Official Series Description


Lab Data Summary

Aggregate lab data for the RITCHEY soil series. This aggregation is based on all pedons with a current taxon name of RITCHEY, 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 RITCHEY 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 RITCHEY 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 RITCHEY 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 RITCHEY 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 RITCHEY 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 RITCHEY 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 RITCHEY 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 RITCHEY 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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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 RITCHEY, 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 RITCHEY 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
Ritchey silt loam, 6 to 12 percent slopes311D6429881401257hil09120031:12000
Ritchey silt loam, 2 to 4 percent slopes311B3019881381257fil09120031:12000
Ritchey silt loam, 4 to 6 percent slopes311C2599881391257gil09120031:12000
Marseilles, Northfield, and Ritchey silt loams, 30 to 60 percent slopes794G435413868951hk5kil09920061:12000
Ritchey silt loam, 2 to 4 percent slopes311B672634858v5jil09920061:12000
Ritchey silt loam, 6 to 12 percent slopes311D154618704nrt6il19720021:12000
Ritchey silt loam, 4 to 6 percent slopes311C85635442pb74il19720021:12000
Ritchey loam, 2 to 6 percent slopesRhB10691721805s56oh04319981:12000
Ritchey loam, 0 to 2 percent slopesRhA10301721795s55oh04319981:12000
Ritchey loam, 6 to 12 percent slopesRhC2141721815s57oh04319981:12000
Ritchey and Romeo silt loams, 12 to 35 percent slopes, moderately erodedRmF21381692695p49oh04719681:15840
Ritchey and Romeo silt loams, 2 to 12 percent slopesRmC1381692685p48oh04719681:15840
Ritchey silt loam, 2 to 6 percent slopesRhB7531679315mr4oh04919771:15840
Ritchey silt loam, 12 to 18 percent slopes, erodedRhD25551679325mr5oh04919771:15840
Ritchey silt loam, 12 to 18 percent slopesRhD3671693415p6moh05719741:15840
Ritchey silt loam, 2 to 6 percent slopesRhB3041693395p6koh05719741:15840
Ritchey silt loam, 18 to 25 percent slopes, moderately erodedRhE22611693425p6noh05719741:15840
Ritchey silt loam, 6 to 12 percent slopesRhC2191693405p6loh05719741:15840
Ritchey silt loam, 18 to 50 percent slopesRhE2691695365pdxoh10919731:15840
Ritchey silt loam, 2 to 6 percent slopesRhB1701695345pdvoh10919731:15840
Ritchey silt loam, 6 to 18 percent slopesRhC1341695355pdwoh10919731:15840
Ritchey silt loam, 12 to 25 percent slopes, moderately erodedReE25051703055q6qoh11319691:15840
Ritchey silt loam, 6 to 12 percent slopes, moderately erodedReC24221703045q6poh11319691:15840
Ritchey silt loam, 25 to 50 percent slopes, moderately erodedReF23581703065q6roh11319691:15840
Ritchey silt loam, 2 to 6 percent slopesReB2551703025q6moh11319691:15840
Ritchey silt loam, 2 to 6 percent slopes, moderately erodedReB21821703035q6noh11319691:15840
Ritchey silty clay loam, 6 to 18 percent slopes, severely erodedRfD3971703075q6soh11319691:15840
Ritchey silt loam, 1 to 6 percent slopesRpB18315922211qftzoh14719781:15840
Ritchey loam, 2 to 6 percent slopesRsB815922071qftjoh14719781:15840
Ritchey loam, 0 to 2 percent slopesRhA5391682715n33oh17320001:12000
Ritchey loam, 2 to 6 percent slopesRhB1991682725n34oh17320001:12000
Ritchey loam, stony, 0 to 2 percent slopesRkA1041682735n35oh17320001:12000
Ritchey silt loam, 1 to 6 percent slopesRhB20951696585pjvoh17519801:15840
Ritchey silt loam, 6 to 12 percent slopesRhC2021696595pjwoh17519801:15840
Rock land and Ritchey soils, 6 to 45 percent slopesRkE1226423746g6y7wi04719741:20000
Ritchey silt loam, 6 to 12 percent slopes, erodedRhC2948423744g6y5wi04719741:20000
Ritchey silt loam, 12 to 20 percent slopes, erodedRhD2663423745g6y6wi04719741:20000
Ritchey silt loam, 2 to 6 percent slopes, erodedRhB2524423743g6y4wi04719741:20000
Ritchey silt loam, 1 to 6 percent slopesRkB953403335g95zwi07920231:15840
Ritchey silt loam, mottled subsoil variant, 1 to 3 percentRlA253403329g962wi07920231:15840
Ritchey silt loam, 6 to 12 percent slopes, erodedRkC223403334g960wi07920231:15840
Ritchey silt loam, 0 to 6 percent slopesRkB200426013g99cwi08919671:15840
Ritchey silt loam, 6 to 20 percent slopes, erodedRkD2125426014g99dwi08919671:15840
Ritchey soils and rock outcrop, 20 to 35 percent slopesRoE6334422188g59zwi10919751:15840
Ritchey silt loam, 12 to 20 percent slopes, erodedRnD21304422187g59ywi10919751:15840
Ritchey silt loam, 6 to 12 percent slopes, erodedRnC2500422186g59xwi10919751:15840
Ritchey silt loam, 2 to 6 percent slopesRnB362422185g59wwi10919751:15840
Ritchey silt loam, 2 to 6 percent slopesRkB492425767g91fwi13119671:15840
Ritchey silt loam, 6 to 12 percent slopes, erodedRkC2188425768g91gwi13119671:15840
Ritchey silt loam, 1 to 6 percent slopesRkB8723403504g95zwi13320231:15840
Ritchey silt loam, mottled subsoil variant, 1 to 3 percentRlA7873403496g962wi13320231:15840
Ritchey silt loam, 6 to 12 percent slopes, erodedRkC22093403503g960wi13320231:15840
Ritchey silt loam, 12 to 30 percent slopesRkE1593403500g961wi13320231:15840
Ritchey silt loam, 6 to 12 percent slopes, erodedRhC2430422826g5zkwi13919771:20000
Ritchey silt loam, 2 to 6 percent slopesRhB394422825g5zjwi13919771:20000
Ritchey silt loam, 12 to 30 percent slopes, erodedRhD2347422827g5zlwi13919771:20000

Map of Series Extent

Approximate geographic distribution of the RITCHEY 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 .