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Electrochemical Water Splitting at Bipolar Interfaces of Ion Exchange Membranes and Soils

Brian M. Desharnais*,a and Barbara Ann G. Lewisb

a Dep. of Civil and Environmental Engineering, Tri-State Univ., 1 University Ave., Angola, IN 46703
b Dep. of Civil Engineering, Northwestern Univ., 2145 Sheridan Road, Evanston, IL 60208



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Fig. 1. Schematic of water splitting within a bipolar ion exchange membrane (based on Strathmann et al., 1993).

 


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Fig. 2. Inhibition of acid front with the anode encapsulated with an anion exchange membrane.

 


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Fig. 3. Accelerated water splitting at the bipolar itnerface of an anion exchange membrane (AEM) and low permeable soil possessing a significant net cation exchange capacity (CEC). The free pore solution is absent due to the electroosmotic flow towards the cathode, which is caused by the electromigration of cations on the surface of the soil.

 


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Fig. 4. Accelerated water splitting at the bipolar interface of a cation exchange membrane (CEM) and low permeable soil possesing a significant net anion exchange capacity (AEC). The free pore solution is absent due to the electroosmotic flow towards the anode, which is caused by the electromigration of anions on the surface of the soil.

 


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Fig. 5. Diagram of electrochemical testing cell.

 


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Fig. 6. Detail of ion exchange membrane sandwich. (typ.) = typical measurement.

 


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Fig. 7. Cell configuration. AEM = anion exchange membrane; CEM = cation exchange membrane; DW = deioinized water.

 


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Fig. 8. Experimental setup.

 


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Fig. 9. Pore diameters for dry samples of IONAC with and without Ottawa sand and talc.

 


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Fig. 10. pH values in the ion exchange membrane sandwiches for mixtures of bentonite clay and Ottawa sand.

 


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Fig. 11. pH values in the ion exchange membrane sandwiches for mixtures of talc clay and Ottawa sand.

 


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Fig. 12. pH values in the ion exchange membrane sandwiches for mixtures of IONAC resin and Ottawa sand.

 


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Fig. 13. pH values in the ion exchange membrane sandwiches for mixtures of IONAC, talc, and Ottawa sand.

 


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Fig. 14. pH profiles for long-term experiments with a low permeable mixture comprised of 10% bentonite and 90% Ottawa sand.

 





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