Potassium doping increases biochar carbon sequestration potential by 45%, facilitating decoupling of carbon sequestration from soil improvement

Scientific Reports, Apr 2019

Negative emissions technologies offer an important tool to limit the global warming to <2 °C. Biochar is one of only a few such technologies, and the one at highest technology readiness level. Here we show that potassium as a low-concentration additive in biochar production can increase biochar’s carbon sequestration potential; by up to 45% in this study. This translates to an increase in the estimated global biochar carbon sequestration potential to over 2.6 Gt CO2-C(eq) yr−1, thus boosting the efficiency of utilisation of limited biomass and land resources, and considerably improving the economics of biochar production and atmospheric carbon sequestration. In addition, potassium doping also increases plant nutrient content of resulting biochar, making it better suited for agricultural applications. Yet, more importantly, due to its much higher carbon sequestration potential, AM-enriched biochar facilitates viable biochar deployment for carbon sequestration purposes with reduced need to rely on biochar’s abilities to improve soil properties and crop yields, hence opening new potential areas and scenarios for biochar applications.

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Potassium doping increases biochar carbon sequestration potential by 45%, facilitating decoupling of carbon sequestration from soil improvement

potassium doping increases biochar carbon sequestration potential by 45%, facilitating decoupling of carbon sequestration from soil improvement Ond?ej Ma?ek Wolfram Buss Peter Brownsort Massimo Rovere Alberto t agliaferro Ling Zhao Xinde Cao Guangwen Xu Negative emissions technologies offer an important tool to limit the global warming to <2 ?C. Biochar is one of only a few such technologies, and the one at highest technology readiness level. Here we show that potassium as a low-concentration additive in biochar production can increase biochar's carbon sequestration potential; by up to 45% in this study. This translates to an increase in the estimated global biochar carbon sequestration potential to over 2.6 Gt CO2-C(eq) yr?1, thus boosting the efficiency of utilisation of limited biomass and land resources, and considerably improving the economics of biochar production and atmospheric carbon sequestration. In addition, potassium doping also increases plant nutrient content of resulting biochar, making it better suited for agricultural applications.Yet, more importantly, due to its much higher carbon sequestration potential, AM-enriched biochar facilitates viable biochar deployment for carbon sequestration purposes with reduced need to rely on biochar's abilities to improve soil properties and crop yields, hence opening new potential areas and scenarios for biochar applications. - 3, Technologies for CO2 removal from the atmosphere (so called Negative Emission Technologies) will be required to limit the global warming to <2 ?C1,2. Sequestering carbon in soil in the form of biochar has been discussed for around a decade and has shown great potential as a carbon negative strategy3?5. Although uncertainties still exist regarding estimation of the residence time of biochar in soil based on its physical and chemical properties and soil conditions6, it is generally accepted that carbon in biochar has a residence time in soil several orders of magnitude greater than the biomass it was produced from7. Therefore, many studies use proxies for assessing the amount of stable carbon in biochar8?10. Most relevant is the amount of carbon stable after 100 years in soil, the duration typically used to calculate the global warming potential of greenhouse gases11. In various articles the carbon sequestration potential of biochar has been calculated to be in the range of 0.7?1.8 Gt CO2-C(eq) yr?13,12,13. Biochar is produced as one of the co-products of pyrolysis, which is the thermochemical conversion of biomass in the absence of free oxygen at temperatures above around 350 ?C. This process yields three co-products in the form of pyrolysis solids (biochar), pyrolysis liquids (organic acids, phenolic compounds, etc.), and gases (CO, CO2, H2, CH4, C2H4, etc.)14,15. The yield of biochar, and also its carbon stability, are dependent on feedstock and pyrolysis conditions16,17. Increasing the percentage of stable carbon content in biochar is one way of increasing its carbon sequestration potential (the other is increasing biochar yield); this is typically achieved by increasing the severity of the pyrolysis process (higher temperature and longer residence time, which reduces solids yield, increasing C release as gas, leading to higher CO2 emissions when burned)8,18. In context of carbon capture and storage, however, the increase of the stable carbon yield, i.e. the amount of stable carbon that can be obtained from the same amount of biomass, is more relevant. Increasing the stable carbon yield relative to the parent biomass feedstock is in effect equivalent to reducing the amount of biomass needed to sequester a unit of carbon. The stability of biochar carbon is related to its condensed aromatic nature19, which in turn is affected by the composition of biomass feedstock and by processing conditions, mainly highest treatment temperature (HTT). Besides organic constituents (cellulose, hemicellulose and lignin), biomass also contains inorganic constituents, which content and composition is dependent on the type of biomass, growing location and to some extent the method of harvest and subsequent treatment20,21. Previous studies showed that concentrations of certain constituents of the mineral matter, especially alkali metals (AM) and alkaline earth metals (AEM), such as K, Na, Ca, Mg, strongly affect biochar yields22?26, with biochar yields increasing with elevated levels of AMs and AEMs due to catalysis of biochar formation. Yet, little is know about the effects of AMs and AEMs on the yield of stable carbon in biochar.?In some studies the carbon retention in biochar was increased using additives, though very high additive to biomass ratios (w/w) were used, e.g. in Ren et al.26 Ca(OH)2 in a ratio of 1:9 was applied, in Zhao et al.25 H3PO4 was applied in ratios of 0.359:1 and 0.718:1. In this study, we have used an order of magnitude lower loading of a low-cost additive (1 and 2%) which at the same time provides K to plants when resulting biochar is applied to soil. The potential ability of AMs to catalyse biochar formation together with the fact that potassium is a valuable macronutrient makes the use of AMs as additives in biochar production a potentially attractive proposition. This is especially true, if the AM catalysed biochar has at least similar or better properties in terms of carbon stability as biochar produced without AM doping. Despite extensive research on biochar stability, no systematic investigation of stability of AM catalysed biochar has been reported to date. The research presented in this paper focused on increasing the carbon sequestration potential of biochar derived from the energy crop Miscanthus giganteus, by increasing biochar yield and stability using a common, low-cost additive, potassium acetate, and comparing the effects with those of sodium acetate doping. Results and Discussion Potassium doping increases biochar and stable carbon yield. Our results show that, as expected based on previous research and published literature, the biochar yield of Miscanthus biomass was strongly affected by the presence of AMs. Doping with AMs (1 wt% K+, 2 wt% K+ and 1 wt% Na+) unequivocally resulted in higher biochar yields, by 10.5?21.1% relative to the untreated biomass control, in the whole temperature range tested (350?750 ?C) (Figs?1A, 2A). The relative biochar yield change compared to un-amended biomass pyrolysis (Fig.?3A) shows that in the tested temperature range the biochar yield increase was independent of the HTT. Besides biochar yield, the content of stable carbon and subsequently the yield of stable carbon are the other two important parameters in terms of biochar?s ability to sequester carbon efficiently. In this study the stable carbon content was determined using a hydrogen peroxide oxidation method calibrated so that it corresponds to approx. 100 years of ageing in soil8,9,27. The yield of stable carbon was determined as a product of biochar yield and stable carbon content. Both Na+ and K+ doping showed similar performance in increasing both biochar (Fig.?2A) and stable carbon (Fig.?2B) yields. The increase in biochar yield is a result of catalysis of the charring process by AM catalysts in the pyrolysis of lignocellulosic materials. In the presence of these metals the reaction process favours charring and dehydrating reactions, versus fragmentation and depolymerization pathways, in the primary decomposition of the holocellulosic fraction28. In addition, AMs also enhance dehydration, demethoxylation, decarboxylation, and biochar formation in lignin pyrolysis29,30. All AM treatments considerably increased the stable carbon yield (Fig.?2C) compared to the untreated controls. The relative change was between+ 9.5% (1% K+ 650 ?C) and +45.0% (2% K + 450 ?C) (SI Table?4) and the average change was +20.4% for all AM treatments and pyrolysis temperatures. This finding was confirmed with a different biomass feedstock material. Willow chips treated in the same way with 1% w/w K+ were also pyrolysed at 350, 550 and 750 ?C (described in SI). The stable carbon yield was highest at a HTT of 550 ?C with a 31.8% higher yield relative to the feedstock biomass than the corresponding untreated willow sample (SI Table?3). This shows that the effect of AM doping on stable carbon yield is not specific to one type of biomass (Miscanthus). 450 ?C pyrolysis maximises the carbon sequestration potential of miscanthus biochar. Tailoring the pyrolysis conditions and hence the biochar properties to suit the biochar end use is a profound and essential feature of biochar production, and therefore any effects of AM additives on available range of processing parameters are of high importance. In general, both AMs performed comparably in terms of stable carbon yield when added at the same concentration (1wt %) (Fig.?2B). Increased AM loading reduced the HTT at which the highest stable carbon yield was obtained. While pyrolysis of Miscanthus loaded with 1% K+ yielded most stable carbon at 550 ?C, in the case of Miscanthus loaded with 2% K+ this was observed at 450 ?C (Fig.?2B). At higher temperatures these differences between AM loading levels became less pronounced (Fig?1B, 2B). Taking all AM-treatments together the relative increase in stable carbon yield was highest at 450 ?C (Fig.?3B) with +33.9% on average for both AM doping levels. This observation has very important practical implications, as it means that production units operating at the lower end of usual pyrolysis temperature ranges (450?500 ?C) could be used. Such units would not require high-grade stainless steel as a material for construction, reducing costs compared to units specified for higher temperatures. With increasing pyrolysis temperature, the pH and surface area of biochar increase while at the same time the functionality (O/C, H/C ratios) decreases31?33. Therefore, producing biochar at moderate pyrolysis temperatures, i.e. 450?550?C, is a good compromise, not only providing high yield of stable carbon, but also yielding biochar with beneficial properties for soil amelioration (high surface area, high CEC). AMs affect biochar microstructure and carbon stability. The increased stability of carbon can be explained by the catalytic effect of AMs on biomass pyrolysis, such as enhanced cross-linking reactions (e.g., dehydration forming C=C or C-O-C) resulting in a highly cross-linked biochar, compared to biochar from untreated biomass34,35. To further corroborate these findings, the structure of the biochar was investigated using Raman spectroscopy and X-ray diffraction (XRD), focusing on differences in the biochar carbon structure resulting from K+ doping. Raman spectra of the six biochar types investigated are shown in SI Fig.?2. Meaningful features of the spectra are (i) the position of the G peak, (ii) the relative intensity of the D and G peaks (the so-called ID/IG ratio), (iii) the shift of the D peak, and (iv) the width of the peaks. SI Fig.?2 shows that for both series the increase of temperature leads to a) a shift of the D-peak to lower wavenumbers, indicating a slight reduction in the size of defect free and/ or edge free regions, b) a decrease in the width of the D peaks with increasing temperature, indicating a reduction in the structural disorder. At any given process temperature, the use of K+ (1 and 2 wt%) leads to lower G peak intensities, i.e. to higher ID/IG ratio. This indicates that the amount of disordered material as determined by Raman spectroscopy is larger for K+ treated Miscanthus biochar. The XRD analysis of Miscanthus and K+ Miscanthus biochar confirmed the differences in biochar structure resulting from doping with potassium (see SI Table?5). The content of graphitic carbon, although small, increases because of K+ doping at all temperatures, with the effect being strongest at the lower end of the temperature range investigated. This is comparable with the trend seen for yield of stable carbon. Based on this evidence we can conclude that although the carbon structure in the K+ Miscanthus biochar appears to be less ordered and more defective than that of untreated Miscanthus biochar, it has a comparable recalcitrance. It is important to note here that in comparing the information obtained from Raman spectroscopy and XRD care has to be taken since XRD is a bulk technique while Raman is sampling a few hundred nanometres close to the surface. Hence findings from these two techniques must be looked at as complementary. The overall effect of AM on biochar and stable carbon yield is schematically shown in SI Fig.?6. This finding is fundamental for developing biochar for carbon sequestration purposes as it means that use of AM doping can make pyrolysis much more efficient in converting biomass carbon to stable biochar carbon. AMs doping enhances biochar?s role as a carbon sequestration tool. The potential of biochar to store atmospheric carbon has been estimated to be between 0.7?1.8 Gt CO2-C(eq) yr?13,12,13. Assuming a stable carbon increase of 45% as observed in this study for 2% potassium addition increases the carbon sequestration potential of biochar to between 1 and 2.6 Gt CO2-C(eq) yr?1, which corresponds to over 7% of current annual GHG emissions36 and close to 25% of annual atmospheric CO2 removal necessary to maintain atmospheric concentrations of CO2 at safe levels37. Another conclusion that can be drawn from this finding is that to sequester a given amount of carbon in form of biochar, 31% less biomass, and therefore land would be required, compared to biochar without AM additives. This would further reduce biochar?s already relatively low land requirement, compared to other NETs options13. In addition, tests of the K+-enhanced biochar showed that the majority of the K+ contained in the biochar was available and could be utilised by plants upon application of the amended biochar to soil (based on 0.01 M CaCl2-extraction (SI Table?6)). Therefore, K+-enhanced biochar provides not only a better tool for carbon sequestration, but also a better slow-release K-fertiliser, compared to unamended biochar. To date, viable biochar applications have been inextricably linked to biochar?s ability to increase crop yields5,38. Due to its much higher carbon sequestration potential, AM-enriched biochar offers a price competitive option for atmospheric carbon removal compared to bioenergy and carbon capture and storage (BECCS), and direct air capture (DAC) etc., especially if low-cost sources of potassium, such as ash39, can be utilised. Under such scenario, crop growth improvements would still be a desirable option40, in fact a more likely one due to the increased K content, but no longer as critical for viable biochar implementation. This opens-up a whole new range of potential applications where carbon sequestration can be achieved, but where only small or no crop yield benefits could be expected, e.g., fertile soils, contaminated land, as well as non-soil applications (e.g., building materials, underground storage). This is a breakthrough approach to biochar deployment and a paradigm shifting finding. Methods Biochar production. To prepare AM-loaded Miscanthus with 1% and 2% w/w K+ content (0.256 and 0.513 mmol g?1 dry feedstock), potassium was added in a similar manner to previous work23,41,42 by spraying an aqueous solution (174.7 g L?1 and 349.5 g L?1) of potassium acetate (Sigma-Aldrich, ?99.0%) onto oven-dried Miscanthus chips (approximately 10 mm in size) spread in a thin layer. In this way the desired level of potassium was introduced, and the biomass moisture was restored to the original level of ~12 wt%. Similarly, Na+ in form of an aqueous solution of sodium acetate (anhydrous, 98% pure, Fisher Scientific) (146 g L?1 sodium acetate) was applied to Miscanthus chips to introduce the same concentration in moles per weight of Miscanthus as 1% (w/w) K+ (256.4 ?mol g?1 dry feedstock). This ensures that the same molar amount of AM is present in the 1% AM treatments independently of their molar weight which is equivalent to 0.59% (w/w) Na+. These organic salts were selected as additives due to their easy applicability, relatively low costs (potassium acetate 650?850 USD t?143), bulk availability, widespread use (e.g., de-icing, drilling muds, fertilisers, etc.), and low environmental impact44,45. The untreated Miscanthus samples were pyrolysed at 350, 450, 550, 650 and 750 ?C with a continuous auger reactor described in Buss et al.21 with mean residence time of the biomass in the heated zone of around 21.5 minutes. The 1% K+ doped Miscanthus was pyrolysed in the same temperature range, but with duplicate at 550 ?C. Miscanthus doped with the other two AM treatments (2% K and 1% Na) was pyrolysed at the HTTs of 450 ?C, 550 ?C and 650 ?C. Biochar carbon stability. In this work, the chemical stability of biochar against oxidation in the environment was tested using a hydrogen peroxide wet oxidation method9. This method has been calibrated on naturally aged charcoal samples and corresponds to 92 and 187 years at mean annual temperatures of 17 ?C and 7 ?C, respectively. Hence, the stable carbon content determined in this study reflects the amount of carbon that is sequestered in the soil and for which carbon credits could be given. The method has also been cross-referenced with other proxies for carbon stability8, such as fixed carbon determined by proximate analysis (comparison of the two methods on the biochar samples from this study is provided in the supplementary information). The method is described in Cross et al.9 and in brief here. Before analysis, all biochars were ground to fine powder using a pestle and mortar, and homogenised sub-samples were used for the test. A char sample containing 0.1 g of C was mixed in a test tube with 0.01 mol of H2O2 in 7 mL of DI water. The test tubes were subsequently heated to 80 ?C and kept at this temperature, with occasional agitation, for two days until the solution had evaporated. Subsequently, the remaining material was dried overnight at 105 ?C before weighing the amount of residual char, and C content analysis. The carbon amount prior and post ageing was then calculated using the char amount and carbon content. The ratio of retained C to initial C gives the % stable carbon content. stable carbon content(%) = residual char mass ? residual char carbon content initial char mass ? initial char carbon content The analysis was performed in triplicate. By multiplying the stable carbon content by the char yield the stable carbon yield was calculated as described for the fixed carbon content by Antal and Gr?nli (2003)18. This corresponds to the efficiency of carbon conversion from biomass to biochar and serves as the key parameter for comparison in this work. Raman spectroscopy. Raman spectra measurements were performed using a Renishaw InviaH instrument equipped with a green laser source (wavelength: 514.5 nm). All samples were taken as received (crushed) and placed on a microscope glass slide and flattened to obtain an optical field as flat as possible to improve the focus on the sample. Several points were examined for each sample. For each point we started with a low magnification objective (5x) zooming-in using a 20x and finally recording spectra with a 50x objective. The area of each spot examined had a width of about 2 ?m2. Raman analysis being a volume technique, the signal is gathered from the sample surface up to a depth that varies with the optical properties of the analysed materials. In sp2-rich carbon materials this depth is of a few hundred nanometres (Ni, Z., Wang, Y., Yu, T. et al. Raman spectroscopy and imaging of graphene Nano Res. (2008) 1: 273. doi.org/10.1007/s12274?008?8036?1). The laser power was set at 5mW in order to obtain a good signal-to-noise ratio while avoiding damage of the sample due to excessive heating. Each measurement was carried out in extended mode (100 cm?1 to 3500 cm?1) with an exposure time of 10 s and with 3 accumulations. X-ray diffraction (XRD). A Bruker D8 advance XRD instrument with a Cu Anode was used at 40 mA and 40 kV with a NaI detector which analysed at 1.5 s/step from 2 to 65? in 0.025?/step increments. The raw data were evaluated with the software TOPAS 3.0 Rietveld analysis. The biochar samples were spiked with 20% calcite to quantitatively measure the composition of mineral in the samples relative to a known concentration of calcite. Statistics. Two-sample, two-sided, equal variances t-tests in Microsoft Excel were performed to determine effects of the 1% K+ addition on stable carbon yields. One-way ANOVAs followed by Tukey post-hoc tests (in SigmaPlot 13.0) were used to investigate the effect of the various AM treatments on stable carbon yield and the effect of the HTT on char yield and stable carbon yield taking the AM treatments as replications. Significant differences are given with a significance level of p < 0.05. Data Availability All data related to this experiment are provided within the article and the Supplementary Information. Acknowledgements The authors would like to acknowledge the financial support of the Engineering and Physical Sciences Research Council (EPSRC) for the impact acceleration award that enabled this work. Author Contributions Ond?ej Ma?ek led the research design and manuscript preparation, he also contributed to sample analysis, data collection, data analysis and interpretation. Wolfram Buss led the data analysis and interpretation, and contributed to experimental work, sample analysis, and manuscript preparation. Peter Brownsort contributed to research design, experimental work, sample analysis, data collection, data analysis and interpretation, and manuscript preparation. Massimo Rovere contributed to sample analysis, data collection, data analysis and interpretation, and manuscript preparation. Alberto Tagliaferro contributed to sample analysis, data collection, data analysis and interpretation, and manuscript preparation. Ling Zhao provided advisory support, contributed to data interpretation, and manuscript preparation. Xinde Cao provided advisory support, contributed to data interpretation, and manuscript preparation. Guangwen Xu provided advisory support, contributed to data interpretation, and manuscript preparation. Competing Interests: The authors declare no competing interests. Publisher?s note: Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations. Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. 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Additional Information Supplementary information accompanies this paper at https://doi.org/10.1038/s41598-019-41953-0.


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Ondřej Mašek, Wolfram Buss, Peter Brownsort, Massimo Rovere, Alberto Tagliaferro, Ling Zhao, Xinde Cao, Guangwen Xu. Potassium doping increases biochar carbon sequestration potential by 45%, facilitating decoupling of carbon sequestration from soil improvement, Scientific Reports, 2019, DOI: 10.1038/s41598-019-41953-0