Official Series Description


Lab Data Summary

Aggregate lab data for the CLEBIT soil series. This aggregation is based on all pedons with a current taxon name of CLEBIT, 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 CLEBIT 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
11992P025791OK127001Clebit7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.6741676,-95.0425034

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CLEBIT 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 CLEBIT 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 CLEBIT 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 CLEBIT 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 CLEBIT 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 CLEBIT series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the CLEBIT 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 .

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

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 CLEBIT, 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 CLEBIT 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
Pirum-Zafra-Clebit complex, 3 to 8 percent slopes55152723179390lynmar01919831:20000
Zafra-Carnasaw-Clebit complex, 20 to 40 percent slopes97137323179436lyq3ar01919831:20000
Carnasaw-Pirum-Clebit complex, 20 to 40 percent slopes2153850565606lzkcar05119861:20000
Bismarck-Sherless-Clebit complex, 12 to 30 percent slopes, very stony14291435655982z9cmar05119861:20000
Pirum-Clebit-Carnasaw complex, 40 to 60 percent slopes3016964565616lzkpar05119861:20000
Bismarck-Sherless-Clebit complex, 8 to 12 percent slopes, stony13142205655972z9cnar05119861:20000
Pirum-Clebit-Carnasaw complex, 20 to 40 percent slopes2911723565614lzkmar05119861:20000
Bismarck-Clebit-Sherless complex, 3 to 8 percent slopes, stony12109945655962z9cpar05119861:20000
Sherless-Clebit complex, 3 to 8 percent slopes329888565618lzkrar05119861:20000
Carnasaw-Clebit complex, 3 to 15 percent slopes187357565602lzk7ar05119861:20000
Sherless-Clebit complex, 12 to 30 percent slopes347207565620lzktar05119861:20000
Clebit-Pirum-Rock outcrop complex, 3 to 15 percent slopes242961565609lzkgar05119861:20000
Sherless-Clebit complex, 8 to 12 percent slopes332810565619lzksar05119861:20000
Carnasaw-Pirum-Clebit complex, 40 to 60 percent slopes222130565607lzkdar05119861:20000
Pirum-Clebit-Carnasaw complex, 8 to 20 percent slopes281892565613lzklar05119861:20000
Bismarck-Clebit complex, 40 to 60 percent slopes, very stony1116225655952y1lpar05119861:20000
Pirum-Zafra-Clebit complex, 3 to 8 percent slopes5549303179280lynmar05919831:20000
Zafra-Carnasaw-Clebit complex, 20 to 40 percent slopes9722613179326lyq3ar05919831:20000
Sherwood-Carnasaw-Clebit complex, 15 to 35 percent slopes, rubbly48F5785577510mcycar09719971:24000
Carnasaw-Sherless-Clebit complex, 35 to 60 percent slopes, rubbly16G5371577511mcydar09719971:24000
Carnasaw-Sherless-Clebit complex, 15 to 35 percent slopes, rubbly16F4918577514mcyhar09719971:24000
Clebit-Carnasaw-Rock outcrop complex, 3 to 15 percent slopes, very rubbly20CD2318577483mcxhar09719971:24000
Clebit-Caston-Pirum complex, 35 t0 60 percent slopes, very rubbly21G1884577477mcx9ar09719971:24000
Bismarck-Honobia-Clebit complex, 35 to 70 percent slopes, rubbly10G17075775182y1m9ar09719971:24000
Sherwood-Carnasaw-Clebit complex, 3 to 15 percent slopes, extremely stony47CD1067577513mcygar09719971:24000
Carnasaw-Pirum-Clebit association, steep7104880566108m02kar10519801:20000
Carnasaw-Pirum-Clebit association, rolling692880566107m02jar10519801:20000
Clebit-Carnasaw-Pirum association, very steep98940566110m02mar10519801:20000
Carnasaw-Zafra-Clebit complex, 15 to 35 percent slopes, moderately eroded, rubbly187310154290530x8zar10920051:20000
Zafra-Carnasaw-Clebit complex, 35 to 60 percent slopes, rubbly10190415429041nsj3ar10920051:20000
Clebit-Carnasaw-Pirum complex, 3 to 15 percent slopes, rubbly2134715428751nsh5ar10920051:20000
Caston-Clebit-Octavia complex, 35 to 60 percent slopes, very rubbly13G6692570852m50lar11319911:20000
Clebit-Carnasaw-Pirum complex, 15 to 35 percent slopes, very rubbly15F2972570882m51kar11319911:20000
Clebit-Carnasaw-Pirum complex, 3 to 15 percent slopes, very rubbly15CD1951570858m50sar11319911:20000
Carnasaw-Sherless-Clebit complex, 20 to 35 percent slopesCNF45103566311m093ar12719931:20000
Carnasaw-Sherless-Clebit complex, 8 to 20 percent slopes, rocky, extremely stonyCNE223305663102zphjar12719931:20000
Clebit-Sherless-Carnasaw complex, 35 to 60 percent slopesCSG5490566319m09car12719931:20000
Carnasaw-Sherless-Clebit complex, 3 to 8 percent slopesCNC3810566309m091ar12719931:20000
Nashoba-Bismarck-Clebit complex, 35 to 60 percent slopes20F112817075162y1mfar13319961:24000
Carnasaw-Sherless-Clebit complex, 20 to 40 percent slopes1339814564970lywvar14919851:20000
Carnasaw-Zafra-Clebit complex, 15 to 35 percent slopes, rubblyNG2783953724953861qfzmar14919851:20000
Carnasaw-Sherless-Clebit complex, 8 to 20 percent slopes, rocky, extremely stony12280015649692zphjar14919851:20000
Bengal-Carnasaw-Clebit complex, 15 to 35 percent slopes, extremely stonyNG4021036524953811qfz4ar14919851:20000
Zafra-Carnasaw-Clebit complex, 35 to 60 percent slopes, rubblyNG394366424953871qfzqar14919851:20000
Littlefir-Carnasaw-Clebit complex, 3 to 15 percent slopes, extremely stonyNG298350324953801qfz3ar14919851:20000
Nashoba-Bismarck-Clebit complex, 35 to 70 percent slopes, rubblyNG30815524953821qfz5ar14919851:20000
Bengal-Carnasaw-Clebit complex, 35 to 60 percent slopes, rubblyNG20113524953831qfz8ar14919851:20000
Clebit-Caston-Pirum complex, 35 to 60 percent slopes, very rubblyNG2871724953941qg07ar14919851:20000
Clebit-Carnasaw-Rock outcrop complex, 3 to 15 percent slopes, very rubbly (158)NG398224953901qfzxar14919851:20000
Carnasaw-Clebit association, 8 to 25 percent slopes22111146571335m5j5ok00519771:24000
Carnasaw-Clebit association, 25 to 45 percent slopes2334444571336m5j6ok00519771:24000
Carnasaw-Clebit complex, 5 to 8 percent slopes2111840571334m5j4ok00519771:24000
Carnasaw-Clebit complex, 3 to 5 percent slopes206520571333m5j3ok00519771:24000
Clebit-Tuskahoma association, 8 to 12 percent slopes143668571203m5cxok02319771:24000
Carnasaw-Bengal-Clebit complex, 15 to 30 percent slopesEhE61905571680m5w9ok06119721:24000
Carnasaw-Bengal-Clebit complex, 3 to 15 percent slopesEhD32873571679m5w8ok06119721:24000
Carnasaw-Clebit association, 8 to 30 percent slopes4112515571510m5ptok07719801:24000
Carnasaw-Pirum-Clebit association, 3 to 12 percent slopes852942571526m5qbok07719801:24000
Carnasaw-Clebit-Rock outcrop complex, 3 to 8 percent slopes610110571524m5q8ok07719801:24000
Carnasaw-Clebit-Pickens variant association, 30 to 45 percent slopes56502571521m5q5ok07719801:24000
Bengal-Clebit complex, 3 to 8 percent slopes16478571477m5nrok07719801:24000
Octavia-Carnasaw-Clebit association, 30 to 45 percent slopes, cool274262571496m5pcok07719801:24000
Clebit-Pirum complex, 5 to 12 percent slopes123316571480m5nvok07719801:24000
Clebit-Pirum-Rock outcrop complex, 15 to 40 percent slopes132063571481m5nwok07719801:24000
Bengal-Clebit association, 3 to 15 percent258163571402m5lbok07919811:24000
Bengal-Pirum-Clebit complex, 5 to 15 percent slopes533978571435m5mdok07919811:24000
Carnasaw-Clebit complex, 5 to 15 percent slopes822714571468m5ngok07919811:24000
Pirum-Clebit complex, 3 to 5 percent slopes5121439571437m5mgok07919811:24000
Clebit-Carnasaw-Pirum complex, 4 to 35 percent slopes, cool167644571398m5l6ok07919811:24000
Pirum-Clebit complex, 3 to 5 percent slopes, eroded525077571438m5mhok07919811:24000
Clebit stony fine sandy loam, 10 to 30 percent slopes144781571396m5l4ok07919811:24000
Clebit stony fine sandy loam, 30 to 60 percent slopes152161571397m5l5ok07919811:24000
Clebit-Carnasaw-Stapp association, 12 to 20 percent slopesGsE240120571150m5b6ok08919701:24000
Clebit-Carnasaw-Stapp association, 20 to 40 percent slopesGsF159134571151m5b7ok08919701:24000
Carnasaw-Clebit association, 12 to 20 percent slopesCmE82987571141m59xok08919701:24000
Clebit-Rock outcrop complex, 35 to 60 percent slopesHkF19440571154m5bbok08919701:24000
Bengal-Clebit-Clearview complex, 5 to 30 percent slopesEhE302854571544m5qxok12119661:24000
Bengal-Clebit-Rock outcrop complex, 30 to 60 percent slopesEhF60773571545m5qyok12119661:24000
Clebit-Clearview complex, 3 to 5 percent slopesHhC19971571555m5r8ok12119661:24000
Clebit-Clearview complex, 3 to 8 percent slopes, severely erodedHhD315854571556m5r9ok12119661:24000
Carnasaw-Pirum-Clebit association, 12 to 20 percent slopes11197325571261m5fsok12719771:24000
Tuskahoma-Clebit-Sobol association, 8 to 12 percent slopes5597883571309m5hbok12719771:24000
Carnasaw-Pirum-Clebit association, 12 to 20 percent slopes, dry1275164571262m5ftok12719771:24000
Clebit-Pirum-Carnasaw association, 20 to 45 percent slopes1873852571268m5g0ok12719771:24000
Clebit-Pirum-Carnasaw association, 20 to 45 percent slopes, dry1933206571269m5g1ok12719771:24000
Clebit-Rock outcrop association, 20 to 45 percent slopes206841571271m5g3ok12719771:24000
Clebit-Sobol complex, 5 to 20 percent slopes, extremely stonyCnE2706571885m62xok13519661:24000

Map of Series Extent

Approximate geographic distribution of the CLEBIT 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 .