Official Series Description


Lab Data Summary

Aggregate lab data for the APRON soil series. This aggregation is based on all pedons with a current taxon name of APRON, 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 APRON 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
3240A3101S1965WY013011Apron6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.1205559,-108.3324966
3240A3102S1965WY013012Apron6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0694427,-108.3833313

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the APRON 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 APRON 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 APRON 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 APRON 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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Competing Series

Soil series competing with APRON 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 APRON 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 APRON 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.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with APRON, 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 APRON 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
Apron fine sandy loam, 4 to 7 percent slopesAs5048345679clpymt11119661:20000
Apron loamy fine sand, 4 to 7 percent slopesAr3395345678clpxmt11119661:20000
Worland-Persayo complex, 3 to 30 percent slopes805469152129539dwy04319761:24000
Apron-Worland sandy loams, 0 to 10 percent slopes32211152074537mwy04319761:24000
Apron-Worland sandy loams, 1 to 12 percent slopes41118152084537ywy04319761:24000
Apron sandy loam, 0 to 3 percent slopes28031520635378wy04319761:24000
Persayo-like-Apron-Cosmos-like complex, 4 to 35 percent slopesS30332533052ztk0wy6031:24000
Apron-Worland sandy loams, 0 to 35 percent slopes -- Draft442AD24309172mlkpwy6031:24000
Apron sandy loam, saline, 0 to 6 percent slopes -- Draftb1AB325338053wcwy6031:24000
Apron sandy loam, 0 to 10 percent slopes -- Draft42AC563215221053d0wy6031:24000
Apron sandy loam, 3 to 6 percent slopes -- Draft42B385515221153d1wy6031:24000
Apron sandy loam, 0 to 3 percent slopes -- Draft42A362515220953czwy6031:24000
Apron-Worland sandy loams, 3 to 10 percent slopes -- Draft442BC268715221953d9wy6031:24000
Apron sandy loam, 6 to 10 percent slopes -- Draft42C104315221253d2wy6031:24000
Apron sandy loam, 3 to 6 percent slopesApB2287715733158q6wy61319691:20000
Trook-Apron association, 0 to 6 percent slopesTUB1896215739258s5wy61319691:20000
Apron sandy loam, 0 to 3 percent slopesApA1133615733058q5wy61319691:20000
Trook-Clifterson association, moderately steepTVD801915739358s6wy61319691:20000
Apron sandy loam, 6 to 10 percent slopesApC296715733258q7wy61319691:20000
Apron sandy loam, saline, 0 to 6 percent slopesAtB238515733558qbwy61319691:20000
Apron sandy loam, alkali substratum, 0 to 6 percent slopesAsB61515733458q9wy61319691:20000
Effington-Apron associationEP46515734858qrwy61319691:20000
Apron sandy loam, wet, 0 to 6 percent slopesAuB39915733658qcwy61319691:20000
Apron sandy loam, alkali, 0 to 6 percent slopesArB32315733358q8wy61319691:20000
Apron sandy loam, 0 to 3 percent slopes -- Draft42A15256653rhwy6291:24000
Apron sandy loam, 0 to 10 percent slopes -- Draft42AC15256753rjwy6291:24000
Apron sandy loam, 3 to 6 percent slopes -- Draft42B15256853rkwy6291:24000
Apron-Wallson-Tipperary complex, 2 to 6 percent slopes820129690602wxlhwy6291:24000
Apron sandy loam, saline, 0 to 6 percent slopes -- Draftb1AB15268653wcwy6291:24000
Apron sandy loam, 0 to 2 percent slopesApA185673820b2swy6471:24000
Apron-Wallson-Worland association, 1 to 15 percent slopes0215115115743058tdwy6471:24000
Apron-Lostwells complex, 0 to 10 percent slopes011553015742358t5wy6471:24000
Binton-Apron, saline complex, 0 to 3 percent slopes08554461577065939wy6471:24000
Apron fine sandy loam, 0 to 6 percent slopes014349215743758tmwy6471:24000
Trook-Apron complex, 0 to 6 percent slopes408308516830591thc7wy6471:24000
Youngston-Lostwells-Apron complex, 0 to 3 percent slopes199449580427mgzgwy6471:24000
Apron sandy loam, 2 to 6 percent slopesApB61185687020b71wy6471:24000
Apron sandy loam, 6 to 10 percent slopesApC13185686920b70wy6471:24000
Trook-Clifterson-Apron association, 3 to 15 percent slopesTVD5185738120brjwy6471:24000
Apron-Wallson-Worland association, 1 to 15 percent slopes10922522502972jwcxwy71319861:24000
Apron-Lostwells complex, 0 to 10 percent slopes10811704502971jwcwwy71319861:24000
Youngston-Lostwells-Apron complex, 0 to 3 percent slopes2259402503105jwj6wy71319861:24000

Map of Series Extent

Approximate geographic distribution of the APRON 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 .