Official Series Description


Lab Data Summary

Aggregate lab data for the PHAROAH soil series. This aggregation is based on all pedons with a current taxon name of PHAROAH, 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 PHAROAH 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
11213N0439S2012OK035001Pharoah7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.8586528,-95.1248333
11213N0448S2012OK147001Pharoah7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.9923722,-95.8247556

Water Balance

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

Competing Series

Soil series competing with PHAROAH 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 PHAROAH 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 PHAROAH 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 PHAROAH, 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 PHAROAH 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
Pharoah silt loam, 0 to 1 percent slopesCa5285571588m5sbok02919691:24000
Pharoah silt loam, 0 to 1 percent slopesCa8841064932w7kzok03519681:20000
Okemah-Pharoah complex, 1 to 3 percent slopesOkB80835716462zcc3ok06319651:24000
Okemah-Pharoah complex, 1 to 3 percent slopes, erodedOkB216275716472zcc4ok06319651:24000
Pharoah silt loam, 0 to 1 percent slopes478365717512w7kzok09119801:24000
Pharoah silt loam, 1 to 3 percent slopes, eroded56774571762m5yyok09119801:24000
Pharoah-Burwell complex, 0 to 3 percent slopes62185571770m5z6ok09119801:24000
Parsons-Pharoah complex, 0 to 1 percent slopes5517871064192w7l0ok10119841:24000
Okemah-Pharoah-Parsons complex, 0 to 1 percent slopesOPPA154473841902zcc2ok10719961:24000
Dennis, Eram and Pharoah soils, 1 to 8 percent slopes, severely erodedDEPD3127173841442wqfjok10719961:24000
Pharoah-Oil waste land complex, 1 to 5 percent slopesPOWD4247384194dwscok10719961:24000
Pharoah-Parsons complex, 0 to 1 percent slopesDwA34191064602w7l1ok11119681:24000
Agra-Pharoah complex, 1 to 5 percent slopes17436746234122y2s8ok11319751:24000
Parsons-Pharoah complex, 0 to 3 percent slopes4921325623444nxr3ok11319751:24000
Dennis-Pharoah-Eram complex, 3 to 5 percent slopes, severely erodedDnC322927571541m5qtok12119661:24000
Parsons-Pharoah complex, 1 to 3 percent slopes, erodedPdB26085571563m5rjok12119661:24000
Parsons-Pharoah complex, 0 to 1 percent slopesPaPA732697359rdngok12119661:24000
Pharoah silt loam, 0 to 1 percent slopesDwA2492384621dx74ok12319671:24000
Pharoah silt loam, 0 to 1 percent slopes51268384712dxb2ok12519751:24000
Pharoah silt loam, 0 to 1 percent slopesDwA2741066602w7kzok13119631:24000
Okemah-Pharoah complex, 0 to 3 percent slopes321734384819dxfjok13319761:24000
Okemah-Parsons-Pharoah complex, 0 to 1 percent slopes44272051067272zcc1ok14319751:12000
Dennis-Pharoah complex, 1 to 3 percent slopes15220361066952wqf6ok14319751:12000
Pharoah silt loam, 0 to 1 percent slopesBv4941067522w7kzok14519721:24000
Pharoah-Parsons complex, 0 to 1 percent slopesDwA17231068042w7l1ok14719651:20000

Map of Series Extent

Approximate geographic distribution of the PHAROAH 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 .