A study of the spatially resolved water-occupied pore size distribution in
a drying concrete cylinder is reported. Pore sizes are obtained from freezi
ng point depression of pore water for a temperature range of 0 to -40 degre
es C, assuming that the freezing point is inversely proportional to pore di
ameter. Single-point magnetic resonance imaging techniques were used to mon
itor unfrozen water content as functions of position and temperature. It wa
s observed that freezing began at -10 degrees C in the cylinder center, whi
ch had the highest moisture content, and with a further temperature decreas
e, the freezing region gradually spread to the exposed end surfaces. The ce
ntral region had a broad water-occupied pore size distribution, with pore d
iameters as large as 10 nm. The occupied pore sizes became progressively sm
aller as the moisture content decreased in proximity to the exposed surface
s. (C) 2000 American Institute of Physics. [S0021- 8979(00)02619-0].