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. 2011 Jul 27;41(2):170–179. doi: 10.1007/s13280-011-0177-x

Table 2.

Changes (absolute [Δ] and percent [%]) in mean (and median) lake concentrations between the 1997 and 2007 lake surveys (n = 60). Statistical difference between surveys was assessed with the non-parametric Wilcoxon signed paired test

Variable Units Δ Change % Change Wilcoxon§
SO42− μmolc l−1 −7.6 (−12.0) −9.3 (−14.8) 0.001
nmSO42− μmolc l−1 −10.5 (−8.1) −57.6 (−46.2) 0.000
pH −0.03 (0.08) −0.60 (1.60) 0.352
Cl μmolc l−1 28.6 (30.9) 4.6 (5.4) 0.025
Conductivity μS cm−1 −1.1 (−0.6) −1.1 (−0.7) 0.763
Alkalinity μmolc l−1 5.0 (6.1) 47.3 (62.5) 0.003
Ca2+ μmolc l−1 −3.7 (0.1) −5.9 (0.2) 0.007
Mg2+ μmolc l−1 0.3 (−7.5) 0.2 (−5.6) 0.903
nmCa2+ μmolc l−1 −4.8 (−0.4) −11.8 (−1.4) 0.000
nmMg2+ μmolc l−1 −5.3 (−7.8) −22.9 (−35.9) 0.004
nmK+ μmolc l−1 −0.3 (0.0) −10.6 (2.2) 0.594
DOC mg l−1 0.7 (1.6) 13.7 (47.9) 0.054
AlT μmol l−1 −0.03 (−0.002) −1.2 (−0.1) 0.683

§Changes in lake chemistry between surveys were assumed to be statistically significant at p < 0.05. Units: 1 mol of charge (molc) is equal to 1 equivalent (eq)