Official Series Description


Lab Data Summary

Aggregate lab data for the SALIDA soil series. This aggregation is based on all pedons with a current taxon name of SALIDA, 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 SALIDA 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 SALIDA 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 SALIDA 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 SALIDA 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 SALIDA 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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Click the image to view it full size.

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

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Click the image to view it full size.

Competing Series

Soil series competing with SALIDA 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 SALIDA 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 SALIDA 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 SALIDA, 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. IA-2011-05-31-32 | Greene County - 1985

    Pattern of soils and parent material in the Clarion-Coland-Storden association (Soil Survey of Greene County, Iowa; 1985).

Map Units

Map units containing SALIDA 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
Storden-Salida complex, 14 to 25 percent slopes639E3592550292fjfcia01519771:15840
Storden-Salida complex, 9 to 14 percent slopes639D1542550291fjfbia01519771:15840
Salida-Storden complex, 9 to 16 percent slopes639D449403563fjy5ia02719791:15840
Salida-Storden complex, 5 to 9 percent slopes639C219403562fjy4ia02719791:15840
Salida gravelly loamy sand, 2 to 5 percent slopes73B616405648fm3fia06319891:15840
Salida gravelly loamy sand, 18 to 40 percent slopes73G257405660fm3tia06319891:15840
Salida gravelly loamy sand, 9 to 14 percent slopes, moderately eroded73D2217405654fm3mia06319891:15840
Storden-Salida complex, 5 to 14 percent slopes, moderately eroded639D2177405628fm2sia06319891:15840
Salida gravelly loamy sand, 5 to 9 percent slopes, moderately eroded73C287405651fm3jia06319891:15840
Salida-Storden complex, 5 to 9 percent slopes, moderately erode639C2672406255fmr0ia07319831:15840
Salida-Storden complex, 9 to 14 percent slopes, moderately eroded639D2286406256fmr1ia07319831:15840
Salida sandy loam, 7 to 14 percent slopes, moderately eroded73D2321406418fmx8ia07719681:15840
Salida gravelly sandy loam, 2 to 9 percent slopes, moderately eroded73C2352406589fn2sia08119871:15840
Sunburg-Salida complex, 9 to 14 percent slopes, moderately eroded642D2223406580fn2hia08119871:15840
Storden-Salida complex, 9 to 14 percent slopes, moderately eroded639D2430408397fpz3ia10919801:15840
Storden-Salida complex, 5 to 9 percent slopes, moderately erode639C2415408396fpz2ia10919801:15840
Salida gravelly sandy loam, 2 to 9 percent slopes, moderately eroded73C2224408402fpz8ia10919801:15840
Salida gravelly sandy loam, 9 to 25 percent slopes, moderately eroded73E2210408403fpz9ia10919801:15840
Estherville-Salida complex, 9 to 14 percent slopes541D563409126fqqmia11919731:15840
Estherville-Salida complex, 5 to 9 percent slopes541C381409125fqqlia11919731:15840
Salida sandy loam, 18 to 40 percent slopes73F287409138fqr0ia11919731:15840
Storden-Salida complex, 25 to 40 percent slopes639G246410086frqlia14119771:15840
Salida sandy loam, 18 to 40 percent slopes73F226410095frqwia14119771:15840
Salida sandy loam, 9 to 18 percent slopes73E148410094frqvia14119771:15840
Clarion-Estherville complex, 5 to 9 percent slopes, moderately eroded181C2913410263frx9ia14719731:15840
Storden-Salida complex, 9 to 14 percent slopes639D247410295frybia14719731:15840
Storden-Salida complex, 14 to 18 percent slopes639E141410296frycia14719731:15840
Storden-Salida complex, 5 to 9 percent slopes639C79410294fry9ia14719731:15840
Estherville-Salida complex, 5 to 10 percent slopes541C263410407fs1yia15119821:15840
Salida gravelly sandy loam, 2 to 7 percent slopes73B403412329fv1yia18919841:15840
Salida gravelly coarse sandy loam, 2 to 12 percent slopes42C486396864f9z2mn03719801:15840
Salida gravelly sandy loam, 12 to 35 percent slopes42E1533400776fg18mn10919771:15840
Salida gravelly sandy loam, 0 to 6 percent slopesEbB515427967gcbdmn13919881:20000
Salida gravelly sandy loam, 0 to 6 percent slopes, moderately erodedEbB2136427968gcbfmn13919881:20000
Salida gravelly sandy loam, 6 to 12 percent slopes, moderately erodedEbC276427970gcbhmn13919881:20000

Map of Series Extent

Approximate geographic distribution of the SALIDA 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 .