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         Status of Surface & Ground Water Resources 
 
 

The state of Punjab derives its name from 'Punj' + 'Aab' i.e. the land of five rivers (five rivers flowed through erstwhile Punjab namely, Satluj, Beas, Ravi, Jhelum & Chenab). However, after the state's partition first in 1947, and subsequently its reorganisation in 1966, only Satluj and Beas flow through it, while Ravi touches it at its north border. Another small river, the Ghaggar flows through its southern border.The Ravi ,The Beas and the Sutluj are the Perennial rivers. The Ghagger, White Bein, Black  Bein and Sakki Kiran Nala are the seasonal and numerous choes of the sub-shivaliks or the kandi are  the ephemeral rivers. At the point of confluence of Satluj and Beas lies the internationally renowned Harike wetland in 28.5 sq km area (formed due to construction of Harike barrage in 1952) famous for its migratory birds. The state also has 12 natural and 9 manmade wetlands (covering more than 15,500 hq area). Details of capaicity of various canals of Punjab are as :-
 

Name of Head works   Name of off taking channels Capacity
Ropar  Headworks Ropar  

i)   Sirhind Canal

ii)   Bist Doab Canal 

12622 Cs.

1408 Cs  

Harike Headworks, Harike  

i)    Rajasthan Feeder

ii)   Ferozepur Feeder

iii)   Mukhu Canal   

18500 Cs.    

11192 Cs.

 292 Cs.   

Hussainiwala Headworks Ferozepur

 

i)    Bikaner Canal

ii)   Eastern Canal  

2740 Cs.  

3929 Cs.  

Madhopur Head Works            i)    Upper Bari Doab Canal   8200 Cs.
Shah Nehar Headworks            i)    Mukerian Hydel Canal   11500 Cs
Nangal Head works            i)    Bhakra Mainline Canal   12455 Cs.
Source: Irrigation & Drainage Departments ,Punjab


With the advent of green revolution the state has developed its water resources effectively and a mesh of irrigation canals has been laid all over . However, change in cropping pattern (from mixed cropping to wheat-rice rotation), & intensive agriculture has adversely affected the state's water resources. The number of tubewells has trebled since the seventies. This has resulted in decrease in water table in certain central districts and its increase in southern districts causing water logging and salinity problem. However, the average rate of water table decline in sweet ground water area of the state as a whole is 0.2 m 0.3/year
 

GROUND WATER STATUS OF PUNJAB

Sr. No.

District

Ground Water Recharge/Extraction

1.

Gurdaspur

Recharge 20-50% of extraction

2.

Hoshiarpur

Recharge 20-50% of extraction

3.

Ropar

Rcharge higher than 50% of extraction

4.

Amritsar

Recharge equal to extraction (± 20%)

5.

Kapurthala

Extraction exceeding Recharge by more than 50%

6.

Jalandhar

Extraction exceeding Recharge by more than 50%

7.

Ludhiana

Extraction 20-50% of Recharge

8.

Patiala

Extraction exceeding Recharge by more than 50%

9.

Ferozepur

Recharge higher than 50% of extraction

10.

Bathinda

Recharge higher than 50% of extraction

11.

Faridkot

Recharge higher than 50% of extraction

12.

Sangrur

Extraction exceeding Recharge by more than 50%

Source : Irrigation Department, Punjab (Chandigarh) 


The available ground water is estimated at 25.34 MAF-million acre feet, where as the normal requirement is 39.75 MAF (Source: Punjab Agriculture University).This is a substantial deficit which if left  uncorrected   will adversely affect agriculture .The central sweet zone, which is highly Productive with a well –knit irrigation system mainly dependent  upon tubewell, presents a serious challenge because of extensive and intensive rice cultivation. In Punjab the water table is falling at an average rate of 0.23 meters per year, during the past 15 years. The water table was at 5 Meters to 6 meters in 1981. It now showed a fall of 24cm to 25cm per annum . The annual fall in the water table for some district is as fallows .

  • Amritsar,  Kapurthala , Sangrur(Lehra Gaga)--17cm  

  • Jalandhar—22cm  

  • Ludhiana----12cm  

  • Faridkot-----13cm  

  • Patiala----33cm  

  • Sangrur( Barnala)—42cm  

  • Ropar-----8cm  

  • Gurdaspur—1cm  

        In the Southwest  zone which comprises almost one-fourth of the state cultivated area, the underground water is brackish and unfit for the crops and humans.  The water table in the zone which was 11m deep in 1981 is rising continuously at the rate of 9 cm per year in Mansa, 21 cm in Bathinda and 17 cm in Ferozepur.  This has motivated farmers to give up ‘white gold’ and sow paddy.

 

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