Biochar, Biomass, Soil and Agriculture - Information for public adoption
KshithijUrs
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May 08, 2024
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About This Presentation
Introduction to Biochar
Size: 4.02 MB
Language: en
Added: May 08, 2024
Slides: 60 pages
Slide Content
Biochar
Is it a viable option for soil C stabilization and sequestration?
The Carbon Cycle
Four Reservoirs of Carbon:
1.Sedimentary Rock
2.Ocean
3.Land Surface
4.Atmosphere
Eachofthesereservoirs
“breathes”CO
2causing
atmosphericCO
2tovaryover
time.
What we know: Terra Preta
Marris. 2006. Nature 442: 624-626; Lehmann, et al., 2003. Plant Soil 249: 343-357; Lehmann,
et al., 2003. Kluwer Academic Publishers. 105-124.
• fine dark loamy soil
-up to 9% carbon, (adjacent soil 0.5% C)
-high nutrient content and high fertility
-3 times the phosphorous and nitrogen
• developed over thousands of years by human
habitation correspond to ancient settlements
•resultsfromlong-termmulchingofcharcoal
productionfromhearthsandbonefragments
withsoilapplication
• persistents in soil, recalcitrant, resistant to
decomposition.
Terra preta do indio or the “black earth of the Amazons”
• forest fires and slash-and-burn contribute
very low amounts of charcoal (~3%)
Figure 3. Biochar particles in a dark earth from the Amazon,
with dimensions of several tens of microns to submicrons. Upper
left side shows a quartz grain, inset shows separated biochar
particles. Note the coatings of biochar particles with minerals in
their natural assemblage.
from Lehmann, (2007), Front. Ecol. Environ. 5:381-387.
What we know: Terra Preta
Biochar may come to
the rescue....
….and whatis biochar....? ??
What is Biochar?
-carbon-rich solid -a byproduct
of low-temperature pyrolysis
of biomass.
-also known as charcoal,
biomass derived black
carbon, Agrichar.
-formed under complete or
partial exclusion of oxygen
at low temperatures between
about 400 and 500º C.
-Origins -has been used for centuries
-Cooking, health, water purification, etc
Active research into soil benefits was renewed by Johannes Lehmann at Cornell
University in about 1998 resulting from studies of Terra preta soils of the Amazon.
Peanut hull biochar
It is ...
•Whenbiomassisburntintheabsenceofoxygen,
pyrolysisoccursandthebiomasscanbeturnedintoa
liquid(‘bio-oil’),agasandahigh-carbon,fine-grained
residue:biochar.
•Biocharisfinelygroundcharcoalwithsomesimilarities
toactivatedcharcoal.
•Biocharoffersanextremelyhighsurfaceareatosupport
microbiotathatcatalyseprocessesthat,amongother
things,reducenitrogenlossandincreasenutrient
availabilityforplants.(Winsley,2007)
Any source of biomass:
• Rice husks
• Nut shells (groundnut, hazelnut, macadamia nut,
walnut, chestnut, coconut)
• Bagasse from sugar cane production
• Olive or tobacco waste
• Wood chips, sawdust, bark, etc
• Animal manure
• Peanut hull
• Grasses and corn stover
• Other –sewage sludge tires, peat, lignite, coal
Potential Feedstocks of Biochar
*Notallorganicbiomassissuitableforproducingbiochar
Household,municipalandindustrialwastemaycontain
heavymetalsororganicpollutantswhichcouldcause
environmentalcontaminationbylandapplicationofthe
resultingbiochar.
Biochar Production
Temp &
Duration
Solid
(Biochar)
Liquid
(Bio oil)
Gas
(Syn Gas)
Slow
Pyrolysis
~500C
Days
35% 30% 35%
Fast
Pyrolysis
~500C
Seconds
12% 75% 13%
Gasification>800C
Hours
10% 5% 85%
CHP Gasification Slow Pyrolysis (retort) Slow pyrolysis (kiln)
Biochar Production
Eprida: Hydrogen and Char Fertiliser via Pyrolysis
Dynomotive:
Bio oil via
Fast
Pyrolysis
BEST Energies: Biochar via Slow Pyrolysis
University of Hawaii:
Flash Carboniser (Fast Pyrolysis)
from Lehmann, (2007), Front. Ecol. Environ. 5:381-387.
Low temperature pyrolysis with biochar C
sequestration
Biochar does not
degrade in soils
•Compostandotherorganic
materialinsoilsisvaluablebut
mineralises(convertstoCO
2)in
justafewyears.
•Biochar will remain
essentiallyunchanged for
hundredsoreventhousandsof
years–carbonsequestration
reallyispossible
Charcoal occurs
naturally in soils
•Up to 35 per cent of SOC in
some US soils is charcoal from
natural processes (Skjemstad
et al, 2002)
•Natural charcoal in the US
midwest prairie soils, a result
of ten thousand years of
prairie fires, may play a role in
these soils’ high and sustained
fertility
•Our results provide clear evidence that
immediately after wildfire fresh charcoal can
have important effects in Boreal forest
ecosystems dominated by ericaceous dwarf
shrubs, and this is likely to provide a major
contribution to the rejuvenating effects of
wildfire on forest ecosystems.
(Wardle et al, 1998)
80 per cent of Africans
rely on biomass
for energy
Charcoal market in Khartoum, Sudan
Uganda has lost half
its forest cover in the
last ten years; 97 per
cent of the
population uses
charcoal and
firewood for cooking;
charcoal production
creates 20,000 jobs
‘Slash and burn’ to
‘slash and char’
Over2billionpeoplerelyon
traditionalbiomassforheating
andcookingusinginefficientand
dirtystovesoropenfires.
Improvedstovesthatareclean
andcanalsomakecharcoalcould
improvehealth,reducemortality
andassistinagricultural
transformation
Third generation cooking stove:
Low pollution, production of biochar
(Flanagan and Joseph)
Scanning Electron Microscopy (SEM)
of biochar
Courtesy of UK Biochar Research CentreCourtesy of www.carboncommentary.com
X-ray diffraction spectra of 3 biochars compared with synthetic
graphite. Insert shows spectra with expanded vertical scale.
Nutrient Content of Biochar
• C-content -75-85% largely unavailable to
decomposition; ∆ microbial activity?
• C/N ratio –12-40 100 lbs biochar has ~8-10 lbs N
protection. Tends to NH4 form.
• P content –0.08%
Other nutrients (S, Mg, Ca, micronutrients)?
Some physico-chemical parameters of biochar
Feedstock pH EC(1:5)(dS/m) Ash content (g/kg)
(1:5 H2O)30 min 24h 550
0
C 700
0
C
E. saligna wood7.67+0.100.13+0.010.44+0.01 42+4 37+2
E. saligna leaves9.17+0.051.44+0.233.52+0.15 99+1 40+1
Poultry litter9.20+0.026.32+0.069.27+0.02 423+36 346+1
Cow manure 9.03+0.019.18+0.1412.28+0.19 703+4 704+7
LSD (P=0.05) 0.11 0.29 0.24 36 18
Feedstock Total C Total N CaCO
3
P
(g/kg) (g/kg) (mg/kg)
E. saligna wood694.0+5.12.1+0.2 -3.4+0.9 127+8
E. saligna leaves66.8+2.916.4+0.515.4+1.0 2077+51
Poultry litter431.1+6.851.8+0.358.2+2.4 5763+120
Cow manure 175.0+1.513.5+0.134.8+2.1 4359+47
LSD (P=0.05) 6.5 0.3 276
Feedstock K S Ca Mg
E. salignawood 1756+200 127+33 17994+590 911+184
E. salignaleaves12816+339 910+22 17144+469 4657+144
Poultry litter24851+1376 4900+455 33352+948 6835+210
Cow manure 26429+3468 4526+75 17518+493 10699+218
LSD (P=0.05) 2380 419 5198 529
CEC and exchangeable cationsin biochar
Feedstock CEC
AW
CEC
O
Ca Mg Na K
E. saligna
wood 47.3+47 134.4+3.7 40.1+2.7 1.2+0.2 13.0+0.6 3.3+0.4
E. saligna
leaves 77.7+5.3 71.0+1.3 47.1+2.920.5+0.858.2+0.8 72.2+2.9
Poultry litter172.9+3.7145.1+15.4 28.5+1.346.1+2.9100.1+1.1360.0+12.3
Cow manure 208.8+7.2221.9+5.5 39.9+0.354.0+0.6125.8+1.4475.1+8.3
LSD (P=0.05) 9.3 43 17.9 8.5 3.3 36.1
Oxygenated acidic and basic functional groups (mmol
C/g) of biocharsas determined by Boehm titrations
Feedstock Carboxy1 carboxy1 + lactonicTotal acidityTotal basicity
+ phenolic
E. saligna
wood 0.83+0.11 2.68+0.14 5.71+0.76 0.60+0.16
E. saligna
leaves 0.63+0.11 2.67+0.17 5.34+0.73 0.93+0.05
Poultry litter0.83+0.15 3.23+0.14 5.10+0.30 4.29+0.23
Cow manure 2.01+0.24 5.15+0.09 8.08+0.79 6.46+0.27
LSD
(P=0.05) 0.39 0.42 1.52 1.54
Characteristics of Biochar
Thepropertiesofbiochargreatlydependupontheproductionprocedure.
TemperatureeffectsonCrecovery,CEC,pHandsurfacearea.
fromLehmann(2007),Front.Ecol.Environ.5:381-387.
Schematics for biomass or bio-char remaining after charring
and decomposition in soil. from Lehmann et al., 2006. Mitigation Adap.
Strat. Glob. Change 11: 403–427.
C Sequestration Potential of Biochar
<10-20%
•Biochar effects on :
•Soil structure
•Soil aggregate stability
•Soil water
Soil physics
Soil physics –aggregate stability
•↓ the entry of water into the aggregate pores leading to an ↑ in aggregate stability
•hydrophobic polyaromatic backbone ↓ the entry of water into the aggregate pores
leading to an increased aggregate stability and water availability
http://www.landfood.ubc.ca/soil200/interaction/structure.htm
Soil physics –soil water
•↑waterretentioninAmazoniancharcoalrich
soils
•formationoforgano-mineralcomplexesby
functionalgroupsofthehumicacids
•increasedaggregatestability–holdswater
•↑moistureinsandysoils–mechanisms?
Soil Physics –Research Questions
?
physical characteristics
of biochar on soil
processes -mechanisms
soil workability
mechanisation and application
soil hydrophobicity
physical properties of
biochar change over time
biochar application
influence soil aggregate
stability –link to rates
Soil chemistry
•Biochar effects on :
-soil greenhouse gas emissions
-nutrient dynamics –diffuse pollution
(linked to CEC)
Cation Exchange Capacity (CEC)
http://www.spectrumanalytic.com/support/library/ff/CEC_BpH_and_percent_sat.htm
•biochar –↑ surface area, negative surface
charge & charge density
•retains nutrients –link to crop uptake &
diffuse pollution (associated to NVZs)
•better nutrient uptake by crop, ↓ reliance
on manufactured fertilisers
•adsorbs phosphate –mechanism ?
Figure 4. Adsorption of phosphate to biochar (produced from
Robinia pseudoacacia L at 350°C for 16 hours). from Lehmann
(2007) Front. Ecol. Environ. 5:381-387.
Adsorption of phosphate to biochar
A spore of arbuscular mycorrhiza extends its hypha into a piece of
porous wood charcoal.(Plate provided by R.Soda.)
Soil biology –research questions
?
Biochar-colonising
microorganisms –mechanisms
Bacteria vs. fungi competition
when colonising biochar
surfaces
Fungi influence on altering
soil physiochemical
properties
Indirect effects on
mycorrhizae
through effects on other
soil microbes?
Courtesy of Biochar Farming
Contaminants(e.g.polycyclicaromatichydrocarbons(PAHs),
heavymetals,dioxins)thatmaybepresentinbiocharmayhave
detrimentaleffectsonsoilpropertiesandfunctions.The
occurrenceofsuchcompoundsinbiocharislikelytoderivefrom
eithercontaminatedfeed-stocksortheuseofprocessing
conditionsthatmayfavourtheirproduction.Evidencesuggests
thatatightcontroloverthetypeoffeedstockusedandlower
pyrolysistemperatures(<500
o
C)maybesufficienttoreducethe
potentialriskforsoilcontamination.
Biocharand potential risk for soil contamination
(Source-BiocharApplicationtoSoilsACriticalScientificReviewofEffectsonSoilProperties,ProcessesandFunctions:F.Verheijen,S.
Jeffery,A.C.Bastos,M.vanderVelde,I.Diafas-EuropeanCommission,JointResearchCentreInstituteforEnvironmentand
Sustainability)
•How soil microbial community particularly the soil
heterotrophs will behave under the presence of non-degrading
carbon source?
•Since the decomposition of biochar is extremely slow what
mechanism will be operating for nutrients release/availability?
•What will be the enzymatic activities under the influence of
non degrading substrate like biochar?
•What should be the optimum rate of biochar application?
•What will be the impact of long term application of biochar on
crop yield and soil quality?
•Is there any proven technology for large scale production of
biochar on small farm scale?
Researchable Issues
for patient hearing …
AMANWITHA
NEWIDEAISA
CRANKUNTILTHE
IDEASUCCEEDS!