Precipitation (P)
- The total water received through hailstorm, snowfall, rainfall, etc. over
the area.
Imported water (Wi) - Surface water flowing in
the streams, and ground water inflow in the area.
Stream outflow (R) - The quantity of water outflowing
through streams from the area.
Evapotranspiration (Et) - The quantity of water
lost through evaporation from the ground surface and transpiration through the
leaves of the plants.
Groundwater outflow (Wo) - Ground water flowing
out of the area.
Change in groundwater storage (<Sg)-- The change
in the volume of saturated thickness of the aquifer.
Change in soil moisture storage (<Ss)- The change
in moisture content in top-soil and sub-soil. This is generally taken as negligible
for larger time periods.
The Presently Suggested System: The above water
balance equation does not take into account the water quality factor, and the
requirement of water for various human purposes. For the water balance study,
which takes into account all the requirements and environmental considerations
the following equation can be used.
Requirement of water (quality and quantity-wise)
for all the purposes in the area
<------->
Availability of water (quality and quantity
wise) from all the sources in the area
If the requirement is more than the availability, the area is deficient in water
and on the other hand if the availability of water is more than the requirement
the area is surplus in water. Further, if in a region it is seen that a specific
quality water is falling short while some other quality water is available more
than its requirement, it may be enquired whether this extra water may be treated
to upgrade its quality to meet the shortage of better quality water. This treatment
may be techno-economically more feasible than meeting the shortage by water
transportation. Hence the availability should be assessed and arranged in terms
of both quality and quantity. Using this concept the exercise for balancing
can be done in the manner described later.
As is evident, it is necessary to identify all the water sources and then to
assess the availability of water from them both in terms of quality as well
as quantity. Similarly, it is also necessary to assess the requirement of water
for purposes both quantitatively as well as qualitatively.
A very important point, though understood, worthy mentioning here is, any water
balance study should be made for a complete watershed or a mini- or micro-watershed
and definitely not for a country, state or district.
Identification of Water sources: The water sources in any area can be classified
into the following two categories.
1. Surface water sources
2. Sub-surface and underground water sources
The `Surface Water Sources' include the followings.
* Rainfall.
* Rivers and their tributaries.
* Water storages in the form of lakes, ponds, tanks, etc.
The `Sub-surface and Underground Water sources' include the followings.
* Aquifers, both confined and unconfined.
*Water being pumped out of the workings below land surface of the mines in mining
areas (if it is used through recycling).
Availability of Water: In most area, specially in those
having monsoon type climate or seasonal or occasional rainfall, the total quantity
of water available from the various sources varies. It is expected to be more
in rainy seasons/months and less in dry seasons/months. Therefore, to assess
the availability of water from the sources it is necessary to establish an `availability
pattern' for each source separately.
The availability pattern can be established on the basis of month-wise water
availability data. The data for about 10-years should be taken into consideration
to establish this pattern, which then can be used to anticipate the availability
of water for future.
In the Indian context it will not be possible to get the water availability
data except rainfall for 10-year period and the exercise of water availability
assessment may have to depend on the data for one year only.
Month-wise average availability of water can be computed by the available standard
methodologies, some of which are briefly given next.