Official Series Description


Lab Data Summary

Aggregate lab data for the POGANEAB soil series. This aggregation is based on all pedons with a current taxon name of POGANEAB, 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 POGANEAB 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
28A00P031799UT027001Poganeab8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4258614,-112.6534729

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the POGANEAB 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 POGANEAB 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 POGANEAB 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 POGANEAB 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 POGANEAB 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 POGANEAB 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 POGANEAB 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 POGANEAB, 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. 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 POGANEAB 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
Poganeab silty clay loam, nearly levelPoB1262507870k1gxnm67019761:24000
Green River-Poganeab complex, 0 to 3 percent slopes512777481845j5ddut61819951:24000
Poganeab silt loamPg5090482318j5wnut62719711:24000
Anco-Poganeab-Job complex, 0 to 2 percent slopesA2342824539672nck7ut62719711:24000
Poganeab silt loam, strongly saline-alkaliPh1490482319j5wput62719711:24000
Poganeab silt loam, high lime variantPk900482320j5wqut62719711:24000
Chipman-Poganeab variant complexCm560482235j5szut62719711:24000
Poganeab-Abcal complex, 0 to 1 percent slopes1812802483579j76but6281:24000
Anco-Poganeab-Job complex, 0 to 2 percent slopes1062259483410j70wut6281:24000
Poganeab-Griver complex, 0 to 1 percent slopes1822176483578j769ut6281:24000
Anco-Green River-Poganeab complex, 0 to 4 percent slopes1032071483409j70vut6281:24000
Anco-Green River-Poganeab complex, 0 to 4 percent slopes103104325045222r80gut6291:24000
Poganeab-Griver complex, 0 to 1 percent slopes18270325105882r81nut6291:24000
Poganeab silty clay loam, strongly salinePr6443482415j5zsut63219701:20000
Poganeab silty clay loamPo6350482414j5zrut63219701:20000
Poganeab-Uffens-Uvada associationPU1729482411j5znut63219701:20000
Poganeab silty clay loam, sandy substratumPt1574482416j5ztut63219701:20000
Poganeab clay loam, 1 to 3 percent slopesPxB1000484672j8blut64019671:20000
Poganeab clay loam, deep over clay, 1 to 3 percent slopesPyB380484673j8bmut64019671:20000
James Canyon silty clay loam, heavy variant, salineJo265484614j88qut64019671:20000

Map of Series Extent

Approximate geographic distribution of the POGANEAB 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 .