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Last modified
1/26/2010 2:58:41 PM
Creation date
10/12/2006 4:18:14 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8543.600
Description
San Luis Valley Project
State
CO
Basin
Rio Grande
Date
8/1/1984
Author
USDOI/BOR
Title
San Luis Valley Project - Colorado - Closed Basin Division - Facts and Concepts
Water Supply Pro - Doc Type
Publication
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<br />~i603 <br /> <br />12 <br /> <br />Que s t ion: <br /> <br />Will the Closed Basin Project turn San Lllis Valley into a dust Bowl? <br /> <br />An~H....er: <br /> <br />No, the operation of the Closed Basin Project will not turn the Valley <br />into a dust bo~l. <br /> <br />Th~ fears which many people have expressed on this suhject are based on <br />mi~understanding. This misunderstanding focuses on two official ~tate- <br />mente; about tilt" project. These official statements are: (1) "the <br />Project will salvage water now being lost to evapotranspiration. <br />and (2) "decreased plant vigor may result (from the operation of the <br />project) in some areas. II SomE' people have interpreted these <br />statements to mean that operation of the pro.jeet will result in the <br />loss of existing vegetation from a V85t part of the. valley. That ie; <br />not what the statements say, and it is not reasonable to believe this <br />wi 11 happen. <br /> <br />" <br /> <br />" <br /> <br />in the Closed Basin sump area, the water table is generally 2 to 6 feet <br />below the surface. A. large amount ot 'Water evaporates from the project <br />area every year. Pro.jeet facilities are de~igned to salvage some (not <br />all) of this evaporated water by lowering the water tahle in the Closed <br />Baisn sump area (only within the pr0ject boundary). A lower water <br />table will reduce the amount of water transferred from the soil surface <br />and from sOI:!e of the vegetation to the atmosphere. <br /> <br />Water is transferred to the atmosphere fro~ leaves of growing plants <br />(transpiration) and from the soil surface <evaporation) by a process <br />called evapotranspiration. Plants in the San Luis Valley and the area <br />of the Closed Basin (not including wetlands) are well adapted to low <br />rainfall and moistur~ levels; however, they can and do use large <br />amounts of water when it is available. The efficiency with vhich a <br />plant uses soil moisture often decreases with too much available water. <br />A point can often be reach~d wh~re high moisture levels reduce plant <br />growth and survival. Where there a~e always very tligh water tables, <br />the rate of plant growth will likely be less than if the water table <br />and available water were 1001er. l.m/ering hi8h water tahles within pro- <br />ject boundaries will not automatically result in the death oE all <br />existing vegetation. Some plants will be adversely affected by <br />lowering water tableS. Others will be helped and increased plant <br />~rowth will occur. r:vaporation of soil moisture can be very high when <br />water levels are near or at the soil surface. The evaporation rate <br />from a "et soil surface generally exceeds that transpired by plants <br />under the same climate conditions. Redllcing water levels will decrease <br />total water lost fro~ the soil surface and will often maintain gr?ater <br />plant growth rates. <br />
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