Official Series Description


Lab Data Summary

Aggregate lab data for the RICHINDE soil series. This aggregation is based on all pedons with a current taxon name of RICHINDE, 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 RICHINDE 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
2905N0664S2005NV017003Richinde7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.8371811,-114.9091797

Water Balance

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

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

Soil series sharing subgroup-level classification with RICHINDE, 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 RICHINDE 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
Chubard-Richinde association, steepCRF477519042432whp4nv61119671:24000
Chubard-Richinde associationCRE55719042412whpbnv61119671:24000
Chubard-Richinde-Rock outcrop association, steepCRO19319042422whp6nv61119671:24000
Chubard-Richinde-Zoate association21322588024807132p8d0nv71320141:24000
Richinde-Rock outcrop association2130606324807122v42tnv71320141:24000
Chubard-Rock outcrop-Richinde association1736315224806242p894nv71320141:24000
Chubard-Richinde association2292637619046732whpbnv75419921:24000
Richinde-Chubard-Rock outcrop association22904161190467221xz1nv75419921:24000
Chubard-Richinde association, steep2298261719046752whp4nv75419921:24000
Richinde-Rock outcrop association1993148919046812v42tnv75419921:24000
Richinde-Pintwater-Rock outcrop association1881542190466721xywnv75419921:24000
Richinde-Chubard association1942497190467021xyznv75419921:24000
Richinde-Chubard-Richinde, very stony association1885428190466821xyxnv75419921:24000
Chubard-Richinde-Rock outcrop association, steep229717019046742whp6nv75419921:24000
Chubard-Richinde association, steep22981207622156672whp4nv77820131:24000
Chubard-Richinde-Rock outcrop association, steep2297522156662whp6nv77820131:24000
Chubard-Richinde association, steep2298244919045662whp4nv78319911:24000
Rock outcrop-Chubard-Richinde association2283779190456421xvknv78319911:24000
Richinde-Chubard association1942205190456121xvgnv78319911:24000
Chubard-Richinde association22927519046522whpbnv78319911:24000
Chubard-Richinde association, steep22983775115474792whp4nv78420061:24000
Chubard-Richinde association22922514115367432whpbnv78420061:24000
Chubard-Richinde-Rock outcrop association, steep22972226215474782whp6nv78420061:24000
Richinde-Chubard-Richinde, very stony association18851782614546851ktqbnv78420061:24000
Chubard-Richinde association, cool19451286916011941qr5fnv78420061:24000
Richinde-Rock outcrop association1990115224811792v42tnv78420061:24000
Richinde-Chubard-Rock outcrop association22901041314689151l9jcnv78420061:24000
Richinde-Chubard association1942849314689131l9j9nv78420061:24000
Richinde-Richinde, steep-Rock outcrop association18817385481178j4pwnv78420061:24000
Richinde-Chubard association, cool1949565416011951qr5gnv78420061:24000
Richinde association18821345811916w7vvnv78420061:24000
Rock outcrop-Chubard-Richinde association228397916011981qr5knv78420061:24000
Richinde-Pintwater-Rock outcrop association188049481177j4pvnv78420061:24000

Map of Series Extent

Approximate geographic distribution of the RICHINDE 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 .