Official Series Description


Lab Data Summary

Aggregate lab data for the SESAME soil series. This aggregation is based on all pedons with a current taxon name of SESAME, 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 SESAME 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 SESAME 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 SESAME 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 SESAME 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 SESAME 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 flats position figure.

Competing Series

Soil series competing with SESAME 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 SESAME 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 SESAME 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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Soil series sharing subgroup-level classification with SESAME, 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

No block diagrams are available.

Map Units

Map units containing SESAME 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
Sesame rocky loam, 3 to 8 percent slopesSfB383463160hjynca64819591:20000
Sesame rocky loam, 8 to 30 percent slopesSfD137463161hjypca64819591:20000
Sesame sandy loam, 3 to 8 percent slopesSyB1086463515hkb3ca65119591:20000
Vista-Sesame complex, 3 to 8 percent slopesVsB921463545hkc2ca65119591:20000
Sesame loam, 3 to 8 percent slopesSeB297463511hk9zca65119591:20000
Sesame rocky loam, 8 to 15 percent slopesSkC101463513hkb1ca65119591:20000
Sesame loam, 8 to 15 percent slopesSeC70463512hkb0ca65119591:20000
Sesame rocky sandy loam, 3 to 8 percent slopesSnB44463514hkb2ca65119591:20000
Sesame loam, 3 to 9 percent slopesSlB1614464453hl9cca65419661:24000
Sesame sandy loam, 3 to 9 percent slopesSkB1313464450hl98ca65419661:24000
Sesame sandy loam, 9 to 15 percent slopesSkC1059464451hl99ca65419661:24000
Sesame sandy loam, 15 to 30 percent slopesSkD305464452hl9bca65419661:24000
Sesame loam, 9 to 15 percent slopesSlC191464454hl9dca65419661:24000
Sesame sandy loam, 15 to 30 percent slopes1577963463622hkfkca66019771:24000
Arujo-Feethill-Sesame association, 15 to 45 percent slopes298nk49322181322dg4nca66019771:24000
Sesame sandy loam, 30 to 50 percent slopes158419463623hkflca66019771:24000
Sesame sandy loam, 9 to 15 percent slopes156333463621hkfjca66019771:24000
Sesame sandy loam, 9 to 30 percent slopes2001825457303hbvqca66519771:24000
Arujo-Feethill-Sesame association, 15 to 45 percent slopes29831130467389hpc2ca66820071:24000
Locobill-Backcanyon-Sesame complex, 20 to 60 percent slopes2709642467362hpb6ca66820071:24000
Sesame-Tweedy-Rock outcrop association, 30 to 60 percent slopes2749604467366hpbbca66820071:24000
Strahle-Sesame-Tweedy association, 30 to 75 percent slopes2758809467367hpbcca66820071:24000
Arujo-Feethill-Sesame association, 30 to 60 percent slopes2996269467465hpfjca66820071:24000
Tollhouse-Sesame-Friant association, 30 to 60 percent slopes2825945467374hpblca66820071:24000
Strahle-Rock outcrop-Sesame association, 30 to 60 percent slopes2793160467371hpbhca66820071:24000
Locobill-Backcanyon-Sesame complex, 20 to 60 percent slopes270ne80622180972dg3jca67019771:24000
Strahle-Rock outcrop-Sesame association, 30 to 60 percent slopes279ne50722181022dg3pca67019771:24000
Strahle-Sesame-Tweedy association, 30 to 75 percent slopes275ne20122180992dg3lca67019771:24000
Sesame-Tweedy-Rock outcrop association, 30 to 60 percent slopes274ne16423710282kl7sca76019811:24000
Locobill-Backcanyon-Sesame complex, 20 to 60 percent slopes270ne1823710252kl7pca76019811:24000

Map of Series Extent

Approximate geographic distribution of the SESAME 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 .