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Recently, the 3-D cement hydration and microstructural development model has been modified to include the capability to predict the adiabatic temperature rise for a concrete, i.e. the temperature vs. time curve which would be obtained for a concrete maintained under adiabatic (no heat lost to the surrounding environment) conditions. As hydration occurs, the cumulative heat generated by the hydration reactions is tabulated and the heat capacity of the concrete updated. Based on these two values, the incremental temperature rise from one cycle of dissolution to the next can be calculated as:
T is the incremental change in temperature from cycle (i-1) to
cycle i, Cp(i) is the value of the heat capacity for the concrete at cycle
i, and H(i) is the cumulative heat generated by the hydration reactions through
cycle i. In addition, the equivalent real time which elapses during this
cycle of hydration is estimated using principles based on the maturity
method [2,21] and a user-supplied calibration factor relating
cycles to equivalent time at a temperature of 25oC.
Previously [1,2], the following conversion between cycles and time has been employed to calibrate model results to experimental data:
Figure 7 shows an example comparison between experimental and model predicted temperature rise, based on executing the program disreal3d with the input datafile provided in Appendix D.1. The agreement between model and experiment is quite good, particularly for times less than 30 hours, but it should be kept in mind that the user has had to supply an induction time, initial temperature, activation energy, and cycle-time conversion factor as input parameters to the program.
Figure 7: Experimentally measured and model predicted (solid line) adiabatic
temperature rise for an ordinary portland cement concrete containing
72% aggregates on a mass basis.
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Dale P Bentz