Official Series Description


Lab Data Summary

Aggregate lab data for the SAVO soil series. This aggregation is based on all pedons with a current taxon name of SAVO, 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 SAVO 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
60A89P027388NE165006Savo6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.9324989,-103.9055557

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SAVO 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 SAVO 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 SAVO 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 SAVO 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 mountains figure.

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Competing Series

Soil series competing with SAVO 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 SAVO 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 SAVO 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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Soil series sharing subgroup-level classification with SAVO, 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. SD-2012-03-15-29 | Fall River County - April 1982

    Pattern of soils in the Norka association (Soil Survey of Fall River County, SD; 1982).

  2. SD-2012-03-15-42 | Haakon County - 1998

    Typical pattern of soils and parent material in the Ottumwa-Kirley and Ottumwa-Razor-Midway associations (Soil Survey of Haakon County, SD; 1998).

  3. SD-2012-03-15-55 | Jackson County, Northern Part - July 1987

    Pattern of soils and underlying material in the Weta-Cactusflat and Blackpipe-Wortman associations (Soil Survey of Jackson County, Northern Part, SD; 1987).

Map Units

Map units containing SAVO 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
Savo silty clay loam, 0 to 2 percent slopes524712953580102tzz4ne16519931:20000
Savo silty clay loam, 2 to 6 percent slopes52487623580112tzz5ne16519931:20000
Savo silty clay loam, 0 to 2 percent slopesSdA30183532342tzz4sd01919701:24000
Savo silty clay loam, 2 to 6 percent slopesSdB5803532352tzz5sd01919701:24000
Savo silty clay loam, moist, 2 to 6 percent slopesP448B17226688862rxv8sd01919701:24000
Savo silty clay loam, moist, 0 to 2 percent slopesP448A6826688852rxv7sd01919701:24000
Savo silt loam, 2 to 6 percent slopesSdB251033551522tzz7sd04719801:24000
Savo silt loam, 0 to 2 percent slopesSdA51523551512tzz6sd04719801:24000
Savo silt loam, 2 to 6 percent slopesP444B18827331552rxv5sd04719801:24000
Savo silt loam, 0 to 2 percent slopesP444A17127331542rxv4sd04719801:24000
Savo silt loam, 2 to 6 percent slopesSrB14566354160cwjjsd05519921:24000
Ottumwa-Razor-Savo complex, 6 to 15 percent slopesOyC12385354137cwhssd05519921:24000
Savo silt loam, 0 to 2 percent slopesSrA1866354159cwjhsd05519921:24000
Savo silt loam, 6 to 9 percent slopesSrC6354161cwjksd05519921:24000
Savo silt loam, moist, 2 to 6 percent slopesP446B77427332682rxv6sd08120071:24000
Savo silt loam, 2 to 6 percent slopes639B53319005102tzz7sd08120071:24000
Savo silt loam, 0 to 2 percent slopes639A37619005092tzz6sd08120071:24000
Savo silty clay loam, moist, 0 to 2 percent slopesP448A31227333012rxv7sd08120071:24000
Savo and Blackpipe soils, 2 to 6 percent slopesSkB398933543492tvvysd60019741:24000
Blackpipe-Savo complex, moist, 2 to 6 percent slopesP038B11500274563530wn0sd60019741:24000
Savo silty clay loam, 0 to 2 percent slopesShA89713543482tzz4sd60019741:24000
Tanna-Savo complex, 2 to 6 percent slopesTsB33011355471cxwtsd60119831:24000
Tanna-Savo complex, 6 to 9 percent slopesTsC4425355472cxwvsd60119831:24000
Savo silt loam, 2 to 6 percent slopesSmB1289225809742tzz7sd60620111:24000
Savo silt loam, 0 to 2 percent slopesSmA899025809732tzz6sd60620111:24000
Savo silt loam, 6 to 9 percent slopesSmC51252580975cykjsd60620111:24000
Savo-Blackpipe silty clay loams, 6 to 15 percent slopesU712D73925829442qt0gsd60620111:24000
Savo-Urban land complex, 0 to 9 percent slopesSoB4952580976cykksd60620111:24000
Savo silty clay loam, 2 to 6 percent slopesU711B725829432qt0fsd60620111:24000
Savo-Dawes silt loams, 2 to 6 percent slopesSwB22332582668cy43sd61120111:24000
Savo-Dawes, sodic, silt loams, 2 to 6 percent slopesU715B5525828792qp1hsd61120111:24000
Savo-Tuthill silt loams, 0 to 3 percent slopesU615A212724854282pf93sd61220111:20000
Savo silt loam, 0 to 2 percent slopesU710A60124854432tzz6sd61220111:20000
Savo silty clay loam, 2 to 6 percent slopesU711B25925474322tzz5sd61220111:20000
Savo-Blackpipe silty clay loams, 6 to 15 percent slopesU712D7625474332qt0gsd61220111:20000
Savo-Dawes, sodic, silt loams, 2 to 6 percent slopesU715B2725172162qp1hsd61220111:20000
Savo-Tuthill silt loams, 0 to 3 percent slopesU615A687725828522pf93sd61320111:24000

Map of Series Extent

Approximate geographic distribution of the SAVO 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 .