| 词条 | Pyrogenic carbon capture and storage |
| 释义 |
PrincipleThe principle of PyCCS is that the biomass (e.g. trees) removes CO2 from the atmosphere during its growth via photosynthesis. This biomass is then harvested and pyrolyzed (see below), with a portion of the carbon dioxide bound in the biomass being captured in the ground, after being reduced to carbon and viscous compounds. The flammable gas mixture, which is the lightest fraction in pyrolysis, is collected and used as fuel; the carbon dioxide produced when combusting it is captured traditionally. TechnologyPyrolysis in the context of carbon capture and storage has been descibed by Werner et al. (2018) as "the thermal treatment of biomass at 350 °C–900 °C in an oxygen-deficient atmosphere. Three main carbonaceous products are generated during this process, which can be stored subsequently in different ways to produce [negative emissions]: a solid biochar as soil amendment, a pyrolytic liquid (bio-oil) pumped into depleted fossil oil repositories, and permanent-pyrogas (dominated by the combustible gases CO, H2 and CH4) that may be transferred as CO2 to geological storages after combustion."[2] In low oxygen conditions, the thermal-chemical conversion of organic materials (including biomass) produces both volatiles, termed pyrolytic gases (pyrogases), as well as solid carbonaceous co-products, termed biochar. While the pyrogases mostly condense into liquid bio-oil, which may be used as an energy source, biochar has been proposed as a tool for sequestering carbon in soil.[1] Once mixed into soil, biochar, which is less susceptible to remineralization into CO2 and CH4 than non-pyrogenic biomass,[3] fragments into micro- and nano-particles which can be transported to deeper soil horizons, groundwater, or other compartments that further protect it from degradation. Multiple studies have demonstrated that pyrogenic carbon is stable over centennial timescales.[1][4] See also{{Portal|Energy|Sustainable development}}
References1. ^1 2 {{Cite journal|last=Criscuoli|first=Irene|last2=Alberti|first2=Giorgio|last3=Baronti|first3=Silvia|last4=Favilli|first4=Filippo|last5=Martinez|first5=Cristina|last6=Calzolari|first6=Costanza|last7=Pusceddu|first7=Emanuela|last8=Rumpel|first8=Cornelia|last9=Viola|first9=Roberto|date=2014-03-10|title=Carbon Sequestration and Fertility after Centennial Time Scale Incorporation of Charcoal into Soil|journal=PLoS ONE|volume=9|issue=3|pages=e91114|doi=10.1371/journal.pone.0091114|issn=1932-6203|pmc=3948733|pmid=24614647}} 2. ^1 Constanze Werner et al. (2018): Biogeochemical potential of biomass pyrolysis systems for limiting global warming to 1.5° C. Environmental Research Letters, 13(4), 044036. doi:10.1088/1748-9326/aabb0e 3. ^{{Citation|last=Zimmerman|first=Andrew|title=The Stability of Biochar in the Environment|date=2013-02-21|work=Biochar and Soil Biota|pages=1–40|publisher=CRC Press|isbn=9781466576483|last2=Gao|first2=Bin|doi=10.1201/b14585-2}} 4. ^{{Cite journal|last=Schmidt|first=Hans-Peter|last2=Anca‐Couce|first2=Andrés|last3=Hagemann|first3=Nikolas|last4=Werner|first4=Constanze|last5=Gerten|first5=Dieter|last6=Lucht|first6=Wolfgang|last7=Kammann|first7=Claudia|title=Pyrogenic carbon capture and storage|journal=GCB Bioenergy|language=en|volume=0|doi=10.1111/gcbb.12553|issn=1757-1707|year=2018}} 1 : Climate change mitigation |
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