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Specific criteria Prinw farmlands n all the following criteria: <br />Terms used in this section are defined in USDA publications "Soil <br />Taxoncxrry, Agriculture Handbook 436 "; "Soil Survey hkinual, <br />Agriculture Handbook 18 "; "Rainfall - Erosion Losses from Cropland, <br />Agriculture Handbook 282 "; "Wind Erosion Forces in the United States <br />and Their Use in Predicting Soil Loss, Agriculture Handbook 346" and <br />"Saline and Alkali Soils, Agriculture Handbook 60." <br />1. The soils have: <br />a. Aquic, odic, LlStic, or xeric rmisture regimes and sufficient <br />available water capacity within a depth of 40 inches (1 meter), or <br />in the root zone ( root zone is the part of the soil that is <br />penetrated or can be penetrated by plant roots) if the root zone is <br />less than 40 inches deep, to produce the oomrrordy grown cultivated <br />crops (cultivated crops include, but are not limited to, grain, <br />forage, fiber, oilseed, sugar beets, sugarcane, vegetables, tobacco, <br />orchard, vineyard, am k:Yish fruit crops) adapted to the region in 7 <br />or pore years out of 10: or <br />b. Xeric or ustic moisture regimes in which the available water <br />capacity is limited, but the area has a developed irrigation water <br />supply that is dependable (a dependable water supply is one in which <br />enough water is available for irrigation in 8 out of 10 years for <br />the crops ecmrronly grown) and of adequate quality; or, ( the tern <br />adequate supply of water a_s used in the text of this report is <br />synonymous with dependable water supply), <br />' 3 <br />�1 <br />C. Aridic or torric moisture regimes and the area has a <br />developed irrigation water supply that is dependable and of adequate <br />quality; and, <br />2 The soils have a temperature regime that is frigid, mesic, <br />therrrric, or hyperthermic (pergelic and cryic regimes are excluded). <br />These are soils that, at a depth of 20 inches (50 cm) , have a rman <br />annual temperature higher than 32 °F (0 0 C). In addition, the mean <br />s.Lrvner temperature at this depth in soils with an 0 horizon is <br />higher than 47 °F (8 °C); in Soils that have no 0 lyorizon, the mean <br />summer temperature is higher than 59 °F (15 °C); and, <br />3. The soils have a pH between 4.5 and 8.4 in all horizons within a <br />depth of 40 inches (1 mete.) or in the root zone if the root zone is <br />less than 40 inches deep: j:.n:i <br />4. The soils either hava no water table or have a water table that <br />is maintained at a sufficient depth during the cropping season to <br />allow cultivated crops oorarmn to the area to be grown; and, <br />S. The soils can be rrvanaged so that, in all horizons within a depth <br />of 40 inches (1 meter) or in the root zone if the root zone is less <br />than 40 inches deep, during part of eadi year the conductivity of <br />the saturation extract is less than 4 mmhos /con and the exchangeable <br />sc>dium percentage (ESP) is less than .15; and, <br />• Revised September 2010 (PR06) Attachment 2.04.9 -5 -7 <br />