Degradation kinetics of biochar from pyrolysis and hydrothermal carbonization in temperate soils

Background and Aims Estimates of biochar residence times in soils range over three orders of magnitude. We present the first direct comparison between the biodegradation of a char from hydrothermal carbonization (htcBC) and pyrolysis (pyrBC) with high temporal resolution. Methods Mineralization of t...

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Published inPlant and soil Vol. 372; no. 1/2; pp. 375 - 387
Main Authors Bai, Mo, Wilske, Burkhard, Buegger, Franz, Esperschütz, Jürgen, Kammann, Claudia Irene, Eckhardt, Christian, Koestler, Martin, Kraft, Philipp, Bach, Martin, Frede, Hans-Georg, Breuer, Lutz
Format Journal Article
LanguageEnglish
Published Dordrecht Springer 01.11.2013
Springer Netherlands
Springer Nature B.V
Subjects
Agricultural soils
Agronomy. Soil science and plant productions
Animal, plant and microbial ecology
Biochar
Biodegradation
Biological and medical sciences
Biomedical and Life Sciences
Carbon
Carbon dioxide
Charcoal
Ecology
Fundamental and applied biological sciences. Psychology
General agronomy. Plant production
Grassland soils
Kinetics
Life Sciences
Mineralization
Miscanthus
Organic carbon
Organic soils
Other nutrients. Amendments. Solid and liquid wastes. Sludges and slurries
Plant Physiology
Plant Sciences
Pyrolysis
Raw materials
Regular Article
Sandy loam soils
Soil biochemistry
Soil chemistry
Soil degradation
Soil microorganisms
Soil science
Soil Science & Conservation
Soil-plant relationships. Soil fertility
Soil-plant relationships. Soil fertility. Fertilization. Amendments
Soils
Temperature effects
Germany
Biodegradation
Char
HTC
Soil amendment
CO
efflux
Recalcitrant carbon
Pyrolysis
Carbon dioxide
Biochar
Temperate zone
Soil management
Carbon isotopes
Carbonization
Soils
Amendment
Stable isotopes
Kinetics
Soil plant relation
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Abstract Background and Aims Estimates of biochar residence times in soils range over three orders of magnitude. We present the first direct comparison between the biodegradation of a char from hydrothermal carbonization (htcBC) and pyrolysis (pyrBC) with high temporal resolution. Methods Mineralization of the biochars and their shared Miscanthus feedstock in three soils was determined directly by the ¹³CO₂ efflux using a novel method incorporating wavelength scanned cavity ring-down spectroscopy. Biochar half-life (t ½ ) was estimated with three empirical models. Results (1) The htcBC was readily biodegradable, whereas pyrBC was more recalcitrant. (2) Cumulative degradation of both biochars increased with soil organic carbon and nitrogen content. (3) The corrected Akaike information criterion (AIC C ) showed an overall preference for the double exponential model (DEM) reflecting a labile and a recalcitrant C-pool, over the first-order degradation model (FODM) and a logarithmic model. (4) The DEM resulted in t ½ ranging from 19.7-44.5, 0.7-2.1 and 0.8-1.3 years for pyrBC, pyrBC and feedstock, respectively. Conclusion The degradation was rather similar between feedstock and htcBC but one order of magnitude slower for pyrBC. The AIC C preferred FODM in two cases, where the DEM parameters indicated no distinction between a labile and recalcitrant carbon pool.
AbstractList Background and Aims Estimates of biochar residence times in soils range over three orders of magnitude. We present the first direct comparison between the biodegradation of a char from hydrothermal carbonization (htcBC) and pyrolysis (pyrBC) with high temporal resolution. Methods Mineralization of the biochars and their shared Miscanthus feedstock in three soils was determined directly by the 13 CO 2 efflux using a novel method incorporating wavelength scanned cavity ring-down spectroscopy. Biochar half-life (t 1/2 ) was estimated with three empirical models. Results (1) The htcBC was readily biodegradable, whereas pyrBC was more recalcitrant. (2) Cumulative degradation of both biochars increased with soil organic carbon and nitrogen content. (3) The corrected Akaike information criterion (AIC C ) showed an overall preference for the double exponential model (DEM) reflecting a labile and a recalcitrant C-pool, over the first-order degradation model (FODM) and a logarithmic model. (4) The DEM resulted in t 1/2 ranging from 19.7–44.5, 0.7–2.1 and 0.8–1.3 years for pyrBC, htcBC and feedstock, respectively. Conclusion The degradation was rather similar between feedstock and htcBC but one order of magnitude slower for pyrBC. The AIC C preferred FODM in two cases, where the DEM parameters indicated no distinction between a labile and recalcitrant carbon pool.
Background and Aims Estimates of biochar residence times in soils range over three orders of magnitude. We present the first direct comparison between the biodegradation of a char from hydrothermal carbonization (htcBC) and pyrolysis (pyrBC) with high temporal resolution. Methods Mineralization of the biochars and their shared Miscanthus feedstock in three soils was determined directly by the ¹³CO₂ efflux using a novel method incorporating wavelength scanned cavity ring-down spectroscopy. Biochar half-life (t ½ ) was estimated with three empirical models. Results (1) The htcBC was readily biodegradable, whereas pyrBC was more recalcitrant. (2) Cumulative degradation of both biochars increased with soil organic carbon and nitrogen content. (3) The corrected Akaike information criterion (AIC C ) showed an overall preference for the double exponential model (DEM) reflecting a labile and a recalcitrant C-pool, over the first-order degradation model (FODM) and a logarithmic model. (4) The DEM resulted in t ½ ranging from 19.7-44.5, 0.7-2.1 and 0.8-1.3 years for pyrBC, pyrBC and feedstock, respectively. Conclusion The degradation was rather similar between feedstock and htcBC but one order of magnitude slower for pyrBC. The AIC C preferred FODM in two cases, where the DEM parameters indicated no distinction between a labile and recalcitrant carbon pool.
Background and Aims: Estimates of biochar residence times in soils range over three orders of magnitude. We present the first direct comparison between the biodegradation of a char from hydrothermal carbonization (htcBC) and pyrolysis (pyrBC) with high temporal resolution. Methods: Mineralization of the biochars and their shared Miscanthus feedstock in three soils was determined directly by the super(13)CO sub(2) efflux using a novel method incorporating wavelength scanned cavity ring-down spectroscopy. Biochar half-life (t sub(1/2)) was estimated with three empirical models. Results: (1) The htcBC was readily biodegradable, whereas pyrBC was more recalcitrant. (2) Cumulative degradation of both biochars increased with soil organic carbon and nitrogen content. (3) The corrected Akaike information criterion (AIC sub(C)) showed an overall preference for the double exponential model (DEM) reflecting a labile and a recalcitrant C-pool, over the first-order degradation model (FODM) and a logarithmic model. (4) The DEM resulted in t sub(1/2) ranging from 19.7-44.5, 0.7-2.1 and 0.8-1.3 years for pyrBC, htcBC and feedstock, respectively. Conclusion: The degradation was rather similar between feedstock and htcBC but one order of magnitude slower for pyrBC. The AIC sub(C) preferred FODM in two cases, where the DEM parameters indicated no distinction between a labile and recalcitrant carbon pool.
Background and Aims Estimates of biochar residence times in soils range over three orders of magnitude. We present the first direct comparison between the biodegradation of a char from hydrothermal carbonization (htcBC) and pyrolysis (pyrBC) with high temporal resolution. Methods Mineralization of the biochars and their shared Miscanthus feedstock in three soils was determined directly by the [sup.13]C[O.sub.2] efflux using a novel method incorporating wavelength scanned cavity ring-down spectroscopy. Biochar half-life ([t.sub.1/2]) was estimated with three empirical models. Results (1) The htcBC was readily biodegradable, whereas pyrBC was more recalcitrant. (2) Cumulative degradation of both biochars increased with soil organic carbon and nitrogen content. (3) The corrected Akaike information criterion ([AIC.sub.C]) showed an overall preference for the double exponential model (DEM) reflecting a labile and a recalcitrant C-pool, over the first-order degradation model (FODM) and a logarithmic model. (4) The DEM resulted in [t.sub.1/2] ranging from 19.7-44.5, 0.7-2.1 and 0.8-1.3 years for pyrBC, htcBC and feedstock, respectively. Conclusion The degradation was rather similar between feedstock and htcBC but one order of magnitude slower for pyrBC. The [AIC.sub.C] preferred FODM in two cases, where the DEM parameters indicated no distinction between a labile and recalcitrant carbon pool. Keywords Char * HTC * Soil amendment * Recalcitrant carbon * Biodegradation * [sup.13]C[O.sub.2] efflux
Issue Title: In Memory of Horst Marschner Estimates of biochar residence times in soils range over three orders of magnitude. We present the first direct comparison between the biodegradation of a char from hydrothermal carbonization (htcBC) and pyrolysis (pyrBC) with high temporal resolution. Mineralization of the biochars and their shared Miscanthus feedstock in three soils was determined directly by the ^sup 13^CO2 efflux using a novel method incorporating wavelength scanned cavity ring-down spectroscopy. Biochar half-life (t^sub 1/2^) was estimated with three empirical models. (1) The htcBC was readily biodegradable, whereas pyrBC was more recalcitrant. (2) Cumulative degradation of both biochars increased with soil organic carbon and nitrogen content. (3) The corrected Akaike information criterion (AIC^sub C^) showed an overall preference for the double exponential model (DEM) reflecting a labile and a recalcitrant C-pool, over the first-order degradation model (FODM) and a logarithmic model. (4) The DEM resulted in t^sub 1/2^ ranging from 19.7-44.5, 0.7-2.1 and 0.8-1.3 years for pyrBC, htcBC and feedstock, respectively. The degradation was rather similar between feedstock and htcBC but one order of magnitude slower for pyrBC. The AIC^sub C^ preferred FODM in two cases, where the DEM parameters indicated no distinction between a labile and recalcitrant carbon pool.[PUBLICATION ABSTRACT]
Audience Academic
Author Eckhardt, Christian
Koestler, Martin
Kraft, Philipp
Frede, Hans-Georg
Wilske, Burkhard
Buegger, Franz
Esperschütz, Jürgen
Kammann, Claudia Irene
Bach, Martin
Bai, Mo
Breuer, Lutz
Author_xml – sequence: 1
  givenname: Mo
  surname: Bai
  fullname: Bai, Mo
– sequence: 2
  givenname: Burkhard
  surname: Wilske
  fullname: Wilske, Burkhard
– sequence: 3
  givenname: Franz
  surname: Buegger
  fullname: Buegger, Franz
– sequence: 4
  givenname: Jürgen
  surname: Esperschütz
  fullname: Esperschütz, Jürgen
– sequence: 5
  givenname: Claudia Irene
  surname: Kammann
  fullname: Kammann, Claudia Irene
– sequence: 6
  givenname: Christian
  surname: Eckhardt
  fullname: Eckhardt, Christian
– sequence: 7
  givenname: Martin
  surname: Koestler
  fullname: Koestler, Martin
– sequence: 8
  givenname: Philipp
  surname: Kraft
  fullname: Kraft, Philipp
– sequence: 9
  givenname: Martin
  surname: Bach
  fullname: Bach, Martin
– sequence: 10
  givenname: Hans-Georg
  surname: Frede
  fullname: Frede, Hans-Georg
– sequence: 11
  givenname: Lutz
  surname: Breuer
  fullname: Breuer, Lutz
BackLink http://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=27914993$$DView record in Pascal Francis
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ID FETCH-LOGICAL-c440t-b904473822f8a8f9267f2a328332d0d82fc7461a7ceee095ccc9afe36792c5113
IEDL.DBID AGYKE
ISSN 0032-079X
IngestDate Fri Aug 16 23:10:02 EDT 2024
Thu Oct 10 20:59:02 EDT 2024
Fri Feb 02 04:08:21 EST 2024
Thu Sep 12 16:58:18 EDT 2024
Thu Nov 24 18:35:41 EST 2022
Sat Dec 16 12:02:06 EST 2023
Sun Oct 20 12:49:48 EDT 2024
IsPeerReviewed true
IsScholarly true
Issue 1/2
Keywords Biodegradation
Char
HTC
Soil amendment
CO
efflux
Recalcitrant carbon
Pyrolysis
Carbon dioxide
Biochar
Temperate zone
Soil management
Carbon isotopes
Carbonization
Soils
Amendment
Stable isotopes
Kinetics
Soil plant relation
Language English
License CC BY 4.0
LinkModel DirectLink
MergedId FETCHMERGED-LOGICAL-c440t-b904473822f8a8f9267f2a328332d0d82fc7461a7ceee095ccc9afe36792c5113
Notes ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
PQID 1443983350
PQPubID 54098
PageCount 13
ParticipantIDs proquest_miscellaneous_1458545707
proquest_journals_1443983350
gale_infotracacademiconefile_A354199846
crossref_primary_10_1007_s11104_013_1745_6
pascalfrancis_primary_27914993
springer_journals_10_1007_s11104_013_1745_6
jstor_primary_42953070
PublicationCentury 2000
PublicationDate 2013-11-01
PublicationDateYYYYMMDD 2013-11-01
PublicationDate_xml – month: 11
  year: 2013
  text: 2013-11-01
  day: 01
PublicationDecade 2010
PublicationPlace Dordrecht
PublicationPlace_xml – name: Dordrecht
PublicationSubtitle An International Journal on Plant-Soil Relationships
PublicationTitle Plant and soil
PublicationTitleAbbrev Plant Soil
PublicationYear 2013
Publisher Springer
Springer Netherlands
Springer Nature B.V
Publisher_xml – name: Springer
– name: Springer Netherlands
– name: Springer Nature B.V
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Snippet Background and Aims Estimates of biochar residence times in soils range over three orders of magnitude. We present the first direct comparison between the...
Background and Aims Estimates of biochar residence times in soils range over three orders of magnitude. We present the first direct comparison between the...
Issue Title: In Memory of Horst Marschner Estimates of biochar residence times in soils range over three orders of magnitude. We present the first direct...
Background and Aims: Estimates of biochar residence times in soils range over three orders of magnitude. We present the first direct comparison between the...
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SubjectTerms Agricultural soils
Agronomy. Soil science and plant productions
Animal, plant and microbial ecology
Biochar
Biodegradation
Biological and medical sciences
Biomedical and Life Sciences
Carbon
Carbon dioxide
Charcoal
Ecology
Fundamental and applied biological sciences. Psychology
General agronomy. Plant production
Grassland soils
Kinetics
Life Sciences
Mineralization
Miscanthus
Organic carbon
Organic soils
Other nutrients. Amendments. Solid and liquid wastes. Sludges and slurries
Plant Physiology
Plant Sciences
Pyrolysis
Raw materials
Regular Article
Sandy loam soils
Soil biochemistry
Soil chemistry
Soil degradation
Soil microorganisms
Soil science
Soil Science & Conservation
Soil-plant relationships. Soil fertility
Soil-plant relationships. Soil fertility. Fertilization. Amendments
Soils
Temperature effects
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Title Degradation kinetics of biochar from pyrolysis and hydrothermal carbonization in temperate soils
URI https://www.jstor.org/stable/42953070
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