Sentence examples for moderate positive loading from inspiring English sources

VF3 explaining 17.1% of the total variance had strong positive loadings on HCO3 and F, moderate positive loading on Na and moderate negative loading on SO4.

On the second principal component, Fe and NO3− concentrations have high positive loadings (0.867 0.903), and the concentration of Mg2+ shows moderate positive loading (0.576).

For the data set pertaining to cluster 1, VF1, which explained 47.4% of the total variance had strong positive loadings on Ca, Mg, TDS, EC and TH and moderate positive loading on Na.

The concentrations of EC, TDS, TA, TH, Na+, K+, Ca and HCO3− show high loadings (0.743 0.959), and the concentration of Cl− has moderate positive loading (0.616) on the first principal component.

The fourth component (PC4) which explained 9.05% of total variance has a moderate positive loading of Zn.

PC2 accounts for 18.6% of the total variance and moderate positive loading on Cl− and PO4 2− and negative score (moderate) with NO3 −, BOD and TC.

The moderate positive load of Fe is influenced by geological activities (Adamu et al. 2015).

The first component (PC1) accounted for 49.14% of total variance and includes strong positive loadings of pH, turbidity, alkalinity, total hardness, colour, calcium hardness, magnesium hardness, Mg2+, Ca2+, SO42−, CO32−, HCO32− and total CO2; and moderate positive load of TDS, EC, free CO2 and Fe.

The second component (PC2) explaining 20.68% of the total variance, have a strong positive loading of temperature; moderate positive loadings of TDS and Fe and weak loadings of EC.

VF2 explaining 23.3% of the total variance had strong positive loading on F, HCO3 and SO4; and moderate positive loadings on EC, TDS and Mg.

Component 2 explains approximately 14.67% of the total variance (Table 8) and has moderate negative loadings for HCO3 −, pH; moderate positive loadings for NO3 N and Mn and a strong negative loading for SiO2 (Table 7) reflecting a natural source (silicate/aluminosilicate weathering by carbon-dioxide charged water) and anthropogenic source (use of inorganic fertilizer in agricultural activities).