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<br /> <br />- 4 - <br /> <br />Reservoirs - To provide for permanent storage of sediment and either tem- <br />por~ry or permanent water storage. <br /> <br />Revetments - Materials placed on the stream bank to protect it from erosion <br />by stream flow. <br /> <br />Sills - Structures of rock, masonry, rails, etc., placed at channel grade <br />to prevent stream'downcutting. <br /> <br />Disturbed Area Protection - This measure may include any of the above treat- <br />men~s and structures. In addition, it often includes stabilizing steep <br />slopes, lining road ditches, etc. <br /> <br />Applicability of Management and Land Treatment Measures for Erosion and <br />Sediment Control <br /> <br />The soils, climate, topographic and other factors which tend to create the <br />most severe erosion and sediment problems also increase the difficulty of <br />control. Similarly, many measures are usually more successful under con- <br />ditions of low or moderate erosion and -sediment yield than they are under <br />hig~ yield. The broad trends in the principal factors affecting erosion <br />indicate the reasons for this. Vegetative measures are dependent on favor- <br />abl~ moisture conditions and proper grazing control. Although there are some <br />notable exceptions in the Pacific Southwest, the more humid sections usually <br />show less sediment yield than more arid sections, as more favorable moisture <br />furnishes greater support to vegetation. Similarly, the mechanical treat- <br />ment measures which require disturbing, molding, or reshaping the soil are <br />mos:t successful where the soils have p~operties which inherently make them <br />res:istant to erosion. The other factors operate in much the same way and <br />in 'an interdependent fashion. As the slope increases, for instance, problems <br />of 'establishing and maintaining vegetation, applying mechanical treatment <br />and obtaining proper grazing use also increase. <br /> <br />Figure 1 shows the climatic environments of the Pacific Southwest. The indi- <br />cated large variations are most pronounced in the mountains and valleys of <br />the region where the mountain peaks may be humid and the valley bottoms arid. <br />This variation causes many planning problems. <br /> <br />Th~ measures that are used for erosion and sediment control in the Pacific <br />So~thwest may be classified by purpose into several groups: (1) to inter- <br />cept and/or conserve moisture; (2) to increase infiltration capacity; (3) <br />to reduce or eliminate stress on existing cover; (4) to preserve existing <br />coYer regarded as adequate or in the process of becoming adequate with time; <br />(5) to increase the protection of the soil by a change in the type as well <br />as density of vegetation. <br />