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Quantifying Rates of Soil Water Evaporation: Implementing a Soil Water Oxygen Isotope Model in Matlab Erik Oerter EPS 209 27 April 2011.

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Presentation on theme: "Quantifying Rates of Soil Water Evaporation: Implementing a Soil Water Oxygen Isotope Model in Matlab Erik Oerter EPS 209 27 April 2011."— Presentation transcript:

1 Quantifying Rates of Soil Water Evaporation: Implementing a Soil Water Oxygen Isotope Model in Matlab Erik Oerter EPS April 2011

2 Project Motivation: Soil Water Oxygen Isotopes Soil Water originates as meteoric water, preserving the isotopic signature of precipitation Hydrogen and Oxygen isotopes undergo Rayleigh fractionation as water evaporates Enrichment in 18 O relative to precipitation The 18 O/ 16 O can be sampled: Directly as soil water (contemporary water) Indirectly as CaCO 3 (ancient water) Use 18 O/ 16 O to estimate evaporation rate Climate Proxy

3 Evaporation Rate via Soil Water Oxygen Isotopes 18 O/ 16 O of water at z in soil profile Depth in soil profile Evap. Rate Depth of evap. front Diff coef. of water in soil 18 O/ 16 O of water at depth 18 O/ 16 O of water at evap. front (Barnes and Allison, 1988, J. of Hydrology) L = Total depth of soil profile

4 Project Idea: Fit modeled Oxygen isotope profile to observed data and find the evaporation rate Model 18 O profile Observed 18 O profile Data from Wang et al., 1996

5 Project Approach: m-file Sequence of Events 1)Load in observed data as text file 2)Initialize variables - Make an initial guess for evaporation rate - Populate a vector with evap guesses (~100) Specify the step between evap guesses - Initialize a matrix for calculated 18 O profiles (# depth increments x # evap guesses) 3)Loop over all evap guesses, calculating 18 O profiles - Now have O profiles…

6 Project Approach: m-file Sequence of Events

7 Some Results Diffusion Coefficient of Water in Soil = 1.5* m 2 /sec Starting Evap Rate Guess = 5x m/sec (0.15 cm/year) E guess step = 1* m/sec Best fit Evap rate = 1.02* m/sec (0.32 cm/year)

8 Future Work This interpretation of the Barnes and Allison Model: - Single wet soil zone with the evaporating front at the surface Barnes and Allison envisioned a dry zone of soil overlying the wet zone and evaporating front at some depth Implement the two zone scheme - Allow for a migrating (+/- depth) evaporation front Allow for resetting of the 18 O input value (Allow it to rain on the soil)


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