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  <titleInfo>
    <title>Land evaluation and crop suitability rating of the acid sulphate soils of Kuttanad for sustainable land use planning</title>
  </titleInfo>
  <name type="personal">
    <namePart>Beena V I</namePart>
    <role>
      <roleTerm authority="marcrelator" type="text">creator</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Manorama Thampatti K C(Guide)</namePart>
  </name>
  <typeOfResource>text</typeOfResource>
  <originInfo>
    <place>
      <placeTerm type="code" authority="marccountry">xx</placeTerm>
    </place>
    <place>
      <placeTerm type="text">Vellayani</placeTerm>
    </place>
    <publisher>Department of Soil Science and Agricultural Chemistry, College of Agriculture</publisher>
    <dateIssued>2005</dateIssued>
    <dateIssued encoding="marc">9999</dateIssued>
    <issuance>monographic</issuance>
  </originInfo>
  <language>
    <languageTerm authority="iso639-2b" type="code">und</languageTerm>
  </language>
  <physicalDescription>
    <form authority="marcform">print</form>
    <extent>196</extent>
  </physicalDescription>
  <abstract>An investigation was carried out at College of Agriculture, Vellayani during 
2001- 2004 to delineate acid sulphate soils of Kuttanad and to develop sustainable 
land use plan for the area based on land evaluation and crop suitability rating with the 
help of GIS technology. The study consists of generation of detailed soil maps of 
acid sulphate soils of Kuttanad, various thematic maps of acid sulphate soils of 
Kuttanad, interpretation of soil maps, qualitative and quantitative evaluation of land 
use systems of the area, and development of a sustainable land use model taking into 
account the climatology, productivity and socio- economic constraints of the area. 
Kuttanad is a lowlying deltaic region lying 0.6 to 2.2 m below mean sea level. 
The reconnaissance soil survey of the area was conducted according to the principles 
envisaged in IARI (1970). Two profile pits were dug from each series identified and 
morphological features were described and surface as well as subsurface samples 
were drawn for detailed laboratory examination. Soil classification was done based 
on field survey, soil correlation and laboratory investigation and soil map of acid 
sulphate soils of Kuttanad was prepared based on GIS technique. Land capability 
classification was done based on inherent soil characteristics, degree of limitations 
etc. Soil site suitability classificatio~ was done to find the suitability of different 
crops in the region and fertility capability classification was also done for evolution 
of sustainable agricultural management. These soils were thoroughly evaluated to 
study the present land use, its suitability and to suggest alternate land use plan for the 
area. 
 
The morphological and physico- chemical characteristics of the area showed 
great degree of variation. The soils were deep with a hue of7.5 YR to 10 YR, sticky 
and plastic, angular blocky to sub angular blocky in structure with textural variation 
from sandy to clayey with random deposits of lime shells and humus. Presence of 
faint to prominent reddish yellow or brown mottles in most of the soil layers. Some 
of the special characteristics observed were partially burned wooden logs and reddish 
brown root channels. 
The soils were extremely acidic with high organic carbon content. The CEC, 
ECEC and available nutrients except phosphorous were high for these soils. Due to P 
fixation, phosphorous deficiency is widespread. However the base saturation was 
below 50 per cent. 
As per USDA classification, the entire study area was classified under the 
order Entisols, with suborder Aquent, great group Sulfaquent, subgroup Typic 
Sulfaquent with six soil series viz., Ambalapuzha, Purakkad, Thotapally, Thuravur, 
Kallara and Thakazhi. As per FAO classification, these soils were included under 
Thionic Fluvisols. 
The region enjoys a humid tropical climate. Based on soil mapping of the 
area it is revealed that acid sulphate soils of Kuttanad cover an area of 14277.51 ha 
comprising of six soil series. Kallara series occupied the largest area of 6860.17 ha. 
The soils of the region were deep, poorly drained loamy soils in control section and 
are very gently sloping with slight erosion. 
Land capability classification of the area showed five soil senes ViZ., 
Ambalapuzha, Purakkad, Thuravur, Kallara and Thakazhi covenng an area of 
13099.60 ha came under the class IV sw. The Thotapally series was grouped under 
 
III sw. While considering the soil site suitability for paddy, Thotapally and Thuravur 
series come under subclass S2 xf ie these are moderately suitable for paddy 
cultivation with limitations due to fertility and pH. For coconut cultivation, all the 
series except Thuravur are grouped under S2 xf. Soil site suitability for mango 
cultivation revealed that Ambalapuzha, Purakkad and ThotapalJy senes are 
moderately suitable with limitations due to excess wetness, low pH and fertility 
limitations. As per Fertility Capability Classification, the soils belong to the units 
Lgac, Lgac, LCgac, Cgaics, Lgac and LCgaic respectively for Ambalapuzha, 
Purakkad, Thotapally, Thuravur, Kallara and Thakazhi series. The modifiers that are 
relevant to the acid sui phate soi I condition are "g" which defi nes wet land soi Is, "a" 
aluminium toxicity, "i" denotes high P fixation by iron, "c" denotes the acid sulphate 
soil condition. 
Socio - economic, cultural and ecological traits were also taken in to account 
along with land, crop and climatological characteristics of the area for the 
development of a probable land use model. Based on the study the land use models 
that can be suggested for the area are rotational farming involving paddy, fish and 
livestock. 

</abstract>
  <note>PhD </note>
  <classification authority="ddc">631.4 BEE/LA</classification>
  <identifier type="uri">http://krishikosh.egranth.ac.in/handle/1/5810015051</identifier>
  <location>
    <url>http://krishikosh.egranth.ac.in/handle/1/5810015051</url>
  </location>
  <recordInfo>
    <recordCreationDate encoding="marc">140128</recordCreationDate>
    <recordChangeDate encoding="iso8601">20221001161232.0</recordChangeDate>
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