Cit:Franzen.etal:2017

Aus Salzwiki
Zur Navigation springen Zur Suche springen
Autor Franzen, Christoph; Aulitzky, Martin; Pfefferkorn, Stephan
Jahr 2017
Titel Moisture transport during poultice application
Bibtex @inproceedings {Franzen.etal:2017,

title = {Moisture transport during poultice application}, booktitle = {Proceedings of SWBSS 2017. Fourth International Conference on Salt Weathering of Buildings and Stone Sculptures, University of Applied Sciences Potsdam, Germany, 20-22 September 2017}, year = {2017}, editor = {Laue, Steffen}, pages = {168-175}, month = {september}, organization = {Fachhochschule Potsdam}, publisher = {Verlag der Fachhochschule Potsdam}, note = {fulltext, conference paper}, key = {SWBSS2017}, doi = {10.5165/hawk-hhg/334}, author = {Franzen, Christoph; Aulitzky, Martin; Pfefferkorn, Stephan} }

DOI 10.5165/hawk-hhg/334
Link Datei:SWBSS 2017 Proceedings 168-175 Franzen Aulitzky Pfefferkorn.pdf
Bemerkungen in: Proceedings of SWBSS 2017 - Fourth International Conference on Salt Weathering of Buildings and Stone Sculptures. University of Applied Sciences, Potsdam, Germany, 20-22 September 2017


Eintrag in der Bibliographie

[Franzen.etal:2017]Franzen, Christoph; Aulitzky, Martin; Pfefferkorn, Stephan (2017): Moisture transport during poultice application. In: Laue, Steffen (Hrsg.): Proceedings of SWBSS 2017. Fourth International Conference on Salt Weathering of Buildings and Stone Sculptures, University of Applied Sciences Potsdam, Germany, 20-22 September 2017,Verlag der Fachhochschule Potsdam 168-175, 10.5165/hawk-hhg/334.Link zu Google ScholarLink zum Volltext

Abstract[Bearbeiten]

Water movement is the key parameter in poultice application for desalination. Water is the eluent and transport medium for the salts to be extracted from the porous substrate. While from the hypothetical point of view the dynamical processes of water ingress, dissolution of salts, transportation and precipitation seems to be well known, measured data on the water quantities at specific stages of the process are scarce. Especially, time approximations about the change in main movement direction of the water are unidentified. By experimental data we give indications to the total amount of water used with different poultice compositions and the development of the water ratio during the process until equilibrium dryness is reached. In conclusion we suggest increasing the ratio of water and probably the poultice layer thickness from cycle to cycle to increase the effective cross section stepwise.