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soils with a cyclic rainfall system will usually have two wet periods in the summer. the rainfall in the fall also can be variable. these soils commonly have a greater than normal water potential at tileline but under dry conditions flow back to an irrigated agricultural mode. such soils are usually identified by high organic matter content, dark coloration, and a porous soil texture (e.g., a high n value).
a soil is described as ‘well drained’ when enough water is available for plant use for periods of months during the winter and spring months. such soils may be referred to as u-type, z-type, or weakly drained, depending on the depth to which the water drains. well drained soils are typically composed of silty loam, silt loam, or sandy clay loam soil types.
the pxós of the us soil classification are summarized in table 2.1. the pxós of subsoils are derived from the parent soil by fractional sampling, thus a pxó of a subsoil may be greater than the pxó of its parent soil. the pxós reported in table 2.1 are derived from the soil classification nomenclature, which is no longer the official national cooperative soil survey system (ncss) soil classification methodology. new soil classifications are being developed by the ncss to replace the pxó nomenclature. soil classifications not listed in the pxó column are listed in the parent soil column.
the design criteria for foundation construction may include the size, depth, and number of the footings and pillars to be driven. if footings and pillars are required, design and test the subsoil in the area to evaluate the stability of the footing and any associated lateral settlement.
while the percentage of farmland converted from grass or soybean to winter wheat is increasing, the percentage converted to corn and grain sorghum has been declining, thereby decreasing the yield and potential for future erosion.
soil erosion and runoff are expressed as both loss and runoff. total loss is the volume lost as rainwater and lateral flow. runoff is the volume of run-off measured at the soil surface during one storm event. runoff is divided into the amount discharged during the storm and the amount discharged during a time interval after the storm. in some cases, an interval is specified for the runoff measurement (e.g., 1, 2, 4, 8, 24, or 48 hours). runoff is divided into either total runoff or peak runoff. total runoff is the volume of run-off as measured from the soil surface during a specified time interval and can be a period beginning with the beginning of the storm that is followed by a specified time interval.
if the rub data is available, sia is based on a dri2000 scale of three-point densities ranging from 1 for very light (a minimum of 1 kg/m3) to 3 for very dense (a minimum of 21 kg/m3). if the rub data is not available, sia is based on a dri2000 scale of four-point densities ranging from 1 for very light to 4 for very dense. the sia range is 1 to 4 for very light to very dense.
soil water retention. water retention is the capacity of soils to retain water. as a result, the rub is a measure of the soil’s capacity to retain moisture and remains reasonably constant at 0 to 4.7 cm (1-2 inches). water retention is significant because it is the principal contributor to the rate at which moisture may be lost through irrigation, evaporation, transpiration, and other factors.
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