Abstract
On the basis of anion exclusion volume measurements, the average quantities of mineral plates in soil tactoides, as well as average distance between them, were determined before and after saturation of the soil exchange complex with calcium ions. It was found that in the soils under investigation the saturation with calcium ions leads to an increase in the average quantity of mineral plates in the tactoides while the distance between them remains approximately constant. -Authors
| Original language | English |
|---|---|
| Pages (from-to) | 53-58 |
| Number of pages | 6 |
| Journal | Polish Journal of Soil Science |
| Volume | 22 |
| Issue number | 1 |
| State | Published - 1989 |
| Externally published | Yes |