Filling the Gaps - From Microscopic Pore Structures to Transport Properties In Shales 2016
DOI: 10.1346/cms-wls-21.18
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Monitoring water-chemistry evolution in the bentonite buffer using magnets: Effects of corrosion on buffer stability

Abstract: Bentonite has been chosen as a buffer material by several national nuclear-waste management companies because of its swelling capacity and low water permeability, and because it retards the transport of radionuclides and corrosion products toward the geosphere. The aim of the present study was to develop a magnetic material that has the ability to detect changes in groundwater compositions in an underground nucleardeposit facility through variation in its magnetic properties with time.The present study has inv… Show more

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(4 citation statements)
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“…The degradation of magnetic properties and signatures caused by fluid-induced corrosion of the different magnets are quantified to allow an evaluation of the sensitivity of magnetic monitoring with fluid ingress and saturation. We also summarise the effects of magnet corrosion on the bentonite matrix in order to understand if such corrosion might have a negative impact on the swelling properties of the bentonite buffer in a GDF [17].…”
Section: Experimental Program and Designmentioning
confidence: 99%
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“…The degradation of magnetic properties and signatures caused by fluid-induced corrosion of the different magnets are quantified to allow an evaluation of the sensitivity of magnetic monitoring with fluid ingress and saturation. We also summarise the effects of magnet corrosion on the bentonite matrix in order to understand if such corrosion might have a negative impact on the swelling properties of the bentonite buffer in a GDF [17].…”
Section: Experimental Program and Designmentioning
confidence: 99%
“…The clay matrix evolution in the NdB experiments has been addressed in [17], which showed that the clays in close contact with intensely corroded magnets reacted in saline solutions are characterised by weak and broad powder X-ray diffraction (PXRD) peaks that most likely reflect low-temperature dissolution/reprecipitation. Such broad and weak peaks are produced by a combination of fine particle size and poor crystallinity with complex or random interstratification within the clay.…”
Section: Bentonite Response and Evolutionmentioning
confidence: 99%
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