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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
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Significant Bomb D14C 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
California Grassland Soil % Modern Carbon (1950 atmosphere) 120 80 100 60 1997 Depth (cm) 1952 ∆14C (‰, pre-bomb atm.= 0)
Koputaroa, New Zealand Goh et al, 1976 Syers et al, 1970
Judgeford, New Zealand O’Brien and Stout, 1978
Understanding Carbon Storage and Turnover • The balance between inputs and outputs Outputs Soil Organic Matter Inputs
Concentration vDOM kDOM DOM The Model
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
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 D14C 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
Koputaroa Soil, New Zealand Cumlative Soil Mass (g cm-2) D14C (per mil)
Koputaroa 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!