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In T~ible 10, loamy sand and sand are combined. The parameter values that are shown in <br />the table are for loamy sand. XKSAT for sand is often used as 4.6 inches/hour, and PSIF is <br />often used as 1.9 inches. Using those parameters values for drainage areas can result in <br />the qeneration of no rainfall excess which may or may not be correct. Incorrect results <br />coulci cause serious consequences for flood control planning and design. Therefore, it is <br />recommended that for watersheds consisting of relatively small sub-areas of sand, the <br />Green and Ampt parameter vafues for loamy sand be used for the sand portion of the <br />watershed. If the area contains a large portion of sand, either the Green and Ampt method <br />should be used with the parameter values for loamy sand or the Initial Loss and Uniform <br />Loss Rate method should be used with the appropriately determined values for the <br />para meters. New research relating soil texture with XKSAT has recently been published <br />(Sax~:on and Rawls, 2004). This information has not been evaluated and tested to <br />determine its application for hydrologic modeling, but may be of value in the future. <br />The methods presented herein can be accomplished using hand computation techniques <br />including hard copy maps and use of a planimeter or other suitable method for estimating <br />the ~~reas of irregular polygons. More complex watersheds with detailed soils mapping <br />including numerous polygons defining multiple soil textures may, from a practical <br />stancipoint, require analysis using CADD or GIS software. <br />These guidelines are based on the following presumptions, but the user should note that <br />the quidelines herein can also be accomplished following the same basic procedures using <br />hand computations or CADD software. <br />1. ESRI ArcMap GIS software will be used to facilitate the computations. The <br />guidelines presented herein provide an outline level of guidance that can be <br />implemented at various levels of detail using GIS. These guidelines can be applied <br />using standard GIS software, but there are third-party software programs such as <br />WMS, DDMSW and various CADD software packages that will also perform many of <br />the computation steps documented herein, except for determining a controlling soil <br />texture for each soil map unit present in a given study area. <br />2. The user has a base map in GIS format or a hard-copy map for the study area of <br />interest with the drainage area delineated into sub-basins. <br />19 March 2007 34 <br />