Official Series Description


Lab Data Summary

Aggregate lab data for the CLAPRYCH soil series. This aggregation is based on all pedons with a current taxon name of CLAPRYCH, 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 CLAPRYCH 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 CLAPRYCH 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 CLAPRYCH 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 CLAPRYCH 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 CLAPRYCH 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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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with CLAPRYCH 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 CLAPRYCH 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 CLAPRYCH 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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Soil series sharing subgroup-level classification with CLAPRYCH, 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 CLAPRYCH 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
Claprych-Luman very gravelly sandy loams, 0 to 10 percent slopes130386481044873hqkwy03119981:24000
Claprych-Selpats sandy clay loams, 0 to 3 percent slopes13163701044883hqlwy03119981:24000
Claprych-Sweatbee complex, 3 to 20 percent slopes13259041044893hqmwy03119981:24000
Claprych gravelly fine sandy loam, 0 to 3 percent slopes12918741044863hqjwy03119981:24000
Eaglenest-Claprych complex, 0 to 3 percent slopes210432532952vz1hwy6031:24000
Larim-like-Claprych complex, 10 to 35 percent slopes540932532502w7h3wy6031:24000
Claprych-Sweatbee complex, 3 to 20 percent slopes12113416698191t1l4wy60920061:24000
Eaglenest-Claprych complex, 0 to 3 percent slopes210431970422vz1hwy6171:24000
Larim-like-Claprych complex, 10 to 35 percent slopes540931708592w7h3wy6171:24000
Claprych, stony-Hiland-Ralstonflats complex, 2 to 40 percent slopes2D01330285130144wy6171:24000
Hollywell-like-Claprych, extremely stony-Romberg, extremely stony complex, 25 to 60 percent slopes555932030832zbsgwy6291:24000
Claprych-Tonra-like complex, 0 to 4 percent slopes, very stony215332504852zv76wy6291:24000
Eaglenest-Claprych complex, 0 to 3 percent slopes210429614302vz1hwy6291:24000
Cascajo-Remmit-like-Claprych complex, 2 to 15 percent slopes223929119772y4z0wy6291:24000
Claprych gravelly sandy loam, 6 to 15 percent slopes, stony233732504322zv5mwy6291:24000
Claprych, extremely bouldery-Copeman complex, 2 to 45 percent slopes235332504872zv78wy6291:24000
Claprych-Hiland complex, 4 to 25 percent slopes235432504882zv7bwy6291:24000
Claprych very gravelly sandy loam, 15 to 35 percent slopes241131332572ynmjwy6291:24000
Hiland-Claprych-Remmit complex, 1 to 20 percent slopes242131709522z1zgwy6291:24000
Larim-like-Claprych complex, 10 to 35 percent slopes540929118532w7h3wy6291:24000
Shingle-like-Claprych-Zigweid-like complex, 10 to 50 percent slopes549732504902zv7cwy6291:24000
Claprych gravelly sandy loam, 6 to 15 percent slopes, stony233732505132zv5mwy65620081:24000

Map of Series Extent

Approximate geographic distribution of the CLAPRYCH 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 .