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San Joaquin County, California 123 <br /> rooting depth of the crops commonly grown in the thick. The next 5 inches is light brownish gray and <br /> county is limited by an apparent water table that is grayish brown clay loam. Below this to a depth of 60 <br /> _ regulated at a depth of 3 to 4 feet by pumping. This soil inches is a variegated dark grayish brown and brown, <br /> is subject to subsidence. Runoff is very slow, and the weakly cemented to strongly cemented hardpan. In <br /> hazard of water erosion is slight. The rate of water some areas the surface layer is silty clay loam or loam. <br /> intake in irrigated areas is 4.0 inches per hour. The Included in this unit are small areas of Archerdale <br /> hazard of soil blowing is severe. The soil is subject to and Cogna soils on the slightly higher parts of the <br /> rare flooding, which occurs during years of abnormally landscape and Hollenbeck soils in landscape positions <br /> high precipitation. similar to those of the Stockton soil. Also included are <br /> Most areas are used for irrigated crops. This unit small areas of Stockton soils that are fine textured <br /> may provide wetland functions and values. These throughout. Included areas make up about 15 percent <br /> should be considered in plans for enhancement of of the total acreage. <br /> _ wildlife habitat or land use conversion. Permeability is slow in the Stockton soil. Available <br /> This unit is suited to irrigated row and field crops. water capacity is high. The shrink-swell potential also is <br /> The main limitations are subsidence and the high water high. The effective rooting depth is limited by the <br /> table. General management considerations include the hardpan at a depth of 40 to 60 inches. Depth to the <br /> severe hazard of soil blowing. Because this soil is water table is more than 5 feet, but water may be briefly <br /> subject to differential subsidence, frequent leveling of perched above the hardpan after periods of heavy <br /> the fields is needed to improve the efficiency of rainfall or irrigation. Runoff is slow, and the hazard of <br /> - irrigation. Areas adjacent to levees are subject to lateral water erosion is slight. The rate of water intake in <br /> seepage in wet years when the water level is high. irrigated areas is 1.5 inches per hour. The soil is <br /> Careful applications of irrigation water are needed to subject to rare flooding, which occurs during years of <br /> prevent the buildup of a high water table. Large ditches abnormally high precipitation. <br /> and small spud ditches provide subirrigation and Most areas of this unit are used for irrigated crops or <br /> improve drainage. Subirrigation, furrow, border, and orchards. A few areas are used for homesite <br /> sprinkler systems are suitable. Where a subirrigation development. <br /> - system is used, the water table is raised to a depth of 1 This unit is suited to irrigated row, field, and orchard <br /> foot at planting time and then is slowly lowered during crops. The main limitations are the slow permeability <br /> the growing season until it is at a depth of about 5 feet and depth to the hardpan. Because of the restricted <br /> _ at harvest time. When the wind velocity is high in permeability, water applications should be regulated so <br /> spring, the hazard of soil blowing can be reduced by that the water does not stand on the surface and <br /> properly managing all crop residue and by minimizing damage the crops. The hardpan limits the suitability for <br /> tillage. Levees should be checked periodically, and a deep-rooted crops. Where feasible, deep ripping of this <br /> proper maintenance program should be developed. restrictive layer can help to overcome this limitation. <br /> This map unit is in capability units Illw-10 (MLRA-16), Furrow, border, and sprinkler irrigation systems are <br /> irrigated, and IVw-10 (MLRA-16), nonirrigated. It is in suitable. Maintaining crop residue on or near the <br /> vegetative soil group E. surface helps to prevent excessive runoff and helps to <br /> maintain the rate of water intake and the organic matter <br /> 24$—Stockton fine sandy loam, 0 to 2 percent content. <br /> Slopes, overwashed. This somewhat poorly drained, If this unit is used for homesite development, the <br /> nearly level soil is in basins. It is deep to a hardpan. It main limitations are the high shrink-swell potential, the <br /> formed in alluvium derived from mixed rock sources. slow permeability, depth to the hardpan, and low <br /> Mottles in the profile indicate a somewhat poorly strength. The rare flooding is a hazard. Properly <br /> drained soil; however, drainage has been improved by designing foundations and footings and diverting runoff <br /> levees and reclamation projects. A few areas are away from buildings help to prevent the structural <br /> dissected by intermittent sloughs that have been filled damage caused by shrinking and swelling. On sites for <br /> tha result of land leveling. Elevation is 20 to 70 feet. septic tank absorption fields, the slow permeability can <br /> e average annual precipitation is about 14 inches, be overcome by increasing the size of the absorption <br /> Fe average annual air temperature is about 60 degrees field, backfilling the trench with sandy material, and <br /> and the average frost-free period is about 270 days. installing long absorption lines. Ripping the hardpan <br /> TyPically, the surface layer is grayish brown fine improves permeability and thus also improves the <br /> S. loam about 16 inches thick. It is underlain by a suitability of the soil for septic tank absorption fields. <br /> boned surface layer of dark gray clay about 37 inches Properly designing buildings and roads can offset the <br /> ri <br />