Soil salinization in Patagonian meadows with different grassland condition
Patagonian meadows (locally named “mallines”) are wetlands that develop in the lower parts of the landscape, were runoff water accumulates, and organic and humid soils appear, contrasting with the surrounding steppe. An internal soil moisture gradient generates different types of vegetation, dominat...
| Autores principales: | , |
|---|---|
| Formato: | info:ar-repo/semantics/documento de conferencia |
| Lenguaje: | Inglés |
| Publicado: |
2018
|
| Materias: | |
| Acceso en línea: | http://hdl.handle.net/20.500.12123/3329 |
Ejemplares similares: Soil salinization in Patagonian meadows with different grassland condition
- Spatial and temporal variation of primary production of Patagonian wet meadows
- Long-term grazing negatively affects nitrogen dynamics in Northern Patagonian wet meadows
- Is forage productivity of meadows influenced by the afforestation of upstream hillsides? A study in NW Patagonia
- Particulate organic carbon is a sensitive indicator of soil degradation related to overgrazing in Patagonian wet and mesic meadows
- Argentina: Ornamental meadow plants in the Institute of Floriculture
- Grazing intensity levels influence C reservoirs of wet and mesic meadows along a precipitation gradient in Northern Patagonia