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CENTRAL GROUND WATER BOARD

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Ground Water is a Precious National Resource - Preserve it, Protect it and Don't Pollute it.

State Profile 


Ground Water Scenario of Manipur


Area (Sq.km)

22,327

Physiography

Four major units

  • Hills  
  • Eroded hills with flat land
  • Intermontane valleys 
  • Alluvial plains 

Drainage

Mainly drained by river and tributaries of Meghna and Chindwin basin.                                    

Rainfall (mm)

1454( average annual)

Total Districts / Blocks

9 Districts 

Hydrogeology 

The Manipur valley is underlain by a thin veneer of alluvial deposits, which is largely clayey in nature, underlain by rocks of Tertiary age. Ground water occurs under un-confined and confined conditions. Since the upper formations are mainly silty and clayey, open wells have poor yield prospects. However the deeper zone, consisting of sand stones of Tertiary age, forms good aquifers which are under confined conditions, Autoflow conditions are observed in Imphal where the yield of the tubewells vary from 0.5 to 4 m3/hr. The water bearing formations are not extensive. The quality of ground water is generally good.


Dynamic Ground Water Resources (2011)

Annual Replenishable Ground water Resource

0.44 BCM

Net Annual Ground Water Availability

0.40 BCM

Annual Ground Water Draft

0.004 BCM

Stage of Ground Water Development

1.02 %

Ground Water Development & Management

Over Exploited

NIL

Critical

NIL

Semi- critical

NIL

Artificial Recharge to Ground Water (AR)

    1. Feasible AR structures
    2. Check dam-300
    3. Weirs-500
    4. Gabian structure-500
    5. RTRWH-300
    6. Development of springs-150

 

Ground Water Quality Problems

Contaminants

Districts affected (in part)

Iron (>1.0 mg/l)
Arsenic(>0.05 mg/l)

Bishnupur, Thoubal
Bishnupur, Thoubal

Central Ground Water Authority


Areas Notified for Regulation of ground water development

NIL