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Pa'auilo Final Enviromental Assessment
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Pa'auilo Final Enviromental Assessment
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8/17/2011 10:16:07 AM
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PA`AUILO LANDS <br /> FINAL ENVIRONMENTAL ASSESSMENT <br /> Honokaa Silty Clay Loam, Low Elevation, 10-20% slopes (HsD) constitutes approximately <br /> 48 percent of the Pa`auilo Lands. This soil is similar to Honokaa silty clay loam 10 to 20 percent <br /> slopes, except that it occurs at a lower elevation where the soil temperature is warmer. This soil <br /> is used principally for sugarcane. Small areas are used for pasture and macadamia nuts. These <br /> soils are in Capability Class IV. <br /> Honokaa Silty Clay Loam, slopes Low Elevation, 20-35% (HsE) constitutes approximately <br /> 20 percent of the Pa`auilo Lands. This soil is similar to Honokaa silty clay loam 10 to 20 percent <br /> slopes, except that it is steep and occurs at a lower elevation where the soil temperature is <br /> warmer. Runoff is medium, and the erosion hazard is moderate. This soil is used mostly for <br /> sugarcane. Small areas are used for pasture and macadamia nuts. These soils are in Capability <br /> Class VI. <br /> Maile Silt Loam, 6-20% slopes (MLD) constitutes approximately 4 percent of the Pa`auilo <br /> Lands. This soil is at intermediate elevations on the windward side of Mauna Kea. It has a <br /> dominant slope of approximately 15 percent. A representative profile has a surface layer of dark <br /> reddish-brown to very dark brown silt loam approximately 14 inches thick. The subsoil is <br /> approximately 46 inches thick. It consists of dark yellowish-brown and very dark brown silty <br /> clay loam. The subsoil dehydrates irreversibly into fine sand-size aggregates. The profile grades <br /> from medium acid in the surface layer to slightly acid and neutral in the subsoil. Included in this <br /> mapping are small, steep drainageways and gullies. Permeability is moderately rapid, runoff is <br /> slow, and the erosion hazard is slight. Roots can penetrate to a depth of 5 feet or more. This soil <br /> is used for pasture and woodland. These soils are in Capability Class IV. <br /> Rough broken land, (RB) constitutes approximately 7 percent of the Pa`auilo Lands. Rough <br /> broken land is a miscellaneous land type that consists of very steep, precipitous land broken by <br /> many intermittent drainage channels. It occurs primarily in gulches, and the slope is dominantly <br /> 35 to 70 percent. The soil material ranges from very shallow to deep. Stones and rock outcrops <br /> are common in some areas. Elevation ranges from near sea level to 3,000 feet, and the annual <br /> rainfall ranges from 50 inches to more than 150 inches. Vegetation varies with rainfall. Kukui <br /> trees are common in the gulches. There are a few, scattered waterfalls. Rough broken land is <br /> used for pasture, woodland, wildlife habitat, and recreation areas. Adapted pasture plants and <br /> yields are similar to those for soils associated with this land type. These soils are in Capability <br /> Class Vii. <br /> Soil capability grouping shows, in a general way, the suitability of soils for most kinds of field <br /> crops. Soils are classed from I to VIII, with Capability Class I being the best suited for <br /> agriculture and Class VIII being the least suited. The Pa`auilo Lands comprise soils in Classes <br /> ITT, TV,VT, and Vii. <br /> • Class III soils have severe limitations that reduce the choice of plants, require special <br /> conservation practices, or both. <br /> • Class IV soils have very severe limitations that reduce the choice of plants, require very <br /> careful management, or both. <br /> • Class VI soils have severe limitations that make them generally unsuited to cultivation <br /> and limit their use largely to pasture or range, woodland, or wildlife. <br /> 19 <br />
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