Official Series Description


Lab Data Summary

Aggregate lab data for the CLEARVIEW soil series. This aggregation is based on all pedons with a current taxon name of CLEARVIEW, 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 CLEARVIEW 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
118B79-OK-32-479-OK063-32-4Clearview4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.2378333,-96.0977778

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CLEARVIEW 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 CLEARVIEW 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 CLEARVIEW 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 CLEARVIEW 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 CLEARVIEW 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 CLEARVIEW 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 CLEARVIEW 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 CLEARVIEW, 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 CLEARVIEW 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
Clearview fine sandy loam, 1 to 3 percent slopes4448015713592sp21ok00519771:24000
Clearview fine sandy loam, 3 to 5 percent slopes4546605713602sp1yok00519771:24000
Clearview fine sandy loam, 3 to 5 percent slopes, eroded4627955713612sp22ok00519771:24000
Clearview-Hector complex, 3 to 5 percent slopes, gullied475415713622sp26ok00519771:24000
Homa-Clearview complex, 3 to 5 percent slopesHhC20507571599m5spok02919691:24000
Clearview fine sandy loam, 3 to 5 percent slopesHaC112425715962sp1yok02919691:24000
Clearview fine sandy loam, 3 to 5 percent slopes, erodedHaC264965715972sp22ok02919691:24000
Clearview fine sandy loam, 3 to 5 percent slopes, severely erodedHeC339515715982x7r0ok02919691:24000
Clearview fine sandy loam, 1 to 3 percent slopesHaB37375715952sp21ok02919691:24000
Clearview fine sandy loam, 3 to 5 percent slopes, erodedHaC2123635716352sp22ok06319651:24000
Clearview-Hector complex, 3 to 5 percent slopesHhC123525716362sp23ok06319651:24000
Clearview fine sandy loam, 1 to 3 percent slopesHaB96435716332sp21ok06319651:24000
Clearview fine sandy loam, 3 to 5 percent slopesHaC91605716342sp1yok06319651:24000
Clearview-Hector complex, 3 to 5 percent slopes, gulliedHsC278295716372sp26ok06319651:24000
Hector-Clearview complex, 3 to 5 percent slopes, very rockyHeCC106073841662sp25ok10719961:24000
Hector-Clearview complex, 5 to 12 percent slopesHeCE56823841672xdv2ok10719961:24000
Clearview fine sandy loam, 3 to 5 percent slopes, erodedClrC229853841382sp22ok10719961:24000
Shermore-Clearview-Gullied land complex, 3 to 5 percent slopesSCGC42886384201dwslok10719961:24000
Clearview fine sandy loam, 1 to 3 percent slopesClrB8193841362sp21ok10719961:24000
Clearview fine sandy loam, 3 to 5 percent slopesClrC3823841372sp1yok10719961:24000
Hector-Clearview complex, 1 to 5 percent slopesHhC167721064632sp24ok11119681:24000
Clearview fine sandy loam, 1 to 3 percent slopesHaB15381064622sp21ok11119681:24000
Bengal-Clebit-Clearview complex, 5 to 30 percent slopesEhE302854571544m5qxok12119661:24000
Clebit-Clearview complex, 3 to 5 percent slopesHhC19971571555m5r8ok12119661:24000
Clearview fine sandy loam, 3 to 5 percent slopes, erodedHaC2177475715542sp22ok12119661:24000
Clebit-Clearview complex, 3 to 8 percent slopes, severely erodedHhD315854571556m5r9ok12119661:24000
Endsaw-Hector-Clearview complex, 1 to 15 percent slopes, extremely stonyEHCF90246973512sp27ok12119661:24000
Clearview fine sandy loam, 1 to 3 percent slopesHaB59595715522sp21ok12119661:24000
Clearview fine sandy loam, 3 to 5 percent slopesHaC55575715532sp1yok12119661:24000
Clearview-Hector complex, 3 to 5 percent slopesClHC15186973422sp23ok12119661:24000
Clearview fine sandy loam, 1 to 5 percent slopes, erodedClrC25246973432t278ok12119661:24000

Map of Series Extent

Approximate geographic distribution of the CLEARVIEW 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 .