Spatial and temporal moisture movement within surface-zone concrete under simulated hot climatic conditions
Abstract
The ambient environment has a significant influence on the permeation properties of the
surface and near-surface zone of concrete (i.e. the cover zone). Monitoring the water
transport properties within this region is crucial in evaluating the long-term concrete
performance for a particular exposure condition.
This research presents an experimental study of water and moisture transport within the
surface region of concrete samples with and without supplementary cementitious
materials. The samples were conditioned under two regimes representing poor and good
curing; the samples were then exposed to a simulated hot environment with a diurnal
temperature fluctuation of 20–40°C and 60% ambient relative humidity, which was
represented by ambient conditions of North Africa.
Water diffusivity (D𝜣) is a fundamental hydraulic property that is important to
characterise water transport of unsaturated concrete. However, its evaluation is
complicated, time-consuming and involves expensive equipment. Therefore, in addition
to monitoring the water movement into concrete, this study also presents initial
developments in application of discretized electrical conductivity measurements as a
relatively simple and low-cost technique to evaluate the water diffusivity of concrete
(D𝜣).
Moisture movement within the surface region was monitored using discretised electrical
conductivity measurements, which, together with gravimetric measurements, allowed
evaluation of the volumetric uptake and sorptivity of the concrete and the rate and depth
of water penetration into the concrete cover zone; it is shown that when these are
combined, the degree of saturation, effective porosity and total porosity of the surface
region could be estimated. Electrical measurement, taken at discrete depths from the
exposed concrete surface, showed that, during absorption, the penetration of water into
concrete could be modelled by a sigmoidal function. The results also showed that the
convective zone could be estimated by evaluating the electrical conductivity profile
through the surface zone prior to and after water absorption.