Irrigation works : $b the principles on which their design and working should be based, with special details relating to Indian canals and some proposed improvementsBellasis, E. S. (Edward Skelton)
Science
Irrigation works : $b the principles on which their design and working should be based, with special details relating to Indian canals and some proposed improvements
Bellasis, E. S. (Edward Skelton)
Canals; Irrigation
There is an obvious connection between the duty of water and the total
depth of the water, known in India as “delta,” given to the fields.
Calculations are much simplified, while still being accurate enough for
all practical purposes, by assuming that the number of seconds, (86,400)
in a day is twice the number of square feet, (43,560) in an acre.
Assuming this to be the case a discharge of 1 c. ft. per second for a
day gives 2 acre-feet, i.e., it will cover an acre of ground to a depth
of 2 feet in a day; and in six months it will cover 100 acres to depth
of 3·65 feet. In Northern India the year is divided into two halves in
each of which a crop is grown and the duty is calculated for each crop.
In this case, if the flow of a canal has been continuous, a duty of 100
acres per cubic foot of its mean discharge per second, corresponds to a
total depth of 3·65 feet over the area irrigated. Generally the flow in
the half-year has not been continuous. In other countries, and in India
on canals other than the perennial canals, the periods of flow vary a
great deal. The duty cannot be calculated from delta or _vice versa_
until the period of flow is stated.
The daily gauge-readings and daily discharges corresponding to them,
having been booked, the discharges are added up. The total, divided by
the number of days on which the canal has been running, gives the
average daily discharge. Suppose that during the “kharif” or summer crop
which is considered to last from 1st April to 30th September or 183
days, the canal was closed for 13 days and that the total of the daily
discharges on the remaining 170 days comes to 850,000 c. ft. per second.
The average daily discharge is 5,000 c. ft. per second. Suppose the
kharif area irrigated to be 500,000 acres, the kharif duty is 100 acres.
To find delta the total of the daily discharges has to be multiplied by
the number of seconds in a day and divided by the number of square feet
in an acre (these figures are, as already stated, very nearly in the
ratio of two to one) and divided again by the number of acres irrigated.
Thus, in the above case, delta is very nearly 850,000 × 2/500,000 or 3·4
feet. For comparing the results of one canal or one year with another,
delta is the more convenient figure to take. As soon as the areas
irrigated by the canals are known for any crop, the Chief Engineer of
the province issues a statement of the value of delta for each perennial
canal and compares them with those for previous years. The value of
delta for the Punjab canals ranges from 3 to 4 feet for the kharif and
from 1·8 to 2·1 feet for the “rabi” or winter crop. Individual canals
vary greatly, the worst having nearly twice as high a figure as the
best. The differences are due to the causes already mentioned.
Public-domain text, read in full here on John Shaqi.
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