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A simple, efficient, and economic way to
provide localized sub-surface irrigation known as “pitcher
irrigation” was developed at the Central Soil Salinity
Research Institute, Karnal, India (Mandal, 1974). In this
technique, a baked earthen pot called as pitcher is used to
provide and distribute water in the rootzone. |
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The
pitcher is buried in the soil and filled with water.
Through the pores, water oozes out and wets the soil in
the vicinity of the pitcher, thus making it fit for sowing
seeds and planting seedlings (see figure).
Water is filled in the pitcher manually, through a hose
or by buckets, once or twice a week depending upon the
water depletion rate, which in turn depends upon the type
of crop, stage of growth, and the climatic conditions. |
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Fertilisers and
insecticides are also added in the pitcher itself for uniform
application. Various aspects of pitcher irrigation are
discussed below.
Functioning
of Pitcher Irrigation |
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a) Water
discharge rates |
The amount of
water that can flow out though the walls of the pitcher, i.e.,
discharge per unit surface area per unit time, depends
upon:
i) The
waterhead at a point: This is maximum at the bottom and thus
move water flows through the bottom surface.
ii) The
apertures and intensity of pores in the earthen wall:
Normally, the pores are quite small and thus the discharge is
slow but enough to meet the needs of the plants. Within a
reasonable limit, one can increase or decrease the size of
apertures by varying the ratio of clay and sand, which are the
basic materials used for making the pitchers.
iii) Evapotranspiration
need of the plant: It is greater during the day than at
night. The water flow is affected by the suction created by
the evapotranspiration of the plant.
iv) Texture
of the soil: The discharge is usually greater in a
light-textured soil than in a heavy textured soil.
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b) Wetting
front |
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When the pitcher
is filled, water starts coming out through the pores and
wetting front advances both horizontally and vertically.
However, the horizontal movement is restricted and can be
predicted by the following power curve, expressed as:
L = at b
Where L = length
of advance from the centre of the pitcher,
t =
time in days, and
a,b = are the empirical constants, the value of which depends
upon soil type, evaporative demand, discharge of the
distributor, and the salinity of the irrigation water. During
the winter, value of a was 16.0 and for b for a 0.25. sandy
loam soil. Generally, for a pitcher of 30 cm diameter and 10
litres water holding capcity, wetted surface area is around
0.7 m 2 It is sufficient to grow at least four
plants of any vegetable crop.
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c) Moisture
content of the soil |
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The moisture content of the soil around
the pitcher varies from a maximum of 20 per cent near the
pitcher wall to normal levels of dry soil, i.e. 5 to 10 per
cent, at the end of the wetting front. The maximum moisture
is nearly equal to field capacity of the soil and thus is most
favourable for the growth of plants. Due to limited hydraulic
conductivity of the pitcher wall, moisture levels above these
are rarely obtained, except at night when, because of low
evapotranspiration demand, the moisture percentage may
slightly increase and encourage deep percolation losses.
However, these losses can be minimized by compacting the soil
or putting a plastic sheet just below the pitcher.
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d)
Salinity development in the soil |
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The pitcher irrigation method being
essentially a sub-surface irrigation system, the salts
accumulate at the soil surface and at the boundaries of the
wetted front, leaving the rootzone in equilibrium with the
salinity of the irrigation water used in the pitcher.
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e)
Life of the pitcher |
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Baked clay
pitchers can be continuously used for 3 to 6 years. Clogging
of pores due to preceipitation of salts, as with the dripper,
is a remote possibility when the pitcher is kept wet
continuously. Clogging of pores from outside due to salts
from the soil is limited because the flux is always continuous
and occurs outwards, i.e. away from the wall of the pitcher.
The plant roots can neither enter the pitcher by penetrating
through the pores nor seal the surface from outside. They
also do not exert enough pressure to break the wall of the
pitcher.
To
prolong the life of the pitcher, the following precautions
should be taken:
i) While
not irrigating, keep the mouth of the pitcher covered. This
will minimize the loss of water as well as prevent sunlight
from entering the pitcher and minimize algal information and
growth.
ii)
Only clean water should be used for filing the
pitcher. Muddy runoff from rainfall should be used after it
is passed it through a sand filter.
iii)
Before storing the pitchers, wash them with good
quality water so as to remove the salts and to prevent their
precipitation and subsequent clogging of the pores on drying.
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f)
Applicability to other situations: |
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Pitcher
irrigation is a most effective and low-cost technology for
using a limited supply of good quality water and also for
using saline water resources, it is most suited to the
following situations:
i)
Where availability of good quality water is scarce.
ii) Undulating
areas where soils are difficult to level for uniform
application of irrigation waters.
iii) Light
soils with high infiltration rate, which cannot be efficiently
irrigated by surface method.
iv) Areas
with highly saline water sources, which cannot normally be
used through surface method of irrigation.
Though
this technique is costlier than surface irrigation system, it
is worth the additional cost in view of the easy labour
availability in many developing countries and the saving of
water it provides.
Source
: Summarised from the topic "Irrigation & Salinity Control" by
Ranbir Chhabra, Author, Soil Salinity & Water Quality |
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