Official Series Description


Lab Data Summary

Aggregate lab data for the OCTAGON soil series. This aggregation is based on all pedons with a current taxon name of OCTAGON, 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 OCTAGON were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
108A40A280767IL089003aOctagon7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.7852924,-88.3939311
110NW83141983IN111014Octagon3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7442028,-87.4843972
11085IL1050111985IL105011Octagon2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8122139,-88.8563667
111CWH76281976IN181028Octagon3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6477778,-86.8660194
111CWH77031977IN181003Octagon3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6647194,-87.0824056
111CJR79201979IN073020Octagon3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.9781333,-87.1465444
111CJR79211979IN073021Octagon2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.9800528,-87.1401139
111DMY80041980IN107004Octagon3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.1850611,-86.9256833
111DTI84201984IN157020Octagon3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.3465778,-86.8347778
111D82P0844S1982IN107007Octagon6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.1845856,-86.9260178
111D82P0845S1982IN107008Octagon6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.1845856,-86.9260178

Water Balance

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the OCTAGON series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the OCTAGON series and siblings. 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 OCTAGON 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 .

Click the image to view it full size.

Click the image to view it full size.

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

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

Click the image to view it full size.

Competing Series

Soil series competing with OCTAGON share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the OCTAGON 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 OCTAGON 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.

Click the image to view it full size.

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 OCTAGON, 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 OCTAGON 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
Octagon silt loam, 4 to 6 percent slopes, eroded656C2374118393365dbil03719981:12000
Octagon silt loam, 2 to 4 percent slopes656B259218393265d9il03719981:12000
Octagon silt loam, 5 to 10 percent slopes, eroded656C29961019432136sxil04120041:12000
Octagon silt loam, 2 to 4 percent slopes656B69061988606nxvil08920001:12000
Octagon silt loam, 4 to 6 percent slopes, eroded656C262211988616nxwil08920001:12000
Octagon silt loam, 6 to 12 percent slopes, eroded656D220061988626nxxil08920001:12000
Octagon silt loam, 2 to 4 percent slopes656B1422182769645sil11119971:12000
Octagon silt loam, 4 to 6 percent slopes, eroded656C2743182770645til11119971:12000
Octagon silt loam, 6 to 12 percent slopes, eroded656D258415920621qfnvil17720061:12000
Octagon silt loam, 4 to 6 percent slopes, eroded656C244715920611qfntil17720061:12000
Octagon silt loam, 2 to 6 percent slopes, erodedObmB211832424268486in04519991:12000
Octagon silt loam, 6 to 12 percent slopes, erodedObmC27592424258485in04519991:12000
Octagon fine sandy loam, 6 to 12 percent slopes, erodedOcC26181613745dxmin07319851:15840
Octagon loam, 2 to 6 percent slopesOnB9541630445gnhin10719841:15840
Octagon loam, 6 to 12 percent slopesOnC3551630455gnjin10719841:15840
Octagon-Ayr complex, 2 to 6 percent slopes, erodedOkB242421636935hbfin11119901:15840
Octagon loam, 6 to 12 percent slopes, erodedOcC25521636895hb9in11119901:15840
Octagon silt loam, 2 to 6 percent slopes, erodedOmB235731642015hvtin15719901:15840
Toronto-Octagon complex, 2 to 6 percent slopes, erodedTnB222961643315j00in15719901:15840
Octagon silt loam, 6 to 12 percent slopes, erodedOmC210511642035hvwin15719901:15840
Octagon clay loam, 6 to 12 percent slopes, severely erodedOpC34661642105hw3in15719901:15840
Octagon silt loam, 2 to 6 percent slopesOcB8391618595ff8in18119791:20000
Octagon silt loam, 6 to 12 percent slopes, erodedOcC21471618605ff9in18119791:20000

Map of Series Extent

Approximate geographic distribution of the OCTAGON 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 .