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| Content Provider | Springer Nature Link |
|---|---|
| Author | Vodyanitskii, Yu. N. |
| Copyright Year | 2014 |
| Abstract | The existing geological classification of heavy metals (HMs) is not suitable for their characterization in soils. The carriers of HMs in soils differ from those in the lithosphere. These are clay minerals; iron oxides, whose composition varies between the background and urban soils; various manganese oxides; and different groups of organic substances. The mineral composition of HM carriers can vary significantly. The main iron oxides are ferrihydrite, goethite, feroxyhyte, and lepidocrocite in the background soils and technogenic magnetite in the urban soils. The different structures of manganese oxides determine their affinity for specific HMs. Metallic iron and green rust are very efficient in artificial geochemical barriers, although they act as strong reducers there. HM compounds strongly vary in soils because of the unstable conditions. |
| Starting Page | 255 |
| Ending Page | 265 |
| Page Count | 11 |
| File Format | |
| ISSN | 10642293 |
| Journal | Eurasian Soil Science |
| Volume Number | 47 |
| Issue Number | 4 |
| e-ISSN | 1556195X |
| Language | English |
| Publisher | Pleiades Publishing |
| Publisher Date | 2014-04-29 |
| Publisher Place | Moscow |
| Access Restriction | One Nation One Subscription (ONOS) |
| Subject Keyword | geological classification of heavy metals soil classification of heavy metals Geotechnical Engineering & Applied Earth Sciences |
| Content Type | Text |
| Resource Type | Article |
| Subject | Earth-Surface Processes Soil Science |
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