Surface water is diverted from the Rio Grande into the Closed Basin for recharge of a shallow aquifer. The groundwater is subsequently pumped from the aquifer and used to irrigate crops.
The Closed Basin occupies the northern portion of the San Luis Valley, and is separated from the Rio Grande’s alluvial valley by a low topographic divide and a shallow groundwater divide oriented roughly parallel to the river. Water imported into the Closed Basin does not naturally return to the Rio Grande.
The Prairie Ditch and the San Luis Valley Canal Companies recognize that continued importation of direct flow surface water from the Rio Grande, in conjunction with groundwater recharge, is crucial to sustaining the shallow groundwater reservoir that allows the continuing operation of their center pivot sprinkler systems. To this end, Company shareholders have constructed groundwater recharge facilities to artificially recharge groundwater.
Deere & Ault performed an investigation of the historical water use practiced by the Prairie Ditch and San Luis Valley Canal Companies. The objectives of this investigation were to confirm their historical practice of recharging the unconfined aquifer of the Closed Basin, and to present a methodology and accounting procedure to quantify the volume of recharge to the unconfined aquifer of the Closed Basin from their water rights.
Deere & Ault’s staff performed a hydrologic analysis of the Closed Basin, updating the location of the groundwater divide. Our staff provided expert witness testimony on the Prairie Ditch Case, which was settled in late-2001. The San Luis Valley Canal Case is currently pending.
Client: Prairie Ditch Company and San Luis Valley Canal Company
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