Influence of the In-Stream Structure on Solute Transport in the Hyporheic Zone.

On the whole, with the increase in H and the decrease in D , the upwelling flux (4.68 × 10 −7 ~5.73 × 10 −5 m 2 ·s −1 ) and the downwelling flux (−5.20 × 10 −7 ~−5.74 × 10 −5 m 2 ·s −1 ) showed an increasing trend, and the total flux Q increased with the increase in H (9.88 × 10 −7 ~1.15 × 10 −4 m 2 ·s −1 ).

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