Soil Data Explorer - POPOSHIA

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 (updated 2020-03-13). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Pedons used in the lab summary:

MLRA	Lab ID	Pedon ID	Taxonname	CI	NSSL / NASIS Reports	Link To SoilWeb GMap
67A	89P0818	89WY021004	Poposhia	8	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.2338905,-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.

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 (updated 2024-10-24), parsed OSD records (updated 2024-10-23) and snapshot of SC database (updated 2024-10-23).

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 (updated 2024-10-23).

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 (updated 2024-10-23).

Competing Series

Soil series competing with POPOSHIA share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2024-10-23) and snapshot of the SC database (updated 2024-10-23).

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 (updated 2024-10-23).

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 (updated 2024-10-23).

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 (updated 2024-10-23).

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 slopes	129	348	497628	jptj	co644	1980	1:24000
Poposhia silt loam, 0 to 6 percent slopes	200	740	104434	3hnv	wy031	1998	1:24000
Poposhia-Chaperton association, 6 to 12 percent slopes	203	455	104557	3hst	wy031	1998	1:24000
Poposhia-Forelle complex, 1 to 8 percent slopes	204	369	104559	3hsw	wy031	1998	1:24000
Poposhia-Blazon silt loams, 3 to 30 percent slopes	201	66	104435	3hnw	wy031	1998	1:24000
Poposhia-Blazon, thin solum-Rock outcrop complex, 5 to 35 percent slopes	202	4	104436	3hnx	wy031	1998	1:24000
Poposhia loam, 0 to 3 percent slopes	161	824	1862617	20j6f	wy041		1:24000
Obadia-Poposhia association, 0 to 3 percent slopes	182	548	1862620	20j6j	wy041		1:24000
Poposhia loam, 6 to 10 percent slopes	3534C	351	2484094	2pcx2	wy041		1:24000
Poposhia-Forelle complex, 1 to 8 percent slopes	198	63638	501742	jv37	wy601	1991	1:24000
Poposhia-Chaperton association, 6 to 12 percent slopes	199	38339	501743	jv38	wy601	1991	1:24000
Chaperton-Poposhia complex, 3 to 30 percent slopes	140	5003	501677	jv14	wy601	1991	1:24000
Poposhia-Blazon complex, 3 to 15 percent slopes	197	4188	501741	jv36	wy601	1991	1:24000
Poposhia-Blazon complex, 3 to 15 percent slopes	240	2339	502366	jvrc	wy625	1985	1:24000
Poposhia-Evanston complex, 6 to 40 percent slopes -- Draft	5502		2482753	2pbht	wy629		1:24000
Poposhia-Havre overflow complex, 0 to 6 percent slopes -- draft	406	10327	2421005	2m87y	wy630		1:24000
Tisworth-Poposhia complex, 0 to 8 percent slopes -- draft	414	5728	2455475	2nf3w	wy630		1:24000
Poposhia loam, 2 to 6 percent slopes -- draft	349AB	4782	2378259	2kts1	wy630		1:24000
Poposhia loam, 0 to 2 percent slopes -- draft	349A	549	2393893	2lc1c	wy630		1:24000
Poposhia-Redgap-Zagpeed complex, 0 to 10 percent slopes	2243	1203	2554737	2rc08	wy635		1:24000
Poposhia loam, 3 to 6 percent slopes	162	7567	504021	jxgr	wy638	1990	1:24000
Poposhia clay loam, 0 to 3 percent slopes	164	2534	504023	jxgt	wy638	1990	1:24000
Poposhia loam, 0 to 3 percent slopes	161	2160	504019	jxgp	wy638	1990	1:24000
Poposhia loam, 6 to 10 percent slopes	163	2076	504022	jxgs	wy638	1990	1:24000
Delphill-Iyers-Poposhia complex, 3 to 25 percent slopes	119	1478	503962	jxdv	wy638	1990	1:24000
Spicerton-Poposhia complex, 0 to 3 percent slopes	182	1256	504045	jxhj	wy638	1990	1:24000
Poposhia very fine sandy loam, strongly alkaline, 1 to 3 percent slopes	166	774	504025	jxgw	wy638	1990	1:24000
Poposhia clay loam, 3 to 6 percent slopes	165	734	504024	jxgv	wy638	1990	1:24000
Poposhia-Blazon-Carmody complex, 3 to 45 percent slopes	045	24126	157574	58z1	wy647		1:24000
Forelle-Poposhia loams, 2 to 12 percent slopes	294	12116	157478	58vy	wy647		1:24000
Poposhia loam, 1 to 6 percent slopes	043	9053	157544	58y2	wy647		1:24000
Poposhia-Grieves complex, 0 to 6 percent slopes	046	3852	157573	58z0	wy647		1:24000
Gypsids-Poposhia gravelly loams, 0 to 6 percent slopes	089	2543	157714	593k	wy647		1:24000
Forelle-Poposhia association, 2 to 12 percent slopes	53	2182	1901555	21tqh	wy677	1975	1:24000
Poposhia-Blazon-Carmody complex, hilly	55	2055	1901571	21tr0	wy677	1975	1:24000
Poposhia loam, 1 to 6 percent slopes	51	97	1901570	21tqz	wy677	1975	1:24000
Forelle-Poposhia association, 2 to 12 percent slopes	148	47793	503013	jwf7	wy713	1986	1:24000
Poposhia-Blazon-Carmody complex, hilly	186	47347	503051	jwgg	wy713	1986	1:24000
Poposhia, sodic-Blazon complex, rolling	187	9709	503052	jwgh	wy713	1986	1:24000
Sandbranch-Ryan Park variant-Poposhia complex, 1 to 8 percent slopes	206	3654	503079	jwhc	wy713	1986	1:24000
Absher-Poposhia-Sinkson complex, 1 to 10 percent slopes	101	2685	502959	jwch	wy713	1986	1:24000
Tisworth-Poposhia complex, undulating	213	2351	503090	jwhq	wy713	1986	1:24000
Poposhia loam, 1 to 6 percent slopes	185	1224	503050	jwgf	wy713	1986	1:24000
Poposhia-Trimad complex, 3 to 15 percent slopes	162	52750	104963	3j6x	wy721	1994	1:24000
Poposhia silt loam, 0 to 6 percent slopes	158	15571	104959	3j6s	wy721	1994	1:24000
Poposhia-Blazon, thin solum-Rock outcrop complex, 5 to 35 percent slopes	160	8873	104961	3j6v	wy721	1994	1:24000
Poposhia-Blazon silt loams, 3 to 30 percent slopes	159	7590	104960	3j6t	wy721	1994	1:24000
Urban land-Poposhia-Trimad complex, 3 to 15 percent slopes	189	5934	104990	3j7s	wy721	1994	1:24000
Trimad-Poposhia complex, dry, 6 to 15 percent slopes	179	5888	104980	3j7g	wy721	1994	1:24000
Urban land-Poposhia complex, 0 to 6 percent slopes	188	5025	104989	3j7r	wy721	1994	1:24000
Blazon-Blazon, thin solum-Poposhia silt loams, 0 to 6 percent slopes	108	4695	104909	3j55	wy721	1994	1:24000
Poposhia-Piezon silt loams, 0 to 6 percent slopes	161	3758	104962	3j6w	wy721	1994	1:24000
Cumberhill-Sandbranch-Poposhia complex, 4 to 15 percent slopes	6338		3073238	2xgc5	wy723		1:24000
Poposhia-Lamanga complex, 0 to 2 percent slopes	1117		3160901	2yx3f	wy723		1:24000
Forelle, moderately deep-Rock River-Poposhia complex, 0 to 6 percent slopes -- draft	7141	23936	2518744	2q048	wy723		1:24000
Scooby-Obadia-Poposhia complex, 1 to 6 percent slopes	2429	1188	2611920	2l3f6	wy723		1:24000
Poposhia-Forelle-Scooby complex, 0 to 6 percent slopes	4424		3406459	3133l	wy737		1:24000
Slipperyjim-Poposhia-Thenipel complex, 1 to 8 percent slopes	4239		3222511	30j6y	wy737		1:24000
Poposhia, sodic surface-Poposhia-Blanfort complex, 1 to 15 percent slopes	4245		3406446	316pd	wy737		1:24000
Poposhia-Hawkstone-Redcreek family, complex, 1 to 8 percent slopes	4421		3406456	3133h	wy737		1:24000
Poposhia family-Schrute-Redgap complex, 2 to 8 percent slopes	4129		3406432	31d7y	wy737		1:24000
Chanute-Colnevee-Poposhia family complex, 2 to 8 percent slopes	4223		3222348	30j6f	wy737		1:24000
Scooby-Obadia-Poposhia complex, 1 to 6 percent slopes	2429	29888	2572303	2l3f6	wy737		1:24000
Poposhia-Redgap-Zagpeed complex, 0 to 10 percent slopes	2243	3259	2554730	2rc08	wy737		1:24000
Blackhall-Blazon-Poposhia complex, 3 to 30 percent slopes -- draft	590	83	2572292	jx2s	wy737		1:24000

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 (updated 2024-10-30).