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Samples with lower TDS values fall slightly below the equimolar line.
Samples with lower (HPL-1), standard (STDHPL), and higher (HPL-2) porosity HPL were prepared.
The higher concentration of fluoride is noted in the samples with lower EC (Fig. 7).
In core samples with lower permeability, water cannot fully penetrate the pore throats and remove the formed deposits.
The samples with lower porosity and water absorption exhibited less strength loss due to wet dry cycles.
14C concentrations of samples with lower CFCs were measured, and corrected for addition of 14C-free dissolved inorganic carbon.
Evaluations based on an independent validation sample set showed that the addition of samples with lower representativeness generally led to a decrease of root mean square error (RMSE).
Samples with lower moisture contents exhibited typical thawing characteristics of solutions with phase change drawn out in a wider temperature range.
Samples with lower ratios indicate additional HCO3− input from albite mineral weathering, rather than from Ca2+ and Mg2+ production reactions alone.
As in the case of samples with lower ABET, the micropore size distribution taken from CO2 adsorption agrees with pore size distribution calculated from N2 adsorption.
The samples with lower resistances (up to 1 MΩ) were measured on the commercially available multimeter UNI-T 83 (Uni-Trend Group Limited, Kowloon, Hong Kong).
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