C: Do We have Groundwater Management Crisis?
Groundwater crisis, in general, refers to the scarcity
of good quality and quantity of groundwater from a basin-wide common aquifer
relative to the demands of land and water users. Obviously, in case of
ineffective groundwater resources management, imbalance of recharge and
discharge from an aquifer occurs that can have two kinds of consequences: (1)
if recharge is in excess of discharge, the result is water-logging and salinity
like areas where our surface water duties are too high and groundwater
extractions are minimum; and (2) if discharge from aquifer is more than
recharge, the potential outcomes are a drop in water-table and the rise of
saline-fresh water interface from the lower depths (dominant case in our
context) to push up pumping cost higher and to cause quality
deterioration. Because of pumping phenomenon, brackish water intrusion into
relatively fresh groundwater is happening both vertically as well as
horizontally because of brackish groundwater in nearby locations as we observe
in many of our areas between two rivers in the Indus Basin.
Obviously, we are facing severe groundwater crisis
mainly on two main fronts: (1) Lack of supply-side groundwater management where
over-abstractions are causing excessive stress on aquifer conditions by
dropping water-tables and quality deterioration and (2) absence of demand-side
groundwater management is causing unbridled greed for more and more water
extractions by the land-owners and other and water users as population keeps
exploding.
As reported by Usman Karim (Imno25@hotmail.com),
there were 1000 tube-wells in 1950, 0.5 million in 2000 and 0.7 millions in
2008 just alone in Punjab and total numbers of tube- wells in Pakistan are reported to be 1.1 million (2008) as per
the same estimate. At present, based on
the trend derived from the referred data, we can expect more than 1 and 1.2
million tube-wells in Punjab and Pakistan, respectively. With this unplanned
and free-for-all regime is causing over extraction of groundwater to push down
water-tables, the rise of saline-freshwater interface and saline-water
intrusion to effect the quality of this on-site resource. Moreover, according to
a book authored by Qureshi andBarrett-Lennard in 1998, 70% of tube-wells pump
sodic water in the Indus Basin.
Because of excessive use of fertilizers and
pesticides, industrial waste-water and sewerage water, excessive aquifer
pollution is happening. As a consequence of this phenomenon, the contamination
of ground and surface water is causing huge health hazards. Some reports
suggest that 40% of prevalent diseases and 20-40% hospitalization is mainly attributed
to water borne diseases. Usman Karim also reports results of 747 samples
collected from various cities of Pakistan. Water analyses show that 19% of
total samples had nitrate concentration more than permissible limit of 10 mg/L.
To be more precise, this concentration ranges from 11 to 160 mg/L. This
contamination jumped to 23% for the water samples collected from Punjab and
Baluchistan.
Groundwater use in all sub-sectors is under stress
to an extent of crisis. This kind of outcome is mainly because of allowing an
access that is free-for-all individuals to pump groundwater from a common pool
without any restriction imposed through regulations or any institutional
structures.
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