https://www.scipedia.com/wd/index.php?action=history&feed=atom&title=Nilsson_2013b 2026-04-18T20:48:49Z Revision history for this page on the wiki MediaWiki 1.27.0-wmf.10 https://www.scipedia.com/wd/index.php?title=Nilsson_2013b&diff=177275&oldid=prev 2020-10-26T10:16:24Z

<p>Scipediacontent moved page <a href="/public/Draft_Content_295366087" class="mw-redirect" title="Draft Content 295366087">Draft Content 295366087</a> to <a href="/public/Nilsson_2013b" title="Nilsson 2013b">Nilsson 2013b</a></p> <table class="diff diff-contentalign-left" data-mw="interface"> <tr style='vertical-align: top;' lang='en'> <td colspan='1' style="background-color: white; color:black; text-align: center;">← Older revision</td> <td colspan='1' style="background-color: white; color:black; text-align: center;">Revision as of 10:16, 26 October 2020</td> </tr><tr><td colspan='2' style='text-align: center;' lang='en'><div class="mw-diff-empty">(No difference)</div> </td></tr></table>

Scipediacontent https://www.scipedia.com/wd/index.php?title=Nilsson_2013b&diff=177274&oldid=prev 2020-10-26T10:16:21Z

<p>Created page with &quot; == Abstract == A number of methods for measuring moisture transport properties of cementitious materials were compared in a series of experiments. Two OPC mortars with two w...&quot;</p> <p><b>New page</b></p><div><br /> == Abstract ==<br /> <br /> A number of methods for measuring moisture transport properties of cementitious materials were compared in a series of experiments. Two OPC mortars with two water-binder-ratios were wet cured for six months and used to produce specimens as discs with different thicknesses and diameters.&lt;br /&gt; The cup methods were easy to use, reliable and fairly rapid but need a stable, surrounding, CO2-free climate, however. Evaluating the fundamental potential PSI eliminates the derivation that adds to the uncertainty.&lt;br /&gt; Steady-state moisture distribution measurements are very time-consuming and the RH-profiling is a delicate matter. Moisture contents are scattering. Sorption experiments are very easy to perform but difficult to evaluate, because of the peculiar moisture-dependency of the diffusivity Dw and the difficulties to estimate the equilibrium conditions. Initial uniform conditions are difficult to obtain for low w/c-materials, except to initial self-desiccation.&lt;br /&gt; Sorption experiments in small steps are uncertain; the initial and final conditions are difficult to define properly.<br /> <br /> Document type: Report<br /> <br /> == Full document ==<br /> &lt;pdf&gt;Media:Draft_Content_295366087-beopen242-7999-document.pdf&lt;/pdf&gt;<br /> <br /> <br /> == Original document ==<br /> <br /> The different versions of the original document can be found in:<br /> <br /> * [http://lup.lub.lu.se/record/3800179 http://lup.lub.lu.se/record/3800179],[http://lup.lub.lu.se/record/3800179/file/3800180.pdf http://lup.lub.lu.se/record/3800179/file/3800180.pdf]<br /> <br /> * [https://lup.lub.lu.se/record/3800179 https://lup.lub.lu.se/record/3800179],[https://portal.research.lu.se/ws/files/3139440/3800180.pdf https://portal.research.lu.se/ws/files/3139440/3800180.pdf]</div>

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