O4 – correlations amongst these elements would reflect their common origin
O4 – correlations between these elements would reflect their prevalent origin, i.e., 0.61). The (r = 0.61). The correlations components would reflect their reflect their typical coming i.e., coming from former times, reflecting a longtime. origin, from former instances, reflecting a long SARS-CoV-2 Trimeric S Protein Proteins Gene ID residence residence time. coming from former occasions, reflecting a lengthy residence time.Figure 9. Spearman’s rho correlation coefficients. Circled values are substantial at the five level: (a) low water, and (b) higher Figure 9. Spearman’s rho correlation coefficients. Circled values are important in the five level: (a) low water, and (b) higher Figure water. 9. Spearman’s rho correlation coefficients. Circled values are important at the five level: (a) low water, and (b) higher water. water.In the high-water period, EC is strongly correlated with HCO3 – (r = 0.96), Ca2 Inside the high-water period, Na is strongly correlated with HCO33- (r = 0.96), Ca2 (r = (r = 0.81), and to a lesser extent ECis strongly correlated 0.65) (Figure-8b). These components Inside the high-water period, EC (r = 0.65) and K (r = with HCO (r = 0.96), Ca2 (r = 2 (r = 0.65) and K (r = 0.65) (Figure 8b). Na , and K are 0.81), and to Ubiquitin-Specific Protease 6 Proteins custom synthesis contribute for the boost in water salinity.0.65) (Figure 8b). These elements significantly a lesser extent Na 0.81), and to a lesser extent Na (r = 0.65) and K (r = Additionally, Ca , These elements significantly contribute towould indicate awater salinity. Additionally, Ca2,, Na,, and K are positively correlated and the improve in popular origin. drastically contribute for the enhance in water salinity. Furthermore, Ca2 Na and K are In periods of low and high water, a widespread origin. positively correlated and would indicateCl- and NO3 – ions do not show any constant positively correlated and would indicate a typical origin. optimistic correlation with other ions precise to the underground technique which include Na and Ca2 , which could reflect an external origin. Additionally, Na and SO4 2- ions, which are correlated (r = 0.61) in low water, do not present a consequent correlation coefficient in higher water (r = 0.43) and translate an enrichment from the underground medium in Na in high water within the deep aquifers. The dendrogram of variables, from the hierarchical clustering evaluation (HCA) method, allowed separation into three homogeneous groups (Figure ten). Group 1, characterized byWater 2021, 13,In periods of low and higher water, Cl and NO3 ions do not show any constant good correlation with other ions distinct to the underground method for instance Na and Ca2, which could reflect an external origin. Additionally, Na and SO42- ions, that are correlated (r = 0.61) in low water, do not present a consequent correlation coefficient in high water (r = 0.43) and translate an enrichment from the underground medium in Na in high 11 of 22 water in the deep aquifers. The dendrogram of variables, from the hierarchical clustering evaluation (HCA) method, permitted separation into three homogeneous groups (Figure ten). Group 1, characterized HCO3 – ,EC, HCO3,-, and Ca2,by formed by piezometers and SaG, located in the high EC, by high and Ca2 is formed is piezometers S11, S11P, S11, S11P, and SaG, situated inand southern ridge (Table S2 in Supplementary Materials). Group two, characterized eastern the eastern and southern ridge (Table S2 in Supplementary Supplies). Group 2, characterized by low EC values and relatively higher NO3- concentrations,piezometers S1, by low EC values and fairly high NO3 – concentrations, cons.