Management
of Soil Fertility
Introduction
Soil fertility is
concern with the inherent capacity of soil to provide nutrients in adequate amounts and in
proper balance for the growth of specified plants when other growth factors such as light
moisture and temperature and the physical condition of the soil are favourable. Soil
fertility is an aspect of the soil plant relationship viz. plant growth with reference to
plant nutrients available in soil. A fertile soil is considered to be one that produces
abundant crops under suitable environmental conditions. Only a very small fraction of the
total nutrient content of soil can be utilize by plants. To get quickly a measure of
nutrient availability following soil fertility evaluation methods used: -
biological,
visual symptoms of
nutrient deficiency or toxicity,
plant analysis, and
soil analysis.
Soil factors influencing
nutrient availability
Soil
reaction (pH) is the most important factor, which governs availability of nutrients in
soil. The pH range of 6.5 to 7.5 is the optimum for availability of most of the nutrient
availability.
The ammonifiers and
nitrifies are active at pH 5.5 to 6.0, below which nitrogen availability decreases.
Phosphorus
availability is maximum in the pH range of 6.5 to 7.5. In red and lateritic soils the
phosphate availability depends on the amount of sesquioxides. Liming of acid soils
increase phosphate availability.
Potassium availability
depends on exchangeable potassium, potassium saturation of exchange complex, CEC and pH.
Calcium and magnesium
are available in cationic form and their availability is decreased governed by the factors
which control exchange equilibrium in soil at low pH (below 6.0) their availability
decreases.
Micro Nutrient
Availability
These are available to
at low pH range. Alternate drying and heating the soil increases availability soil
manganese. Availability of boron decreases below pH 5.0 and above 7.0 but above pH 8.5 it
again increases. Availability of molybdenum increases above pH 6.5.
Maintenance of soil fertility
Nutrients are
continuously removed from the soil by crops in addition to losses by leaching and erosion.
It is therefore, essential that sound soil and crop management practices are adopted to
improve and maintain soil fertility and soil physical conditions for the purpose of
sustained crop production. The management practices that play an important role in the
maintenance and improvement of soil fertility are given below: -
Crop rotation
The benefits of a good
crop rotation are, increased organic matter, nitrogen supply and improved soil structure.
Especially deep rooted legumes or crops capable of feeding themselves efficiently at
various soil depth. Deep rooted crops increased permeability of soil at lower depths to
air and water. The other benefits of crop rotation are keeping soil under crop, control of
run off, soil erosion and efficient use of fertilizers e.g. cereals-legumes.
Manures and Fertilisers
Balance fertilization
with nitrogen, phosphorus and potassium fertilizers helps in maintaining soil fertility.
Application of organic manures and chemical fertilizers helps to improve and maintain soil
fertility, soil productivity and soil physical conditions. Soil fertility and agricultural
production can be maintain only by efficient and judicious management of nutrient addition
to the soil from external sources.
Organic manures bind
the sandy soil and improve its water holding capacity. They open the clayey soil and help
in aeration better root growth. They add plant nutrients in small percentage and also add
micro nutrients which are essential for plant growth the microbial activity is increased
which helps in releasing plant nutrients in available for e.g. bulky organic manures- FYM,
compost from organic waste, night soil, sludge, sewage, sheep folding, green manures,
concentrated organic manures- oilcakes (edible, non-edible), blood meal, fish meal, bone
meal. Organic manures should be incorporated before the sowing or planting because of slow
release of nutrients.
Chemical fertilisers
play an important role in crop production as the nutrient elements in fertiliser are
present in higher concentration and in forms which can be readily utilize by plants
directly or after rapid transformation. Their dose can be adjusted to suit the requirement
as determine by soil fertility evaluation. Fertilisers applied through straight
fertilisers- providing single nutrient or complex and mixed fertilisers- supplies two or
more nutrients. While application of fertilisers following consideration should be taken
in account-
The coarse texture
soils are poorer in available nutrients than fine texture soils. Hence, it is necessary to
apply nitrogenous, phosphatic and potassic fertilisers more frequently than in fine
texture soils. Higher the soil fertility the lower is the response of crops to fertiliser.
Soil reaction is important in selection of right type of phosphatic fertiliser. Efficient
use of fertilisers by the crop is more in the higher organic matter status of soil.
These include
temperature, rainfall, evaporation, and length of day and growing season. The rate of
nitrification is slower in a cooler climate that in a warmer climate. Hence, more
ammonical nitrogenous fertilisers will needed in a cool climate. In region of high
rainfall because of higher yield potential and leaching loss of soil and fertilisers
nutrients, require higher fertiliser. In arid region soil moisture is the limiting factor
in fertiliser use. If soil moisture is conserve efficiently fertiliser becomes very
effective.
Application of
fertiliser is by using proper methods and time is important in crop production.
Nitrogenous fertiliser should be applied in split doses while slow releasing, phosphorus
and potassium should be applied at the time of sowing or planting. Instead of broadcasting
fertilisers should be applied by placement method or through fertigation.
Reclamation of problem soils
Problematic soils viz.
acidic, saline and alkaline soils can be bring in proper condition for raising the crop
satisfactorily and economically, special measures have to be adopted. Acidic soils can be
corrected by liming. Saline and alkaline soils can be reclaimed by improving drainage
scrapping off surface soils and using gypsum, sulphur, molasses and adopting agronomical
measures viz. green manuring, adding organic manures, mulching and suitable crops
rotation.
Management of Khar Land
Along the coastal
districts extensive area have become Khar land and are unfit for economic cultivation. The
reclamation of these lands consists of 1-construction of earthen embankment above the
highest tide level to guard against the ingress of sea water. 2- Provision of sluice drain
away the excess run off water alongwith dissolved salts.3- construction of field ditches
at suitable distance in order to hasten desalinization and to channelize the water. 4-
cultivate salts resistant paddy varieties, application of liberal doses of FYM or green
manuring. |