Method to compare water content values determined on the basis of different oven-drying temperatures

The dry mass of a test specimen generally decreases for higher oven-drying temperatures as a result of small amounts of residual pore water evaporating from the void space (t < 100DGC), and some slight charring or slaking of the solid particles (t > 85DGC). Hence the apparent water content det...

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Veröffentlicht in:	Géotechnique 2005-05, Vol.55 (4), p.329-332
1. Verfasser:	Kelly, B C O
Format:	Artikel
Sprache:	eng
Schlagworte:	Earth sciences Earth, ocean, space Engineering and environment geology. Geothermics Engineering geology Exact sciences and technology Soils Surficial geology
Online-Zugang:	Volltext
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