Official Series Description


Lab Data Summary

Aggregate lab data for the CLAPPER soil series. This aggregation is based on all pedons with a current taxon name of CLAPPER, 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 CLAPPER 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
3279P022179WY003001Clapper7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.7611122,-108.1597214
3279P0215S1979WY029003Clapper7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.7400017,-109.0199966

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CLAPPER 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 CLAPPER 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 CLAPPER 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 CLAPPER 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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Competing Series

Soil series competing with CLAPPER 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 CLAPPER 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 CLAPPER 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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Soil series sharing subgroup-level classification with CLAPPER, 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 CLAPPER 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
Clapper-Agua Fria complex, moist, 25 to 65 percent slopes, extremely stony1203484509467k34fco66019941:24000
Clapper-Agua Fria complex, moist, 5 to 25 percent slopes, extremely stony1192593509466k34dco66019941:24000
Clapper-Agua Fria complex, 25 to 65 percent slopes, extremely stonyMC25420383170435k08pco66019941:24000
Clapper-Agua Fria complex, 5 to 25 percent slopes, extremely stonyMC25315833170442k08nco66019941:24000
Clapper-Ustic Torriorthents complex, 5 to 40 percent slopes366044502043jvdyco67519861:24000
Clapper loam, 1 to 8 percent slopes352124502041jvdwco67519861:24000
Clapper-Agua Fria complex, 25 to 65 percent slopes, extremely stonyMC2541313170499k08pco67919761:24000
Clapper-Agua Fria complex, 5 to 25 percent slopes, extremely stony2532089506715k08nco68019701:31680
Clapper-Agua Fria complex, 25 to 65 percent slopes, extremely stony2541779506716k08pco68019701:31680
Barx-Clapper complex, 3 to 12 percent slopes200219506707k08dco68019701:31680
Clapper very stony loam, 12 to 25 percent slopes24335506714k08mco68019701:31680
Clapper very stony loam, 25 to 65 percent slopes237159496683jnv1co68219861:24000
Clapper very stony loam, 12 to 25 percent slopes224802496682jnv0co68219861:24000
Barx-Clapper complex, 3 to 12 percent slopes43934496701jnvmco68219861:24000
Barx-Clapper complex, 3 to 12 percent slopesMC2001313170509k08dco68219861:24000
Clapper very stony loam, 12 to 25 percent slopesMC24333170508k08mco68219861:24000
Clapper gravelly loam, 2 to 25 percent slopes25384629862p4f4co68619921:31680
Clapper-Abracon complex, 8 to 50 percent slopes12177506205jzr6co69219981:24000
Clapper clay loam, 15 to 35 percent slopesCa4791345700clqmmt11119661:20000
Clapper gravelly loam, 7 to 15 percent slopesCg2965345701clqnmt11119661:20000
Thedalund-Clapper complex, hillyTHa26528346173cm6wmt60719701:24000
Clapper-Midway complex, hillyCK17862345897clxzmt60719701:24000
Clapper-Harvey complex, rollingCH7542345896clxymt60719701:24000
Colby-Clapper silt loams, rollingCU6008345898cly0mt60719701:24000
Spearfish-Clapper complex, hillySSa3271346142cm5wmt60719701:24000
Gerst-Clapper-Bullpen complex, 12 to 65 percent slopes, extremely stonyGME851624417082myssut0131:24000
Clapper-Montwel complex, 2 to 40 percent slopes52305116981281v01but0131:24000
Clapper very cobbly loam, 4 to 25 percent slopes4621595505588jz39ut04719991:24000
Clapper-Montwel complex, 2 to 50 percent slopes5211894505594jz3hut04719991:24000
Clapper gravelly loam, 2 to 25 percent slopes4411149505585jz36ut04719991:24000
Clapper gravelly loam-Badland-Rock outcrop complex, 25 to 50 percent slopes456932505586jz37ut04719991:24000
Clapper very cobbly loam, 25 to 50 percent slopes476696505587jz38ut04719991:24000
Clapper very cobbly loam-Badland-Rock outcrop complex, 25 to 50 percent slopes485188505589jz3but04719991:24000
Clapper-Abracon complex, 3 to 25 percent slopes494278505590jz3cut04719991:24000
Splimo-Clapper complex, 25 to 50 percent slopes2203895505496jz0but04719991:24000
Clapper complex, 25 to 50 percent slopes431921505584jz35ut04719991:24000
Clapper-Hanksville complex, 4 to 50 percent slopes511741505593jz3gut04719991:24000
Clapper-Abracon complex, 8 to 50 percent slopes50143505592jz3fut04719991:24000
Goblin-Clapper complex, 8 to 65 percent slopes0543841884046217hput62320111:24000
Goblin-Clapper, extremely stony complex, 8 to 65 percent slopes3130402319410530njnut6251:24000
Hernandez family-Clapper complex, 2 to 8 percent slopes682324504464jxy1ut63619841:24000
Clapper cobbly loam, 30 to 60 percent slopes361480504429jxwxut63619841:24000
Clapper cobbly loam, 5 to 30 percent slopes351361504428jxwwut63619841:24000
Clapper very gravelly loam, 2 to 15 percent slopes1673424304342ml23ut6421:63360
Goblin-Clapper complex, 8 to 65 percent slopes29123425560382qdrkut68519901:24000
Milok-Clapper complex, 2 to 20 percent slopes4230525149992qdqqut68519901:24000
Catahoula-Clapper, dry complex, 15 to 60 percent slopes503028902597752067ut68620041:24000
Clapper very gravelly loam, 2 to 15 percent slopes5125889598052076ut68620041:24000
Chilton-Clapper complex, 5 to 35 percent slopes, extremely stony52624216202m8wswy6031:24000
Chilton very gravelly-Clapper extremelly stoney complex, 6 to 10 percent slopes -- Draft526C24309412mllgwy6031:24000
Clapper-Maysdorf-like-Larim complex, 1 to 3 percent slopes214933028782zc5jwy6171:24000
Naturita-Clapper complex, 0 to 2 percent slopes -- Draft215A24834262pc6jwy6291:24000
Naturita-Clapper complex, 2 to 6 percent slopes -- Draft215AB15248453nvwy6291:24000
Clapper-Forkwood complex, 6 to 45 percent slopes -- Draft326BE15251853pywy6291:24000
Clapper-Maysdorf-like-Larim complex, 1 to 3 percent slopes214932066582zc5jwy6291:24000
Clapper-Cascajo-Eaglenest complex, 2 to 6 percent slopes223631328322yn92wy6291:24000
Clapper, stony-Hiland-Cambria complex, 2 to 12 percent slopes225932066782zc64wy6291:24000
Ulm-like-Clapper-Cambria complex, 6 to 20 percent slopes233132066792zc65wy6291:24000
Clapper-Forkwood complex, 4 to 8 percent slopes235632504972zv7kwy6291:24000
Clapper-Romberg-like-Remmit complex, 8 to 25 percent slopes242632030782zbs9wy6291:24000

Map of Series Extent

Approximate geographic distribution of the CLAPPER 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 .