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After immersion for up to 60 days the micro- and mesoporosity increase slightly, which could be attributed to dissolution of the β-TCP phase confirmed by transmission electron microscopy.
Thus high positive loadings of sodium and potassium can also be attributed to dissolution of alkali feldspars.
This variation in chemical facies can be attributed to dissolution of salts deposited by evapotranspiration of irrigation water and subsequent mixing with groundwater.
Elevated Ca concentrations may be attributed to dissolution of limestones, Ca-rich feldspars, and potentially due to biodegradation or organic matter in upper soil horizons.
Furthermore, the overall hydrochemical profiles revealed the main hydrochemical facies as Ca Mg -HCO3 (dominant) and Na(K)-HCa Mg -HCO3 water types which can be attributedominantsolution of minerand iNathe various rocK -HCO3 in the study area.
The retardation effect of La2O3 might be attributed to dissolution of some of La2O3 (La3+) cation in the lattices of Co3O4 and/or Mn3O4 assuming that Co3O4 consisted of (2CoO and Co2O3, i.e., cobalt cations existed in di- and/or tetra-valent states.
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Hot isostatic pressing (HIP) improved mechanical properties, which was attributed to dissolution of undesirable Laves and δ-phase as well as pore closure.
Transient releases at high pH are attributed to dissolution of amphoteric secondary phases such as ferrihydrite that are inferred from saturation calculations and solid analyses to form during the conditioning interval.
This was attributed to dissolution of DNAPL mudstone aquitard associated sources at the base of the continuous gravel as well as contaminated groundwater from surrounding less permeable sand and gravel horizons draining into this permeable conduit.
The films rinsed with water revealed less fluorine, oxygen and titanium compared with those rinsed with ethanol that was attributed to dissolution of the fluoride-rich matrix by water.
The increase in dissolved arsenic concentrations is attributed to dissolution of particulate or adsorbed arsenic from the influent water, or dissolution of trace amounts of arsenic present in the original gravel substrates themselves.
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