Official Series Description


Lab Data Summary

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

Click the image to view it full size.

Click the image to view it full size.

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 PRILL, 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 PRILL 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
Wylie-Prill-Badland complex, 20 to 50 percent south slopes4005BO85312015621zl7or60720181:24000
Prill gravelly clay loam, 15 to 35 percent south slopes510925734346852mkvor6181:24000
Prill-Gwinly complex, 35 to 60 percent south slopes511536934261682mkyor6181:24000
Tub-Prill-Elderflat complex, 12 to 30 percent north slopes113316734349652mrnor6181:24000
Prill complex, 1 to 15 percent slopes512221934376292mkxor6181:24000
Prill-Tub-Elderflat complex, 35 to 60 percent north slopes114161634375182mrcor6181:24000
Prill-Kishwalk complex, 5 to 15 percent slopes184C55334262052nb2xor6181:24000
Prill-Kaskela-Gwinly complex, 10 to 35 percent south slopes171D51934262022lp3vor6181:24000
Prill-Gwinly complex, 2 to 20 percent slopes162C713426199nk6cor6181:24000
Prill-Gwinly complex, 2 to 20 percent slopes162C78583425091nk6cor6271:24000
Wylie-Prill-Badland complex, 20 to 50 percent south slopes161E7323342506921zl7or6271:24000
Prill-Starkey-Rock outcrop complex, 20 to 50 percent south slopes174D5576342510025xtlor6271:24000
Gwinly-Devnot-Prill complex, 2 to 20 percent slopes631C544234262482ss4qor6271:24000
Wylie-Prill complex, 2 to 20 percent slopes161C21443425101znhtor6271:24000
Tub-Prill-Rockly complex, 2 to 50 percent slopes172E13633425108nk6por6271:24000
Tub-Prill-Rockly association, 2 to 50 percent slopes172D133934294891nv9hor6271:24000
Tub-Prill-Badland complex, 20 to 50 percent north slopes165E11893429517nk6hor6271:24000
Prill-Starkey complex, 20 to 50 percent slopes174E11343429521vykvor6271:24000
Prill-Tub complex, MLRA 9, 2 to 20 percent slopes626C76334319512ss4mor6271:24000
Prill gravelly silty clay loam, 2 to 15 percent slopes138C31342509526hwor6271:24000
Watama-Rockly-Prill complex, 2 to 30 percent slopes153120976315123q4or67419931:24000
Prill-Kaskela-Rock outcrop complex, 2 to 30 percent slopes11072526306823mgor67419931:24000
Prill-Kaskela complex, 2 to 30 percent slopes10932806306523mcor67419931:24000
Prill-Rock outcrop complex, 30 to 55 percent slopes1113656307023mjor67419931:24000
Prill gravelly silty clay loam, 30 to 55 percent slopes1081896306323m9or67419931:24000
Prill-Gwinly complex, 2 to 20 percent slopes162C132013391654nk6cor6771:24000
Prill-Kishwalk complex, 5 to 15 percent slopes184C820533849882nb2xor6771:24000
Prill-Kaskela-Gwinly complex, 10 to 35 percent south slopes171D711733916372lp3vor6771:24000
Prill gravelly silty clay loam, 15 to 30 percent north slopes138D3999339164226j0or6771:24000
Zweygardt-Prill-Starkey complex, 25 to 55 percent south slopes187E317934217832p1zgor6771:24000
Prill-Starkey-Rock outcrop complex, 20 to 50 percent south slopes174D2898339168625xtlor6771:24000
Prill gravelly silty clay loam, 2 to 15 percent slopes138C2118339166426hwor6771:24000
Sweek-Prill complex, 2 to 20 percent south slopes180C92833916922ltsyor6771:24000
Prill-Starkey complex, 20 to 45 percent south slopes190E69233916982p5xtor6771:24000
Wylie-Prill-Badland complex, 20 to 50 percent south slopes161E572342443521zl7or6771:24000
Prill-Badland complex, 30 to 60 percent north slopes137E534339167226hxor6771:24000
Tub-Prill-Rockly complex, 2 to 50 percent slopes172E4843424538nk6por6771:24000
Wylie-Prill complex, 2 to 20 percent slopes161C2883391687znhtor6771:24000
Prill-Gwinly complex, 35 to 60 percent south slopes5117634247972mkyor6771:24000

Map of Series Extent

Approximate geographic distribution of the PRILL 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 .