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The environmental heterogeneity within the M area was evaluated using the Spatial Distribution Modeling SDMToolbox 1.1c in ArcGIS41.
Furthermore, the overburden protective capacity in the area was evaluated using longitudinal unit conductance (Si) derived from the first-order parameters obtained from the VES results (Henriet 1976; Oladapo et al. 2004).
The hydrogeochemistry of groundwater in the study area was evaluated using the concentrations of major cations (Ca2+, Mg2+, Na+ and K+) and anions (({text{HCO}}_{3}^), ({text{SO}}_{4}^{2 - }) and Cl−) in meq/l.
The geochemical evolution/hydrochemistry of groundwater in the study area was evaluated using the concentrations of major cations (Ca2+, Mg2+, Na+ and K+) and anions (HCO3 −, SO4 2−, and Cl−) in meq/l.
Sprouting area was evaluated using the Image Pro program.
The glial scar area was evaluated using an anti-GFAP antibody (1 500, DAKO, Queluz, Portugal).
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In the first step of the approach, the main and interactive effects of three hydration variables on sorbent surface area were evaluated using a full factorial design.
Soil classification, soil amplification, natural soil predominant period, resonance phenomena and liquefaction potential of the study area were evaluated using borehole data and microtremor measurements.
The overall extraction rate coefficients defined by the product of the interfacial extraction rate constant and the specific interfacial area were evaluated using the experimental data and ranged from 3.5 × 10−3 to 6.7 × 10−3 s−1, which was close to the value of 3.4 × 10−3 s−1 obtained by batch extraction.
Measurements of the wound area were evaluated using the Image-J program (National Institutes of Health).
Associations between log-transformed LTL and continuous MD measurements (volume and area) were evaluated using linear regression models adjusted for age and body mass index.
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