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Spatio-Temporal Simulation of the Field-Scale Evolution of Organic Carbon over the Landscape

C. Walter*,a, R. A. Viscarra Rosselb and A. B. McBratneyb

a ENSA-INRA Rennes, 65 rue de St Brieuc, CS 84215, 35042 Rennes, France
b Faculty of Agriculture, Food and Natural Resources, The University of Sydney, NSW 2006, Australia



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Fig. 1. Framework of the combination of stochastic and deterministic approaches to simulate the initial spatial field of soil organic C content over the landscape. DEM, digital elevation model; HI, hydromorphic index; OC, organic C.

 


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Fig. 2. (a) Topography of the virtual study area and (b) initial land use under (P) long-term pastures; (T) short-term pastures; (C) cereals and (M) maize. Simulations of land use was conducted over 4500 virtual fields.

 


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Fig. 3. (a) Short-range semivariogram of organic carbon (OC) from 360 samples of a nested survey in southern Brittany and (b) its corresponding random function (RF) [Y1(x)]; (c) representation of a linear model of OC as a function of the redoximorphic index (HI) used to derive (d) the medium-range spatial field [Y3(x)]; (e) long-range semivariogram of OC based on 40 000 regional samples in Brittany, and (f) its simulated RF [Y2(x)].

 


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Fig. 4. (a) Block diagram of the additive spatial field that combines the short-, medium-, and long-range fields, and (b) the additive semivariogram model for soil organic C in the study region and the semivariograms of its three spatial components. The additive semivariogram was fitted with a triple exponential model.

 


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Fig. 5. Simulations of land use over time driven by the transition matrix given in Table 1, for maize (M), cereals (C), temporary pastures (T), and permanent pastures (P).

 


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Fig. 6. Block diagrams of land use evolution at (a) the start of the simulation, (b) 10 yr after, (c) 20 yr after, and (d) at the end of the simulation: permanent pastures (P), temporary pastures (T), cereals (C), and maize (M).

 


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Fig. 7. Maps of organic C content at different dates considering simulations that account only for land use.

 


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Fig. 8. Maps of organic C content at different dates considering simulations that account for land use and the influence of soil waterlogging.

 


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Fig. 9. Evolution of the organic C semivariograms at different dates considering simulations that (a) account for only land use, and (b) account for land use and the influence of soil waterlogging.

 


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Fig. 10. Evolution of soil organic carbon (SOC) content (a) field mean values and the (b) mean within-field variability.

 





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