-existing cracks, pellets contain regions with different surface texture with interparticle gaps and voids result of poor adhesion between adjacent biomass fibers during the pelletization process47. The pelletization process also produces regions with fiber ends and particles sticking out of the surface as a result of adhering structures being torn apart47. These regions were detected by the microscope as they differ from the pellet material lighter color. In the manuscript such regions and cracks are referred to as “damage”. Although large damaged areas were easy to detect automatically, the manual marking mode was used to include small cracks in the computation of the total area of the cracks. The percentage of increase in the damaged area was calculated as the difference between the damaged area after storage and before storage related to the damaged area before storage.
The apparent depth of surface cracks was determined using the built-in tool from the digital microscope to construct a 3D surface profile measurement of the front face of the pellet. The built-in tool is based on photographic stitching combined with a depth composition function and multi-lighting48. A line was drawn between two points along the front face of the pellet to get a profile graph of the surface. Three profile lines were drawn along the front face of each sample to ensure repeatability.
Surface and elemental composition analysis
Observations related to the morphology and composition of pellets before and after 1 month of storage were obtained by SEM-EDS. SEM analysis was performed on a JEOL IT100 Scanning Electron Microscope using a backscattered electron detector, coupled with an EDS analyser. Data were processed with the corresponding InTouchScope™ software. The diameter of the analysed area was a few hundred micrometres and the analysed depth around 1 µm. EDS measurements were carried at low-vacuum due to the nonconductivity of the samples. Images were recorded in a compositional mode using an accelerated voltage of 10 kV and probe current of 65 pA. The cross section of the samples was mechanically ground up to 800 grit with SiC grinding sandpaper and glued to the sample holder using double-sided tape. Just the side, which was grinded, was taped to the SEM-EDS holder to avoid the detection of Si and C from the grinding paper. A mark was made on one side of each sample to ensure that the observation area remained constant during the three sampling dates. For comparison, SEM was conducted on the cross section of the sample pellets before storage and after one month of storage. We examined six pellets, two samples per each type of pellet and inspected two regions per each sample. The notation of these samples is the following: wp1_sample4-5, wp2_sample4-5 and tor_sample4-5. In average we selected 4 points per each region per each sample for scanning, on the matrix and on the inclusions. The elemental composition of biomass comprises: major (>1% at.), minor (1–0.1% at.), and trace (<0.1% at.) elements.
Once the images were taken, all samples were returned to the climate chamber. SEM images were also analysed with the area measurement built-in function of the digital microscope. This method was used to determine the number and area of the inclusions before and 1 month after storage.
3D characterization of biomass pellets
To confirm the previous findings of this study, we used micro-CT scanner (Phoenix Nanotom 180NF) to map the microstructure of the pellets and follow the development of cracks and inclusions in the internal cavities during the storage period. All samples were scanned from the top to the bottom of the pellets, one per each type. The scanned pellet length was 4 mm. Prior to the scanning, each biomass pellet was glued to a cylindrical glass rod. Once the scan was performed, the sample was removed from the glass rod and returned to the climate chamber. Images were taken using X-rays at 90 kV and a 2284 × 2304 pixel detector. The voxel size used was between 0.004 × 0.004 × 0.004 µm. Image analysis of micro-CT scans and movies were carried out using AVISO software, version 2019.1. To create 3D images of the porosity and inclusions, we reconstructed 4-mm length of the pellets. A segment of 0.7 mm of pellet length was used for monitoring inclusion growth and for creating Supplementary Movies 1–3. AVISO software was also used to estimate the porosity of the pellets and the inclusion-to-pellet ratio after different times of storage. Porosity is defined as the fraction of the total volume, which is void (free) space in the pellet. The inclusion-to-pellet volume ratio is defined as the ratio of the volume of the inclusions to the total volume of the pellet. Image processing steps comprises image segmentation (quantification and image separation), noise reduction filters, and label analysis to extract statistical and numerical information49.
In order to determine associations between the storage time, volume expansion, porosity and weight change for all three type of pellets, we used Pearson’s correlation analysis and calculated the corresponding p values. After we applied a logarithmic transformation LogWorth to convert relatively small p values into a more readable scale. Detailed statistical analysis is provided in Supplementary Note 8. P < 0.01 was used to indicate significance.
Data supporting the findings presented in this paper are available within the manuscript and in the Supplementary Material. Datasets for 3D reconstruction of micro-CT images of pellets are available from the corresponding author upon request.
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This work was supported by the Top Consortium for Knowledge and Innovation for the Biobased Economy under grant TKI-BBE project number BBE-1801. Additional support was provided by the European Union’s Horizon 2020 research and innovation programme under the Marie Skłodowska-Curie grant agreement No. 707404 and TKI BioBased Economy project No. 1713 “Biomass pellets: degradation during transport and handling”. We would also like to acknowledge W. Verwaal, E. Meijvogel-de Koning for assistance with micro-CT scans measurements, and J.G. van Meel for guidance regarding the 3D reconstructions of micro-CT data.
The authors declare no competing interests.
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Cutz, L., Tiringer, U., Gilvari, H. et al. Microstructural degradation during the storage of biomass pellets. Commun Mater 2, 2 (2021). https://doi.org/10.1038/s43246-020-00113-y