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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />o <br />~ <br />-J <br />~ <br /> <br />-50- <br /> <br />agricultural loading values tend to be much smaller. This <br />is due to the fact that the agricultural salinity contri- <br />bution was based solely on concentrating effects. <br />Natural runoff contributes 52 percent of the salt load <br />from the Upper Basin (EPA, 1971). In an effort to control <br />any salinity effects due to soil disturbance by livestock <br />grazing and energy development in the basin, the Bureau of <br />Land Management is pursuing a program of more restrictive <br />grazing controls, inter seeding of contour furrows, and chain- <br />ing and seeding to control salinity from surface hydrologic <br />events (Bently et al. 1978). Much of this program is based <br />on work by Gifford et al. (1975) in the Price River area. <br />Ponce (1975) and Ponce et al. (1975) reported on non- <br />point salt loading from grazing and its effects on Mancos <br />Shales in the Price River Basin. Whitmore (1976) and White <br />(1977) reported on the salinity aspects of Mancos soils and <br />the effect of microchannels, respectively. All of these <br />studies basically concluded that a practice which compacts <br />or otherwise disturbs the soil structure, reduces infiltra- <br />tion and increases runoff and/or erosion on saline soils <br />will increase salt yields. Similar results were obtained by <br />Laronne and Schumm (1977) for the Grand Valley area. Thomas <br />(1975) investigated the use of gully plugs and contour fur- <br />rows to control erosion and had good success. McWhorter and <br />Skogerboe (l979) investigated inter flow as a transport <br />mechanism for salt on Mancos soils, and determined that it <br />had little effect. <br />