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Small-Scale Variability in Solute Transport Processes in a Homogeneous Clay Loam Soil

Fernando Garridoa, Masoud Ghodratia, Michael Chendoraina and Chris G. Campbella

a Division of Ecosystem Sciences, Dep. of Environmental Science, Policy and Management, Univ. of California, Berkeley, CA 94720-3110 USA



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  		Fig. 1 Schematic of multiplexed fiber-optic miniprobe system

 


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  		Fig. 2 Breakthrough curves of the 20 fiber-optic miniprobes (FOMPs) from the first miscible displacement experiment with 19 irrigation drip points and at a flux of 1.07 cm h-1. Pv refers to normalized time expressed as pore volumes. Concentration is in mg/L

 


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  		Fig. 3 Breakthrough curves of the 20 fiber-optic miniprobes (FOMPs) from the second miscible displacement experiment with 19 irrigation drip points and at a flux of 1.07 cm h-1. Pv refers to normalized time expressed as pore volumes. Concentration is in mg/L

 


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  		Fig. 4 Average breakthrough curves (BTCs) and corresponding coefficient of variation as a function of time for (a) BTC 1, (b) BTC 2, (c) BTC 3, (d) BTC 4, and (e) BTC 5

 


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  		Fig. 5 Average breakthrough curves (BTCs) and corresponding fits of the mobile–immobile water model (MIM) and convective–dispersive equation (CDE) for (a) BTC 1, (b) BTC 2, (c) BTC 3, (d) BTC 4, and (e) BTC 5

 




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