SOIL ASSOCIATIONS -
 DURNHILL

Soils Landcover Regional Landscapes Soils & Sustainability


DERIVATION:

Quartzites and quartzose grits.

TYPES OF PARENT MATERIALS MAPPED:

Glacial till
Glacial drift, often shallow
Cryogenic

COLOUR:

Light yellowish brown in subsoil.

TEXTURE:

Till deposits range from loamy sand to sandy clay loam but drifts are loamy sand and sandy loam often with abundant, mainly angular stones, moderate to abundant in amount.

DOMINANT LAND USE:

Arable, permanent pasture, rough grazing, some forestry.

 


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LANDFORMS:

Mainly hills, valley sides and mountains often with steep slopes being scree-covered.

SOIL CHEMISTRY:

Inherently low fertility, low pH (around pH5 in the subsoil), extremely low base saturation (<15%) and low levels of trace elements are characteristic.

SOIL PHYSICAL PROPERTIES:

Potential rooting depth is generally around less than 35cm with intense induration, an iron pan or high stone content impeding root penetration. Weak subsoil structure.

 SERIES NAME  SOIL TYPE   DRAINAGE  PARENT MATERIAL
 Aigan  Humus iron podzol  Free  Drift and till
 Aldamph  Peaty podzol  Imperfect  Drift and till
 Balloch  Peaty gley  Poor and very poor  Drift and till
 Corryhabbie  Alpine podzol  Free  Cryogenic
 Dubhain  Peaty ranker  Poor  Drift and organic
 Durnhill  Peaty podzol  Free below iron pan  Drift and till
 Durnskel  Skeletal soil  Variable  Very shallow drift
 and residual
 Ferneybrae  Humus iron podzol  Imperfect  Drift and till
 Kilbady  Noncalcareous gley (SW)  Poor  Drift and till
 Monksburn  Peaty gley  Very Poor  Pliocene (quartzite)
 gravel
 Neuchry  Peaty gley (SW)  Poor  Drift and till
 Scraulac  Subalpine podzol  Free  Cryogenic
 Windyhills  Peaty podzol  Free below iron pan  Pliocene (quartzite)
 gravels
 
Updated: 30 October 2009