Official Series Description


Lab Data Summary

Aggregate lab data for the SALIX soil series. This aggregation is based on all pedons with a current taxon name of SALIX, 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 SALIX 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
107B96P0048S1995IA193005Salix7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.228611,-96.2500534

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SALIX 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 SALIX 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 SALIX 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 SALIX 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.

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Click the image to view it full size.

Competing Series

Soil series competing with SALIX 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 SALIX 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 SALIX 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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There are insufficient data to create the 3D mountains figure.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with SALIX, 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-2010-09-02-24 | Monona County - 2003

    Typical pattern of soils and parent material in the Luton-Salix association (Soil Survey of Monona County, Iowa; 2003).

  2. IA-2010-09-03-09 | Woodbury - 2006

    Typical pattern of soils and underlying material in the Luton-Tieville association (Soil Survey of Woodbury County, Iowa; 2006).

  3. NE-2012-02-14-14 | Washington County - September 1964

    Soil pattern of the Luton-Volin and Albaton-Haynie associations (Soil Survey of Washington County, Nebraska; September 1964).

  4. SD-2010-11-01-07 | Clay County - 2003

    Relationship of the major soils to parent material and position on the Missouri River flood plain (Soil Survey of Clay County, South Dakota; 2003).

Map Units

Map units containing SALIX 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
Salix silty clay loam364735406136fmm5ia07119681:20000
Salix silty clay loam364284406764fn8fia08519711:15840
Salix silty clay loam, 0 to 2 percent slopes362555409565fr5sia12919791:15840
Salix silty clay loam, 0 to 2 percent slopes, rarely flooded368872447325h0gvia13319941:12000
Salix silty clay loam, 0 to 2 percent slopes361006410347fs00ia14919721:20000
Salix silty clay loam, leached subsoil variant, 0 to 2 percent slopes607565410353fs06ia14919721:20000
Salix silty clay loam, 0 to 2 percent slopes361201410478fs47ia15519861:15840
Salix silt loam, 0 to 2 percent slopes, rarely flooded364469401905fh6pia19320031:12000
Salix silty clay loam, 0 to 2 percent slopes, rarely flooded135762302902699z9bbmo00519881:24000
Salix silty clay loam, rarely flooded78082150427859gc6xne02119781:20000
Salix silty clay loam, rarely flooded78081647395503f8k5ne17720001:12000
Salix silty clay loam, 0 to 2 percent slopesSa1423445605gypcsd02719951:24000
Salix silty clay loamSa3591453716h740sd12719741:20000
Salix silty clay loamSa511418102g125sd13519771:20000

Map of Series Extent

Approximate geographic distribution of the SALIX 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 .