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Revision as of 20:45, 16 September 2016 by Debra Tabron (talk | contribs) (Newell - Figure 3. Diffusion Mechanism Leading to Plume Attenuation and Persistence. This process is controlled by diffusion and the presence of geologic heterogeneity with sharp contrasts between transmissive and low permeability media)
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Newell - Figure 3. Diffusion Mechanism Leading to Plume Attenuation and Persistence. This process is controlled by diffusion and the presence of geologic heterogeneity with sharp contrasts between transmissive and low permeability media

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current20:45, 16 September 2016Thumbnail for version as of 20:45, 16 September 2016670 × 492 (58 KB)Debra Tabron (talk | contribs)Newell - Figure 3. Diffusion Mechanism Leading to Plume Attenuation and Persistence. This process is controlled by diffusion and the presence of geologic heterogeneity with sharp contrasts between transmissive and low permeability media
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