Accepted Manuscript
Biomass Proximate Analysis using Thermogravimetry
Roberto Garca, Consuelo Pizarro, Antonio G. Lavn, Julio L. Bueno
PII: S0960-8524(13)00601-9
DOI: http://dx.doi.org/10.1016/j.biortech.2013.03.197
Reference: BITE 11657
To appear in: Bioresource Technology
Received Date: 24 July 2012
Revised Date: 27 March 2013
Accepted Date: 29 March 2013
Please cite this article as: Garca, R., Pizarro, C., Lavn, A.G., Bueno, J.L., Biomass Proximate Analysis using
Thermogravimetry, Bioresource Technology (2013), doi: http://dx.doi.org/10.1016/j.biortech.2013.03.197
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Biomass Proximate Analysis using Thermogravimetry
Roberto Garca, Consuelo Pizarro(*), Antonio G. Lavn, Julio L. Bueno
Department of Chemical Engineering and Environmental Technology, Faculty of
Chemistry, University of Oviedo. Julin Clavera 8, 33006, Oviedo, Spain
ABSTRACT
This work proposes a 25 minutes-last thermogravimetric method as a tool to determine
biomass samples proximate analysis data (moisture, ash, volatile matter and fixed
carbon contents) just by direct measure of weight changes on each samples TG chart.
Compared with international standards commonly used to that aim, TG is a faster and
easier to develop technique. Obtained results were satisfactory, with AEE under 6% for
moisture and volatile matter, close to 10% for fixed carbon determination and AAD of
1.6 points for ash content.
Key words
Biomass, proximate analysis, thermogravimetry
* Representing Author: Tel +0034 985 103438; Fax +0034 985 103434
E-mail address: pizarroconsuelo@uniovi.es (C. Pizarro)
E-mail addresses: garciafroberto@uniovi.es (Roberto Garca),
pizarroconsuelo@uniovi.es (Consuelo Pizarro), agl@uniovi.es (Antonio G. Lavn),
jlbueno@uniovi.es (Julio L. Bueno)
1. Introduction
As widely reported, biomass constitutes an important feedstock in the current world
energetic scenario (McKendry, 2002; Muthuraman et al., 2010; Jorquera et al., 2010). It
presents some environmental advantages, such as gaseous CO2 emissions neutrality (Gil
et al., 2010; Munir et al., 2009), or low NOx and SO2 emissions (Li et al., 2009; Qian et
al., 2011). In addition to this, it has social advantages too, providing a source of wealth
in rural areas, avoiding its depopulation (Bahng et al., 2009). Finally it is cheap and
easy to produce. In that way, biomass is an autonomous resource, which partly avoids
dependence on fossil fuels, which are produced in only a limited number of countries.
In addition to this, the low price of raw materials and the development of biomass-
consuming energy systems have made them economically competitive with traditional
fossil fuels.
Because of that, biomass appears as an important role-playing fuel in several national
and international policies (Gaska and Wandrasz, 2008; Rosendahl et al., 2007), such as
the European Union White Papers on energy saving, or the PER (Renewable Energy
Plan) in Spain (Lapuerta et al., 2004).
As can be seen, the future of biomass energy conversion appears to be quite optimistic,
but its energetic use also presents some problems, the most important one being related
to its own nature, even though it is a highly heterogeneous fuel, with plenty of different
origins, from a huge variety of industrial wastes to wood transformation industry-
residues or energy crops. Taking this into account, biomass characterization is required,
to reliably predict its behaviour as a fuel. When considering biomass thermal
conversion, proximate analysis is one of the most important characterization methods.
This consists in determining moisture, ash, volatile matter and fixed carbon contents of
the raw biofuel. These values are essential ascertain moisture, volatile matter and fixed
carbon affect both on the combustion behaviour and the plant design. In that way, high
moisture values decrease the combustion yield, while high volatile matter/fixed carbon
ratios are related with the fuels reactivity. On the other hand, ash deeply influences the
transport, handling and management costs of the process. It is also influential in
corrosion and slag formation. Traditionally, these measures are developed following
different national and international normative, such as ASTM E-871 for moisture,
ASTM E-830, D-1102 or UNE-EN 14775 for ash or ASTM E-872 and ASTM E-1755
for volatile matter determination (Demirbas, 2004; Khalil et al., 2008). Fixed carbon is
usually determined by difference. All those methods are time-consuming and tedious
(Karatepe and Kckbayrak, 1993), and the success of the operation is highly
influenced by the operators skills. In that way, a fast, simple, reliable and highly
accurate method for routine tests, would be desirable. Since all the above mentioned
standards basically establish heating a sample under different specific conditions
(Mayoral et al., 2001), and a weight difference determination, then a thermobalance
and a conveniently adapted thermogravimetric study appears as an effective tool
(Warne, 1991), resulting in both time-saving, from several hours to just a few minutes
in each experiment (Sadek and Herrell, 1984) and sample quantity reduction, as it
requires matter weight in the range of milligrams (Beamish, 1994).
As is well known, thermal analysis can be defined as a group of methods for measuring
the property of a substance when subjected to a controlled temperature program. It is a
highly developed technique with many different uses when applied to biomass. Some
authors have used it to study the thermal behaviour of biomass and fuel blends in both
oxidative and inactive atmospheres (Ghetti et al., 1996; Varol et al., 2010; Wilson et al.,
2010). Others used this technique as a tool to thermally characterize fuels and ashes, by
studying its melting behaviour or structural changes (Biswas et al., 2011; Miranda et al.,
2011, Ross et al., 2008) while others used TG as a tool to develop kinetic modelization
(Ramajo-Escalera et al., 2006; Wilson et al., 2011). However, but not so many works
have been developed for biomass proximate analysis, whilst, on the other hand,
thermogravimetry is often used in that way for coals (Ottaway, 1982; Slaghuis and
Raijmakers, 2004).
In this context, the aim of this work is to determinate if TG analysis can be used as an
effective tool to approach ultimate analysis data of biomass fuels and propose a method,
based on modified-coal methods to reliably and accurately obtain these data.
2. Materials and methods.
Firstly, thirteen biomass samples were grinded and sieved to 500 m to guarantee its
homogeneity in a proximate analysis routine by using ASTM standards E 871, E 1755
and E872; for moisture, ash and volatile matter respectively. In addition to this, fixed
carbon content was calculated by difference using the balance:
% FC = 100 (% Ash + %VM ) [1]
where %FC, %Ash and %VM respectively mean the mass percentages of fixed carbon,
ash and volatile matter of the raw sample.
All these procedures were detailed and referenced in our previous works (Garca et al.,
2012). After this routine every sample was tested using a Perkin Elmer STA 6000
thermobalance, using 10 and 20 mg of sample, and 40 ml/min flow of flue gas, for both
nitrogen and air. Samples were selected all around Spain trying to track every possible
biomass origin, commercial fuels, agri-food industry wastes, forest wastes, energy crops
and cereals (Fernndez et al., 2012) with the aim of obtaining a general method, suitable
for a wide range of biomass fuels, with different characteristics and compositions.
The bibliographical review search for methods developed for coals showed two basic
groups, some simpler ones, which consist in a chosen continuous temperature ramp path
between room temperature and the final set-point (TR1 and SP1, as detailed in table 1).
In this group we may include works proposed by Mayoral et al., 2001(MAY3), Sadek
and Herrell, 1984) (SDK1) or (Lapuerta et al., 2004)(LAP). On the other hand, there are
some other proceedings consisting in continuous heating (TR1, 2 or 3 depending on the
number of this steps) combined with intermediate dwellings (DT1, 2 and 3) to reach
different intermediate or final set-point (SP1, 2 or 3). In this group we can include some
other Mayoral proposed methods (MAY1, MAY2 and MAY4 ), Ottaway(OTT)
(Ottaway, 1982), Sadek and Herrel (SDK2), Karatepe and Kckbayrak, 1993(KAR),
Warne (WAR) (Warne, 1991), and Beamish (BEA) (Beamish, 1994). Table 1
summarizes the conditions required in each of these works, with each temperature ramp
(TR), intermediate and final setpoints (SP) and dwelling times (DT) required when each
set-point is reached. Most of them are conducted in inactive atmosphere (using argon,
helium or nitrogen depending on the author) to measure moisture, volatile matter and
fixed carbon and with a final combustion time in oxidative environment (oxygen or air),
when set-point is reached, to measure ashes. On the other hand, Lapuertas work is
completely carried out in oxidative atmosphere. Some of these works explain how
relevant data must be obtained from Thermogravimetry. TG diagrams commonly
present a number of slopes, each kinetics showing different phase changes. A first,
normally, small one represents moisture release due to drying, occuring at a temperature
under 150C (Zheng and Kozinski, 2000). In the range between 200 and 900 C, a huge
mass loss is seen. In the context of different phenomena that can be observed. Thus,
between 200 and 600 C the biggest mass loss occurs due to the release of CO2 and
CH4, these gases coming from hemicelluloses (190-320 C), cellulose (280-400 C) and
lignin (320-450 C) decomposition (Strezov, 2004), and a later chemically bonded CO2
and chemically formed water release (450-600 C). Finally, from 600 to proximately
900 C mass loss rate decreases, due to the evolution of carbon-containing species (COx,
CxHy and tars) and char oxidation until constant weight is reached (Haykiri-Ama,
2003).
Five methods originally developed, and described in the literature, for coals and cokes
proximate analysis determination, were tested. In this work once observed which of
them presents the best results, they were slightly adapted to biomass samples, aiming to
reduce the experimental time without impoverishing the obtained results. The tested
methods were LAP, MAY1, SDK and KAR. In addition to this a variation of OTT,
called OTT* consisting in a second dwelling of five minutes at 550C, was used.
Obtained results are compared with proximate analaysis data determined using
international standards, provided in Table 2 (Garca et al., 2012), experimental errors
are calculated and average absolute error values shown in Figure 1.
The error criteria used are the average experimental error (AEE) and the average bias
error (ABE) commonly used by several authors in this field (Ahmaruzzaman, 2008;
Majumder et al., 2008). In addition to this, the average absolute deviation (AAD) is also
used. Those criteria are defined as follows:
[2]
[3]
[4]
As can be seen in figure 1, the KAR method presents the best results for both moisture
and volatile matter determination, and so, because of this will be considered as a base
method to develop future variations, trying to improve accuracy in both of this
parameters and ash and fixed carbon contents.
3. Results and discussion
Once KARs method has been chosen and carried out as the base one, some changes are
developed therein, aiming to obtain a more suitable method for biomass proximate
analysis data determination. In that way, biomass is reportedly far more reactive than
coal, and so, faster heating ramps can be used without losing complete conversion
during combustion. In that way, some new methods are tested, proving that the best
results were found when beginning with a heating ramp of 50C/min, from room
temperature until obtaining an isothermal 120C for 3 minutes, then a new 100C/min
heating ramp is programmed until 950C.When this point is reached, a cooling process
with -100C/min ramp starts until reaching 450C. Until this set-point, the process is
developed using nitrogen, to guarantee a non oxidative environment, but, when 450C is
reached, flue gas is changed for air. Then, a new 100C/min heating ramp begins until
800C, which provides better results than previous methods, and is isothermally
maintained for 3 minutes, when the program is finished, totalling 25 minutes per
experiment, enabling two experiments per hour, including cooling and stabilization of
the experimental equipment, which entails a great time saving compared to several
hours taken for the moisture and ash determination. This method is also more
convenient than ASTM standard, and so, volatile matter determination implies working
with a furnace at 950C, involving physical risk for the operator when introducing and
withdrawing samples. This proposed method requires direct measure of moisture,
volatile matter, fixed carbon and ash by difference from slope to slope. Volatile matter
and fixed carbon values are thus obtained by applying Beamishs correction which
means adding values obtained with the next formulae to the measured value.
[5]
[6]
where VM, FC, VMTG and FCTG are, respectively, the obtained volatile matter and fixed
carbon and those measured in TG, and M and A, moisture and ash content read on the
TG profile. These corrections are proven to slightly improve the results.
Finally, results obtained for each of the samples are detailed in Table 3, and the average
values are compared (named as NEW MET) with the coal-developed methods in Figure
1. As can be seen, moisture and volatile matter experimental errors are satisfactory, with
AEE under 6 %, resulting in AAD of 0.5 and 4.4 points, respectively. On the other
hand, fixed carbon and especially ash results highly improve the values obtained using
coal-developed methods, offering values close to 10 and 50 %, respectively. Taking into
account that fixed carbon determination is obtained empirically by difference, with the
entailing precision and accuracy limits, an 11% average error and 2.0 average absolute
deviation points, can be considered as quite acceptable result. Regarding ash
determination, this involves a problem already referred to by other authors (Mayoral et
al., 2001). As can be seen in Table 3, there exists a big difference in measured EE
depending on the considered sample. In that way, beetroot pellets or wheat grain present
accurate results, with an experimental error close to 5%, while the same error in some
other samples such as hazelnut shell or both brands of wood pellets approaches 90 %.
As can be observed with the absolute deviation, those values are not high at all; in fact
the AAD is just over that of the moisture, presenting a 1.6 % value. However, as
expected, ash values are really low in biomass, mainly in woody samples. Low absolute
errors imply really high deviations, in relative bases, like AEE, may be due to the
formation of highly specific weight oxides when the oxidative environment is reached.
4. Conclusions
This work proposes a suitable method to determine proximate analysis data of biomass.
Obtained results, with average experimental errors under 6 % for moisture and volatile
matter and close to 10 % for fixed carbon greatly improve coal-developed methods, for
the same tested samples. Ash determination entails average absolute deviation of 1.6
points, but the low expected values imply higher experimental errors. Other important
advantages are time saving and simplicity, as this method requires 25 minutes to obtain
all four data sets while only moisture or ash determination take several hours each,
using the standard normative.
ACKNOWLEDGMENTS
PSE-ARFRISOL, Ref. PS-120000-2005-1, is a science-technology project qualified as
Strategic by 2004-07 Spanish National Research Plan, Development and Diffusion, co-
financed by European Regional Development Funds and the Spanish Ministry of
Science and Education. We wish to acknowledge all members of the PSE-ARFRISOL
partnership for their cooperation.
We would also like to thank a number of companies such as Pellets Asturias, Factor
Verde, Molygrasa, Dibiosur, Enfosur, Acciona, Nutral Arroceras Dorado, CarsanBio,
Parque Verde, Vinos Viadecanes, Cooperativa Agrcola de Cangas del Narcea, Vino
de la Tierra de Cangas, Gebio, Bioenerga Aragonesa, Cafs el Gallego, Biomasas
Herrero, Ecowarm and Carbones Lamuo for their generous collaboration in supplying
most of the required samples.
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by thermogravimetry. New Zealand J. Geol. Geoph. 37, 387-392.
Biswas, A.K., Umeki, K., Yang, W., Blasiak, W., [22] 2011. Change of pyrolysis
characteristics and structure of woody biomass due to steam explosion pretreatment.
Fuel Process. Technol. 92, 18491854.
Demirbas, A., [12] 2004. Combustion characteristics of different biomass fuels.
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Karatepe, N., Kckbayrak, S., [14] 1993. Proximate analysis of Turkish lignites by
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Khalil, R.A., Meszaros, E., Grnli, M.G., Vrhegyi, G., Mohai, I., Marosvolgyi, B.,
Hustad, J.E., [13] 2008. Thermal analysis of energy crops Part I: The applicability of a
macro-thermobalance for biomass studies. J. Anal. Appl. Pyrolysis. 81, 5259.
Lapuerta, M., Hernndez, J.J., Rodrguez, J., [11] 2004. Kinetics of devolatilisation
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Thermal analysis and devolatilization kinetics of cotton stalk, sugar cane bagasse and
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Acta. 448, 111116.
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6504
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Physical characterization of biomass fuels prepared for suspension firing in utility
boilers. Biomass Bioenerg. 31, 318-325.
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combustion characteristics of low quality lignite coals and biomass with
thermogravimetry analysis. Thermochim. Acta. 510,195-201.
Warne, S.S.J., [16] 1991. Proximate analysis of coal, oil shale, low quality fossil
fuels and related materials by thermogravimetry. Trends in Anal. Chem. 10(6), 195-
199.
Wilson, L., John, G.R., Mhilu, C.F., Yang, W., Blasiak, W., [21] 2010. Coffee husks
gasification using high temperature air/steam agent. Fuel Process. Technol. 91,1330
1337.
Wilson, L., Yang, W., Blasiak, W., John, G.R., Mhilu, C.F., [26] 2011. Thermal
characterization of tropical biomass feedstocks. Energy Conserv. Manag. 52,191-198.
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Sorted numerically
[1] McKendry, P., 2002. Energy production from biomass (Part 1): overview of
biomass. Bioresour. Technol. 83, 37-46.
[2] Muthuraman, M., Namioka, T., Yoshikawa, K., 2010. A comparison of co-
combustion characteristics of coal with wood and hydrothermally treated municipal
solid waste. Bioresour. Technol. 101, 2477-2482.
[3] Jorquera, O., Kiperstok, A., Sales, E.A., Embiruu, M., Ghirardi, M.L., 2010.
Comparative energy life-cycle analyses of microalgae biomass production in open
ponds and photobioreactors. Bioresour. Technol. 101, 1406-1413.
[4] Gil, M.V., Oulego, P., Casal, M.D., Pevida, C., Pis, J.J., Rubiera, F., 2010.
Mechanical durability and combustion characteristics of pellets from biomass blends.
Bioresour. Technol. 101, 8859-8867.
[5] Munir, S., Daood, S.S., Nimmo, W., Cunliffe, A.M., Bibbs, B.M., 2009.
Thermal analysis and devolatilization kinetics of cotton stalk, sugar cane bagasse and
shea meal under nitrogen and air atmospheres. Bioresour. Technol. 100,1413-1418.
[6] Li, Z., Zhao, W., Li, R., Wang, Z., Li, Y., Zhao, G., 2009. Combustion
characteristics and NO formation for biomass blends in a 35-ton-per-hour travelling
grate utility boiler. Bioresour. Technol. 100, 2278-2283.
[7] Qian, F.P., Chyang, C.S., Huang, K.S., Tso, J., 2011. Combustion and NO
emission of high nitrogen content biomass in a pilot-scale vortexing fluidized bed
combustor. Bioresour. Technol. 102, 1892-1898.
[8] Bahng, M.K., Mukarakate, C., Robichaud, D.J., Nimlos, M.R., 2009. Current
technologies for analysis of biomass thermo-chemical processing: A review. Anal
Chim Acta. 651, 117-138.
[9] Gaska, K., Wandrasz, A.J., 2008. Mathematical modeling of biomass fuels
formation process. Waste manag. 28, 973-985.
[10] Rosendahl, L.A., Yin, C., Kaer, S.K., Friborg, K., Overgaard, P., 2007.
Physical characterization of biomass fuels prepared for suspension firing in utility
boilers. Biomass Bioenerg. 31, 318-325.
[11] Lapuerta, M., Hernndez, J.J., Rodrguez, J., 2004. Kinetics of devolatilisation
of forestry wastes from thermogravimetric analysis. Biomass Bioenerg. 27, 385 391
[12] Demirbas, A., 2004. Combustion characteristics of different biomass fuels.
Prog. Energy Comb. Sci. 30, 219-230.
[13] Khalil, R.A., Meszaros, E., Grnli, M.G., Vrhegyi, G., Mohai, I.,
Marosvolgyi, B., Hustad, J.E., 2008. Thermal analysis of energy crops Part I: The
applicability of a macro-thermobalance for biomass studies. J. Anal. Appl. Pyrolysis.
81, 5259.
[14] Karatepe, N., Kckbayrak, S., 1993. Proximate analysis of Turkish lignites by
thermogravometry. Thermochim. Acta. 213,147-150.
[15] Mayoral, M.C., Izquierdo, M.T., Andrs, J.M., Rubio, B., 2001.Different
approaches to proximate analysis by thermogravimetry analysis. Thermochim. Acta
370, 91-97.
[16] Warne, S.S.J., 1991. Proximate analysis of coal, oil shale, low quality fossil
fuels and related materials by thermogravimetry. Trends in Anal. Chem. 10(6), 195-
199.
[17] Sadek, F.S., Herrell, A.Y. 1984. Methods of proximate analysis by
thermogravimetry. Thermochim Acta. 81, 297-303.
[18] Beamish, B.B., 1994. Proximate analysis of New Zealand and Australian coals
by thermogravimetry. New Zealand J. Geol. Geoph. 37, 387-392.
[19] Ghetti, P., Ricca, L., Angelini, L., 1996. Thermal analysis of biomass and
corresponding pyrolysis products. Fuel. 75(5), 565573.
[20] Varol, M., Atimtay, A.T., Bay, B., Olgun, H., 2010. Investigation of co-
combustion characteristics of low quality lignite coals and biomass with
thermogravimetry analysis. Thermochim. Acta. 510,195-201.
[21] Wilson, L., John, G.R., Mhilu, C.F., Yang, W., Blasiak, W., 2010. Coffee husks
gasification using high temperature air/steam agent. Fuel Process. Technol. 91,1330
1337.
[22] Biswas, A.K., Umeki, K., Yang, W., Blasiak, W., 2011. Change of pyrolysis
characteristics and structure of woody biomass due to steam explosion pretreatment.
Fuel Process. Technol. 92, 18491854.
[23] Miranda, M.T., Arranz, J.I., Romn, S., Rojas, S., Montero, I., Lpez, M., Cruz,
J.A., 2011. Characterization of grape pomace and Pyrenean oak pellets. Fuel Process.
Technol. 92, 278283.
[24] Ross, A.B., Jones, J.M., Kubacki, M.L., Bridgeman, T., 2008. Classification of
macroalgae as fuel and its thermochemical behaviour. Bioresour. Technol. 99, 6494
6504
[25] Ramajo-Escalera, B., Espina, A., Garca, J.R., Sosa-Arnao, J.H., Nebra, S.A.,
2006. Model-free kinetics applied to sugarcane bagasse combustion. Thermochim.
Acta. 448, 111116.
[26] Wilson, L., Yang, W., Blasiak, W., John, G.R., Mhilu, C.F., 2011. Thermal
characterization of tropical biomass feedstocks. Energy Conserv. Manag. 52,191-198.
[27] Ottaway, M., 1982.Use of thermogravimetry for proximate analysis of coals
and cokes. Fuel. 61, 713-716.
[28] Slaghuis, J.H., Raijmakers, N., 2004. The use of thermogravimetry in
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Figure 1 Average experimental errors observed for the tested methods.
INACTIVE ATMOSPHERE OXIDATIVE ATMOSPHERE
METHOD TR1 SP1 DT1 TR2 SP2 DT2 CT TR3 SP3 DT3
MAY 1 20 105 5 20 900 - 20 - - -
MAY 2 20 900 5 -25 450 - - 20 700 -
MAY 3 80 1020 10 - - - - - - -
MAY 4 20 105 3 80 850 - - - - -
OTT 250 110 1-5 250 900 1-5 1 - - -
SDK 1 100 1000 3 - - - 3 - - -
SDK 2 100 135 2 100 1000 3 3 - - -
KAR 20 110 30 40 950 7 - -20 750 5
WAR 100 110 2 100 950 3 3 - - -
BEA 50 110 5 50 950 7 42 - - -
TR1 SP1 DT1 TR2 SP2 DT2 CT TR1 SP1 DT1
LAP - - - - - - 18-108 10-60 1100 -
Table 1 Summary of the studied analysis methods developed for coals and methods
assayed for biomass.
Where: TR 1, 2 and 3 are the first, second and third temperature ramps respectively,
measured in C/min. SP is the set-point for each temperature ramp, measured in C and
DT is the dwelling time after each ramp, measured in minutes. CT is the combustion
time in oxidative atmosphere when set-point is reached.
Sample %M %A % VM % FC
Apple tree leaves 9.3 12 71.9 16.1
Beetroot pellets 12.5 9 76 15
Chestnut tree leaves 8.2 4.9 72.41 22.69
Hazelnut shell 8.74 2.2 77 20.8
Miscanthus 7.53 9.6 79 11.4
Nectarine stone 8.2 1.1 76 22.9
Peach stone 8.55 0.5 75.6 23.9
Pine and pine apple leaf pellets 8.25 3.2 74.5 22.3
Pistachio shell 8.75 1.3 82.5 16.2
Soya grain 10.4 4.8 77 18.2
Wheat grain 10.3 2.8 80 17.2
Wood pellets 1 7.96 1.3 82 16.7
Wood pellets 2 7.53 0.66 84 15.34
Table 2 Data obtained for moisture (M), ash (A), volatile matter (VM) and fixed
carbon (FC) content of biomass samples using ASTM normative, measured in mass
percentage.
MOISTURE ASH VOLATILE MATTER FIXED CARBON
M MV EE BE AD MV EE BE AD MV EE BE AD MV EE BE AD
Apple tree leaves 13.3 8.3 11.0 -11.0 1.0 6.45 46.2 -46.2 5.5 67.3 6.4 -6.4 4.6 16.6 3.1 3.1 0.5
Beetroot pellets 12.1 11.0 11.8 -11.8 1.5 8.43 6.3 -6.3 0.6 62.5 17.8 -17.8 13.5 10.7 28.8 -28.8 4.3
Chestnut tree leaves 13.0 8.1 1.4 -1.4 0.1 2.90 40.9 -40.9 2.0 70.8 2.2 -2.2 1.6 20.2 10.8 -10.8 2.5
Hazelnut shell 14.1 8.5 2.5 -2.5 0.2 0.15 93.4 -93.4 2.1 73.5 4.5 -4.5 3.5 23.3 11.8 11.8 2.5
Miscanthus 11.8 7.9 5.5 5.5 0.4 6.37 33.7 -33.7 3.2 69.6 11.8 -11.8 9.4 13.5 18.6 18.6 2.1
Nectarine stone 18.6 7.9 4.1 -4.1 0.3 0.52 53.1 -53.1 0.6 80.7 6.2 6.2 4.7 21.1 7.7 -7.7 1.8
Peach stone 19.5 7.9 7.4 -7.4 0.6 0.73 46.8 46.8 0.2 81.8 8.1 8.1 6.2 20.4 14.7 -14.7 3.5
Pine and pine apple leaf pellets 13.0 8.8 6.8 6.8 0.6 1.81 43.3 -43.3 1.4 70.5 5.4 -5.4 4.0 21.3 4.6 -4.6 1.0
Pistachio shell 14.7 8.2 6.1 -6.1 0.5 0.53 59.1 -59.1 0.8 79.7 3.4 -3.4 2.8 17.5 7.8 7.8 1.3
Soya grain 19.1 9.4 9.3 -9.3 1.0 2.78 42.0 -42.0 2.0 76.6 0.5 -0.5 0.4 18.1 0.7 -0.7 0.1
Wheat grain 17.0 10.2 0.7 -0.7 0.1 2.95 5.3 5.3 0.1 77.6 3.0 -3.0 2.4 13.0 24.3 -24.3 4.2
Wood pellets 1 14.1 7.8 2.5 -2.5 0.2 0.21 84.0 -84.0 1.1 79.8 2.7 -2.7 2.2 18.4 10.1 10.1 1.7
Wood pellets 2 13.4 8.0 5.7 5.7 0.4 0.08 88.3 -88.3 0.6 81.9 2.5 -2.5 2.1 15.4 0.4 0.4 0.1
Average values 5.8 -3.0 0.5 49.4 -41.4 1.6 5.7 -3.5 4.4 11.0 -3.1 2.0
Table 3 Values obtained for each of the chosen samples.
Where M is the mass of sample (mg), Mv the measured value (%), EE, BE and AD are respectively experimental error (%), the BIAS error and
the absolute deviation for each individual sample. The average values are presented in the last row.
- A method to determinate proximate analysis data in biomass by TG is proposed
- Coal developed methods are compared and improved for biomass use.
- Satisfactory results are obtained, main on moisture and volatile matter values.