Official Series Description


Lab Data Summary

Aggregate lab data for the RILEA soil series. This aggregation is based on all pedons with a current taxon name of RILEA, 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 RILEA 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
192P1053S1992OR011001Rilea6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.746666,-124.1497192
192P1055S1992OR015006Rilea6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.6511116,-124.1319427

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the RILEA 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 RILEA 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 RILEA 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 RILEA 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 hills figure.

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There are insufficient data to create the 3D terrace figure.

There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with RILEA 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 RILEA series and competing. 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 RILEA 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 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 RILEA, 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 RILEA 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
Stackyards-Rilea-Yorel complex, cool, 30 to 60 percent north slopes82E8216126621rbor01119831:20000
Bobsgarden-Rilea-Yorel complex, cool, 0 to 30 percent slopes70D7246125421qyor01119831:20000
Stackyards-Rilea-Euchrand complex, cool, 60 to 90 percent north slopes78F3556126221r6or01119831:20000
Bobsgarden-Rilea-Euchrand complex, cool, 60 to 90 percent south slopes67F1786124721qqor01119831:20000
Stackyards-Rilea-Rock outcrop complex, cool, 30 to 60 percent north slopes81E1616126521r9or01119831:20000
Rilea-Stackyards-Rock outcrop complex, cool, 60 to 90 percent north slopes76F1576126021r4or01119831:20000
Bobsgarden-Rilea-Euchrand complex, 60 to 90 percent south slopes68F1436124921qsor01119831:20000
Bobsgarden-Rilea-Rock outcrop complex, conglomerate substratum, 30 to 60 percent south slopes69E1176125021qtor01119831:20000
Stackyards-Rilea-Euchrand complex, 60 to 90 percent north slopes79F846126321r7or01119831:20000
Bobsgarden-Rilea-Euchrand complex, cool, 30 to 60 percent south slopes67E556124621qpor01119831:20000
Bobsgarden-Rilea-Euchrand complex, 30 to 60 percent south slopes68E476124821qror01119831:20000
Stackyards-Rilea-Rock outcrop complex, conglomerate substratum, cool, 30 to 60 percent north slopes80E406126421r8or01119831:20000
Bobsgarden-Rilea-Rock outcrop complex, conglomerate substratum, 60 to 90 percent south slopes69F166125121qvor01119831:20000
Stackyards-Rilea-Yorel complex, 30 to 60 percent north slopes251F42506528525xzor01519951:24000
Bobsgarden-Rilea-Euchrand complex, 30 to 60 percent south slopes28F3782653512603or01519951:24000
Bobsgarden-Rilea-Rock outcrop complex, 30 to 60 percent south slopes31F287365375260wor01519951:24000
Stackyards-Rilea-Yorel complex, cool, 30 to 60 percent north slopes250F27736528325xxor01519951:24000
Bobsgarden-Rilea-Yorel complex, 0 to 30 percent slopes33E2368653842615or01519951:24000
Rilea-Euchrand-Rock outcrop complex, 60 to 90 percent south slopes211G21186519025txor01519951:24000
Stackyards-Rilea-Rock outcrop complex, 30 to 60 percent north slopes249F20226527825xror01519951:24000
Stackyards-Rilea-Euchrand complex, cool, 60 to 90 percent north slopes244G18716526725xdor01519951:24000
Bobsgarden-Rilea-Yorel complex, cool, 0 to 30 percent slopes32E1631653802611or01519951:24000
Rilea-Stackyards-Rock outcrop complex, 60 to 90 percent north slopes213G14146519425v1or01519951:24000
Bobsgarden-Rilea-Euchrand complex, cool, 30 to 60 percent south slopes27F12916534225ztor01519951:24000
Bobsgarden-Rilea-Rock outcrop complex, conglomerate substratum, 30 to 60 percent south slopes29F111665363260hor01519951:24000
Stackyards-Rilea-Euchrand complex, 60 to 90 percent north slopes245G11076526925xgor01519951:24000
Bobsgarden-Rilea-Rock outcrop complex, conglomerate substratum, 60 to 90 percent south slopes29G80265364260jor01519951:24000
Bobsgarden-Rilea-Euchrand complex, cool, 60 to 90 percent south slopes27G7026534325zvor01519951:24000
Bobsgarden-Rilea-Rock outcrop complex, cool, 30 to 60 percent south slopes30F70065368260nor01519951:24000
Bobsgarden-Rilea-Euchrand complex, 60 to 90 percent south slopes28G526653522604or01519951:24000
Stackyards-Rilea-Rock outcrop complex, conglomerate substratum, cool, 60 to 90 percent north slopes246G4306527125xjor01519951:24000
Rilea-Stackyards-Rock outcrop complex, cool, 60 to 90 percent north slopes212G4216519225tzor01519951:24000
Stackyards-Rilea-Rock outcrop complex, conglomerate substratum, 60 to 90 percent north slopes247G4036527425xmor01519951:24000
Bobsgarden-Rilea complex, conglomerate substratum, 0 to 30 percent slopes34E314653872618or01519951:24000
Stackyards-Rilea-Rock outcrop complex, conglomerate substratum, 30 to 60 percent north slopes247F2426527325xlor01519951:24000
Stackyards-Rilea-Rock outcrop complex, conglomerate substratum, cool, 30 to 60 percent north slopes246F2016527025xhor01519951:24000
Stackyards-Rilea-Rock outcrop complex, cool, 30 to 60 percent north slopes248F1846527625xpor01519951:24000
Rilea-Euchrand-Rock outcrop complex, cool, 60 to 90 percent south slopes210G1836518825tvor01519951:24000

Map of Series Extent

Approximate geographic distribution of the RILEA 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 .