Official Series Description


Lab Data Summary

Aggregate lab data for the POPOSHIA soil series. This aggregation is based on all pedons with a current taxon name of POPOSHIA, 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 POPOSHIA 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
67A89P081889WY021004Poposhia8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.2338905,-105.0961075

Water Balance

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

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Competing Series

Soil series competing with POPOSHIA 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 POPOSHIA 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 POPOSHIA 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.

Click the image to view it full size.

Click the image to view it full size.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with POPOSHIA, 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 POPOSHIA 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
Poposhia-Trimad complex, 3 to 15 percent slopes129348497628jptjco64419801:24000
Poposhia silt loam, 0 to 6 percent slopes2007401044343hnvwy03119981:24000
Poposhia-Chaperton association, 6 to 12 percent slopes2034551045573hstwy03119981:24000
Poposhia-Forelle complex, 1 to 8 percent slopes2043691045593hswwy03119981:24000
Poposhia-Blazon silt loams, 3 to 30 percent slopes201661044353hnwwy03119981:24000
Poposhia-Blazon, thin solum-Rock outcrop complex, 5 to 35 percent slopes20241044363hnxwy03119981:24000
Poposhia loam, 0 to 3 percent slopes161824186261720j6fwy0411:24000
Obadia-Poposhia association, 0 to 3 percent slopes182548186262020j6jwy0411:24000
Poposhia loam, 6 to 10 percent slopes3534C35124840942pcx2wy0411:24000
Poposhia-Forelle complex, 1 to 8 percent slopes19863638501742jv37wy60119911:24000
Poposhia-Chaperton association, 6 to 12 percent slopes19938339501743jv38wy60119911:24000
Chaperton-Poposhia complex, 3 to 30 percent slopes1405003501677jv14wy60119911:24000
Poposhia-Blazon complex, 3 to 15 percent slopes1974188501741jv36wy60119911:24000
Poposhia-Blazon complex, 3 to 15 percent slopes2402339502366jvrcwy62519851:24000
Poposhia-Evanston complex, 6 to 40 percent slopes -- Draft550224827532pbhtwy6291:24000
Poposhia-Havre overflow complex, 0 to 6 percent slopes -- draft4061032724210052m87ywy6301:24000
Tisworth-Poposhia complex, 0 to 8 percent slopes -- draft414572824554752nf3wwy6301:24000
Poposhia loam, 2 to 6 percent slopes -- draft349AB478223782592kts1wy6301:24000
Poposhia loam, 0 to 2 percent slopes -- draft349A54923938932lc1cwy6301:24000
Poposhia-Redgap-Zagpeed complex, 0 to 10 percent slopes2243120325547372rc08wy6351:24000
Poposhia loam, 3 to 6 percent slopes1627567504021jxgrwy63819901:24000
Poposhia clay loam, 0 to 3 percent slopes1642534504023jxgtwy63819901:24000
Poposhia loam, 0 to 3 percent slopes1612160504019jxgpwy63819901:24000
Poposhia loam, 6 to 10 percent slopes1632076504022jxgswy63819901:24000
Delphill-Iyers-Poposhia complex, 3 to 25 percent slopes1191478503962jxdvwy63819901:24000
Spicerton-Poposhia complex, 0 to 3 percent slopes1821256504045jxhjwy63819901:24000
Poposhia very fine sandy loam, strongly alkaline, 1 to 3 percent slopes166774504025jxgwwy63819901:24000
Poposhia clay loam, 3 to 6 percent slopes165734504024jxgvwy63819901:24000
Poposhia-Blazon-Carmody complex, 3 to 45 percent slopes0452412615757458z1wy6471:24000
Forelle-Poposhia loams, 2 to 12 percent slopes2941211615747858vywy6471:24000
Poposhia loam, 1 to 6 percent slopes043905315754458y2wy6471:24000
Poposhia-Grieves complex, 0 to 6 percent slopes046385215757358z0wy6471:24000
Gypsids-Poposhia gravelly loams, 0 to 6 percent slopes0892543157714593kwy6471:24000
Forelle-Poposhia association, 2 to 12 percent slopes532182190155521tqhwy67719751:24000
Poposhia-Blazon-Carmody complex, hilly552055190157121tr0wy67719751:24000
Poposhia loam, 1 to 6 percent slopes5197190157021tqzwy67719751:24000
Forelle-Poposhia association, 2 to 12 percent slopes14847793503013jwf7wy71319861:24000
Poposhia-Blazon-Carmody complex, hilly18647347503051jwggwy71319861:24000
Poposhia, sodic-Blazon complex, rolling1879709503052jwghwy71319861:24000
Sandbranch-Ryan Park variant-Poposhia complex, 1 to 8 percent slopes2063654503079jwhcwy71319861:24000
Absher-Poposhia-Sinkson complex, 1 to 10 percent slopes1012685502959jwchwy71319861:24000
Tisworth-Poposhia complex, undulating2132351503090jwhqwy71319861:24000
Poposhia loam, 1 to 6 percent slopes1851224503050jwgfwy71319861:24000
Poposhia-Trimad complex, 3 to 15 percent slopes162527501049633j6xwy72119941:24000
Poposhia silt loam, 0 to 6 percent slopes158155711049593j6swy72119941:24000
Poposhia-Blazon, thin solum-Rock outcrop complex, 5 to 35 percent slopes16088731049613j6vwy72119941:24000
Poposhia-Blazon silt loams, 3 to 30 percent slopes15975901049603j6twy72119941:24000
Urban land-Poposhia-Trimad complex, 3 to 15 percent slopes18959341049903j7swy72119941:24000
Trimad-Poposhia complex, dry, 6 to 15 percent slopes17958881049803j7gwy72119941:24000
Urban land-Poposhia complex, 0 to 6 percent slopes18850251049893j7rwy72119941:24000
Blazon-Blazon, thin solum-Poposhia silt loams, 0 to 6 percent slopes10846951049093j55wy72119941:24000
Poposhia-Piezon silt loams, 0 to 6 percent slopes16137581049623j6wwy72119941:24000
Cumberhill-Sandbranch-Poposhia complex, 4 to 15 percent slopes633830732382xgc5wy7231:24000
Poposhia-Lamanga complex, 0 to 2 percent slopes111731609012yx3fwy7231:24000
Forelle, moderately deep-Rock River-Poposhia complex, 0 to 6 percent slopes -- draft71412393625187442q048wy7231:24000
Chanute-Colnevee-Poposhia family complex, 2 to 8 percent slopes4223322234830j6fwy7371:24000
Thenipel, sodic-Poposhia-Thenipel complex, 1 to 8 percent slopes4239322251130j6ywy7371:24000
Poposhia-Redgap-Zagpeed complex, 0 to 10 percent slopes2243325925547302rc08wy7371:24000
Blackhall-Blazon-Poposhia complex, 3 to 30 percent slopes -- draft590832572292jx2swy7371:24000

Map of Series Extent

Approximate geographic distribution of the POPOSHIA 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 .