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. 2014 Jan 14;43(7):878–890. doi: 10.1007/s13280-013-0487-2

Table 2.

Partial correlation coefficients (r x·t) for logMeHg versus log(indicated variable) when t (time) was held constant. T (temperature) above the sediment surface was not log-transformed. All individual samples except identified outliers were included in the calculations

Sediment TP TS TFe TC LOI TFe:TS TN T THg
F1 0–1 cm 0.49* 0.61* 0.23 −0.33* −0.34* −0.05 0.56* 0.40* 0.10
F1 1–5 cm 0.59* 0.63* 0.36* −0.58* −0.45* 0.12 0.58* 0.32* −0.06
F2 0–1 cm 0.13 0.21 −0.02 −0.06 −0.03 −0.18 0.25 0.27* 0.57*
F2 1–5 cm 0.45* 0.46* 0.23 −0.31* −0.40* −0.09 0.55* 0.32* 0.18
A1 0–1 cm 0.06 −0.54* −0.52* 0.82* 0.85* −0.13 0.06 0.39* 0.49*
A1 1–5 cm 0.29* −0.45* −0.12 0.20 0.52* 0.64* 0.26 0.29* 0.32*

* p < 0.05