Official Series Description


Lab Data Summary

Aggregate lab data for the SEES soil series. This aggregation is based on all pedons with a current taxon name of SEES, 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 SEES 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
14740A4039S1960WV003003Sees6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4747505,-78.032486
14740A4040S1960WV003004Sees6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4400291,-78.0563736
99HK-0081956-OH063-008Sees3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.9821129,-83.5605698

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SEES 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 SEES 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 SEES 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 SEES 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 SEES 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 SEES series and competing. 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 SEES 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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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 SEES, 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. KY-2012-01-26-23 | Bath County - September 1963

    Typical landscape showing the relative position of the principal soils in a limestone valley in association 9 (Soil Survey of Bath County, Kentucky; September 1963).

  2. KY-2012-01-26-25 | Bath County - September 1963

    Cross section of Bath County showing the major soils and their relationship to the rock formations and to relief (Soil Survey of Bath County, Kentucky; September 1963).

  3. OH-2012-02-16-34 | Monroe County - March 1974

    Relationships of soils in associations 1 and 6 to topography and underlying materials along the Ohio River (Soil Survey of Monroe County, Ohio; March 1974).

Map Units

Map units containing SEES 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
Sees silt loam, 2 to 4 percent slopes, occasionally floodedSe375550318lgn6ky13519981:20000
Sees silt loam, 0 to 4 percent slopes, rarely floodedSc331550539lgwbky17319831:20000
Sees silty clay loam, 12 to 18 percent slopes, moderately erodedSeD24401688235nnxoh02519721:20000
Sees silty clay loam, 4 to 12 percent slopes, moderately erodedSeC22841688225nnwoh02519721:20000
Sees silty clay loam, 2 to 6 percent slopesSeB467536947l0qwoh05919981:15840
Sees-Woolper silt loams, 18 to 35 percent slopesSsE1997537818l1mzoh11119681:15840
Vandalia-Sees silt loams, 18 to 35 percent slopesVdE917537825l1n6oh11119681:15840
Sees-Woolper silt loams, 12 to 18 percent slopesSsD505537817l1myoh11119681:15840
Woolper and Sees silt loams, 6 to 12 percent slopesWyC124537838l1nmoh11119681:15840
Vandalia-Sees very stony silt loams, 18 to 35 percent slopes, moderately erodedVsE2102537826l1n7oh11119681:15840
Sees silty clay loamSc940523579kktntn18719611:15840
Sees silt loamSc369515437k9c0wv07519921:24000

Map of Series Extent

Approximate geographic distribution of the SEES 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 .