Table 3 Exponential curve equations of the dFe and HS concentrations using data obtained from a previous study and our results.

From: Capacity of humic substances to complex with iron at different salinities in the Yangtze River estuary and East China Sea

Species

Study Area

Fitted Equation

R-square (R2)

Salinity range

Removal rate

Number of points

Data Sources

dFe

Ob River estuary

y = 552.73*exp(−0.16 S) + 8.50

0.9948

1.3–34

99%

7

ref. 40

dFe

Yenisey River estuary

y = 240.99*exp(−0.15 S) + 3.64

0.9996

0–34

99%

7

ref. 40

dFe

Galveston Bay

y = 418.23*exp(−0.31 S) + 5.40

0.9985

0–33.9

97%

9

ref. 47

dFe

Millica River estuary

y = 24379.0*exp(0.32 S) + 757.2

0.9951

0–29

99%

16

ref. 29

dFe

Zaire River estuary

y = 232.84*exp(−0.14 S) + 16.61

0.9825

0–31

97%

8

ref. 46

HS

San Francisco Bay

y = 7190.3*exp(−0.66 S) + 41.33

0.9892

4.0–34

94%

5

ref. 51

dFe

Yangtze River estuary

y = 175.28*exp(−0.28 S) + 9.86

0.9939

0–34

96%

20

This study

FA

Yangtze River estuary

y = 2044.5*exp(−0.16 S) + 422.0

0.9936

0–34

79%

20

This study

HA

Yangtze River estuary

y=1503.0*exp(−0.19 S)+305.2

0.9950

0–34

84%

20

This study

  1. “S” represents the salinity of the estuary and “y” represents is the dFe/HS/FA/HA content remaining at salinity S.