Official Series Description


Lab Data Summary

Aggregate lab data for the SAWYER soil series. This aggregation is based on all pedons with a current taxon name of SAWYER, 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 SAWYER were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
135B04N0319S03AR109005Sawyer7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.9820557,-93.4945526

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SAWYER 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 SAWYER 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 SAWYER 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 SAWYER 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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There are insufficient data to create the 3D mountains figure.

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Click the image to view it full size.

Competing Series

Soil series competing with SAWYER 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 SAWYER series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the SAWYER 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 .

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

There are insufficient data to create the 3D mountains figure.

There are insufficient data to create the 3D terrace figure.

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

Soil series sharing subgroup-level classification with SAWYER, 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. FL-2012-04-25-03 | Gadsden County - January 1961

    Geologic formations and some principal soils in relative positions (Soil Survey of Gadsden County, Florida; January 1961).

  2. MS-2012-04-27-11 | Newton County - February 1960

    Soil associations of Newton County, Mississippi (Soil Survey of Newton County, Mississippi; February 1960).

  3. TX-2012-03-21-05 | Harrison County - October 1994

    Pattern of soils and parent material in the Cuthbert-Bowie-Kirvin general soil map unit (Soil Survey of Harrison County, TX; 1994).

Map Units

Map units containing SAWYER 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
Sawyer fine sandy loamSa382329291c1n9al05119481:20000
Sawyer fine sandy loam, 0 to 2 percent slopesSeA1320329704c22mal06320131:
Sawyer fine sandy loam, eroded, very gently sloping phaseSbB22417330956c3d0al10119581:20000
Sawyer fine sandy loam, eroded, gently sloping phaseSbC21524330957c3d1al10119581:20000
Sawyer fine sandy loam, eroded, sloping phaseSbD2780330958c3d2al10119581:20000
Sawyer fine sandy loam, very gently sloping phaseSbB598330955c3czal10119581:20000
Sawyer sandy clay loam, severely eroded, sloping phaseScD3479330960c3d4al10119581:20000
Sawyer sandy clay loam, severely eroded, gently sloping phaseScC3274330959c3d3al10119581:20000
Sawyer very fine sandy loam, nearly level phaseSfB3187565196lz44ar01119591:20000
Sawyer very fine sandy loam, eroded nearly level phaseSfB22473565197lz45ar01119591:20000
Sawyer very fine sandy loam, eroded gently sloping phaseSfC21264565199lz47ar01119591:20000
Sawyer very fine sandy loam, gently sloping phaseSfC1188565198lz46ar01119591:20000
Sawyer very fine sandy loam, level phaseSfA606565195lz43ar01119591:20000
Sawyer very fine sandy loam, moderately steep phase (sacul)SfE217565200lz48ar01119591:20000
Sawyer loam, 3 to 8 percent slopes7232193179409lyp7ar01919831:20000
Sawyer loam, 1 to 3 percent slopes7124293179408lyp6ar01919831:20000
Sawyer very fine sandy loam, 1 to 8 percent slopes14C2109317159061vljtar05320061:24000
Sawyer loam, 3 to 8 percent slopes4416532565671lzmgar05719761:20000
Sawyer loam, 1 to 3 percent slopes4310231565670lzmfar05719761:20000
Sawyer loam, 3 to 8 percent slopes7226513179299lyp7ar05919831:20000
Sawyer loam, 1 to 3 percent slopes7122233179298lyp6ar05919831:20000
Sawyer very fine sandy loam, 3 to 8 percent slopesSrC21622721518s6ssar09920001:24000
Sawyer very fine sandy loam, 1 to 3 percent slopesSrB1637721517s6srar09920001:24000
Sacul-Sawyer complex, 1 to 8 percent slopesScC1766455792072zry6ar13919921:24000
Sacul-Sawyer complex, 8 to 15 percent slopesScD27350579206mfq2ar13919921:24000
Sawyer very fine sandy loam, 1 to 8 percent slopesSeC23191579188mfphar13919921:24000
Sacul-Sawyer association, gently rolling1920658564673lyl8ar62019771:20000
Sawyer silt loam, 3 to 8 percent slopes246284564679lylgar62019771:20000
Sawyer silt loam, 1 to 3 percent slopes232137564678lylfar62019771:20000
Sawyer silt loam, 3 to 8 percent slopes4616325564869lyslar66019751:20000
Sawyer silt loam, 1 to 3 percent slopes4512494564868lyskar66019751:20000
Sawyer silt loam, 1 to 3 percent slopes6911829564946lyw2ar67019811:20000
Sawyer silt loam, 3 to 8 percent slopes704593564948lyw4ar67019811:20000
Sawyer silt loam, 3 to 8 percent slopes3311462564317ly6sar68019801:20000
Sawyer-Susquehanna cobbly loamy sands, 2 to 8 percent slopes, erodedSSC2615324660bwtxga09519651:20000
Sawyer-Susquehanna loamy sands, 2 to 5 percent slopes, erodedSUB2610324661bwtyga09519651:20000
Sawyer-Susquehanna cobbly loamy sands, 0 to 5 percent slopesSSB595324659bwtwga09519651:20000
Sawyer loamy sand, 2 to 5 percent slopesSfB3765324824bx06ga16519661:20000
Sawyer loamy sand, 5 to 8 percent slopes, erodedSfC21595324825bx07ga16519661:20000
Sawyer, Norfolk, and Cuthbert loamy sands, 2 to 5 percent slopesSlB1900324998bx5tga28319621:20000
Sawyer, Norfolk, and Cuthbert loamy sands, 5 to 8 percent slopes, erodedSlC2780325001bx5xga28319621:20000
Sawyer, Norfolk, and Cuthbert loamy sands, 2 to 5 percent slopes, erodedSlB2765324999bx5vga28319621:20000
Sawyer, Norfolk, and Cuthbert loamy sands, 5 to 8 percent slopesSlC475325000bx5wga28319621:20000
Gilead (cowarts), Lakeland (blanton), and Sawyer (nankin) soils, 5 to 8 percent slopesGCC2525125071464kga30519621:20000
Gilead (cowarts), Lakeland (blanton), and Sawyer (nankin) soils, 2 to 5 percent slopesGCB1960125069464hga30519621:20000
Gilead (cowarts), Lakeland (blanton), and Sawyer (nankin) soils, 8 to 12 percent slopesGCD825125073464mga30519621:20000
Gilead (cowarts), Lakeland (blanton), and Sawyer (nankin) soils, 5 to 8 percent slopes, erodedGCC2625125072464lga30519621:20000
Gilead (cowarts), Lakeland (blanton), and Sawyer (nankin) soils, 2 to 5 percent slopes, erodedGCB2575125070464jga30519621:20000
Gilead (cowarts), Lakeland (blanton), and Sawyer (nankin) soils, 17 to 30 percent slopes, erodedGCF2280125076464qga30519621:20000
Gilead (cowarts), Lakeland (blanton), and Sawyer (nankin) soils, 12 to 17 percent slopes, erodedGCE2270125075464pga30519621:20000
Gilead (cowarts), Lakeland (blanton), and Sawyer (nankin) soils, 8 to 12 percent slopes, erodedGCD2240125074464nga30519621:20000
Sawyer very fine sandy loam, 1 to 5 percent slopesSnC1809017246071vwlhla01319921:24000
Sawyer very fine sandy loam, 1 to 5 percent slopesSnC65190322121wg7la06919831:24000
Sawyer very fine sandy loam, 1 to 5 percent slopesSaC3824013842llv0la08119731:24000
Sawyer silt loam, 1 to 5 percent slopesSk1118017253641vxcxla11119921:24000
Sawyer silt loam, 5 to 8 percent slopesSL186417253651vxcyla11119921:24000
Sawyer very fine sandy loam, 1 to 5 percent slopesSeC598117255731vxlnla11519921:24000
Sawyer silt loam, 0 to 3 percent slopes36111025575282m9mhtx03719781:20000
Sawyer-Urban land complex, 0 to 3 percent slopes371757575283m9mjtx03719781:20000
Sawyer very fine sandy loam, 0 to 2 percent slopesSrA12429576463mbvltx20319891:24000

Map of Series Extent

Approximate geographic distribution of the SAWYER 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 .