Abstract
Suggests that with pH increasing from 2 to 8, the stepwise exchange of zinc occurs on δ-MnO2 and montmorillonite in their mixture. The stepwise exchange and the heterogenity of the binding sites on δ-MnO2 surface are the reason for the non-additive exchange. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 261-265 |
| Number of pages | 5 |
| Journal | Acta Oceanologica Sinica |
| Volume | 7 |
| Issue number | 2 |
| State | Published - 1988 |
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