Tree Planting in Problem Soils - Salt affected Soils
Salt affected Soils
These soils are those in which either
the salt contents of lower horizons concentrate in or on the soil surface or
normal proportion of various cations and anions present in soil is disturbed in
a big way by excess or shortage of certain ions. This redistribution of salts
of salts in soil profile is generally caused by the rising of water table
accompanied by intensive evaporation from the surface. The saline water moves
up through capillaries and evaporates into the atmosphere while leaving the
salts on the soil surface. These salts are frequently seen in the form of thin
white crust in the saline area. This crust is quite conspicuous during winter.
It has been estimated that about 1/4 to 1/3 of our irrigated area has gone out
of production because of salinity. Product vising these areas by tree planting
is a major breakthrough.
Salinity of soils is rightly
considered as enemy number one of World’s Agriculture. In Pakistan about 16.75
million acres area (33% of cultivated land) are already salt affected to
varying degrees. It has been estimated that about 200 acres of our fertile
irrigated crop land goes out of production per day because of salinity. The
plants growing in saline or sodic soils have to face some or all of the
following problems:
Ø
Concentration of soil solution is greater than
that of cell sap in the root, which results in loss of water from the root.
Ø
The imbalance of ions in the soil solution may
have toxic effect on cell physiology.
Ø
Water drainage, root penetration and root
respiration are restricted due to deflocculation and rising water table.
The solution of above mentioned
problems is based on lowering of water table and ensuring free drainage. This
would stop the upward movement of salts. The excess salts on the soil surface
are then simply washed down into deeper layers and into the drains by repeated
heavy irrigations. The ionic imbalance and deflocculation is corrected by
liberal addition of Ca in the form of powdered gypsum and organic manuring.
This treatment cannot be extended to all the affected areas. It is thus logical
to turn to biological approach which is sample, cheap and self-perpetuating.
The following points explain the working of biological approach:
Ø
Woody vegetation lowers the water table
effectively; trees being natural tube wells.
Ø
Saline water moves up through vegetation rather
than moving through soil capillaries and leaving salts on soil surface. In the
presence of vegetation, water transpires into the atmosphere while leaving the
salts in the plant tissue.
Ø
Vegetation canopy and litter drastically reduce
evaporation from soil surface.
Ø
The addition of organic matter, root penetration
and activities of associated fauna improve the soil structure and ensures good
drainage. This facilitates the washing down of excessive salts from the soil
surface into deeper horizons. It should be noted that these salts are highly
soluble in water. A few light irrigations or showers are enough for downward
leaching salts.
Ø
Periodic removal of vegetation reduces the total
salts concentration in the site.
There a number of woody species
which can tolerate varying degrees of salinity are called Halophytes. It may be
pointed out that different halophytic species use various adaptations to
overcome the problem of salinity. It is generally considered that halophytes
have to overcome the additional problem of physiological drought. It has been
reported that many drought tolerant plants can easily overcome salinity
provided there is no hindrance to their root respiration. Fortunately it is
quite easy to select suitable salt tolerant species from our indigenous flora
i.e. Acacia, Tamarix, Azadirachta. Some exotic species have also been very
useful for this purpose i.e. Eucalyptus and Atriplex.
Following techniques should be
kept in view while planting:
Ø
Use large and vigorous plants. Entire plants
with a ball of earth or potted plants be selected. Shoot or root cutting etc.
must be avoided.
Ø
For pit planting, top 8 cm or more of saline
surface soil be removed from planting site and should not be used for
re-filling the pit. Relatively large pit be dug, i.e. 1 meter diameter and 1.25
meter depth. If possible powdered gypsum farmyard manure and/or coarse sand be
mixed with dug-out soil and this mixture be used for filling the pit; the
surface of filled pit should be 15 cm below the soil surface to retain added
water. It is better to cover the pit surface with 5-8 cm thick layer of coarse
sand of litter. This layer would cut off evaporation and prevent salt
accumulation on pit surface. A ridge should be provided around every pit to
prevent surface run-off of saline water from bringing salts from surrounding
area into the pit.
Ø
Fresh water should provide at short regular
intervals during the initial stages. Later on the watering intervals may
increase along with an increase in its intensity.
Ø
Plants should be rigorously protected from
climatic and biotic stresses such as frost, hot dry winds, extremes solar
radiation, extremely high temperature of soil surface, trampling and browsing,
etc. Most plants can overcome one problem, waterlogging, drought etc. at a
time; plants, however, fail to survive when these are faced with two or more
problems simultaneously. One should, therefore, try to minimize the number and
intensity of problems. Fluctuations of surface soil temperature should, for
example, be moderated by providing litter mulch and keeping the soil moist.
Ø
If there is very heavy deposition of salts, it
is better not to undertake any planting on large scale unless it is supported
by research and experience.
Ø
If salinity and alkalinity are found coupled
with high water table, deep drains will have to be provided much before
planting as a vital part of site preparation.