Geofluids / 2018 / Article / Fig 4

Research Article

Advective Displacement Method for the Characterisation of Pore Water Chemistry and Transport Properties in Claystone

Figure 4

(a) Breakthrough of deuterated water and bromide versus time expressed as pore volume (water content); (b) modelled breakthrough curves with optimum values for Péclet numbers and the ratio of the anion average linear velocity relative to water, . The dashed lines are for a model including small mixing cells at both ends of the sample, representing the filter discs.

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