Official Series Description


Lab Data Summary

Aggregate lab data for the SEMINOE soil series. This aggregation is based on all pedons with a current taxon name of SEMINOE, 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 SEMINOE 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 SEMINOE 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 SEMINOE series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

There are insufficient data to create the sibling sketch figure.

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

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.

Competing Series

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

There are insufficient data to create the competing sketch figure.

Select annual climate data summaries for the SEMINOE 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 SEMINOE 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 SEMINOE, 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 SEMINOE 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
Seminoe-Cusheet complex, 4 to 15 percent slopes7341979829598582wsxkwy6301:24000
Seminoe sandy loam, 2 to 8 percent slopes7351904229598572wsxjwy6301:24000
Seminoe sandy loam, 2 to 10 percent slopes7281576830038542x7bxwy6301:24000
Zagplat-Blackleaf-Seminoe complex, 5 to 25 percent slopes729993130038552x7bywy6301:24000
Seminoe-Kayso complex, 5 to 25 percent slopes725980730038532x7bwwy6301:24000
Gerdrum-Seminoe-Galbreth family complex, 0 to 6 percent slopes7658273341051631gb8wy6301:24000
Seminoe-Snakerattle complex, 1 to 8 percent slopes724814130038522x7bvwy6301:24000
Seminoe, very stony-Rock outcrop-Jewel, very stony complex, 5 to 30 percent slopes7677202341051731gb9wy6301:24000
Seminoe-Snakedraw-Rock outcrop complex, 2 to 20 percent slopes716707630038462x7bnwy6301:24000
Taylordraw-Seminoe complex, 2 to 8 percent slopes701691830038362x7bbwy6301:24000
Seminoe-Bonhigh complex, 2 to 10 percent slopes715529630038452x7bmwy6301:24000
Seminoe-Coyoteflats complex, 0 to 4 percent slopes7805172341053031v1mwy6301:24000
Seminoe-Bonhigh complex, 3 to 15 percent slopes7214520341049131g9bwy6301:24000
Seminoe-Twinadams complex, 2 to 10 percent slopes704440029598472wsx7wy6301:24000
Seminoe-Bonfri complex, 4 to 15 percent slopes733433829598512wsxbwy6301:24000
Seminoe-Yamacall complex, 3 to 8 percent slopes7593958341051431gb6wy6301:24000
Seminoe-Kayso complex, 3 to 12 percent slopes83936403365721312f8wy6301:24000
Seminoe-Shooter-Snakerattle complex, 0 to 8 percent slopes7783460341052831v1kwy6301:24000
Cusheet-Seminoe complex, 2 to 10 percent slopes717341930038472x7bpwy6301:24000
Seminoe-Kayso-Alkalicreek complex, 0 to 10 percent slopes8863391341044031g7hwy6301:24000
Seminoe-Taylordraw-Kobarter family complex, 2 to 24 percent slopes9292889346503131y53wy6301:24000
Pinehill-Seminoe complex, 0 to 8 percent slopes7542771341050931gb1wy6301:24000
Jemdilon-Seminoe-Kayso complex, 2 to 10 percent slopes8812770341043531g79wy6301:24000
Seminoe-Geohrock complex, 2 to 12 percent slopes706271430038382x7bdwy6301:24000
Seminoe-Assinniboine-Evanston complex, 4 to 20 percent slopes924253634618393168twy6301:24000
Radersburg family, very stony-Seminoe, very stony-Bonhigh complex, 8 to 40 percent slopes7582167341051331gb5wy6301:24000
Seminoe-Duneysands complex, 2 to 10 percent slopes731199530038562x7bzwy6301:24000
Tootall-Bonfri-Seminoe complex, 0 to 6 percent slopes7791747341052931v1lwy6301:24000
Rock outcrop-Standing Elk-Seminoe complex, 5 to 25 percent slopes8871378341044131g7jwy6301:24000
Seminoe-Evanston complex, 3 to 10 percent slopes7551350341051031gb2wy6301:24000
Seminoe-Zagplat complex, 1 to 10 percent slopes723132430038512x7btwy6301:24000
Shooter-Seminoe-Scobey complex, 0 to 6 percent slopes7711216341052131v1bwy6301:24000
Zagplat-Seminoe complex, 3 to 15 percent slopes84911903365720312fcwy6301:24000
Seminoe-Berlake complex, 1 to 15 percent slopes7381056341047831g91wy6301:24000
Seminoe-Yamacall-Rock outcrop complex, 3 to 8 percent slopes760996341051531gb7wy6301:24000
Seminoe-Taylordraw complex, 0 to 8 percent slopes91896534618313168mwy6301:24000
Coyoteflats-Chickenhill-Seminoe complex, 0 to 3 percent slopes909859341056931v2qwy6301:24000
Seminoe sandy loam, 1 to 5 percent slopes810836341046731g8nwy6301:24000
Cacklin, very bouldery-Seminoe, stony-Picketlake, very bouldery complex, 3 to 10 percent slopes798663341054831v27wy6301:24000
Coyoteflats family-Seminoe-Evanston complex, 0 to 8 percent slopes92163134618333168qwy6301:24000
Evanston-Seminoe complex, 4 to 10 percent slopes756514341051131gb3wy6301:24000
Pinehill-Pylon-Seminoe complex, 0 to 8 percent slopes92250934618343168rwy6301:24000
Cusheet-Seminoe complex, 3 to 15 percent slopes8604003365732312fzwy6301:24000
Seminoe-Scobey-Evanston complex, 4 to 20 percent slopes926380346184131699wy6301:24000

Map of Series Extent

Approximate geographic distribution of the SEMINOE 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 .