by Rob Tribble
Aquifer Storage and Recovery (ASR) projects, once limited in quantity and scope, are now commonplace in many cities throughout the U.S. and around the world. These projects vary in complexity and application but have several common elements involving the transfer of surface water from above ground to the aquifer below. Although basin recharge and vadose zone applications are two methods of ASR technology, this article looks at a valve system for use in direct recharge or direct injection into an aquifer.
Although many applications involve direct injection of potable water into a confined aquifer, this is not always the case. Many times, the source water is from a water reclamation facility. Other applications involve the injection of stormwater runoff, surface water from canals or streams, extracted and treated groundwater from tainted wells, and agricultural, industrial and process industry waste streams.
Water from these sources can be used for potable dual use wells, irrigation storage, groundwater remediation, salt-water intrusion barrier wells, and groundwater source heat pumps. Though not an exhaustive list, ASR technology is used for each of these source water applications.
Treatment standards vary depending on the permit requirements and the intended use of the injected water. Secondary filtration, tertiary treatment, microfiltration, UV and reverse osmosis are all used in some form on direct injection wells. In some cases the dual-purpose use of ASR wells brings an otherwise unusable well into compliance with water quality standards due to the higher quality of injected water. This is true where naturally occurring compounds, such as arsenic, and high TDS levels exist in the native waters. ASR also helps in aquifer restoration, where plumes of toxic compounds migrate into drinking water aquifers. This type of treatment is ongoing with many groundwater remediation sites.
Regulating Flow, Pressure
These various project types all share a common operational logic: Water must be injected into the aquifer while under positive pressure to prevent air entrainment and the precipitation of minerals and air fouling that can occur from the cascading effect of water flowing into a well without backpressure at the bottom of the column pipe.