assessing douglas-fir water-use history using stable isotope ( 13 c and 18 o) in tree rings:...
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![Page 1: Assessing Douglas-fir water-use history using stable isotope ( 13 C and 18 O) in tree rings: principles and potential J. Renée Brooks Western Ecology Division,](https://reader035.vdocuments.us/reader035/viewer/2022062421/56649d375503460f94a109e6/html5/thumbnails/1.jpg)
Assessing Douglas-fir water-use history using stable isotope (13C and 18O) in tree rings:
principles and potential
J. Renée BrooksJ. Renée Brooks Western Ecology Division, Corvallis ORWestern Ecology Division, Corvallis OR
Environmental Protection AgencyEnvironmental Protection Agency
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Stable Isotopes in Tree ringsStable Isotopes in Tree rings Isotopes Isotopes indicateindicate the magnitude of key the magnitude of key
ecological processesecological processes 1313C – intrinsic water-use efficiencyC – intrinsic water-use efficiency 1818O – RH, stomatal conductanceO – RH, stomatal conductance
Isotopes Isotopes recordrecord these responses to these responses to changing environmental condition.changing environmental condition. Tree rings are formed incrementally creating a Tree rings are formed incrementally creating a
record over time. record over time. Isotopes Isotopes integrateintegrate ecological processes ecological processes
over timeover time An annual ring integrates over the year. An annual ring integrates over the year.
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leaf
leafair
C
CC13
1313
1
a
i
c
caba )(
Carbon isotope discrimination
and its relationship to leaf physiology
Where a = 4.4 (diffusion of CO2); b = ~27 (enzymatic fractionation), ci internal [CO2], ca = ambient [CO2]
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transpirationrate
water stress
humidity
photon fluxcanopy leaf areaCO2
leafconductance
ci
ca
productivity
Growth, reproductive output
photosynthetic rate
Nitrogen
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Carbon Isotope Discrimination Carbon Isotope Discrimination a measure of Intrinsic Water-Use Efficiencya measure of Intrinsic Water-Use Efficiency
WUE Ag
Ci Cain trinsic
( ).1 6
a
i
c
caba )(
Where a = 4.4 (diffusion of CO2); b = ~27 (enzymatic fractionation), ci internal [CO2], ca = ambient [CO2]
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Interpreting Interpreting 1313C C
A
gs
Same
13 C Valu
e
Increased 13C Value
Decreased 13C Value
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Interpreting Interpreting 1313C and C and 1818O O power of dual isotopespower of dual isotopes
Grams et al. 2007 PCE, Scheidegger et al. 2000 Oecol.
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Oxygen isotopes in plant tissues
Oxygen isotopes in plant tissues
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What happens to leaf water?What happens to leaf water?What happens to leaf water?What happens to leaf water?
Craig Gordon (1965), Farquhar and Lloyd (1993)
18Oe k (18Ov k )eaei
+ Equilibrium fractionation
k Kinetic fractionation
18Ov Water vapor
ea/ei Atmosphere - leaf vapor gradient
18Oe enrichment of leaf water (above the source)
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Transpiration
Leaf surface
Mass flow of leaf water
Back diffusion of 18O enriched water
18O enrichment according to Craig-Gordon Model (1965)
(preferential loss of H216O)
Péclet Effect
Stronger Transpiration less 18O in leaf water
Stomatal conductance, gH2O [mmol m-2 s-1]
18O
[p
er
mil]
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Bulk Water vs. site of evaporationBulk Water vs. site of evaporationthe Péclet effect the Péclet effect
ee
L
1
CD
LE
Where C = molar density of water, D = diffusivity of H2
18O in water, E = transpiration rate L = effective path length
Barbour et al. (2007)Barbour et al. (2007)
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Model for Cellulose Model for Cellulose 1818OO
ƒƒoo = fraction exchanged with xylem water = fraction exchanged with xylem water wl = leaf waterwl = leaf water wx = xylem waterwx = xylem water cx = xylem cellulosecx = xylem cellulose εεoo = fractionation factor (+27 ‰) = fractionation factor (+27 ‰)
owloowxocx OfOfO 181818 1
Roden et al. 2000
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Isotopic applications Isotopic applications to field studiesto field studies
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Effects of soil WaterEffects of soil Water
Dupouey et al. 1993 PCE
Relative Extractable Water (%)
13C
(‰
)
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TranspirationTranspiration
Livingston and Spittlehouse 1993
13C
(‰
)
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Ba
sal A
rea
Incr
emen
t (c
m2 )
0
10
20
30
40
50
60
70
80
Year
1980 1985 1990 1995 2000
Dis
crim
inat
ion
(‰
)
14.5
15.0
15.5
16.0
16.5
17.0
17.5
a
b
Effects of ThinningEffects of Thinning
McDowell et al. 2003 PCE
Thinned
Control
200 year-old Ponderosa Pine
Thinning
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A (m
ol
m-2 s
-1)
9
10
11
12
g (
mo
l m-2 s
-1)
0.07
0.08
0.09
0.10
0.11
0.12
ThinnedControl
Year
1980 1985 1990 1995 2000
% c
ha
ng
e i
n
A a
nd
g a
fte
r th
inn
ing
-10
0
10
20
30
a
b
c
McDowell et al. 2003 PCE
1980 1985 1990 1995 2000
Effects of Thinning
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Effects of FertilizationEffects of FertilizationWind River Fertilization Experiment
Year
1940 1945 1950 1955 1960 1965 1970 1975 1980 1985 1990 1995 2000 2005
Bas
al A
rea
Incr
emen
t (m
m2 )
0
1000
2000
3000Control157 Kg/ha314 Kg/ha471 Kg/ha
Brooks & Coulombe in review
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Fertilization effects on Fertilization effects on
18.0
18.5
19.0
19.5
20.0
20.5
21.0Early Wood
Year
1954 1956 1958 1960 1962 1964 1966 1968 1970 1972 1974
13 C
(‰
)
18.0
18.5
19.0
19.5
20.0
20.5
21.0
Control157 kg/ha314 kg/ha471 kg/ha
Late Wood
N addition
Brooks & Coulombe in review
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Leaf Gas-Exchange Leaf Gas-Exchange
1954 1956 1958 1960 1962 1964 1966 1968 1970 1972 1974
Cha
nge
in A
/gs
(m
ol m
ol-1
)
rela
tive
to c
ontr
ols
-5
0
5
10
15Control157 kg/ha314 kg/ha471 kg/ha
N addition
Estimated from Late Wood
Brooks & Coulombe in review
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Late Wood
Year
1954 1956 1958 1960 1962 1964 1966 1968 1970 1972 1974
18O
(‰
)N
orm
aliz
ed f
or p
retr
eat
mea
ns
-2
-1
0
1
2
3Control157 kg/ha314 kg/ha471 kg/ha
N addition
1818O response to FertilizerO response to Fertilizer
13Ceffect Leaf Area
effect
Brooks & Coulombe in review
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Late Season Changes in Gas-exchange
g s (
%)
chan
ge fr
om c
ontr
ols
-60
-40
-20
0
20
40
157 kg/ha314 kg/ha471 kg/ha
Year
1954 1956 1958 1960 1962 1964 1966 1968 1970 1972 1974
A (
) ch
ange
from
con
trol
s
-60
-40
-20
0
20
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Late Season Changes in growth and Leaf Area
Late
woo
d B
AI
(Pro
p. o
f con
trol
)
0.5
1.0
1.5
2.0
2.5
3.0
3.5
4.0
4.5
157 kg/ha314 kg/ha471 kg/ha
Year
1954 1956 1958 1960 1962 1964 1966 1968 1970 1972 1974
Leaf
Are
a (p
rop.
of c
ontr
ol)
0
1
2
3
4
5
6
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N Fertilization Created N Fertilization Created Hydraulic ImbalanceHydraulic Imbalance
Leaf area increasedLeaf area increased Roots and sapwood insufficient to support Roots and sapwood insufficient to support
increased leaf areaincreased leaf area Fertilized trees experience drought at the Fertilized trees experience drought at the
end of summer. end of summer. Increase in leaf area offset decrease in Increase in leaf area offset decrease in
leaf gas-exchange – Growth increased.leaf gas-exchange – Growth increased. Hydraulic imbalance lasted 10 yearsHydraulic imbalance lasted 10 years
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Multiple Fertilizer ApplicationsMultiple Fertilizer Applications
Year
1978 1980 1982 1984 1986 1988 1990 1992 1994 1996 1998 2000 2002 2004
13C
16
17
18
19
20
Bald Hill SiteB
asal
Are
a In
crem
ent
(mm
2)
0
1000
2000
3000
4000
5000
6000 FertilizedControl
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Unresponsive SiteUnresponsive SiteB
AI
(mm
2)
0
2000
4000
6000
8000
Ostrander Site
Year
1978 1980 1982 1984 1986 1988 1990 1992 1994 1996 1998 2000 2002 2004
13 C
16
17
18
19
20
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Tree rings records Tree rings records
Extent and duration of growth response is Extent and duration of growth response is recorded in ring width data.recorded in ring width data.
1313C and C and 1818O allow for understanding the O allow for understanding the leaf physiology and whole tree hydraulics.leaf physiology and whole tree hydraulics.
Control trees necessary for separating Control trees necessary for separating management treatments from climate management treatments from climate signals.signals.
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Tree rings provide added insights Tree rings provide added insights into long-term experiments.into long-term experiments.