Official Series Description


Lab Data Summary

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

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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 RIFLEPIT, 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 RIFLEPIT 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
Riflepit-Trebor complex, 10 to 40 percent slopesQ0409E1179323757092kr3ssd08120071:24000
Stovho-Riflepit-Trebor complex, 2 to 12 percent slopesQ0416C886123757202y6dpsd08120071:24000
Riflepit-Stovho complex, 2 to 12 percent slopesQ0407C791123757082kr3rsd08120071:24000
McCooley, cool-Riflepit complex, 3 to 10 percent slopesQ0411C47923757102kr3tsd08120071:24000
McCooley, cool-Riflepit complex, 10 to 40 percent slopesQ0411E2125172132myv8sd08120071:24000
Stovho-Riflepit-Trebor complex, 2 to 12 percent slopesQ0416C3677225864042y6dpsd60720111:24000
Riflepit-Trebor complex, 10 to 40 percent slopesQ0409E179225865982kr3ssd60720111:24000
McCooley, cool-Riflepit complex, 3 to 10 percent slopesQ0411C9725864852kr3tsd60720111:24000
Riflepit-Stovho loams, 3 to 30 percent slopesQ0408E2425865062mvvwsd60720111:24000
Riflepit-Stovho loams, 3 to 30 percent slopesQ0408E431824388902mvvwwy01119781:24000
Riflepit-Trebor complex, 10 to 40 percent slopesQ0409E137525145162kr3swy01119781:24000
Riflepit-Stovho complex, 2 to 12 percent slopesQ0407C95425169792kr3rwy01119781:24000
McCooley, cool-Riflepit complex, 3 to 10 percent slopesQ0411C93125169822kr3twy01119781:24000
McCooley, cool-Riflepit complex, 10 to 40 percent slopesQ0411E71324417542myv8wy01119781:24000
Stovho-Riflepit-Trebor complex, 2 to 12 percent slopesQ0416C8525145352y6dpwy01119781:24000
Riflepit-Trebor complex, 10 to 40 percent slopesQ0409E486825145172kr3swy04519841:24000
Riflepit-Stovho loams, 3 to 30 percent slopesQ0408E247325169852mvvwwy04519841:24000
McCooley, cool-Riflepit complex, 3 to 10 percent slopesQ0411C86325169802kr3twy04519841:24000
Riflepit-Stovho complex, 2 to 12 percent slopesQ0407C16225169782kr3rwy04519841:24000
Stovho-Riflepit-Trebor complex, 2 to 12 percent slopesQ0416C7725145342y6dpwy04519841:24000

Map of Series Extent

Approximate geographic distribution of the RIFLEPIT 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 .