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The influence of char on forest seedlings, soils and trees
Mark ColemanAssoc Professor & IFTNC Director
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Collaborators
Deborah Page-DumroeseRocky Mountain Research Station
Jim ArchuletaUmpqua NFCole MaynBitterroot NF
Margo WelchDeary District
• US FS R&D program on Woody Biomass• McIntire-Stennis• American Recovery and Reinvestment Act• AFRI Sustainable Bioenergy
Terry ShawMark KimseyKristin McElligottDan SmithShan ShanBhanu BhattaraiBrian Bell
Funding Bio-charCharKing
High interest in thinning small diameter stands
• Private investment returns• Public lands are over stocked • Protection: wildfire, pests infestation, drought
• Policy: Healthy Forests Initiative, National Fire Plan, etc., Energy Independence and Security Act
• Adaptation to Climate Change• Cost prohibitive
Background
Utilizing Forest BiomassProvides management opportunities
• Interest in utilizing woody biomass for energy
• What are the ecological consequences of forest biomass removal?
• Can any negative impacts be mitigated?
Fast Pyrolysis
Small scale units• In woods processing • Avoid biomass transport costs• High value oil product• Research required• Funding scarce
Biochar is equivalent to native charcoal in forest ecosystems
• Char is common in fire-adapted ecosystems
• Fire suppression decreases charcoal inputs
• Biomass removal decreases the likelihood of fire occurring
• Applying char as a co-product of pyrolysis removes wildfire hazard and retains soil ecosystem function
Site amendment with charcoalpurports to:
• Return nutrients back tot the site of biomass removal• Improve soil characteristics• Enhance site quality
Objective• Evaluate impacts of biomass removal and char
amendments on forest soil productivity
Questions1. What soil properties are affected by char?2. Do char amendments alter tree growth; if so in
which direction?
Char porosity alters physical soil properties
• Porosity– 80% void space
• Increased surface area– 200-400 m2 / g
• Decreased bulk density– Char BD is 0.2 – 0.4 g/cc– Soil BD ranges from 1.0
to 1.7 g/cc
OM (g g-1)
So
il m
ois
ture
(w
/w)
0.0 0.1 0.2 0.3 0.4 0.50.0
0.2
0.4
0.6AndisolMollisol
012
25
50% char (v/v)
OM (g g-1)
pH
0.0 0.1 0.2 0.3 0.4 0.56.0
6.5
7.0
7.5
8.0AndisolMollisol
Char & soil propertiesIncubation studies
Char responses to char are consistent, but often depend on soil type
• Increased organic matter• Increased water holding capacity• Increased pH
Coleman, Shan & Smith unpublished
Increased sorption and ion exchange capacity retains nutrients from leaching
…. in some soils
McElligott 2011
Char has long residence time in soilCarbon sequestration potential
• Stable aromatic ring structure• Decay resistant
• But, char may speed decomposition of native soil organic matter
• Char enhances microbial activity• Sequestration may not equal the amount
applied if active microbes consume more
Yea
r A
D
Yea
r A
D
Whitlock & Larsen. 2001
Charcoal is used to date ancient fires
Does char speed the loss of soil organic matter ?
Wardle et al 2008
• Litter bags containing: • humus• char• humus + char
• Mixing humus with char causes greater mass loss than expected
Does char increases organic matter decomposition?• Activity of decomposition enzymes decreases with greater char• No effect found on soil respiration• Conclude OM consumption does not increase with char
Cellulase
OM (g g-1)
En
zym
e ac
tivi
ty
( m
ol h
-1 g
-1)
0.0 0.1 0.2 0.3 0.4 0.50
50
100
150
200
250AndisolMollisol
0
12
25
50
% char (v/v)
Chitinase
OM (g g-1)E
nzy
me
acti
vity
( m
ol h
-1 g
-1)
0.0 0.1 0.2 0.3 0.4 0.50
50
100
150AndisolMollisol
Phosphatase
OM (g g-1)
En
zym
e ac
tivi
ty
( m
ol h
-1 g
-1)
0.0 0.1 0.2 0.3 0.4 0.50
100
200
300AndisolMollisol
Peroxidase
OM (g g-1)
En
zym
e ac
tivi
ty
( m
ol h
-1 g
-1)
0.0 0.1 0.2 0.3 0.4 0.50
2
4
6
8AndisolMollisol
Soil Respiration
C (g g-1)
So
il R
esp
irat
ion
(m
ol m
-2 s
-1)
0.0 0.1 0.2 0.32.5
3.0
3.5
4.0
4.5
5.0AndisolMollisol
Coleman, Shan & Smith unpublished
Does char alter organic nitrogen cycling?
• Importance of organic N in forests now accepted
• Litter organic matter, N mineralization are correlated with productivity
• Amino acids are acquired by roots
• Amino acid pools and fluxes are is easily measured
{Nasholm, 2009 #5834}
Soluble organic NField-collected soils
• Amino acid solution concentration increases along an elevation gradient
• Also related to the quality (N%) of the litter layer
0 500 1000 1500 20000
1
2
3
4AMECMERM
Elevation (m)
Am
ino
acid
-N (
mg/
kg)
Shan, Kimsey & Coleman unpublished
500 1000 1500 20000.0
0.5
1.0
1.5
2.0AMECMERM
Elevation(m)O
rgan
ic L
ayer
N (
%)
Char increases Organic N cyclingvaries with elevation of soil origin
Shan, & Coleman unpublished
Low Middle High0.0
0.5
1.0
1.5
2.0
2.5
Elevaton
Am
ino
acid
-N(m
g/k
g)
Low Middle High0
10
20
30
40
50
Elevaton
Am
ino
pep
tid
ase
acti
vity
(nm
ol/g
*h)
Low Middle High0.0
0.5
1.0
68
10
0%10%20%
Elevaton
AA
Tur
nove
r In
dex
(h-1
)
Char causes:• Decreased Amino-N pools• Increased amino acid production
(Amino peptidase activity)• Increased amino acid turnover
– five-fold in low elevation soil– 30% increase in high elevation soil
Field work confirms char increases AA productionindicates greater N cycling
• Amino Acid production– Char rates are twice the control in early season– equal in late season
Smith 2013
Potential forestry applications
Does amino acid turnover indicate differences in site quality?
Testable Hypotheses1. Site quality is directly correlated with amino acid
production rate.2. Forest productivity correlates with soil organic
matter and organic N cycling rates.3. Assays of amino acid production in forests are
analogous to N mineralization measurement in agronomic soils.
4. Amino acid production rate is consistently high during wet season.
How does char affect tree growth?
Poplar grown with various proportions of char and vermiculite-peat potting mix; fertilized
• There is no growth stimulation
100%67%33%0%
aa a
a
Char:VP Mix
Char mixed in soilunfertilized
0% char 25% char 50% char0
1
2
3
4
5 a
bc
bb
c
ab
Abo
ve-g
roun
d B
iom
ass
(g)
0% sand 25% sand 50% sand0
1
2
3
4
5
CA
FA
a
abb b
cc
McElligott 2011
Need assurance that biochar application will not harm forest systems
• Tree growth may actually decrease depending on soil type• Similar response pattern with char and sand suggests the response is
not unique to char
Tree growth response
• Neutral to positive effects of char• Fertilizer enhances growth, but no added benefit with char• Slash effect rivals that of fertilizer• Short-term responses
Purdue Creek
Dia
met
er In
crem
ent
(in
/ y
r)
Control
Bioch
ar0.0
0.2
0.4
0.6
0.8
Swift Creek
Dia
me
ter
gro
wth
(in
2y
r-1)
Control
Char 1
.25
Char 1
0
Char 1
.25
+ Fer
tilize
r0.0
0.2
0.4
0.6
Purdue Creek
Dia
met
er In
crem
ent
(in
/ y
r)
Control
Bioch
arFer
t
Bioch
ar &
Fer
t0.0
0.2
0.4
0.6
0.8
Swift Creek
Dia
me
ter
gro
wth
(in
2y
r-1)
Control
Char 1
.25
Char 1
0
Fertil
izer
Char 1
.25
+ Fer
tilize
r
Char 1
0 +
Fertil
izer
0.0
0.2
0.4
0.6
Purdue Creek
Dia
met
er In
crem
ent
(in
/ y
r)
Control
Keep B
iom
ass
Bioch
arFer
t
Bioch
ar &
Fer
t0.0
0.2
0.4
0.6
0.8
Swift Creek
Dia
me
ter
gro
wth
(in
2y
r-1)
Control
Keep B
iom
ass
Char 1
.25
Char 1
0
Fertil
izer
Char 1
.25
+ Fer
tilize
r
Char 1
0 +
Fertil
izer
0.0
0.2
0.4
0.6
Coleman, Page-Dumroese et al unpublished
Using PCT stands to evaluate biomass removal impacts
• Established trees have exploited site• Seedlings need to become established, delayed inter-tree
competition• Young trees are responsive to treatment
Sustainable Bioenergy
untreated fertilizer untreated fertilizer
biochar fertilizer & biochar biochar fertilizer & biochar
untreated fertilizer untreated fertilizer
biochar fertilizer & biochar biochar fertilizer & biochar
Thinned and No slash retention (0)
Thinned and All slash retained (1x) Thinned and Double Slash retained (2x)
Unthinned control
Utilizing Forest Biomass Conclusions
• Numerous motivations to develop forest bioenergy• Portable units appealing, but require development• Char is a novel forest product
– Used to sequester carbon and enhance soil quality
• Incubation studies demonstrate soil properties:– Water holding capacity, pH, nutrient retention, exchange capacity, etc
• Char doesn’t increases organic matter decomposition• New tools to measure organic N cycling indicates increases
char; applications to forest nutrient management• Monitoring PCT responses is sensitive measure of biomass
removal and soil amendments