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                         METHODOLOGY AND COMPUTATION                        [Back] [Home]

The ground water resources and balance available were computed based on the "Ground Water Estimation Methodology - 1997".  The salient features are given below :

 Unit of Computation 

       The unit of computation proposed in the methodology is 'Watershed'.  Watershed with well-defined hydrogeological boundaries is an appropriate hydrogeological unit for ground water estimation.  However, it also recommends 'block/Tehsil' as the unit of computation for the first few years since there can be non-availability of data.  In the present report 'block' is taken as the unit of computation as in the earlier cases.  This is mainly due to lack of data, especially on number of structures, draft, population, and other vital figures on watersheds.

       Recharge during monsoon and non-monsoon season  

       The methodology recommends computation of 'recharge' figures separately for monsoon and non-monsoon seasons.  The monsoon season is taken as June to September end and the remaining part as non-monsoon. The NE monsoon, which accounts for more than 10% of the total rainfall contributes to he aquifer and hence, recharge is worked out separately as the 'non-monsoon recharge'.

       Sub-units 

      The following sub-units are recommended for the computation of various figures.

  • Hilly areas   Areas with more than 20% slope were removed from the recharge computation.  This was done by using the physiographic map and the block boundary map of the State.

  • Poor ground water quality area             There are no areas which can be mapped as 'poor' ground water quality area.  The poor ground water quality is seen as isolated pockets close to backwater and lagoons and is mostly during summer months.  Since this is negligible, it is not considered for computation of the dynamic resources.  However, it was taken care during the computation of the static resource since brackish water is evaluated in many bore holes drilled along the coastal sedimentaries and crystalline close to back water channels.

  • Command and non-command area        The methodology envisages computation of various figures  'command' and 'non-command' areawise.  However, it could not be done since the data of the command area and the details of various structures in it were not available.  In Kerala, all the surface water projects except Kallada are planned to irrigate paddy and the irrigation canals are contour canals.  Due to the non-availability of map showing the canal network and area irrigated in the command and non-command areas, recharge from the irrigation canals could not be computed for each bloc

For the computation of various figures the units were divided into sub-units as decided above to the extent possible.  Afterwards the areas underlined by various formations were demarcated and the areas were measured separately.

 

Regional Director, Central Ground Water Board, Ministry of Water Resources, Kerala Region,
Kedaram, Kesavadasapuram, Trivandrum - 695 004
Phone: 0471-2442175 , 2440688      e-mail: cgwtvm@sify.com     TeleFax: 0471-2442191
 
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Last modified: 11/05/04