Official Series Description


Lab Data Summary

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

Competing Series

Soil series competing with CINEBAR 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 CINEBAR 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 CINEBAR 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 .

Click the image to view it full size.

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 CINEBAR, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. WA-2012-05-11-34 | Lewis County Area - May 1987

    Pattern of soils and parent material in the Cinebar-Newaukum map unit (Soil Survey of Lewis County Area, Washington; May 1987).

Map Units

Map units containing CINEBAR 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
Cinebar silt loam, 8 to 20 percent slopesCnD23200719742dwrwa01119721:20000
Cinebar stony silt loam, 30 to 70 percent slopesCrG21210719782dwwwa01119721:20000
Cinebar silt loam, 20 to 30 percent slopesCnE20200719752dwswa01119721:20000
Cinebar silt loam, 30 to 70 percent slopesCnG11060719762dwtwa01119721:20000
Cinebar stony silt loam, 3 to 30 percent slopesCrE6590719772dwvwa01119721:20000
Cinebar silt loam, 3 to 8 percent slopesCnB5830719732dwqwa01119721:20000
Cinebar silt loam, 5 to 20 percent slopes2613250723872fb2wa01519941:24000
Cinebar silt loam, 0 to 5 percent slopes252670723732f9mwa01519941:24000
Cinebar silt loam, 30 to 65 percent slopes281665724002fbhwa01519941:24000
Cinebar silt loam, 20 to 30 percent slopes27945723972fbdwa01519941:24000
Cinebar loamy sand, overblown, 5 to 30 percent slopes24570723382f8hwa01519941:24000
Cinebar silt loam, 6 to 15 percent slopes442714741162h3vwa63419861:24000
Klaber-Cinebar silt loams, 0 to 8 percent slopes1071410739022gwywa63419861:24000
Cinebar silt loam, 30 to 45 percent slopes46653741182h3xwa63419861:24000
Cinebar silt loam, 15 to 30 percent slopes45559741172h3wwa63419861:24000
Cinebar silt loam, 8 to 15 percent slopes5020939744442hgfwa64119801:24000
Cinebar silt loam, 0 to 8 percent slopes4917785744422hgcwa64119801:24000
Cinebar silt loam, 15 to 30 percent slopes5114011744452hggwa64119801:24000
Cinebar silt loam, 30 to 65 percent slopes5210073744462hghwa64119801:24000
Cinebar silt loam, till substratum, 8 to 30 percent slopes533126744472hgjwa64119801:24000
Cinebar variant silty clay loam, 30 to 65 percent slopes561092744502hgmwa64119801:24000
Cinebar variant silty clay loam, 8 to 30 percent slopes551082744492hglwa64119801:24000
Cinebar silt loam, till substratum, 30 to 65 percent slopes54614744482hgkwa64119801:24000
Cinebar silt loam, 6 to 15 percent slopes10C448746472hnzwa65319741:24000
Cinebar silt loam, 30 to 45 percent slopes10E431746492hp1wa65319741:24000
Cinebar silt loam, 15 to 30 percent slopes10D115746482hp0wa65319741:24000

Map of Series Extent

Approximate geographic distribution of the CINEBAR 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 .