Research Article

Comparing the Heterogeneity of Copper-Binding Characteristics for Two Different-Sized Soil Humic Acid Fractions Using Fluorescence Quenching Combined with 2D-COS

Table 2

Copper-binding parameters1 calculated by the Ryan-Weber model.

HA size fractionsPeak wavelength (nm) 𝑟 𝐹 M L (%) l o g 𝐾 M 𝐶 𝐶 M (mmol (g C)−1)

1–10 K35720.996* 4 0 . 0 ± 2 . 4 4 . 9 1 ± 0 . 0 6 0 . 6 3 ± 0 . 2 9
45121.000* 7 . 2 ± 6 . 3 5 . 7 0 ± 0 . 0 3 1 . 3 3 ± 0 . 1 4
46230.999* 6 . 3 ± 0 . 7 5 . 8 6 ± 0 . 0 7 1 . 1 7 ± 0 . 0 9
46720.999* 5 . 6 ± 0 . 5 5 . 8 6 ± 0 . 0 5 1 . 5 6 ± 0 . 2 9

>100 K37620.953* 5 9 . 7 ± 1 . 5 6 . 4 8 ± 0 . 5 2 0 . 6 7 ± 1 . 2 2
46030.999* 1 5 . 7 ± 0 . 9 5 . 9 6 ± 0 . 0 8 1 . 1 2 ± 0 . 3 2
46420.999* 1 4 . 5 ± 0 . 8 5 . 9 7 ± 0 . 0 7 1 . 1 2 ± 0 . 2 7

1Correlation coefficients of predicted versus observed fluorescence intensity ( 𝑟 ), relative percentage of fluorescence intensity for copper-saturated complexes ( 𝐹 M L (%)), conditional stability constants ( l o g 𝐾 M ), and complexing capacities ( 𝐶 𝐶 M ) and fraction of the initial fluorescence corresponding to binding sites ( 𝑓 ).
2The peak wavelengths were selected based on peaks observed in the synchronous and asynchronous maps of 2D-COS in Figure 2.
3The peak wavelengths were selected based on the apparent shapes of the synchronous fluorescence spectra in Figure 1.
* 𝑃 value < 0.001.