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Transformation of nitrogen and evolution of Ncontaining species during algae pyrolysis Wei Chen, Haiping Yang, Yingquan Chen, Mingwei Xia, Xu Chen, and Hanping Chen Environ. Sci. Technol., Just Accepted Manuscript • Publication Date (Web): 10 May 2017 Downloaded from http://pubs.acs.org on May 10, 2017
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Environmental Science & Technology
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[Title Page]
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Transformation of nitrogen and evolution of N-containing species during algae
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pyrolysis
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Wei Chen, Haiping Yang*, Yingquan Chen*, Mingwei Xia, Xu Chen, Hanping
7
Chen
8 9
State Key Laboratory of Coal Combustion, School of Power and Energy
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Engineering, Huazhong University of Science and Technology, 430074 Wuhan,
11
China
12 13
E-mail:
[email protected],
[email protected],
14
[email protected],
[email protected],
[email protected],
15
[email protected].
16 17
Correspondence information: Haiping Yang,
[email protected]; Yingquan
18
Chen,
[email protected]; 1037 Luoyu Road, 430074 Wuhan, P. R.
19
China; Tel: +086+027-87542417-8109; fax: +086+027-87545526.
1
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Transformation of nitrogen and evolution of N-containing species during algae
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pyrolysis
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Wei Chen, Haiping Yang*, Yingquan Chen*, Mingwei Xia, Xu Chen, Hanping Chen
23
State Key Laboratory of Coal Combustion, School of Energy and Power Engineering,
24
Huazhong University of Science and Technology, 430074 Wuhan, China
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Abstract
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Transformation and evolution mechanisms of nitrogen during algae pyrolysis were
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investigated in depth with exploration of N-containing products under variant
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temperature. Results indicated nitrogen in algae is mainly in the form of protein-N
29
(~90%) with some inorganic-N. At 400~600°C, protein-N in algae cracked firstly with
30
algae pyrolysis and formed pyridinic-N, pyrrolic-N and quaternary-N in char. The
31
content of protein-N decreased significantly, while that of pyrrolic-N and quaternary-N
32
increased gradually with temperature increasing. Pyridinic-N and pyrrolic-N formation
33
was due to deamination or dehydrogenation of amino acids; subsequently, some
34
pyridinic-N converted to quaternary-N. Increasing temperature decreased amides
35
content greatly while increased that of nitriles and N-heterocyclic compounds
36
(pyridines, pyrroles, and indoles) in bio-oil. Amides were formed through NH3 reacting
37
with fatty acids, that underwent dehydration to form nitriles. Besides, NH3 and HCN
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yields increased gradually. NH3 resulted from ammonia-N, labile amino acids and
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amides decomposition, while HCN came from nitrile decomposition. At 700~800°C, 2
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evolution trend of N-containing products was similar with that at 400~600°C. While N-
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heterocyclic compounds in bio-oil mainly came from pyrifinic-N, pyrrolic-N and
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quaternary-N decomposition. Moreover, cracking of pyridinic-N and pyrrolic-N
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produced HCN and NH3. A mechanism of nitrogen transformation during algae
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pyrolysis is proposed based on amino acids decomposition.
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Key words: Algae; Pyrolysis; Nitrogen transformation; Amino acids; N-containing
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species
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Introduction
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Global interest in renewable and alternative energy resources has greatly increased
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in recent years, due to serious environment problems, fossil fuel depletion, and concerns
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about energy security.1, 2 Among potential renewable energy sources, algae is extremely
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promising because of fast growth rates, high potential biofuel yield, high CO2 use
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capability, and the possibility of cultivation on waste water to remove N, P and heavy
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metals.3, 4 Algae pyrolysis is attracting increasing concern,5-8 as the higher mass yield
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(up to 80 wt.%) of liquid fuel and the more energy (up to 70%) in liquid products.9, 10
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However, different from agricultural straw and woody wastes, algae shows higher
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nitrogen content, which can be as high as 10 wt.%, far more than the content in coal,
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sewage sludge and terrestrial biomass.7,
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emission and transformation might be one main concern for algae pyrolysis, as it might
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be converted to various N-containing compounds, such as NH3, HCN, the NOx
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precursors, which may lead to potential nitrogen-related pollution (such as severe
11-13
Hence, the issue related to nitrogen
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photochemical smog, ozone depletion, acid rains and greenhouse effect).7,
14-20
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Furthermore, nitrogen content of pyrolytic oil can reach 12 wt.%, subsequent utilization
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of which would also lead to the secondary pollution.7 However, the N-containing
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compounds in bio-oil, such as pyrrole, pyridine, and indole, can be used to synthesize
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pharmaceuticals, perfumes and other chemicals.14, 15 N-containing char can be used in
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catalysis, pollutants adsorption and electrode materials.21-23 Thus, understanding
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nitrogen transformation is critical for the utilization of algae pyrolysis. However,
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limited information is available on the nitrogen fate during algae pyrolysis.
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Nitrogen conversion during coal pyrolysis has been investigated widely over the
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past decades.24-28 Kelemen et al.28 pointed out that N-containing species in coal would
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convert to pyridinic-N and quaternary-N in char at higher pyrolysis temperature. Tan et
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al.29, 30 reported that unstable N-containing compounds in the volatiles could generate
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HCN, while stable N-containing species in char could release NH3 during coal pyrolysis.
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However, in algae, nitrogen exists mainly as protein-N,4 whereas in coal, the dominant
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N-containing species are pyridine-N, pyrrole-N and quaternary-N.27, 31 It suggested that
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there might be different conversion processes of nitrogen for algae. Given the
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dominance of protein-N, the N-containing species in pyrolysis products should come
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from amino acids decomposition. Although Gallois et al.32 investigated the pyrolysis
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mechanism of 20 amino acids, and Choi et al.33 found that pyrolysis of amino acid
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monomer could generate lots of N-heterocyclic compounds in bio-oil. However,
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nitrogen evolution in algae is greatly different from amino acid monomer. As Chen et
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al.11 pointed out that lignin could promote nitrogen transformation into gas during co4
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pyrolysis of lignin with amino acid, while cellulose promoted nitrogen conversion into
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bio-oil. Furthermore, Ren et al.13, 34 found that hemicellulose inhibited NH3 formation
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during co-pyrolysis of hemicellulose with amino acid. These studies suggested that
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biomass components had great effect on nitrogen conversion during pyrolysis. However,
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different from lignocellulosic biomass, lipids (consist of triglycerides), carbohydrates
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(consist of alginic acid, mannitol, laminarin, and fucoidan), and proteins (consist of
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amino acids) are the main components of algae, and different pyrolysis behavior of
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these components should be showed.3, 35-38 Thus, lipids and carbohydrates in algae
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could also exert important effect on the formation of N-containing species. However,
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no related information on the formation and evolution of N-containing species could be
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obtained during algae pyrolysis, despite such information being crucial for
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understanding nitrogen decomposition mechanism in algae. Besides, nitrogen sources
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in algae must be elucidated to determine nitrogen reaction pathways. Thus, a better
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understanding of amino acids compositions and structures in algae samples is needed
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to clarify mechanism of nitrogen evolution.
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In this study, nitrogen distribution and transformation mechanisms during algae
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pyrolysis were explored with Spirulina platensis (SP, with higher proteins),
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Nannochloropsis sp. (NS, rich in lipids), and Enteromorpha prolifera (EP, enriched with
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carbohydrates) as typical algae. The possible pathways of nitrogen transformation was
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explored based on the distribution and evolution of pyrolysis products of algae at
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variant temperature. It is significant for the understanding of nitrogen evolution during
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algae pyrolysis and for the controlling nitrogen emission during algae utilization. 5
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Experimental section
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Fast pyrolysis experiment
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Nannochloropsis sp. (NS) was purchased from Yantai Hairong Biology
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Technology Co., Ltd, while Spirulina platensis (SP) and Enteromorpha prolifera (EP)
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were provided by China Agricultural University. The algae were dried at 105°C for 24
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h, then crushed and sieved (600°C).
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Associated content
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Supporting information
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Raw algal characteristics, N-containing species evolution in bio-oil and char from
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NS and EP, and releasing properties of NH3 and HCN (Tables S1-S4 and Figures S120
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S5).
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Author information
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Corresponding Author
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*Phone: +086-027-87542417-8109; email:
[email protected].
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*Phone: +086-027-87542417-8109; email:
[email protected].
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Notes
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The authors declare no competing financial interest.
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Acknowledgements
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The authors wish to express their great appreciation of the financial support from
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the National Nature Science Foundation of China (51406061 and 51622604), the
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National Basic Research Program of China (973 Program: 2013CB228102), the Special
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Fund for Agro-scientific Research in the Public Interest (201303095), the Fundamental
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Research Funds for the Central Universities, the technical support from Analytical and
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Testing
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(http://atc.hust.edu.cn).
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Figure captions
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Abstract Graphic.
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Figure 1. Schematic diagram of algal pyrolysis system for investigating nitrogen
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transformation.
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Figure 2. The nitrogen distribution of algae pyrolysis products.
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Figure 3. Figure 3 N1s spectra of SP pyrolysis chars at different temperature (a)-(e)
571
and relative content of XPS N 1s peaks of three algae (f)-(h).
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Figure 4. The releasing properties of NH3 and HCN from SP pyrolysis (a and b), and
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yields of NH3-N and HCN-N from algae pyrolysis (c).
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Figure 5. Mechanisms of nitrogen transformation and possible reaction pathways
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during algae pyrolysis.
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Amides
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3 NH
Quaternary-N
Nitriles
Indoles
Algae
Char
Inorganic-N Protein-N (amino acids)
Pyrrolic-N
Pyridinic-N HCN
Pyridines
Pyrroles
NH 3 577 578 Abstract Graphic. 579 580
30
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Gas
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Mass flow controller
Quartz basket
Ar
Gas bag
Valve Quartz reactor &
7 0
Ice-water mixture
NaOH H2SO4
ĉ
Temperature controller Electric furnace
PC
Mass spectrometry Air Ċ Color changing silica gel
Ice-water mixture or liquid nitrogen 581 582
Figure 1 Schematic diagram of algal pyrolysis system for investigating nitrogen
583
transformation.
584
31
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Nbio-oil
N yields (wt.%)
60 50 40 30 20 10
400
585
Nchar
Ngas
0 500
600
700
800
Temperature (°C)
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Figure 2. The nitrogen distribution of algae pyrolysis products (Ngas = 100wt.% - Nchar
587
–Nbio-oil). ■: SP; ●: NS; ▲: EP.
588
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a
400°C
b
Protein-N Pyridinic-N
Pyrrolic-N Quaternary-N
404
500°C
Intensity (a.u.)
Intensity (a.u.)
Protein-N
402
400
Pyrrolic-N Quaternary-N
398
404
Binding Energy (eV)
589
c
Quaternary-N
402
400
e
800°C
404
396
Protein-N Pyridinic-N
402
400
Binding Energy (eV)
398
f 90 Relative content (%)
Intensity (a.u.)
Quaternary-N
398
Quaternary-N
398
Protein-N Pyridinic-N
Pyrrolic-N
400
Pyrrolic-N
Binding Energy (eV)
590
402
Binding Energy (eV)
700°C
Intensity (a.u.)
Intensity (a.u.)
Pyrrolic-N
404
d
Pyridinic-N
Protein-N
600°C
Pyridinic-N
SP
50 40 30 20 10
404
402
400
0
398
NS
40 30 20 10 0
400
500
600
Temperature (°C)
700
h 80 Relative content (%)
Relative content (%)
g 90
592
20
Binding Energy (eV)
591
800
EP
40 30 20 10
20
400
500
600
Temperature (°C)
700
800
0
20
400
500
600
Temperature (°C)
700
800
593
Figure 3 N1s spectra of SP pyrolysis chars at different temperature (a)-(e) and relative
594
content of XPS N 1s peaks of three algae (f)-(h). ■: protein-N; ●: pyridinic-N; ▲:
595
pyrrolic-N; ▼: quaternary-N. 33
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NH3
Ion current (A) 0
b
400°C 500°C 600°C 700°C 800°C
500
1000
1500
Time (s)
596
0
c 25
1000
Time (s)
1500
SP NS EP
15
20 15
10
10
5
5
400
500
600
700
Temperature (°C)
HCN-N yield (wt.%)
NH3-N yield (wt.%)
597
500
25
20
0
400°C 500°C 600°C 700°C 800°C
HCN
Ion current (A)
a
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0
800
598
Figure 4. The releasing properties of NH3 and HCN from SP pyrolysis (a and b), and
599
yields of NH3-N and HCN-N from algae pyrolysis (c).
600
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Environmental Science & Technology
HCN
NH3/NO Inorganic-N (1)(2) + (NH4 , NO3 /NO2 ) (3)
Lysine
Glutamic acid
Aspartic acid
(11)
Pyridinic-N (5)(10)
(12)
Pyrrolic-N
(9)
Quaternary-N
(7)
Arginine
(8)
Proline Phenylalanine
Decomposing
(15) (16)
Tyrosine Tryptophan Others
Cracking
(6)
Leucine Protein-N (Amino acids)
Cracking
(4)
Valine Algae (N)
(18)
HCN
NH3
Indoles Pyrroles
Pyridines
(17)
N-heterocyclic compounds NH3/NH2* Fatty acids (13)
(14) Amides Nitriles (Hexadecanamide) (Hexadecannitrile)
601 602
Figure 5. Mechanisms of nitrogen transformation and possible reaction pathways
603
during algae pyrolysis. Black: possible reaction pathways at lower temperatures; red:
604
possible reaction pathways at higher temperatures.
605 606
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607
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Table 1. N-containing compounds in bio-oil derived from SP N-containing compounds Amines and amides 2-Methoxy-p-phenylenediamine 9-Octadecenamide Hexadecanamide N-Methyldodecanamide Nitriles Butanenitrile, 3-methylIsoamyl cyanide Benzonitrile Benzonitrile, 2-methylBenzenepropanenitrile Hexadecanenitrile N-heterocyclic compounds Oxazole Pyridine Pyrrole Pyridine, 2-methyl1H-Pyrrole, 2-methyl1H-Pyrrole, 3-methylPyridine, 3,5-dimethylIndole 1H-Indole, 3-methyl1H-Indole, 2-methylPyrimido[1,2-a]azepine, 2,3,4,6,7,8,9,10-octahydro2-Ethyl-3-methoxypyrazine 6,6-Dimethyl-2-azaspiro[4.4]non-1-ene Propyloctahydroindolizin-8-yl)methanol
Relative content (area %) 400°C 500°C 600°C 700°C 15.76 14.28 12.64 4.62 1.16 1.55 1.14 13.50 12.74 11.50 4.62 1.10 7.99 8.13 9.56 7.62 1.83 2.08 1.20 1.62 1.85 2.11 1.17 1.38 1.79 1.80 5.63 5.13 4.09 1.63 7.75 10.25 11.69 16.59 1.24 2.45 3.26 1.11 2.35 1.73 4.76 4.16 4.45 5.63 1.52 2.44 3.61
800°C 0
3.70 2.27 1.43 20.09 3.91 3.81 1.67 1.06 6.29 1.57 1.77
1.29
1.75
1.32 1.96
1.24
608
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