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1 <br />' The upper 15 inches of the substratum is extremely cobbly sandy loam. The <br /> lower part to a depth of 60 or more inches is extremely cobbly sand. <br />' <br /> Permeability is moderately rapid to rapid. The water holding capacity is <br />' low, The coarse fraction greater than 3 inches diameter in the upper <br /> horizons ranges up to 20 percent by volume. Atypical pedon of the Cascajo <br />' very gravelly sandy loam is included herein. <br /> Kim Series <br />1 i <br />d <br />ll d <br />i <br />d <br />fi <br />l <br />K <br />i <br />d <br />S <br />l <br />f <br />h <br /> oamy, m <br />xe <br />, <br />eep, we <br />ra <br />ne <br />, <br />ne- <br />im ser <br />es are <br />oi <br />s o <br />t <br />e <br />' mesic Ustic Torriorthents. The soils developed in loamy alluvium and occur <br /> on slopes that are nearly level to gently sloping. Typically the surface <br />' layer is a pale brown loam about 4 inches thick. The upper part of the <br /> underlying material is a pale brown loam about 6 inches thick, the next <br />' and the lower <br />t 34 i <br />h <br />s thi <br />k <br />ll <br />i <br />h b <br />l <br />b <br />i <br />li <br />h <br /> nc <br />c <br />, <br />ow <br />rown <br />oam a <br />ou <br />e <br />part <br />s a <br />g <br />t ye <br />s <br />' part is a pale brown loam that extends to a depth of 60 inches or more. A <br /> substratum of sand and gravel is at a depth below 2 feet locally. <br /> Permeability is moderate and the available water capacity is high. A <br /> typical pedon of the Kim loam is included herein. <br />1 <br /> <br /> <br /> <br /> <br />1 <br />1 <br />1 <br />