Soil orders

Allophanic Soils [L]

Allophanic Soils have a large affinity for phosphate. Up to 30 tonnes/ha of phosphorous may be locked away in intensively farmed topsoils.

Allophanic Soils are dominated by allophane (and also imogolite or ferrihydrite) minerals. These stiff, jelly-like minerals coat the sand and silt grains and maintain a porous, low density structure with weak strength. The soils are identified by a distinctly greasy feel when moistened and rubbed firmly between the fingers. The soil is easy to dig and samples crumble easily when crushed in the hand.

Allophanic Gley, East Coast.
Allophanic Gley, East Coast.
Allophanic soil, Taranaki
Allophanic soil, Taranaki

Occurrence

These soils occur predominantly in the North Island volcanic ash and in the weathering products of other volcanic rocks. They also occur in the weathering products of greywacke and schist in the South Island high country. They cover 5% of New Zealand.

View map View map of Allophanic soils.

Physical properties

Because bulk density is low there is little resistance to root growth. Topsoils are stable and resist the impact of machinery or grazing animals in wet weather. Erosion rates are generally low except on steep slopes or exposed sites.

Chemical properties

The ability to retain phosphorous is high. Natural fertility is low.

Biological properties

Soils contain large populations of soil organisms, particularly in A horizons.

Soil groups

Soil orders are divided into soil groups based on variation in factors such as drainage status, parent material, chemical and physical properties

[LP] Perch-Gley Allophanic

Periodic wetness caused by a perched water table

[LG] Gley Allophanic

Periodic wetness caused by a groundwater table

[LI] Impeded Allophanic

Have a hard layer that impedes roots and water

[LO] Orthic Allophanic

Other Allophanic Soils