Plants that are shallow rooted need to be able to cope with a greater fluctuation of water and temperature around the roots, although Smith & Grant (1986) suggest that the shallow roots enable plants to access rainwater sooner than others.
Similarly, the shallow roots also allow plants to access minerals from the ash of fires. However, Mitlöhner (1999) suggests that a high fire frequency may change the soil solution, particularly of the upper soil layers by changing the osmotic potential, that plants may later be unable to obtain sufficient water.
The findings of Timberlake &
Calvert (1993) show that the rooting strategy may be influenced by
soil. Rooting systems of Terminalia sericea in Kalahari sand
extended to lower lying soil layers than in heavier soils. This is
possibly due to the faster infilltration of water to lower soil layers
in loose sand.
Species |
depth (cm) |
depth (cm) |
Reference |
Baikiaea plurijuga |
|
|
Timberlake & Calvert 1998 |
Baphia masaiensis |
|
|
Timberlake & Calvert 1998 |
Burkea africana |
|
|
Rutherford 1983 |
Combretum apiculatum |
|
|
Timberlake & Calvert 1998 |
Combretum colinum |
|
|
Timberlake & Calvert 1998 |
Combretum zeyheri |
|
|
Timberlake & Calvert 1998 |
Guibourtia coleosperma |
|
|
Timberlake & Calvert 1998 |
Lonchocarpus capassa |
|
|
Timberlake & Calvert 1998 |
Ochna pulchra |
|
|
Rutherford 1983 |
Pterocarpus angolensis |
|
|
Vermeulen 1990 |
Schinziophyton rautanenii |
|
|
Timberlake & Calvert 1998 |
Strichnos pungens |
|
|
Timberlake & Calvert 1998 |
Terminalia sericea |
|
|
Rutherford 1983 |
See also: |
The importance of soil texture for root development |