Some old threads on groundwater use and depletion:
[thread=402890]Great column on ground water today.[/thread]
[thread=446685]What does it mean to “use” water?[/thread]
[thread=363400]Things people do with water but don’t need to…[/thread]
Regarding the o.p.'s questions, yes, freshwater aquifer depletion is a significant and serious issue, and it is occurring in many regions of the world where high density population, agriculture, or industry has significant fresh water demands that cannot be serviced by natural fresh water sources that are regularly replenished. The Ogallala Aquifer supports a not inconsiderable section of “America’s Breadbasket”, making semi-arid southern Great Plains states into bountiful agricultural regions yielding water-hungry crops like bread wheat, short grain rice, and cotton. Some aquifers are naturally replenished from glacial or runoff sources, but many, like the Ogallala, have a cycle recharge time of hundreds or thousands of years; furthermore, excessive depletion may cause subsidence, in which the matrix of the aquifer, no longer supported by hydraulic pressure, starts to collapse upon itself and suffers from reduced capacity. In other areas, like the Indus River Valley in Pakistan, while the water source is renewable large scale irrigation projects and increased industrial demand upstream resulting in pollution and silted of water for downstream users causes major disruptions.
How big of a problem is this? The ultimate impact of freshwater depletion and overuse is potentially catastrophic, likely even greater than the impact of global climate changes (although the two issues are intertwined). The “Green Revolution” that permitted unchecked population growth and industrial development in Asia was predicated on access to free or highly subsidized water. Pakistan has the largest irrigation project on the planet; without this, the country could not come close to providing for its own burgeoning population, much less the exports that allow the nation hard currency. And yet, water availability and resulting crop yields are decreasing in recent years in Pakistan and India. The issue isn’t localized, either; because of the export of water-intensive crops, the populations of developed nations that import these crops are using “virtual water”; i.e. they share in the depletion of available water by large scale consumption of goods and grains. Never mind turning off the tap while brushing your teeth; that Egyptian cotton shirt you’re wearing cost several hundred–maybe even thousands, depending on conditions–gallons of water from the progressively silted and dry-running Nile Delta. A significant drop in water availability may cause an unavoidable waive of crop failures across a region, which would then require importation of crops from elsewhere to avoid famine. This may also result in warfare over access to water resources, a likely future conflict between Pakistan and India, or Israel and its neighbors.
Remediating the problem is far more difficult than most people really appreciate. Setting aside the energy problems with mass desalination of water (and what to do with the resultant wastes), physically moving the water from coastal regions inland and upward is an enormous logistical challenge. Large scale projects to move water from available underground and surface water sources to arid regions for agriculture and personal use, like Libya’s Great Manmade River Project (a.k.a. Col. Quadaffi’s “Eight Great Wonder of the World”) have cost billions of dollars (~US$25B for the GMRP), have resulted in enormous losses–more than was pumped from the aquifer and lost into the desert), and have only served to redirect the problem. Ditto for water from the Metropolitan Water District of Southern California from the open-top California and Colorado River aquiducts; a substantial portion is lost to evaporation. Even large surface catchments and reservoirs interfere with the hydrological cycle which supports the aquifers, ultimately reducing the throughput of those systems with concomitant effects on other ecological systems.
And this is a deliverly system that is mostly downhill, with only occasional pumping stations. Most of the “free” inland water we get from natural is “pumped” by the enormous amount of “waste” energy from the Sun which drives the hydrologic cycle, which is powered at ~1kW per square meter. Although the reality is that we only use a small fraction of the water that goes through this cycle, it is still an amount of energy that serves to relocate, distill, purify, and mineralize the water we ultimately use for drinking, bathing, and agriculture.
Because water it is a common resource–and one that is ultimately almost completely renewable–we take it for granted, but in fact there are limits on how quickly even a planetary-size system can process water, and we are in many ways exceeding that with current demand. Short of a nearly-limitless, pollution-free energy source and a massive hydroengineering infrastructure to pump water uphill–which is kind of like pushing string–we’re going to need to learn to conserve, treat, and recycle water on a more local scale. Given the additional cost, and current lack of incentive to do so, it’ll probably take a few famines before it becomes the same sort of issue that global climate change is now, despite far more definitive drawbacks and limits.
Stranger