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<br />Question: Will the Closed Basin Project turn San Luis Valley into a dust bowl? <br /> <br /> <br />,0 <br /> <br />Answer: No, the operation of the Closed Basin Project will not turn the Valley <br />into a dust bowl. <br /> <br />The fears which many people have expressed on this subject are based on mis- <br />understanding. This misunderstanding focuses on two official statements about <br />the project. These official statements are: (1) "the Project will salvage <br />water now being lost to evapotranspiration. . . . . . ," and (2) "decreased <br />plant vigor may result (from the operation of the project) in some areas . <br />" Some people have interpreted these statements to mean that operation <br />of the project will result in the loss of existing vegetation from a vast part <br />of the valley. That is not what the statements say, and it is not reasonable <br />to believe this will happen. <br /> <br />In the Closed Basin sump area, the water table is generally 2 to 6 feet below <br />the surface. A large amount of water evaporates from the project area every <br />year. Project facilities are designed to salvage some (not all) of this evapo- <br />. rated water by lowering the water table in the Closed Basin sump area (only <br />within the project boOndary). A lower water table will reduce the amount of <br />water transferred from the soil surface and from some of the vegetation to <br />the atmosphere. <br /> <br />" <br /> <br />Water is transferred to the atmosphere from leaves of growing plants (trans- <br />piration) and from the soil surface (evaporation) by a process called evapo- <br />transpiration. Plants in the San Luis Valley and the area of the Closed Basin <br />(not including wetlands) are well adapted to low rainfall and moisture levels; <br />however, they can and do use large amounts of water when it is available. The <br />efficiency with which a plant uses soil moisture often decreases with too much <br />available water. A point can often be reached where high moisture levels <br />reduce plant growth and survival. Where there are always very high water <br />tables, the rate of plant growth will likely be less than if the water table <br />and available water were lower. Lowering high water tables within project <br />boundaries will not automatically result in the death of all existing vegetation. <br />Some plants will be adversely affected by lowering water tables. Others will <br />be helped and increased plant growth will occur. Evaporation of soil moisture <br />can be very high when water levels are near or at the soil surface. The <br />evaporation rate from a wet soil surface generally exceeds that transpired <br />by plants under the same climate conditions. Reducing water levels@{H:.8\..1 <br />decrease total water lost from the soil surface and will often maintain <br />greater plant growth rates. <br /> <br /> <br />Both upland and wetland vegetation in the San Luis Valley and the Closed Basin <br />have been studied for many years. A 3-year growth study was conducted by the <br />Bureau of Reclamation on basically upland vegetation. The study area was <br />located where the water table was lowered by a pilot salvage well. The study <br />has shown that shrubs right around project salvage wells will be adversely <br />affected. Most of the shrubs within several hundred feet of the well will <br />be smaller in size and fewer in number after several years of project operation. <br />Younger shrubs will most likely survive even near the wells. These shrubs <br />have the ability to follow the water table down as they continue to utilize <br />surface precipitation. Older shrubs" do not respond to rainfall as well. <br /> <br />The reaction of saltgrass and wiregrass to a lowering <br />more complicated. Where the water table is more than <br />depend'on direct rain and snowfall for annual growth. <br /> <br />water table is a little <br />5 feet down, most grasses <br />In these areas, project <br />