Official Series Description


Lab Data Summary

Aggregate lab data for the SODUS soil series. This aggregation is based on all pedons with a current taxon name of SODUS, 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 SODUS 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
10140A0286S1958NY011002Sodus6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.3661118,-76.6244431
10140A0287S1961NY073007Sodus6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.2569427,-78.1208344

Water Balance

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

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 SODUS 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 SODUS 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 SODUS 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 flats position figure.

Soil series sharing subgroup-level classification with SODUS, 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 SODUS 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
Sodus gravelly loam, 2 to 8 percent slopesSoB35602894939q7hny01119681:15840
Sodus gravelly loam, 8 to 14 percent slopes, erodedSoC314282894959q7kny01119681:15840
Sodus gravelly loam, rollingSoCK13712894969q7lny01119681:15840
Sodus gravelly loam, 14 to 20 percent slopesSoD12642894979q7mny01119681:15840
Sodus gravelly loam, 8 to 14 percent slopesSoC12142894949q7jny01119681:15840
Ira and Sodus very stony loams, 2 to 20 percent slopesIsD8682894239q57ny01119681:15840
Sodus gravelly loam, 20 to 40 percent slopesSoE8352894989q7nny01119681:15840
Sodus gravelly silt loam, 3 to 8 percent slopesSoB9492919179srpny04519811:15840
Sodus gravelly silt loam, 8 to 15 percent slopesSoC5232919189srqny04519811:15840
Sodus gravelly silt loam, 15 to 25 percent slopesSoD2602919199srrny04519811:15840
Sodus gravelly fine sandy loam, 2 to 8 percent slopesSoB6542927699tn5ny05519671:15840
Ira and Sodus very stony soils, moderately steepIUD163232941299w21ny07519731:15840
Ira-Sodus gravelly fine sandy loams, rollingIsC87762941289w20ny07519731:15840
Sodus gravelly fine sandy loam, 3 to 8 percent slopesSgB56492941519w2rny07519731:15840
Sodus gravelly fine sandy loam, 8 to 15 percent slopesSgC37742941529w2sny07519731:15840
Sodus gravelly fine sandy loam, 15 to 25 percent slopesSgD23342941539w2tny07519731:15840
Sodus soils, very steepSHF17682941549w2vny07519731:15840
Sodus gravelly fine sandy loam, 3 to 8 percent slopesSdB50812957849xsfny11719721:15840
Sodus gravelly fine sandy loam, 8 to 15 percent slopesSdC24492957859xsgny11719721:15840
Sodus soils, steepSSE19712957839xsdny11719721:15840
Sodus gravelly fine sandy loam, 15 to 25 percent slopesSdD13942957869xshny11719721:15840

Map of Series Extent

Approximate geographic distribution of the SODUS 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 .