Official Series Description


Lab Data Summary

Aggregate lab data for the PRESTON soil series. This aggregation is based on all pedons with a current taxon name of PRESTON, and applied along 1-cm thick depth slices. Solid lines are the slice-wise median, bounded on either side by the interval defined by the slice-wise 5th and 95th percentiles. The median is the value that splits the data in half. Five percent of the data are less than the 5th percentile, and five percent of the data are greater than the 95th percentile. Values along the right hand side y-axis describe the proportion of pedon data that contribute to aggregate values at this depth. For example, a value of "90%" at 25cm means that 90% of the pedons correlated to PRESTON were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the PRESTON soil series. Monthly precipitation (PPT) and potential evapotranspiration (PET) have been estimated from the 50th percentile of gridded values (PRISM 1981-2010) overlapping with the extent of SSURGO map units containing each series as a major component. Monthly PET values were estimated using the method of Thornthwaite (1948). These (and other) climatic parameters are calculated with each SSURGO refresh and provided by the fetchOSD function of the soilDB package. Representative water storage values (“AWC” in the figures) were derived from SSURGO by taking the 50th percentile of profile-total water storage (sum[awc_r * horizon thickness]) for each soil series. Note that this representation of “water storage” is based on the average ability of most plants to extract soil water between 15 bar (“permanent wilting point”) and 1/3 bar (“field capacity”) matric potential. Soil moisture state can be roughly interpreted as “dry” when storage is depleted, “moist” when storage is between 0mm and AWC, and “wet” when there is a surplus. Clearly there are a lot of assumptions baked into this kind of monthly water balance. This is still a work in progress.

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Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the PRESTON series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

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Select annual climate data summaries for the PRESTON series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the PRESTON series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records .

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Competing Series

Soil series competing with PRESTON share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

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Select annual climate data summaries for the PRESTON series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the PRESTON series and competing. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Shannon entropy values close to 0 represent soil series with relatively consistent geomorphic association, while values close to 1 suggest lack thereof. Source: SSURGO component records .

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Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with PRESTON, arranged according to family differentiae. Hovering over a series name will print full classification and a small sketch from the OSD. Source: snapshot of SC database .

Block Diagrams

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. ID-2010-08-30-04 | Franklin County Area - 2008

    Typical pattern of soils and underlying material in general soil map unit 4 (Welby-Kidman-Preston) (Soil Survey of Franklin County Area, Idaho; 2008).

  2. UT-2012-03-22-03 | East Millard Area - June 1959

    East-west cross section in the northern part of the East Millard Area, near Lynndyl, showing position of soils on the landscape. 1—Mellor, Harding, Woodrow, and Lahontan soils. 2—Preston and Lynndyl soils. 3—Woodrow and Oasis soils. 4—Poganeab soils. 5—Preston and Taylorsflat soils and sand dunes. 6—Taylorsflat and Naples soils. 7—Canyon Mountains (Soil Survey of East Millard Area, UT; 1959).

Map Units

Map units containing PRESTON as a major component. Limited to 250 records.

Map Unit Name Symbol Map Unit Area (ac) Map Unit Key National Map Unit Symbol Soil Survey Area Publication Date Map Scale
Preston-Pass Canyon families association, 30 to 60 percent slopes.3439488471456htl8ca73219981:24000
Preston family-Rock outcrop complex, 30 to 60 percent slopes.3641065471477htlyca73219981:24000
Risue-Abgese-Preston families association, 2 to 15 percent slopes.1529883471568htpwca76319841:24000
Preston family, 1 to 15 percent slopes.1511459471567htpvca76319841:24000
Pacifico-Preston families complex, 15 to 50 percent slopes473930465354hm7fca77619811:24000
Pacifico-Preston families complex, 30 to 50 percent slopesDdF14710471628htrtca77719811:24000
Pacifico-Preston families complex, 2 to 30 percent slopesDdDE13865471627htrsca77719811:24000
Preston loamy sand, 6 to 30 percent slopes1252160485215j8x3id71419971:24000
Preston-Xerorthents complex, 35 to 60 percent slopes1261716485216j8x4id71419971:24000
Preston fine sand, 2 to 6 percent slopes1241613485214j8x2id71419971:24000
Preston fine sand, 0 to 2 percent slopes1231513485213j8x1id71419971:24000
Kidman-Preston association, 2 to 12 percent slopes621638485658j9cdid71519941:24000
PRESTON FINE SAND, 0 TO 10 PERCENT SLOPESPtC311482804j6dbut60319681:20000
Preston fine sand, 1 to 10 percent slopesPxB2247481636j55nut60719651:15840
Preston fine sand, duned, 1 to 10 percent slopesPyB1940481638j55qut60719651:15840
Preston fine sand, 10 to 20 percent slopesPxE479481637j55put60719651:15840
Preston sand, 1 to 10 percent slopesPrD2348482963j6kgut61219671:20000
Knutsen-Preston complex, 10 to 30 percent slopesKsF21783482941j6jrut61219671:20000
Preston sand, 10 to 30 percent slopesPrF658482964j6khut61219671:20000
Preston sandy loam, 1 to 3 percent slopesPsB574482965j6kjut61219671:20000
Kidman-Preston complex, 2 to 30 percent slopes76633481872j5f8ut61819951:24000
Preston fine sand, 2 to 30 percent slopes102422481778j5b7ut61819951:24000
Preston fine sand, 1 to 10 percent slopesPuD773483365j6zfut62119661:20000
Preston loamy fine sand, high water table variantPv285483366j6zgut62119661:20000

Map of Series Extent

Approximate geographic distribution of the PRESTON soil series. To learn more about how this distribution was mapped, or to compare this soil series extent to others, use the Series Extent Explorer (SEE) application. Source: generalization of SSURGO geometry .