| Display title | Chemistry:Liming (soil) |
| Default sort key | Liming (soil) |
| Page length (in bytes) | 9,693 |
| Namespace ID | 3022 |
| Namespace | Chemistry |
| Page ID | 236001 |
| Page content language | en - English |
| Page content model | wikitext |
| Indexing by robots | Allowed |
| Number of redirects to this page | 0 |
| Counted as a content page | Yes |
| Page image |  |
| HandWiki item ID | None |
| Edit | Allow all users (infinite) |
| Move | Allow all users (infinite) |
| Page creator | imported>WikiG |
| Date of page creation | 03:00, 6 February 2024 |
| Latest editor | imported>WikiG |
| Date of latest edit | 03:00, 6 February 2024 |
| Total number of edits | 1 |
| Recent number of edits (within past 90 days) | 0 |
| Recent number of distinct authors | 0 |
Description | Content |
Article description: (description)
This attribute controls the content of the description and og:description elements. | Liming is the application of calcium- (Ca) and magnesium (Mg)-rich materials in various forms, including marl, chalk, limestone, burnt lime or hydrated lime to soil. In acid soils, these materials react as a base and neutralize soil acidity. This often improves plant growth and increases the activity... |
