Experimental conditions

Sorbing materials

Aquatic medium

K_d Values (L/kg)

Metal initial concentration

References

K_d values were calculated directly from the retardation factor (R) and soil properties.

loamy sand media

500

Mean C₀(μg/L)-(68)

(Behbahani et al., 2020)

Batch method (solid-solution ratio: 1:20; pH: 7.5 - 8.55; contact time: 8 h)

River sediments (BRS1)

Milli-Q water

1.32

(Borah et al., 2018)

Batch method (solid-solution ratio: 2:20; contact time: 24 h)

Soil

Water

1.38 - 21.6

(Kandakji et al., 2015)

Batch method

profile soil

10³ - 10⁴

(Yuan et al., 2017)

Batch test

Sediment

Distilled water

3.59

(Yavar Ashayeri & Keshavarzi, 2019)

Batch method

Lake sediments

deionized water

3.4 - 4.5

(Li et al., 2017)

Batch experiment (solid-solution ratio: 1:12.5; contact time: 1 h; 25˚C)

Aquifer sediment

5.08 - 17.3

(Guo et al., 2014)

Batch experiment (solid-solution ratio: 1:2; contact time: 72 h)

Soils

25 - 108

4 - 358 mg/kg

(Mrdakovic Popic et al., 2014)

Batch method

Original JL soil

3.89 - 31.62

7.5 - 14162.7 pmol/cm³

(Wang et al., 2018)

Stream bed sediment

3 < K_d

(Sedeño-Díaz et al., 2019)

Batch experiments in an open laboratory, 7 days at 25˚C

Holocene aquifer sediments

Deionized water

30 - 39

(Chakraborty et al., 2014)

Batch experiment (solid-solution ratio: 0.5:10; contact time: 24 h; 25˚C)

Sediment

1474 - 4255

(Cui et al., 2021)

Batch method

Sediment

130

(Desbarats et al., 2015)

Batch experiment (solid-solution ratio: 1:10; contact time: 24 h; 25˚C)

Amended soil with HFO particles (first harvest)

Deionized water

1.7 × 10³ - 5.4 × 10³

(Huo et al., 2018)

Amended soil with HFO particles (second harvest)

1.9 × 10³ - 5.4 × 10³