As can be seen for moisture a sharp wetting front is observed. However, the Na profiles clearly lag behind the moisture profiles. Almost no Na is observed near the wetting front. This is due to the interaction of the Na ions with the pore surface.Figure 1: The moisture (+) and Na profiles ( ) measured during the absorption of a 4 M NaCl solution. The dashed curves through the points are meant as guides to the eye, whereas the times are given as an indication of the elapsed time.
R.Valckenborg, L. Pel, K. Kopinga, Transport and relaxation of Na ions in porous materials, Proceedings of the 15th European Experimental NMR Conference, 12-17 June, Leipzig, Germany (2000)
L. Rijniers, L. Pel, K. Kopinga, Transport and relaxation of Na ions in porous materials, Proceedings of the 15th European Experimental NMR Conference, 12-17 June, Leipzig, Germany (2000)
L. Pel, K. Kopinga and E.F. Kaasschieter, Saline absorption in calcium silicate brick, IBPC-2000, Eindhoven, The Netherlands (2000)
L. Pel, K. Kopinga, H. P. Huinink and E. F. Kaasschieter, Saline absorption in calcium silicate brick, 2 nd International RILEM workshop on testing and modelling the chloirde Ingress into Concrete, 11-12 Sept Paris (2000)
L. Pel, H.Huinink, K.Kopinga, L.A. Rijniers, E.F. Kaasschieter,
Ion transport in porous media studied by NMR, Mag. Res.
Imaging 19, 549-550 (2001)