| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4721125 | Physics and Chemistry of the Earth, Parts A/B/C | 2012 | 15 Pages |
Overexploitation of groundwater resources has supported rapid social and economical developments in Beijing City in last 30 years. The newly constructed emergency well fields have saved Beijing from a critical water crisis caused by a long drought spell of eight consecutive years from 1999 to 2006. But this unsustainable development has resulted in serious consequences: discharges to rivers ceased, large number of pumping wells went dry, and land subsidence caused destruction of underground infrastructure. The completion of the middle route of South to North water transfer project to transfer water from Yangtze river to Beijing City by 2010 provides opportunity to reverse the trend of groundwater depletion and to achieve a long-term sustainable development of groundwater resources in Beijing Plain. Four options of groundwater development in Beijing Plain were formulated and assessed with a regional transient groundwater flow model. The business as usual scenario was used as a reference for the comparative analysis and indicates fast depletion of groundwater resources. The reduction of abstraction scenario has immediate and fast recovery of groundwater levels, especially at the cone of depression. The scenario of artificially enhanced groundwater recharge would replenish groundwater resources and maintain the capacity of present water supply well fields. The combined scenario of the reduction of abstraction and the increase of recharge could bring the aquifer systems into a new equilibrium state in 50 years. A hydrological sustainability of groundwater resources development could then be achieved in Beijing Plain.
► Overexploitation of groundwater has caused rapid decline of groundwater levels. ► A combined measures of increasing recharge and reducing abstractions are urgently required. ► Reduction of abstraction can immediately recover groundwater levels in deep aquifers. ► Increase of recharge can replenish the depleted storage and maintain the present water supply. ► Uncertainties in recharge and abstraction have much larger impacts on model scenario simulations.
