SOIL ASSOICATIONS -
 BALROWNIE

Soils Landcover Regional Landscapes Soils & Sustainability


DERIVATION:

Old Red Sandstone rocks, principally sandstone with some erratics of Dalradian schist

TYPES OF PARENT MATERIALS MAPPED:

Glacial till, generally water-modified
Glacial drift, generally water-modified or onto rock
Shattered rock in situ
Deeply weathered rock

COLOUR:

Distinctive reddish brown colour within subsoil

TEXTURE:

Sandy loam water-modified material within the upper 60cms overlying sandy silt loam or clay loam at greater depth. Slightly to moderate stony.

 

DOMINANT LAND USE:

Arable, some forestry and limited recreation.



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LANDFORMS

Undulating lowland and foothills with gentle or moderate slopes, all landforms generally free
from rock outcrop.

SOIL CHEMISTRY:

Moderately acidic with low or medium percentage base saturation in subsoil but high in
fine-textured parent material. Low total phosphorus in subsoil.

SOIL PHYSICAL PROPERTIES:

35-60cm depending on thickness of water-modified material or presence of rock.
Till compact at depth and lacks structure.

 
 SERIES NAME  SOIL TYPE  DRAINAGE  PARENT MATERIAL
 Aldbar  Podzol and humus iron podzol  Free  Till
 Balrownie  Brown forest soil with gleying  Imperfect  Till often
 water-modified
 Balrowskel  Skeletal soi  Variable  Very shallow drift
 Buchanyhill  Brown forest soil  Free  Deeply weathered rock
 and till onto rock
 Dunblane  Brown forest soil  Free  Till
 Findowrie  Peaty gley (SW)  Very poor  Till often
 water-modified
 Hayston  Humus iron podzol  Free  Weathering sandstone
 Kippendavie  Brown forest soil with gleying  Imperfect  Till
 Liff  Brown forest soil with gleying  Imperfect  Colluvium
 Lour  Noncalcareous gley  Poor  Till often
 water-modified
 Muirhead  Podzol and humus iron podzol  Imperfect  Till
 Reedie  Brown forest soil  Free  Till often
 water-modified
 Sheriffmuir  Peaty gley (SW)  Poor and very poor  Till
 Shindour  Peaty podzol  Free  Till
 Tullibardine  Peaty podzol  Imperfect  Till
Updated: 30 October 2009