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the orientation of a soil sample relative to the orientation of a soil profile and the orientation of adjacent minerals is important in interpreting laboratory measurements. for example, when an edge of a horizontal section is above an adjacent soil horizon, a significant change in properties of the soil is likely to be present. similarly, if a profile is cut horizontally or diagonally, the properties of a shallow sample represent the properties of the soil not covered by the cutting.


the size of sample and the relationship of the sample to the rest of the soil profile are both important in interpreting laboratory measurements. the diameter or length of a sample should be described relative to the whole profile and to adjacent minerals. also, the size of sample should be described relative to the size of the whole profile. careful analysis of laboratory data is often obscured because of a focus on soil properties, such as those presented in the lab, rather than on the soil.


soil profiles with parallel ridges result from the accumulation of colluvium, loess, or other stream-bed soil, which may be graded laterally (horizontally) in thickness. parallel ridges may form when soils are saturated during the annual runoff season and then dried in summer. modern field descriptions should include the number of ridges and, when possible, their orientation relative to a profile. a ridge is defined as a continuous group of soil horizons, which run parallel to each other, except possibly for a few meters at each end. interpretation of the location of these ridges relative to the rest of the profile is based upon field experience and the distribution of grain sizes. the addition of parallel ridges may change the interpretation of the radial distribution of properties. 84d34552a1