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Biofuels and Biomass
Characteristics of biomass devolatilization and in-situ char gasification tested by the non-isothermal method Xi Zeng, Kaito Kahara, Yasuaki Ueki, Ryo Yoshiie, Guangwen Xu, and Ichiro Naruse Energy Fuels, Just Accepted Manuscript • DOI: 10.1021/acs.energyfuels.9b00672 • Publication Date (Web): 03 Sep 2019 Downloaded from pubs.acs.org on September 3, 2019
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Energy & Fuels
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Characteristics of biomass devolatilization and in-situ char
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gasification tested by the non-isothermal method
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Xi Zeng1, 2*, Kaito Kahara3, Yasuaki Ueki1, Ryo Yoshiie3, Guangwen Xu2, Ichiro Naruse1
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1 Institute of Materials and Systems for Sustainability (IMaSS), Nagoya University, Nagoya
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464-8601, Japan
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2 State Key Laboratory of Multi-Phase Complex Systems, Institute of Process Engineering,
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Chinese Academy of Sciences, Beijing 100190, People’s Republic of China
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3 Department of Mechanical Systems Engineering, Nagoya University, Nagoya 464-8601,
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Japan
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*Authors to whom correspondence should be addressed. Phone: +81-52-789-2710; Fax:
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+81-52-789-5123; E-mail:
[email protected] (Xi Zeng).
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ABSTRACT
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This work examined the reaction behavior and kinetics of in-situ char gasification and
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the corresponding biomass devolatilization by TGA based on the non-isothermal method.
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Four kinds of devolatilization atmosphere (N2, N2+CO2 (10%), N2+CO2 (50%), N2+steam
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(10%)), three kinds of gasification atmosphere (N2+CO2 (10%), N2+CO2 (50%), N2+steam
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(10%)) and different heating rates (5, 10, 20, 30, 40 K/min) were adopted. With the increase
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of heating rate in each atmosphere for biomass devolatilization or char gasification, the
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typical reaction temperatures, including TBD-max, TCG-i, and TCG-max, increased obviously due to
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the delayed effect. At a given heating rate, the adopted devolatilization atmospheres displayed
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very weak influence on the volatiles release behavior and kinetics, even for the CO2 content
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of 50 %, but had obvious influence on the char property. The volume reaction model and
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shrinking core reaction model were suitable to describe the behaviors of biomass
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devolatilization and char gasification, respectively. Compared to biomass devolatilization, the
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reaction atmosphere had a remarkable effect on char gasification, especially in the curve
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shape of reaction rate and kinetic parameters. For the in-situ char gasification, the calculated
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activation energy (E) in the steam atmosphere was much lower than that in the CO2
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atmosphere. While for the char gasification in the steam atmosphere, the E of ex-situ char was
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higher than that of in-situ char, indicating the necessity of adopting the in-situ char for the
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char gasification research.
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Keywords: Biomass; Devolatilization; Gasification; In-situ char; TGA;
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1. INTRODUCTION
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As a renewable and sustainable resource, biomass is a direct and promising alternative to
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traditional fossil fuels because of low cost, CO2 neutrality, abundance, and uniform
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distribution throughout the world [1-3]. Among the diverse technologies for biomass
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utilization, gasification represents one of the most attractive and competitive options by
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converting the carbonaceous solid fuel into the combustible gaseous fuel cleanly and
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high-efficiently [4, 5]. Generally, the typical process in an industrial gasifier always involves
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complex physical change, homogeneous and heterogeneous chemical reactions, and the
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corresponding heat and mass transfer, such as drying, devolatilization, gasification,
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combustion, and tar cracking [6]. Among them, char gasification is much related to the
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process of biomass devolatilization by changing the char property. As the primary
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rate-limiting step, char gasification dominates the whole biomass gasification process [7, 8].
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So an improved and comprehensive understanding of biomass devolatilization and char
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gasification becomes essential and necessary for the design, operation, and scale-up of a
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practical gasifier.
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According to the difference in the char preparation approach for the following char
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gasification experiment, the numerous researches in literature can be divided into in-situ char
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gasification and ex-situ char gasification. For the former, biomass devolatilization and char
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gasification were conducted simultaneously or subsequently in the same reactor and
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atmosphere. During this process, the char was always in the hot state without the operation of
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tar collection. While for the latter, they were performed individually in the different reactors
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with the same or the different atmospheres, or the same reactor but with the different 3
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atmospheres. Generally, two approaches were adopted in the research of ex-situ char
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gasification: (1) preparing char in an apparatus under the inert atmosphere (N2, Ar, etc.) and
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then gasifying the pre-prepared cooled char by another reactor (TGA, drop tube reactor, etc.)
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in the reactive atmosphere (O2, air, CO2, steam, etc.) [9-12]; (2) preparing char firstly in an
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inert atmosphere and then directly switching it to the reactive atmosphere in the same
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apparatus at high-temperature [13-16]. In this study, the char samples from the two
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approaches were marked as the ex-situ char 1 and the ex-situ char 2, respectively. As we
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know, the processes of cooling, annealing, and the secondary heating inevitably influence the
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property of char, such as porous structure and the distribution of active site, further leading to
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the loss of char activity [17]. Moreover, in a commercial gasifier, especially for the fluidized
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bed or entrained flow gasifier, the continuous processes of drying, pyrolysis, and gasification
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occur nearly under the same operating condition. So, compared to the ex-situ char, the in-situ
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char can simulate most closely the fluidized bed gasifier and the entrained flow gasifier.
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These make it very necessary to measure the reaction behavior and kinetics of the in-situ char.
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Due to the limitation in measuring principle and instrument structure, the kinetic
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information of in-situ char, especially for the gasification reaction between char and steam,
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was still scarce [18]. Peng et al. [19] compared the gasification reactivity of in-situ and ex-situ
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coal char in the temperature range of 1273-1673 K. The measured TGA curve was divided
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into coal pyrolysis and char gasification by the special mathematical treatment. Compared to
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the ex-situ char, the reaction rate of in-situ char was much higher, reaching up to six times,
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and the curve shapes of reaction rate versus conversion were also different. To optimize the
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design of a kind of air-staged boiler, Chen et al. [20] measured the reaction characteristics of 4
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in/ex-situ chars on a down-firing furnace and further calculated the gasification kinetics. The
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mass balance can be obtained by measuring the gaseous products on a Fourier transform
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infrared spectroscopy (FTIR) gas analyzer and micro gas chromatography (GC). The tested
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reaction rate of in-situ char was about 4.6 times of that ex-situ char. Wang et al. [21]
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examined the gasification characteristics of in-situ char by decoupling pyrolysis and
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gasification in a micro fluidized bed reactor that connected a fast process mass spectrometer.
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Compared to the adopted ex-situ char sample, the in-situ char had the highest reaction rate
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and the lowest activation energy (E). All of these researches strongly verified the necessity
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and availability of using the in-situ char during the gasification reaction analysis. However, in
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the researches mentioned above, due to adopting the complicated mathematical derivation and
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the limitation of low sampling frequency in the gas analyzers, it always brought in serious
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uncertainty during the definition of the critical point between pyrolysis and gasification.
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Meanwhile, for these isothermal gasification researches, it rarely considered the
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corresponding behavior and kinetics of fuel devolatilization. Moreover, nearly all the existing
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researches of in-situ char gasification were conducted for coal char but not for biomass char.
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Although there were numerous reports on the reaction kinetics of biomass
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devolatilization in the inert atmosphere, the related researches in active atmosphere were not
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only scarce, but also filled with obviously different, even contradictory conclusions. Ferreira
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et al. [22] examined the pyrolysis kinetics of sugarcane straw in different atmospheres (N2,
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N2+O2 (3%), N2+O2 (20%)) from 693 K to 993 K. The results showed that, in the atmosphere
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of N2+O2 (3%), it had the lowest activation energy (E), indicating oxidative pyrolysis as a low
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energy cost and environmentally friend process for converting biomass to the valuable 5
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products. However, Chandrasekaran et al. [23] took an opposite conclusion by pyrolyzing
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switchgrass pellet in different atmospheres. The value of E in the oxidative atmosphere (556
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kJ/mol) was much higher than that in the inert atmosphere (314 kJ/mol). A similar result was
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also obtained by Singh et al. [24]. However, an unexpected conclusion from Bach et al. [25]
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demonstrated that, compared to the inert atmosphere, the oxidative atmosphere (CO2,
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CO2+H2O, CO2+H2O+O2) did not have a noticeable influence on the reaction kinetics from
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473 K to 573 K. Perhaps, these differences were mostly related to the adopted experimental
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approach, heating rate, temperature range, pyrolysis apparatus, reaction atmosphere,
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mathematical analysis method, as well as the feedstock. So, the confusing results and even
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contradictory conclusions not only indicate the research value of devolatilization behavior and
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kinetics in different atmospheres, but also demonstrate the research necessity in the char
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gasification and its corresponding devolatilization/pyrolysis together instead of separately
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[26]. Moreover, to obtain a clear and deep understanding in biomass devolatilization and char
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gasification, a reasonable comparison should be conducted under the same experimental
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method, including biomass sample, reaction condition, data analysis approach, and so on [27].
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Isothermal and non-isothermal methods are conventionally used in the analysis of
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reaction behavior and kinetics. Generally, the isothermal method is performed at a fixed
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reaction temperature, indicating the overall reaction characteristics. While the non-isothermal
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method is conducted by loading sample at room temperature and then heating the sample
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according to a given temperature-programmed procedure. Compared to the isothermal method,
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the non-isothermal method owns many advantages, such as less experiment work, shorter
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operating period, and more information about reaction behavior [28, 29]. 6
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In this research, the experiments of biomass devolatilization and the following char
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gasification in different atmospheres were conducted on a thermogravimetric analyzer (TGA)
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according to the non-isothermal approach. The Coats and Redfern method will be adopted for
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the kinetic estimation. The objectives of this study were threefold. Firstly, the effect of inert,
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CO2-containing, and steam-containing atmospheres on the devolatilization behavior and
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reaction kinetics was examined, including TG/DTG curves, conversion degree, reaction rate,
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char structure, and kinetics of volatiles release. Secondly, the gasification characteristics and
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kinetics of the in-situ chars from the different devolatilization atmospheres were tested and
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compared. Thirdly, the difference between in-situ char and ex-situ char, not only in char
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structure and morphology, but also in gasification characteristics and kinetics, were analyzed
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systematically. By this study, it will provide an approach to test the gasification behavior of
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in-situ char, offset the lack of reaction kinetics not only in in-situ char gasification, but also in
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the corresponding biomass devolatilization, and thus deepen the understanding in the whole
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biomass gasification process.
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2. EXPERIMENTAL
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2.1 Material
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In this study, a kind of Japanese black pine was adopted as the experimental feedstock.
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According to the proximate (air dry basis) and ultimate analysis (dry and ash-free basis), the
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mass contents of moisture, ash, volatile matter, and fixed carbon were 6.96 %, 1.84 %, 79.16
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%, and 12.04 %, respectively, and the contents of C, H, S, O, and N were 50.42 %, 6.77%,
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0.00 %, 42.62 % (by difference), and 0.19 %, respectively. The higher heating value of the
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black pine was about 17.81 MJ/kg. These analyses showed that the experimental sample was 7
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rich in volatile matter, C, and O. Prior to experiment, the black pine pellets were ground,
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sieved, and then dried in an air oven at 380 K for 12 h to obtain the experimental samples
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with a particle size in the range of 0.55 mm-0.83 mm.
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2.2 Apparatus and procedure
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As shown in Fig. 1(a), a thermogravimetric analyzer (NETZSCH, TG-DTA
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2000SE/H/VAP) with the sensitivity of sample mass of 0.001 mg was adopted, consisting of
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an electric heating furnace, a mass measuring unit, a set of gas supplying system, a steam
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generator, a temperature controlling and data logging system. Two streams of carrier gas (N2)
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were used in this apparatus, one as the sweeping gas to restrain the secondary reaction of
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volatile matter and the interaction between the released volatile matter and char, the other as
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the carrier gas to entrain the adopted gasification agent (steam/CO2). Steam was generated in
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an electric oven operated at 473 K by vaporizing purified water via a peristaltic pump. To
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avoid the steam condensation, the temperature of the pipeline from the steam generator to the
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electric heating furnace was maintained at 423 K by a ribbon heater.
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To examine the effect of atmosphere’s kind and content on biomass devolatilization and
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the subsequent char gasification, four kinds of atmosphere were employed, including N2,
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N2+steam (10 %), N2+CO2 (10%), and N2+CO2 (50%). Prior to each experiment, about 10 mg
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biomass sample was loaded into the ceramic crucible at room temperature. Below 380 K, the
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biomass sample was heated in N2 with a heating rate of 20 K/min and residence time of 10
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min. Then, the heating rate was changed to the value of 5/10/20/30/40 K/min, and maintained
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throughout the following heating period. For the in-situ char experiment, at 473 K, the
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gasification agent (steam/CO2) was introduced into the heating furnace, and the reaction 8
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temperature rose continuously to 1273 K for biomass devolatilization and the following char
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gasification. The ending temperature of the biomass devolatilization stage and the initial
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temperature of the char gasification stage can be considered as the same value in each
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experiment. Taking the in-situ char gasification at the heating rate of 30 K/min in the
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atmosphere of N2+CO2 as an example, the critical point can be determined by the TG/DTG
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curves, as shown in Fig. 1 (b).
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Prior to the experiments of ex-situ char gasification (biomass devolatilization in N2, char
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gasification in N2+steam (10%)), the corresponding in-situ char gasification experiments
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(both biomass devolatilization and char gasification in N2+steam (10%)) at different heating
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rates were conducted in advance. According to the TG-DTG curve, the initial temperature
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(TCG-i) of in-situ char gasification can be determined. For the ex-situ char gasification with the
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same heating rate, the biomass sample was firstly devolatilized in N2, and then at the
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temperature of TCG-i, a certain flowrate of steam was introduced into the TGA to form the
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atmosphere of N2+steam (10%), and then begin the ex-situ char gasification quickly.
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Hereafter, to distinguish clearly, the gasification atmospheres of N2+steam (10%) for the
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in-situ char produced in N2+steam (10%) and for the ex-situ char produced in N2, were
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marked as N2+steam-1 and N2+steam-2, respectively. Figure 1 (c) shows the typical TG/DTG
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curves of the ex-situ char gasification at the heating rate of 30 K/min. For each condition, the
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experiment was repeated three times, and the average standard deviation of mass loss was
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below 2 %.
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2.3 Analysis and characterization
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To examine the difference in char property, four kinds of biomass char were prepared in 9
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a horizontal tubular furnace, whose operational conditions were consistent with the
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corresponding devolatilization stages with a heating rate of 10 K /min. An automatic
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volumetric sorption analyzer was used to test the pore structure and specific surface area of
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char sample by the N2 adsorption method at 77 K. Barrett-Joyner-Halenda (BJH) method and
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t-plot method were chosen to analyze the structure of meso pore and micro pore, respectively.
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A Fourier transform infrared spectroscopy (BRUKER TENSOR 27, Germany) was employed
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to analyze the distribution of functional groups on the char surface. A scanning electron
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microscopy/energy dispersive spectrometry (SEM/EDS, JSM-7001 F, X-Max 50) was
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adopted to test the surface morphology and element composition of the char samples.
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For the stages of biomass devolatilization (BD) and char gasification (CG), the realized
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conversion (XBD, XCG) and reaction rate (RBD, RCG) can be defined by the following equations
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from (1) to (4),
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X BD
m0 BD mi BD m0 BD m f BD
(1)
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X CG
m0CG mi CG m0CG m f CG
(2)
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RBD
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RCG
1 m0 BD 1 m0CG
dmi BD dX BD dt dt
(3)
dmi CG dX CG dt dt
(4)
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where m0, mi, and mf are the sample masses at the beginning, given, and final time in the stage
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of biomass devolatilization or char gasification; t is the reaction time in each stage.
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Generally, the typical differential equation of biomass devolatilization and char gasification can be expressed by the equation (5), 10
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Energy & Fuels
E dX n n RT R kf X k 1 X Ae 1 X dt
(5)
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where k is the reaction rate constant expressed by the Arrhenius equation; T, A, and E are the
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absolute reaction temperature, pre-exponential factor, and activation energy, respectively; n is
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the reaction order; R is the universal gas constant.
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For the non-isothermal gasification reaction of char, the common approaches in literature
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include the combination and single heating rate method. Compared to the former, the single
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heating rate method can estimate the reaction characteristics at a given heating rate and obtain
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the corresponding kinetic parameters. A representative single heating rate method was
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proposed by Coats and Redfern [30, 31], as followed by the equation (6) and (7),
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1 1 X 1 n 1 AR E ln 2 ln T E RT 1 n
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ln 1 X AR E ln ln 2 T E RT
229 230 231
(for n≠1)
(6)
(for n=1)
(7)
where β is the heating rate adopted in the non-isothermal experiment. To simplify, four notations, namely, Y, Z, m, and c, were employed in the equation (6) and (7), which can be given in the equations from (8) to (11).
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1 1 X 1 n 1 Y=ln 2 T 1 n
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ln 1 X Y ln T2
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m
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AR c ln E
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Finally, the equation (6) and (7) can be expressed by the following form.
and
Z
and
Z
1 T
1 T
(for n≠1)
(8)
(for n=1)
(9)
E R
(10) (11)
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Y=mZ+c
(12)
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For a given heating rate, by plotting Y versus Z, a good linear relationship will be
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displayed, and the values of E and A can be calculated by the corresponding slope (m) and
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intercept (c) of the fitting straight line, respectively.
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3. RESULTS AND DISCUSSION
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3.1 TG and DTG analysis
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Figure 2 shows the characteristics of biomass devolatilization and the subsequent
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in/ex-situ char gasification under different atmospheres and heating rates. For each
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experiment, the TG/DTG curves can be divided into the biomass drying stage below 473 K,
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the biomass devolatilization stage from 473 K to about 973 K, and the char gasification stage
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from about 973 K to 1273 K. To see more clearly, table 1 summarized the typical
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temperatures from each TG/DTG curve, including the temperatures with the maximum mass
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loss in the stages of biomass devolatilization and char gasification (TBD-max, TCG-max), and the
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initial temperature in the char gasification stage (TCG-i). Here, it is important to point out that
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the ending temperature of biomass devolatilization and the initial temperature of char
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gasification was considered as the same value for a given experiment, which was much higher
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than the TBD-max.
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For a specific reaction atmosphere adopted, with the increase of heating rate from 5
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K/min to 40 K/min, the curves of TG and TDG tended rightward shift, leading to the increase
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of typical reaction temperature. Taking the atmosphere of N2+steam (10%) as an example,
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compared to the values of TBD-max, TCG-i, and TCG-max at the heating rate of 5 K/min, the
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corresponding temperatures at the heating rate of 40 K/min increased from 624 K to 659 K, 12
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900 K to 1010 K, and 1152 K to 1263 K, respectively. Generally, this phenomenon was
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defined as the delayed effect of heating rate, which was much related to the limitations of heat
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and mass transfer between the temperatures of the heating furnace and experimental sample
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[32]. At the lower heating rate, the thermal energy can effectively transfer into the biomass
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sample instantly and heat it sufficiently. However, with the increase of heating rate, the
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heating time became shorter, leading to the inefficient heat transfer between the electrical
265
furnace and sample surface [33, 34]. Moreover, the poor property of thermal conductivity in
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biomass material also caused strong temperature gradients between char particles [35].
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For the adopted four kinds of atmosphere in the biomass devolatilization stage, namely,
268
both BD and CG in N2+steam (10 %), both BD and CG in N2+CO2 (10 %), BD in N2 and CG
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in N2+steam (10 %), and both BD and CG in N2+CO2 (50 %), by varying the heating rate
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from 5 K/min to 40 K/min, the corresponding TBD-max changed in the range of 624-659 K,
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620-654 K, 626-657 K, and 625-659 K, respectively, having the maximum increment of 35 K.
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While in the char gasification stage, the corresponding TCG-max varied in the range of
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1152-1263 K, 1141-1243 K, 1147-1251 K, and 1139-1233 K, respectively, having the
274
maximum increment of 111 K. So, compared to the biomass devolatilization stage, the
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delayed influence on char gasification stage was much more distinct. Perhaps, this was
276
closely related to the strong endothermic reaction and large energy requirement of char
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gasification [36]. The results also showed that, for the single process of biomass
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devolatilization or char gasification, the effect of reaction atmosphere on the TBD-max or TCG-max
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was relatively weak. Perhaps the limited difference can be attributed to the sample
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heterogeneity. Interestingly, for the initial temperature of char gasification (TCG-i), the impact 13
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of reaction atmosphere seemed stronger. For example, at the heating rate of 5 K/min, for the
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chars from the four kinds of atmosphere adopted, the values of TCG-i changed in the range of
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900-933 K, indicating the different char activity for the gasification reaction.
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3.2 Reaction behavior analysis
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Figure 3 illustrated the variation of conversion (X) with reaction temperature for biomass
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devolatilization and char gasification under different heating rates and reaction atmospheres.
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In each atmosphere, regardless of biomass devolatilization and char gasification, with the
288
increase of heating rate, the higher reaction temperature was required for reaching a given
289
conversion. For example, in the atmosphere of N2+CO2 (10%), for the heating rate of 5 K/min
290
and 40 K/min, as shown in Fig.3 (a-1) and (b-1), the reaction temperatures reaching the
291
conversion of 50 % were 606 K and 642 K in the biomass devolatilization, respectively; while
292
they were 1106 K and 1199 K in the char gasification, respectively. In other atmospheres, the
293
corresponding reaction temperatures can be seen in Fig. S1 from the supporting document. To
294
see more clearly, Fig.3 (a-2) and (b-2) compared the atmosphere effect on biomass
295
devolatilization and char gasification at the same heating rate of 30 K/min. For the stage of
296
biomass devolatilization, the four curves of X versus T were nearly overlapped. Perhaps the
297
little difference was much related to the sample heterogeneity and the thermos-physical
298
properties of the adopted gas components, demonstrating the weak influence of the reaction
299
atmosphere on the volatiles release during the biomass devolatilization, even for the CO2
300
content of 50 %. So, the experiments with a higher content of CO2/steam were not conducted
301
in this study. However, at the stage of char gasification, for reaching the same conversion
302
below 50 %, the required gasification temperature followed the order of N2+steam-1 < 14
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N2+CO2 (50%) < N2+steam-2 < N2+CO2 (10%). Although the in/ex-situ chars underwent
304
very similar devolatilization behavior in the release of volatiles, their gasification behaviors
305
were much different, even in the same gasification atmosphere of N2+steam (10%).
306
Taking the heating rate of 20 K/min and 40 K/min as two examples, Figure 4 further
307
compares the reaction rate in the biomass devolatilization and char gasification. For the stage
308
of biomass devolatilization, regardless of 20 K/min and 40 K/min, there was not a visible
309
difference in items of curve shape and the value of reaction rate. The maximum reaction rate
310
appeared in the conversion range of 60 % - 80 %, in which the reaction rate in the
311
atmospheres of N2 and N2+CO2 (10%) were just a little higher than that in the atmospheres of
312
N2+steam (10 %) and N2+CO2 (50%), with the similar values of 0.257 min-1, 0.258 min-1,
313
0.249 min-1, and 0.242 min-1, respectively. However, for the stage of char gasification, both of
314
the curve shape and value of reaction rate were much different. In the atmosphere of N2+CO2,
315
with the increase of CO2 content, the reaction rate had a sharp rise in the conversion range of
316
40% - 90%. Compared to the atmospheres of N2+CO2 (10%, 50%), the maximum gasification
317
rate was much higher in the steam-containing atmosphere, and the corresponding conversion
318
lay in the range of 80 % - 90 % instead of 60 % - 80 %. For the N2+steam atmosphere, the
319
in-situ char showed higher gasification rate than the ex-situ char in the range of 10 % - 80 %.
320
For example, for the heating rate of 20 K/min, the reaction rates of in/ex-suit chars at the
321
conversion of 50 % were about 0.135 min-1 and 0.125 min-1 respectively, with a ratio of 1.08;
322
while at the conversion of 90 %, they were about 0.25 min-1 and 0.22 min-1 respectively, with
323
a ratio of 1.14. For the heating rate of 40 K/min, the ratios at the conversions of 50 % and 90
324
% , were about 1.15 and 1.20, respectively. 15
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Table 2 displayed the results of in-situ and ex-situ char gasification in literature. For
326
most of the coal char adopted, one can see that the differences in the reaction rate between
327
in-situ char and ex-situ char were very distinct, displaying a ratio above 1.4. Compared to the
328
results of coal char in literature, the difference in the gasification rate of in/ex-situ chars from
329
biomass sample in this study was relatively lower, with a maximum ratio below 1.20. A
330
possible explanation was the high specific surface area of biomass char than that of coal char
331
[38]. For example, in literature [21], the total specific surface areas of in situ coal char and
332
ex-situ coal char were 40.48 m2/g and 34.63 m2/g, respectively. While in this study, both of
333
them were about 400 m2/g. The details will be discussed in the following section of 3.3.
334
3.3 Property of char from the devolatilization stage
335
Although the reaction atmosphere did not have a visible effect on the release of volatiles
336
from the devolatilization stage, perhaps it was much different in the property of the produced
337
char. Figure 5 further showed the SEM images of biomass char from the different
338
devolatilization stage. All the char samples presented the typical round tubular structure. By
339
analyzing the four kinds of char sample, one can found that the porous structure of char from
340
the atmosphere of N2+CO2 (10%) was the least developed, while that from the atmosphere of
341
N2+CO2 (50 %) and N2+steam (10%) had much border and deeper cavities, especially for the
342
atmosphere with the CO2 content of 50 %.
343
Table 3 displayed the element compositions of the corresponding char sample in figure 5
344
tested by EDS. Compared to the CO2-containing atmosphere, the char samples produced in
345
the atmosphere of N2 and N2+steam (10%) had higher content of O but lower content of C and
346
K. This indicated the promoting effect of CO2 atmosphere on the decomposition of 16
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oxygen-containing functional groups and its suppressing effect on the release of K. Moreover,
348
in the inert atmosphere of N2, the element content of Mg, Na, and Ca was higher than that in
349
the oxidative atmospheres. As we know, for char gasification reaction, the alkali metal oxides,
350
especially in K2O, always display good catalytic activity.
351
Table 4 listed the porous property of char samples from the devolatilization stages.
352
Compared to the inert atmosphere, there were different change tendency in the tested active
353
atmospheres. For example, in the atmosphere of N2 + CO2 (10%), both the specific surface
354
area of micro pore and meso pore decreased obviously. However, by increasing the CO2
355
content to 50%, one can see that the specific surface area of micro pore increased sharply,
356
while the change of meso pore was similar. In the atmosphere of N2+steam (10%), the
357
specific surface area of micro pore increased distinctly, while that of meso pore decreased.
358
For the atmospheres of N2 and N2+CO2 (50%), the char samples had the similar value of the
359
specific surface area in meso pore, while for the atmosphere of N2+CO2 (10%) and N2+steam
360
(10 %), they were also similar in meso pore. Although both CO2 (50%) and steam can
361
promote the increase of the total specific surface area, for the former, the main increase was
362
attributed to the new generation of micro pore; while for the latter, perhaps it mainly came
363
from the balance of micro pore generation and meso pore extinction due to the merging of
364
adjacent pore structure. The different pore structure in char samples will inevitably lead to the
365
difference in their gasification reactivity.
366
Figure 6 illustrates the distributions of functional group on the surface of the char
367
samples from the devolatilization stages. Generally, the main functional groups in char
368
included: (1) C-H bond in aromatics between 660 and 1011 cm-1, (2) -OH bond in-plane 17
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deformation between 1011 and 1300 cm-1, (3) -CHx bond out of aromatic plane deformation
370
between 1300 and 1465 cm-1, (4) C=C bond in aromatics between 1500 and 1600 cm-1, (5)
371
aliphatic C-H between 2850 and 2920 cm-1, (6) -OH bond of stretching vibrations between
372
3300 and 3650 cm-1, and (7) C=O bond stretching vibration between 1600 and 1700 cm-1 [39,
373
40]. Compared to the inert atmosphere (N2), the char from CO2 atmosphere had lower
374
adsorption intensity of functional group of (1), (2) and (6), while it was similar in the steam
375
atmosphere. For the functional group (7), it was only present in the char sample produced in
376
the atmosphere of N2+steam. While for the functional group (4), it had the highest intensity in
377
the char generated in N2, indicating the strong aromatic structure.
378
All the analyses mentioned above further demonstrated that although reaction
379
atmospheres had weak effect on the release behavior of volatile matter during the
380
devolatilization stage, it indeed influenced the char property. This will further affect the
381
gasification behavior of not only the in-situ char, but also the ex-situ char.
382
3.4 Reaction order and kinetics
383
According to the equation (6) and (7), for the suitable reaction order n, by plotting Y
384
versus Z, it will display a good linear relationship. By taking the heating rate of 10 K/min in
385
the N2+steam atmosphere as an example, figure 7 illustrated all the curves of Y versus Z at the
386
given reaction order for biomass devolatilization and char gasification. By linear fitting of all
387
the data obtained at the different reaction rates, the correlation coefficients (R2) of these
388
curves were calculated, as shown in Table S1 from the supporting document. It was clear that,
389
for the biomass devolatilization and char gasification, the experimental results presented a
390
good linear relationship with high R2 of 0.9948 and 0.9917 at the reaction order of 1 and 0.67, 18
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respectively. Actually, for the other heating rates and atmospheres adopted, similar results can
392
also be obtained, indicating the reliability of the reaction order for 1 and 0.67. The results also
393
verified that the volume reaction model (VRM) and shrinking core reaction model (SCRM)
394
were suitable to describe the behaviors of biomass devolatilization and char gasification,
395
respectively, as shown in the equation (13) and (14) [41],
396 397 398
dX kv 1 X dt 2 dX ks 1 X 3 dt
(13) (14)
where kv and ks are the volumetric and surface reaction rate constant.
399
Figure 8 correlates Y versus Z according to the Coats-Redfern method for biomass
400
devolatilization and char gasification. The corresponding data were displayed in Fig. 3 and
401
Fig. 4. The fitting curves for different heating rates showed good linearity, with all the
402
correlation coefficient above 0.98, further justifying the feasibility of reaction models adopted.
403
Moreover, under each experimental atmosphere, with the increase of heating rate, the curves
404
nearly paralleled with the similar slopes, not only indicating the weak influence of heating
405
rate on reaction kinetics, but also further validating the feasibility of reaction models.
406
According to the slope and intercept of the linear fitting curve in Fig.8 (a, 1-4), the
407
values of E and A for each heating rate in the stage of biomass devolatilization can be
408
calculated, as shown in Table 5. One can see that, for each experimental atmosphere and
409
heating rate, the values of E were much similar, with a fluctuation in the range of ± 4
410
kJ/mol around the average value, showing good reliability. For the same atmosphere of
411
N2+CO2 but with different CO2 content (10 %, 50 %), it found that the values of E were
412
consistent with each other. For the four kinds of atmosphere, the values of E in N2 and 19
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413
N2+steam atmosphere were a little higher than those in N2+CO2 (10 %, 50%), but were not
414
very obvious, just having a variation from 82.3 kJ/mol to 85.6 kJ/mol. This phenomenon was
415
agreed with the results in the literature [42, 43]. So, it was reasonable to consider that the
416
adopted inert and reactive atmosphere did not have an influence on the reaction kinetics of
417
volatile matter release during the biomass devolatilization, which was just a thermal-driving
418
process. Although the existing researches have demonstrated that atmosphere can influence
419
the pyrolysis behavior, product distribution, and gas components in a bench reactor, such as,
420
fluidized bed, fixed bed, and rotary kiln, from the viewpoint of reaction kinetics, this
421
influence was very weak because of short residence time in TGA and the inhibition of
422
interaction among pyrolytic products.
423
According to the approach as mentioned above, the gasification kinetics of in/ex-situ
424
char in different atmospheres and heating rates can be obtained, as shown in Table 6. At a
425
given atmosphere, the values of E for char gasification had a much more significant
426
fluctuation than that in biomass devolatilization, especially for the N2+steam-1, varying from
427
121.8 kJ/mol to 157.7 kJ/mol. Compared to the ex-situ char produced in N2 atmosphere,
428
in-situ char had a much smaller average value of E and higher average value of A. Meanwhile,
429
for the four kinds of reaction atmosphere adopted, the average values of E for the char
430
gasification were ranked as N2+CO2 (50 %) > N2+CO2 (10 %) > N2+steam-2 (10 %) >
431
N2+steam-1 (10 %). Generally, activation energy is defined as the minimum energy barrier to
432
overcome for the initiation of a chemical reaction. A smaller value of E always means higher
433
reactivity of char, lower gasification temperature, and shorter reaction time. Furtherly,
434
compared to N2+steam-2 (10%), the better gasification behavior of in-situ char from 20
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N2+steam-1 (10%) was much related to the more developed micro structure, higher content of
436
K, more abundant oxygen-containing group, and poorer aromatic structure.
437
Table 7 further summarized the experimental condition and reaction kinetics in the
438
literature on biomass devolatilization and char gasification adopting a similar feedstock.
439
From these results, one can see that the values of E for biomass devolatilization, char
440
gasification with CO2 and steam were in the ranges of 69.0 kJ/mol-94.0 kJ/mol, 151.0 kJ/mol
441
-199.0 kJ/mol, and 136.0 kJ/mol-139.0 kJ/mol, respectively. In this study, the corresponding
442
experimental results showed good comparability with those in literature, validating the
443
reliability of the experimental method and results.
444
4. CONCLUSIONS
445
The non-isothermal reaction characteristics and kinetics of biomass devolatilization and
446
in-situ char gasification were investigated by TGA under different atmospheres and heating
447
rates. The volume reaction model and shrinking core reaction model were used to describe the
448
reaction behavior of biomass devolatilization and char gasification, respectively, and the
449
approach of Coats and Redfern was adopted to calculate the reaction kinetics. For biomass
450
devolatilization, although the adopted atmospheres, regardless of inert (N2) and reactive gas
451
(N2+CO2 (10%), N2+CO2 (50%) and N2+steam (10%)), did not have obvious influence on
452
TG-DTG curve, reaction rate versus conversion, and the activation energy of volatiles release,
453
even at the CO2 content of 50 %, it had obvious effect on the produced char porous structure,
454
distribution of functional group, and content of alkali metal and alkaline earth metal. The
455
values of E for volatiles release were in the range of 82.3 kJ/mol - 85.6 kJ/mol. Compared to
456
the biomass devolatilization, the delayed effect of the heating rate in char gasification was 21
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457
much more obvious, and the reaction atmospheres also displayed a stronger effect on the
458
gasification behavior and kinetic parameters. The corresponding maximum reaction rate in the
459
steam-containing atmosphere lay in the conversion range of 80 % - 90 % instead of 60 % - 80
460
% like in the CO2-containing atmosphere. The average values of E in N2+CO2 (50 %),
461
N2+CO2 (10 %), N2+steam-1 (10 %) and N2+steam-2 (10 %) were about 182.7 kJ/mol, 177.2
462
kJ/mol, 144.9 kJ/mol, and 157.5 kJ/mol, respectively. The value of in-situ char gasification in
463
steam was much lower than that in the CO2 atmosphere. Compared to the ex-situ char
464
gasification, the in-situ char gasification in the N2+steam (10%) had higher reaction rate and
465
the lower average value of E. Moreover, it also finds that these differences between in/ex-situ
466
biomass chars were much smaller than that from coal char in literature.
467
ACKNOWLEDGEMENT
468
The authors gratefully acknowledge the financial support provided by the JSPS (Japan
469
Society for the Promotion of Science) International Fellowships for Research in Japan.
470
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of macroalgae Cladophora glomerata. Bioresour. Technol. 2017, 243, 212-217.
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(34) Damartzis, T.; Vamvuka, D.; Sfakiotakis, S.; Zabaniotou, A. Thermal degradation
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studies and kinetic modeling of cardoon (Cynara cardunculus) pyrolysis using
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thermogravimetric analysis (TGA). Bioresour. Technol. 2011, 102, 6230-6238.
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(35) Ma, Z. Q.; Chen, D. Y.; Gu, J.; Bao, B. F.; Zhang, Q. S. Determination of pyrolysis
565
characteristics and kinetics of palm kernel shell using TGA-FTIR and model-free integral 26
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methods. Energ. Convers. Manage. 2015, 89, 251-259.
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(36) Wang, F.; Zeng, X.; Wang, Y. G.; Su, H.; Yu, J.; Xu, G. W. Non-isothermal coal char
568
gasification with CO2 in a micro fluidized bed reaction analyzer and a thermogravimetric
569
analyzer. Fuel 2016, 164, 403-409.
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(37) Guo, Y. Z.; Zhao, Y. J.; Gao, D. Y.; Liu, P.; Meng, S.; Sun, S. Z. Kinetics of steam
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gasification of in-situ chars in a micro fluidized bed. Int. J. Hydrogen Energy 2016, 41,
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15187-15198.
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(38) Zhou, Q. Q.; Zarei A.; Girolamo, A. D.; Yan, Y. X.; Zhang, L.A. Catalytic performance
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of scrap tyre char for the upgrading of eucalyptus pyrolysis derived bio-oil via cracking and
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deoxygenation. J. Anal. Appl. Pyrol. 2019, 139, 167-176.
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(39) Jian, J.; Lu, Z. M.; Yao, S. C.; Li, Y. Q.; Liu, Z. F.; Lang, B.; Chen, Z. B. Effects of
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thermal conditions on char yield and char reactivity of woody biomass in stepwise pyrolysis.
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(40) Xu, K.; Hu, S.; Su, S.; Xu, C. F.; Sun, L. S.; Shuai, C.; Jiang, L.; Xiang, J. Study on char
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surface active sites and their relationship to gasification reactivity. Energy Fuels 2013, 27,
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(41) White, J. E.; Catallo, W. J.; Legendre, B. L. M. Biomass pyrolysis kinetics: A
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comparative critical review with relevant agricultural residue case studies. J. Anal. Appl.
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Pyrol. 2011, 91, 1-33.
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(42) Wang, Z. H.; Ma, X. Q.; Yao, Z. L.; Yu, Q. S.; Wang, Z.; Lin, Y. S. Study of the
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pyrolysis of municipal sludge in N2/CO2 atmosphere. Appl. Therm. Eng. 2018, 128, 662-671.
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(43) Senneca, O.; Cerciello, F.; Heuer, S.; Ammendola, P. Slow pyrolysis of walnut shells in 27
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nitrogen and carbon dioxide. Fuel 2018, 225, 419-425.
589
(44) Aqsha, A.; Mahinpey, N.; Mani, T.; Salak, F.; Murugan, P. Study of sawdust pyrolysis
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and its devolatilisation kinetics. Can. J. Chem. Eng. 2011, 89, 1141-1147.
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(45) Babu, B. V. Biomass pyrolysis: a state-of the-art review. Biofuel Bioprod. Bior. 2008, 2,
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fluidized bed reactor. Fuel 1991, 70, 883-887.
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kinetics in the rapid pyrolysis of sweet gum hardwood. Ind. Eng. Chem. Process Des. Dev.
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600
(49) Fermoso, J.; Stevanov, C.; Moghtaderi, B.; Arias, B.; Pevida, C.; Plaza, M. G.; Rubiera,
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temperatures. J. Anal. Appl. Pyrol. 2009, 85, 287-293.
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(50) Sircar, I.; Sane, A.; Wang, W. C.; Gore, J. P. Experimental and modeling study of
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pinewood char gasification with CO2. Fuel 2014, 119, 38-46.
605
(51) Matsumoto, K.; Takeno, K.; Ichinose, T.; Ogi, T.; Akanishi, M. Gasification reaction
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kinetics on biomass char obtained as a by-product of gasification in an entrained-flow gasifier
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with steam and oxygen at 900-1000 °C. Fuel 2009, 88, 519-527.
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reconcile with gasification reactivity profiles of biomass chars. Fuel 2008, 87, 475-481. 28
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Page 29 of 43 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 58 59 60
Energy & Fuels
610
Table 1 Typical temperatures in BD and CG at different atmospheres and heating rates Heating rate (K/min) Temperature [K] 5
10
20
30
40
case 1
624
634
649
654
659
case 2
620
635
646
651
654
case 3
626
634
647
652
657
case 4
625
636
649
649
659
case 1
900
937
966
973
1010
case 2
931
961
982
997
1017
case 3
918
943
971
984
1015
case 4
933
966
987
1001
1019
case 1
1152
1182
1215
1225
1263
case 2
1141
1167
1202
1220
1243
case 3
1147
1178
1210
1227
1251
case 4
1139
1162
1192
1210
1233
TBD-max
TCG-i
TCG-max
611 612
※
case 1: both BD and CG in N2+steam (10 %); case 2: both BD and CG in N2+CO2 (10 %); case 3: BD in N2, CG in N2+steam (10 %); case 4: both BD and CG in N2+CO2 (50 %);
613 614 615 616 617 618 619 620 29
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621
Page 30 of 43
Table 2 Comparison of gasification reaction rate between in/ex-situ chars in literature Number
Feedstock
Analyzer
Atmosphere
Temperature
Bituminous coal
Rin/ex situ
Reference
3.44a
Subbituminous 1
TGA
Steam
1273 K
3.85a
[19]
coal Lignite
5.78 a
Bituminous
Down
coal
furnace
firing
2
CO2
1627 K
Yima Bituminous coal
4.54a
[20]
1.4b or 2.7 a
Fluidized bed
3
CO2
1073 K
reactor
[21] 2.00b or
Xilinhaote lignite 3.0 a Shenhua 2.0 b bituminous coal
Fluidized bed
Zhundong
reactor
4
Steam
1073 K
[37] 1.8 b
bituminous coal This 5
Black pine
TGA
Steam
1250 K
1.2b study
622 623
※
a
ex-situ 1: the pre-prepared cool char was used in gasification experiment; was directly used for gasification without cooling and annealing.
624 625 626 627 628 629 30
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b
ex-situ 2: char
Page 31 of 43 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 58 59 60
Energy & Fuels
630
Table 3 EDS analysis of char sample from the different devolatilization stages Char 1
Char 2
Char 3
Char 4
C
87.06
92.39
95.23
89.97
O
8.98
2.86
2.02
8.69
Na
0.15
0.1
0
0.04
Mg
0.9
0
0
0.04
Si
0.75
0.71
0.78
0.69
S
0.88
1.74
0.53
0
K
0
1.34
1.05
0.18
Ca
1.28
0.86
0.39
0.39
631 632 633 634 635 636 637 638 639 640 641 642 643 644 31
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645
Page 32 of 43
Table 4 Pore property of char samples from the different devolatilization stage Specific surface area
Pore volume Da*
Char
Atotal
Amicro
Ameso
Vtotal
Vmicro
Vmeso
[m2/s]
[m2/s]
[m2/s]
[mL/g]
[mL/g]
[mL/g]
Char 1
402.4
319.3
83.1
0.29
0.16
0.13
3.824
Char 2
346.2
286.7
59.5
0.25
0.14
0.11
3.828
Char 3
500.0
414.6
85.4
0.33
0.19
0.14
3.822
Char 4
420.8
357.8
63.0
0.27
0.16
0.11
3.821
[nm]
646
Da*: average pore diameter;
647 648 649 650 651 652 653 654 655 656 657 658 659 32
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Energy & Fuels
660
Table 5 Kinetics of biomass devolatilization in different atmospheres Biomass devolatilization in different atmospheres
β
N2+steam
N2+CO2
(10%)
(10%)
N2
N2+CO2 (50 %)
[K/min] E
A
E
A
E
A
E
A
[kJ/mol]
[1/s]
[kJ/mol]
[1/s]
[kJ/mol]
[1/s]
[kJ/mol]
[1/s]
5
82.4
7.4E+7
83.8
9.8E+7
87.1
2.1E+8
86.0
1.5E+8
10
85.6
2.1E+8
84.7
1.8E+8
85.8
2.2E+8
79.2
5.0E+7
20
86.2
3.2E+8
81.8
1.8E+8
85.3
2.8E+8
84.7
2.3E+8
30
83.5
2.5E+8
80.6
1.3E+8
84.5
2.9E+8
79.2
9.3E+7
40
85.2
4.0E+8
81.4
1.8E+8
85.1
3.8E+8
82.6
2.2E+8
84.6
2.5E+8
82.5
1.5E+8
85.6
2.8E+8
82.3
1.5E+8
Averag e 661 662 663 664 665 666 667 668 669 670 671 672 33
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Page 34 of 43
673 674
Table 6 Kinetics of char gasification in different atmospheres Char gasification in different atmospheres
β
N2+steam-1
N2+CO2
N2+steam-2
N2+CO2
(10%)
(10%)
(10%)
(50 %)
[K/min] E
A
E
A
E
A
E
A
[kJ/mol]
[1/s]
[kJ/mol]
[1/s]
[kJ/mol]
[1/s]
[kJ/mol]
[1/s]
5
152.8
8.0E+8
177.8
8.5E+8
159.6
7.3 +E7
171.3
1.1E+8
10
153.9
2.0E+9
184.0
2.0E+9
156.7
3.4 E+7
178.4
1.2E+8
20
157.7
6.8E+8
173.6
6.8E+8
155.3
5.9 E+7
183.6
2.4E+8
30
138.5
8.9E+8
174.5
8.9E+8
161.3
2.2 E+8
195.2
3.4E+9
40
121.8
1.1E+9
176.1
1.7E+9
154.8
1.2 E+8
185.2
2.3E+9
Average
144.9
1.1E+9
177.2
1.2E+9
157.5
7.7 E+7
182.7
1.2E+9
675 676 677 678 679 680 681 682 683 684 685 34
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Energy & Fuels
686 687
Table 7 Kinetics of biomass devolatilization and char gasification in literature
Item
Feedstock
Analyzer
Sawdust
TGA
Pine
TGA
BD
CG
T
E
A
[K]
[kJ/mol]
[1/s]
473-673
79.5
1.1E +8
[44]
798-1133
83.0
7.0E+4
[45]
Gas
Reference
N2 Fire wood
Fluid bed
673-773
94.0
1.9E+4
[46]
Hardwood
Screen heater
600-1400
69.0
4.5E+4
[47]
Spruce/ pine char
Fluidized 1073-1123
151.0
7.0E+3
[48]
(80%/20%)
bed
Slash pine char
TGA
1273-1673
170.5-198.5
8.8E+7
[49]
Pinewood char
Fixed bed
1000-1170
173.0-199.0
CO2
(1.6-12.1) [50] E+3
CG
Spruce/ pine char
Fluidized
(80%/20%)
bed
Japanese
cedar
Drop
char
furnace
Beech char
TGA
tube
H2O
1073 -1123
138.0
3.7E+3
[48]
1173-1473
136.0
9.9E+4
[51]
1073-1223
139.0
2.6E+4
[52]
688 689 690 691 692 693 694 35
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(a)
695
696
697 698
Fig. 1 Schematic of the adopted TG analyzer and typical experiment for biomass devolatilization and
699
in/ex-situ char gasification
700 701 702 703 36
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Energy & Fuels
704
705 706
Fig. 2 TG/DTG curves of biomass devolatilization and in/ex-situ char gasification in different
707
atmospheres and heating rates
708 709 710 711 712 713 714 37
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715
716 717
Fig. 3 Relationship of X-T for BD and CG in different atmospheres and heating rates
718 719 720 721 722 723 724 725 726 727 38
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Energy & Fuels
728
729 730
Fig. 4 Relationship of R-X for BD and CG in different atmospheres and heating rates
731 732 733 734 735 736 737 738 739 740 39
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Page 40 of 43
741 742
(a)
(b)
(c)
(d)
743 744 745
Fig. 5 SEM photograph of biomass char prepared in different devolatilization stages
746
(a) Char 1 produced in N2 with the final temperature of 937 K and heating rate of 10K/min; (b) Char 2
747
produced in N2+CO2 (10%) with the final temperature of 961 K and heating rate of 10 K/min; (c) Char
748
3 produced in N2+CO2 (50%) with the final temperature of 943 K and heating rate of 10 K/min; (d)
749
Char 4 produced in N2+steam (10%) with the final temperature of 966 K and heating rate of 10 K/min;
750 751 752 753 754 755 40
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756 757
Fig.6 FTIR analysis of char sample from the devolatilization stages
758 759 760 761 762 763 764 765 766 767 768 769 770 41
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771
772 773
Fig. 7 Curves of Y versus Z at different values of n for BD and CG
774 775 776 777 778 779 780 781 782 783 784 42
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785
786
787
788 789
Fig. 8 Correlation of Y versus Z for BD and CG under different atmospheres and heating rates
790 791 792 43
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