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AGRICULTURE SOIL FERTILITY MANAGEMENT IN SIKKIM


AGRICULTURE SOIL FERTILITY MANAGEMENT IN SIKKIM

The soil management is the primary function of sustainable land use to satisfy the human needs in such a way that the subsystems of land environment are put to most beneficial uses consistent with their inherent potentialities, while at the same time preserving its qualities for future use.

Soil is directly related to the health of individuals and therefore to the health of nation. In fact in agriculture soil in agriculture soil and water must be considered together if basic resources of land and water are neglected it is bound to have serious economical, social and political repercussions on the community and nation.

Although, the need of good soil fertility status for increase production was realized long ago and local method like organic manure application and use of plant residues as much etc. were developed by the ferment. The use of inorganic fertilizer has received attention only in the last 4 decades. The complexity and magnitude of soil fertility research have assumed much greater dimensions these days due to rapid change from subsistence agriculture to adoption of multiple and intensive cropping for augmenting crop production as a result of introduction of high yielding, short duration, an photo insensitive varieties of important crops. This is causing faster and greater depletion of soil fertility. Severe depletion is soil fertility is bound to occur if suitable steps are not taken simultaneously to restore it through application of balanced organic fertilizer in conjunction with organic manure.

General Description

The trend of mountain system is in general east-west direction, however chief ridges run in a more or less North South direction. The of Sikkim broadly grouped into 5 physiographic Zones based on geomorphology are give in (Table) with their characteristics. The steeply sloping side slope (>52%) cover an area of 43 per cent and soil erosion is the major cause of land degradation and often subjected to land slide or land slip. The National Bureau of Soil Survey and Land Use planning (NBSSLUP), regional centre, Calcutta surveyed the soil of Sikkim and classified the soil in to 3 texonomic orders of Inceptisol (33.4%), Entisols (43%) and Mollisols (23 6%) and 12 great subgroups on the basis of nature and properties of soil (Anonymous 1992). The depth of soil at different places varies considerably because of differences in physiographic position and slope. The fertility of soil also depends much on the geological formation of the rocks.

 

Table 1. physiographic classification of Sikkim soils (Anonymous 1992)

Physiographic

Zone/sub zones % slope

Soil depth

% geographical area

   Land Use

  Constraints

1

soils on summit and Ridge Top
Steep sloping

Moderate steep sloping

Moderately sloping

>30




<30


<15

Deep




Deep to moderate

Deep

161




261


0 28

Forest (D) paddy and maize Temperate Forest (D) cereals Paddy (D) temperate forest

APE. CT. SA




E. SD. SSt


E. SSt

2

Soils of side slope of Hills very sleepy

Thermic soil temperature regime

Isomesic soil temperature regime

Escarpments (Thermic soil temperature regime)

Steeply sloping side hill

Thermic soil temperature regime

Isomesic soil temperature regime

Cryic soil temperature regime moderately steep sloping side hill

Thermic soil temperatue regime


>50



<50




Very steep




33-50




15-30





Moderate deep to deep moderately shallow to

Moderately deep



Moderately deep to deep



Moderately shallow to deep

Shallow to Moderately deep
Shallow to moderately shallow

shallow





Moderately deep to deep






14.43




4.59




5.76




13.50


12.83






11.06






2.21





Temperate forest and maize

Conifers and junipers (D) cereals in patches Temperate Forest (D) maize

Paddy and maize (D) temperate forest

conifers and Alpine pasture (D) careal in patches





Alpine pasture




Paddy, maize, ginger, fruits tropical and temperate






A.E.St


A. SD. St. E





E.A




A.E. st




SD, E. St





SD. St






E.A

3

Soils on Valley Moderately steep sloping valley

Thermic soil temperature regime Isomesic soil temperature regime

15-30

Moderately deep to deep


Moderately shallow to moderately deep

0.77



0.45

Forest careal



Cereals potato temperate fruit forest

E. st




A. St. E.

4

Soils on Cliff and precipitous slope Thermic soil Temperature regime Isomesic soil temperature regime

Shallow Extremely shallow

2.35
9.85

Permanent fallow Barren land  

SD. E SD.E

5

Soil on Glacial Drift Moraines and Boulders Isomesic soil temperature regime

Moraines and boulders

3.59

Forest

SD. St. E