SOIL
TYPES
The soil
map of Kerala is compiled from the map obtained from the Soil Survey Unit of
the Department of Agriculture,
Coastal Alluvium
(Tropopsamments Tropofluvents)
This
soil has originated from recent deposits, predominantly marine, with some
fluvial sediments along the coast line. The soil is immature with high sand content and low water
holding capacity with pH value less than 6.5 in most of the areas.
Riverine Alluvium
(Tropofluvents - Eutropepts - Dystropepts)
This
type of soil, developed along river valleys, occurs throughout the State
cutting across the extensive laterite soils. The soil is very deep with surface
texture ranging from sandy loam to clay. It is very fertile having high water
holding capacity and plant nutrients which are regularly replenished during
floods. It supports cultivation of paddy, arecanut, pepper, tapioca and a wide
variety of vegetables.
Red Loam (Tropudalfs -
Eutropepts)
This
occurs mainly as colluvial deposits in isolated patches in foothills and
hillocks being associated with laterites. The red colour is due to the presence
of iron oxides. The soil being highly porous and friable is not fertile.
Lateritic Soil
(Eutrorthox - Haplorthox -Dystropepets)
This
soil, a typical weathering product under humid tropical conditions, occurs
throughout the State. It shows the development of AB(c) profiles, which are deep
to very deep. The B horizon is well developed in most cases with abundant
ferruginous and quartz gravels. Though this soil, in general, is acidic and
poor in available nitrogen, phosphorus, potash and organic matter, it is well
drained, widely cultivated and responds to management practices. A variety of
crops like coconut, tapioca, rubber, arecanut, pepper, cashew etc, can be
successfully grown by the proper application of fertilizers and irrigation.
Greyish Onattukara
(Troporthents)
This
soil with its characteristic grey colour occurs in the districts of Alleppey
and Quilon. It is generally coarse grained, highly porous with limited capacity
for retaining water and fertilizers. These soils are acidic and are extremely
deficient in major plant nutrients. Additions of sufficient organic matter and
irrigation facilities improve the water holding capacity for cultivation of
paddy, tapioca and other seasonal crops in addition to coconut.
Acidic Saline
(Tropaquepts -FIuvaquents)
This
soil is found mainly in the Kuttanad region. Developed under hydromorphic
conditions, these include the Kari soil (black soil with high organic
content developed in low lying water logged areas), kayal soil (in
reclaimed areas with high clay content) and karappadam soil (soil along
river courses with high silt content). Salinity and waterlogging have put
limitations to crop culture but with careful management, these soils can
sustain good crop production. Paddy is successfully grown in this soil.
Brown Hydromorphic Soil
(Tropaqualfs -Tropaquepts)
This is
commonly found in areas of wetlands and is moderately rich in organic matter,
nitrogen and potash and deficient in lime and phosphate. Acidity is a problem
in some places. For poorly drained areas, provision for drainage is essential.
Hydromorphic Saline Soil
(Tropaqualfs)
The
saline soil of this group is observed along the coastal strip where inundation
by sea causes salinity. The problem of acidity is also observed within this
soil group in some areas.
Black Soils (Chromuderts)
Black
soil is found in the north-eastern part of Palghat district adjacent to
This
soil is developed in the eastern part. of the State within forest area on the
weathered crystalline rocks. The upper layer is highly enriched with organic
matter derived from the decomposed leaves. Due to the presence of excessive
organic matter, the soil is dark reddish brown to black in colour. It is rich
in nitrogen, but poor in bases. The soil is quite fertile under forest cover
and promotes prolific undergrowth. In denuded areas, protection against soil
erosion is recommended.
The
preceding description of the soils of Kerala is quite generalised. The State is
yet to be covered by detailed soil survey. At present, these broad soil groups
have been identified in terms of their principal characteristics.