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Significant Bomb 14 C Enrichment in Deep Soil: A Previously Unrecognized Decadal C Pool? W. Troy Baisden and Roger L Parfitt Landcare Research, Palmerston North, New Zealand Funded by NZ Foundation for Research Science and Technology Ministry of Agriculture and Forestry US-NZ Climate Change Partnership through NZ Govt

Significant Bomb D 14 C Enrichment in Deep Soil: A Previously Unrecognized Decadal C Pool?

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Significant Bomb D 14 C Enrichment in Deep Soil: A Previously Unrecognized Decadal C Pool?. W. Troy Baisden and Roger L Parfitt Landcare Research, Palmerston North, New Zealand. Funded by NZ Foundation for Research Science and Technology Ministry of Agriculture and Forestry - PowerPoint PPT Presentation

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Page 1: Significant Bomb  D 14 C Enrichment in Deep Soil:   A Previously Unrecognized Decadal C Pool?

Significant Bomb 14C Enrichment in Deep Soil: A Previously Unrecognized Decadal C Pool?

W. Troy Baisden and Roger L Parfitt

Landcare Research, Palmerston North, New Zealand

Funded by NZ Foundation for Research Science and TechnologyMinistry of Agriculture and Forestry

US-NZ Climate Change Partnership through NZ Govt

Page 2: Significant Bomb  D 14 C Enrichment in Deep Soil:   A Previously Unrecognized Decadal C Pool?

-400 -200 0 200

0

50

100

150

Dep

th (

cm)

∆14C (‰, pre-bomb atm.= 0)

% Modern Carbon (1950 atmosphere)

80 100 12060

1952

1997

California Grassland Soil

Page 3: Significant Bomb  D 14 C Enrichment in Deep Soil:   A Previously Unrecognized Decadal C Pool?

Baisden et al 2002, Global Biogeochemical Cycles

Page 4: Significant Bomb  D 14 C Enrichment in Deep Soil:   A Previously Unrecognized Decadal C Pool?

Koputaroa, New ZealandGoh et al, 1976Syers et al, 1970

Page 5: Significant Bomb  D 14 C Enrichment in Deep Soil:   A Previously Unrecognized Decadal C Pool?

Judgeford, New ZealandO’Brien and Stout, 1978

Page 6: Significant Bomb  D 14 C Enrichment in Deep Soil:   A Previously Unrecognized Decadal C Pool?

Understanding Carbon Storage and Turnover•The balance between inputs and outputs

Soil Organic Matter

Inputs Outputs

Page 7: Significant Bomb  D 14 C Enrichment in Deep Soil:   A Previously Unrecognized Decadal C Pool?

The Model

DOM

vDOM

kDOM

Concentration

Page 8: Significant Bomb  D 14 C Enrichment in Deep Soil:   A Previously Unrecognized Decadal C Pool?

Model Formulation for DRDSC(Decadally Reactive Deep Soil C)

• Mass (g/m2)

• Downward Transport (cm/yr)

• First Order Loss Coefficient (yr-1)

• E-folding Depth (cm)

• No interactions with other 3 pools

• Is DRDSC from roots or dissolved organic matter (DOM)?– Progressive enrichment in most profiles– Below rooting zone

Page 9: Significant Bomb  D 14 C Enrichment in Deep Soil:   A Previously Unrecognized Decadal C Pool?

Data Assimilation via a Genetic Algorithm

• Evolves a chromosome of parameter values toward the best value for the model fit (based on an ‘objective function’)

• Inefficient but searches parameter space on both sides of the bomb-C spike

• Monte-Carlo style variation in 14C and %C data• Parameter uncertainty estimated from Monte-Carlo

– Greater of:• Standard deviation of best fits with data PDFs• Difference between best fit with and without PDFs included

• Emphasizing fitting DRDSC pool sizes

Page 10: Significant Bomb  D 14 C Enrichment in Deep Soil:   A Previously Unrecognized Decadal C Pool?
Page 11: Significant Bomb  D 14 C Enrichment in Deep Soil:   A Previously Unrecognized Decadal C Pool?
Page 12: Significant Bomb  D 14 C Enrichment in Deep Soil:   A Previously Unrecognized Decadal C Pool?
Page 13: Significant Bomb  D 14 C Enrichment in Deep Soil:   A Previously Unrecognized Decadal C Pool?

Koputaroa Soil, New Zealand

14C (per mil)

Cu

mla

tive

So

il M

ass

(g c

m-2)

Page 14: Significant Bomb  D 14 C Enrichment in Deep Soil:   A Previously Unrecognized Decadal C Pool?

Soil Organic Carbon (SOC) Pools Estimated by the ModelSite Max.

DepthIncluded

inAnalysis

(m)

Total SOC

(MgC/ha)

SOCwith turnover <100 yr

(MgC/ha)

DRDSC

(MgC/ha)

Koputaroa 0.8 148±4 81±4 10±3Judgeford 1.0 192±10 131±7 10.3±0.7*

TurlockLake

1.1 33±2 13±1 4.7±3.3

Riverbank 3.6 39±3 12±2 9.0±1.3*Model appears to underestimate DRDSC pool size.

Page 15: Significant Bomb  D 14 C Enrichment in Deep Soil:   A Previously Unrecognized Decadal C Pool?

Model-Estimated Soil Organic Carbon (SOC) PoolsSite Max.

DepthIncluded

inAnalysis

(m)

Ratio ofDRDSC toTotal SOC

Ratio ofDRDSC toSOC withturnover<100 yr

Koputaroa 0.8 0.07±0.02 0.13±0.04Judgeford 1.0 0.054±0.005* 0.078±0.008*

TurlockLake

1.1 0.14±0.10 0.37±0.27

Riverbank 3.6 0.23±0.05 0.74±0.05*Model appears to underestimate DRDSC pool size.

Page 16: Significant Bomb  D 14 C Enrichment in Deep Soil:   A Previously Unrecognized Decadal C Pool?

DRDSC as a Fraction of Total SOC

•10-20% of Deep Soil C has Decadal Dynamics

•Possibly increasing with Depth?

•Better understanding of DOC needed!

•10-20% of Deep Soil C has Decadal Dynamics

•Possibly increasing with Depth?

•Better understanding of DOC needed!

Koputaroa