Official Series Description


Lab Data Summary

Aggregate lab data for the RUDDLEY soil series. This aggregation is based on all pedons with a current taxon name of RUDDLEY, 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 RUDDLEY 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
43C98P0242S1997OR023032RUDDLEY6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.518611,-118.630556

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the RUDDLEY 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 RUDDLEY 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 RUDDLEY 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 RUDDLEY 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 terrace figure.

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

Competing Series

Soil series competing with RUDDLEY 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 RUDDLEY 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 RUDDLEY 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 RUDDLEY, 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 RUDDLEY 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
Daxty-Ruddley complex, 2 to 20 percent slopes4080AO140733853432qcy9or62620181:24000
Humarel-Ruddley complex, 2 to 20 percent slopes4081AO79333853442qcytor62620181:24000
Lemonex-Ruddley complex, 2 to 20 percent slopes4091AO31533852812wj7ror62620181:24000
Ruddley-Dupratt complex, 20 to 50 percent north slopes4086CO15733853482wj7qor62620181:24000
Lemonex-Ruddley complex, 20 to 50 percent north slopes4331AO8633854152wj80or62620181:24000
Humarel-Ruddley complex, 20 to 50 percent south slopes4081CO7233853452wj7por62620181:24000
Ruddley-Overholt complex, 2 to 20 percent slopes4090AO2433853522sz5yor62620181:24000
Bluecanyon-Ruddley complex, 20 to 50 percent north slopes4326NO2233854102sz69or62620181:24000
Ruddley-Bocker complex, 2 to 20 percent slopes4084AO2033852802qczqor62620181:24000
Ruddley-Rock outcrop complex, 5 to 30 percent slopes4308NO933852862lh85or62620181:24000
Ruddley-Bocker complex, 2 to 20 percent slopes480C322134262912qczqor6271:24000
Daxty-Ruddley complex, 2 to 20 percent slopes477C233134263622qcy9or6271:24000
Ruddley-Quirk-Alding complex, 2 to 20 percent slopes482C225234263652qcztor6271:24000
Lemonex-Ruddley complex, 20 to 50 percent north slopes487E178834294432wj80or6271:24000
Lemonex-Ruddley complex, 2 to 20 percent slopes487C167334294372wj7ror6271:24000
Humarel-Ruddley complex, 2 to 20 percent slopes478C141534294732qcytor6271:24000
Ruddley-Dupratt complex, 20 to 50 percent north slopes483E133434294902wj7qor6271:24000
Ruddley-Overholt complex, 2 to 20 percent slopes486C131034294912sz5yor6271:24000
Ruddley-Dupratt complex, slumps, 2 to 50 percent slopes489E96734295602sz6dor6271:24000
Deck-Analulu-Ruddley complex, 2 to 20 percent slopes481C75934319522w6bgor6271:24000
Humarel-Ruddley complex, 20 to 50 percent south slopes478E62034319952wj7por6271:24000
Daxty-Ruddley complex, 20 to 50 percent north slopes477D41034321002sz5qor6271:24000
Ruddley-Rock outcrop complex, 5 to 30 percent slopes269C8834346632lh85or6271:24000
Deck-Analulu-Ruddley complex, 20 to 50 percent slopes481D6434251682qczror6271:24000
Deck-Analulu-Ruddley complex, 20 to 50 percent slopes481D8834247922qczror6771:24000

Map of Series Extent

Approximate geographic distribution of the RUDDLEY 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 .