III. III. In high-water periods (Figure 11b), the F1 axis, which
III. III. In high-water periods (Figure 11b), the F1 axis, which presents 44.31 ,high-water periods (Figure 11b), the F1 axis, which presents (0.75), K (0.73), and In is SB 271046 Technical Information positively correlated with EC (0.94), HCO3 – (0.97), Ca2 44.31 , is positively (0.72) and negatively correlated with nitrates (- Na correlated with EC (0.94), HCO3- (0.97), Ca2 (0.75), K 0.69), potentially Safranin Formula arising in the use (0.73), and Na (0.72) and negatively of fertilizers for nitrates (-0.69), potentially arising from is anuse of fertilizers dissolution agricultural production. This grouping the indicator of the for agriculcorrelated with of silicate minerals. The F2 axis positively correlated with Mg of silicate minerals. The tural production. This grouping is an indicator with the dissolution two (0.68) and negatively correlated with S04 2- (-0.52) and Cl- (-0.59). On F2, the clustering reflects the anthropic influence on the groundwater mineralization. The three clusters are still differentiated. Nevertheless, the electrical conductivity played a major function in the reclassification of those clusters concerning the high-water period by bringing S1CN and S1CNP into cluster 1 and S5 into cluster two.Water 2021, 13,F2 axis is positively correlated with Mg2 (0.68) and negatively correlated with S042- (-0.52) and Cl- (-0.59). On F2, the clustering reflects the anthropic influence around the groundwater 12 of 22 mineralization. The 3 clusters are still differentiated. Nevertheless, the electrical conductivity played a major role within the reclassification of those clusters regarding the high-water period by bringing S1CN and S1CNP into cluster 1 and S5 into cluster 2.Figure 11. Principal component analysis (PCA) of groundwater: (a) low water and (b) higher water; on the left, the projection Figure 11. Principal component analysis (PCA) of groundwater: (a) low water and (b) higher water; on the left, the projection of variables on the F1 2 plane; around the proper, the projection of men and women around the F1 2 plane. of variables around the F1 2 plane; around the right, the projection of folks on the F1 2 plane.3.two.4. Groundwater Hydrochemical Facies three.2.four. Groundwater Hydrochemical Facies For the duration of low-water periods, the piper diagram (Figure 12a) shows that the waters of In the course of exclusively magnesian calcic bicarbonate. Cluster II presents chloride and cluster I are low-water periods, the piper diagram (Figure 12a) shows that the waters of cluster I are exclusively magnesian calcic bicarbonate. Cluster II presents chloride initially sulfate alcium agnesium facies and calcium agnesium bicarbonate facies. The and sulfate alcium agnesium facies and calcium agnesium bicarbonate facies. The first facies may be the most abundant, reflecting waters beneath the anthropic influence. Cluster III is facies would be the most abundant, reflecting waters beneath bicarbonate influence. Cluster III is shared nearly equally between calcium agnesiumthe anthropicand sodium otassium shared just about equally water to higher water (Figure bicarbonate and sodium otassium bicarbonate. From lowbetween calcium agnesium12b), the existence in the 3 facies bicarbonate. From there’s a to high water (Figure 12b), the existence with the three facies is is noted, though low watermigration of facies in the sodium otassium bicarbonate noted, though there’s a migration of facies from the sodium otassium bicarbonate to to the calcium agnesium bicarbonate as a result of the raise in calcium ions in the water from the calcium agnesium bicarbonate on account of the in.
