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Fig 1.

Map showing the locations of studied area of Dabaoshan Mine.

(● represented the sample sites; S0 was tailings impoundment; the S1 to S11 located in the Hengshi River affected by AMD; C1 to C3 were control sites located in the tributaries).

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Fig 1 Expand

Table 1.

Adapted 7-steps sequential extractions sequences developed for this study.

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Table 1 Expand

Fig 2.

The variation of heavy metals concentration in Hengshi River.

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Fig 2 Expand

Fig 3.

Activity of Fe3+ relative to pH (Solubility lines are as follows: goethite (log aFe3+ = 1.4-3pH), ferrihydrite (logaFe3+ = 4.3-3pH), and schwertmannite (log aFe3+ = 2.83–2.6pH), jarosite (log aFe3+ = -2.5–1.67 pH)).

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Fig 3 Expand

Table 2.

Percentage of iron removed from synthetic minerals in each step of adapted 7-steps sequential extractions.

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Table 2 Expand

Fig 4.

SEM images of sediment samples before extraction (Sh: schwertmannite; Jt: jarosite; Gt: goethite; Fh: ferrihydrite; Gp: gypsum; (The scale of all figures is the same)).

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Fig 4 Expand

Fig 5.

Sequential extractions of sediment samples from sampling sites (S0-S11).

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Fig 5 Expand

Fig 6.

DXRD and semi-quantitative XRD patterns of sediment samples.

((a) and (b) DXRD patterns refer to samples S0 and S1; (c) and (d) refer to the mixture of NaCl with Sh and Fh; (e) and (f): Semi-quantitative XRD patterns of samples S7 and S8; the Sh: schwertmannite; Fh: Ferrihydrite).

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Fig 6 Expand

Fig 7.

The content of heavy metals in the precipitates (A triplicate analysis was performed and the relative standard deviations were below 5%).

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Fig 7 Expand

Fig 8.

Comparison of heavy metals contents in each extract phase of sample S7 (A triplicate analysis was performed and the relative standard deviations were below 5%).

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Fig 8 Expand

Table 3.

Correlation coefficients calculated for the elements in the sediment samples.

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Table 3 Expand