Soil Data Explorer - VERSHIRE

Official Series Description

Lab Data Summary

Aggregate lab data for the VERSHIRE soil series. This aggregation is based on all pedons with a current taxon name of VERSHIRE, 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 VERSHIRE 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
143	84P0794	84VT023010	Vershire	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.1916656,-72.6266632
143	85P0877	S1985VT027015	Vershire	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.7038879,-72.6536102
144B	85P0975	85VT027024	Vershire	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.6244431,-72.5538864
144B	87P0581	87VT027001	Vershire	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.5280571,-72.5041656
144B	87P0583	87VT027003	Vershire	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.6147232,-72.5919418
144B	89P0360	88VT005816	Vershire	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.2866669,-72.1750031
144B	40A1215	S1974VT017007	VERSHIRE	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.9880562,-72.6130524
144B	40A1216	S1974VT017008	VERSHIRE	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.960556,-72.632225
144B	40A1213	S1974VT017009	Vershire	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.9416656,-72.4980545
144B	40A1217	S1974VT017017	VERSHIRE	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.8752785,-72.4800034
144B	85P0978	S1985VT027027	Vershire	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.7597237,-72.2825012
144B	96P0016	S1995VT019004	Vershire	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.9847221,-72.0947189
144B	96P0017	S1995VT019005	Vershire	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.9855537,-72.0977783
n/a	40A1308	S1977VT025001	Vershire	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the VERSHIRE 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 VERSHIRE 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 VERSHIRE 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 VERSHIRE 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 VERSHIRE 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 VERSHIRE 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 VERSHIRE 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 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 VERSHIRE, 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 VERSHIRE 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
Vershire-Lombard complex, 15 to 35 percent slopes, very stony	214D	36414	282863	9hbm	vt005	2006	1:20000
Vershire-Lombard complex, 8 to 15 percent slopes, rocky	14C	18360	282828	9h9h	vt005	2006	1:20000
Vershire-Lombard complex, 15 to 25 percent slopes, rocky	14D	18230	282829	9h9j	vt005	2006	1:20000
Vershire-Glover complex, 15 to 35 percent slopes, very rocky	56D	13023	282932	9hdv	vt005	2006	1:20000
Vershire-Lombard complex, 8 to 15 percent slopes, very stony	214C	12192	282862	9hbl	vt005	2006	1:20000
Vershire-Glover complex, 35 to 60 percent slopes, very rocky	56E	10833	282933	9hdw	vt005	2006	1:20000
Vershire-Lombard complex, 35 to 60 percent slopes, very stony	214E	6956	282864	9hbn	vt005	2006	1:20000
Vershire-Lombard complex, 3 to 8 percent slopes, rocky	14B	3995	282827	9h9g	vt005	2006	1:20000
Vershire-Glover complex, 8 to 15 percent slopes, very rocky	56C	3650	282931	9hdt	vt005	2006	1:20000
Vershire-Lombard complex, 25 to 35 percent slopes, rocky	14E	2204	282830	9h9k	vt005	2006	1:20000
Vershire-Lombard complex, 3 to 8 percent slopes, very stony	214B	895	282861	9hbk	vt005	2006	1:20000
Vershire-Glover complex, 3 to 8 percent slopes, very rocky	56B	265	282930	9hds	vt005	2006	1:20000
Vershire-Lombard complex, 15 to 35 percent slopes, very stony	214D	410	1401207	1j127	vt009	2012	1:
Vershire-Lombard complex, 8 to 15 percent slopes, very stony	214C	405	1401206	1j126	vt009	2012	1:
Vershire-Lombard complex, 3 to 8 percent slopes, very stony	214B	147	1401205	1j125	vt009	2012	1:
Vershire-Glover complex, 15 to 35 percent slopes, very rocky	56D	127	1401099	1j0yr	vt009	2012	1:
Vershire-Glover complex, 8 to 15 percent slopes, very rocky	56C	95	1401098	1j0yq	vt009	2012	1:
Vershire-Lombard complex, 8 to 15 percent slopes, rocky	14C	82	1401023	1j0w9	vt009	2012	1:
Vershire-Lombard complex, 3 to 8 percent slopes, rocky	14B	23	1401022	1j0w8	vt009	2012	1:
Vershire-Glover complex, 35 to 60 percent slopes, very rocky	56E	21	1401100	1j0ys	vt009	2012	1:
Vershire-Lombard complex, 15 to 25 percent slopes, rocky	14D	20	1401024	1j0wb	vt009	2012	1:
Vershire-Glover-Rock outcrop complex, 8 to 25 percent slopes	VgD	24809	279437	9cs3	vt017	1975	1:20000
Vershire-Glover complex, 25 to 50 percent slopes	VhE	6188	279438	9cs4	vt017	1975	1:20000
Vershire-Glover rocky loams, 8 to 15 percent slopes	VeC	5087	279435	9cs1	vt017	1975	1:20000
Vershire-Glover rocky loams, 3 to 8 percent slopes	VeB	2942	279434	9cs0	vt017	1975	1:20000
Vershire-Glover rocky loams, 15 to 25 percent slopes	VeD	1702	279436	9cs2	vt017	1975	1:20000
Vershire-Glover complex, 15 to 35 percent slopes, very rocky	94D	17016	283551	9j1t	vt019	2005	1:20000
Vershire-Glover complex, 8 to 15 percent slopes, very rocky	94C	11258	283550	9j1s	vt019	2005	1:20000
Vershire-Lombard complex, 8 to 15 percent slopes, rocky	3C	10818	283474	9hzb	vt019	2005	1:20000
Vershire-Glover complex, 35 to 60 percent slopes, very rocky	94E	7599	283552	9j1v	vt019	2005	1:20000
Vershire-Lombard complex, 8 to 15 percent slopes, very stony	6C	5542	283517	9j0q	vt019	2005	1:20000
Vershire-Lombard complex, 3 to 8 percent slopes, rocky	3B	4874	283473	9hz9	vt019	2005	1:20000
Vershire-Lombard complex, 15 to 35 percent slopes, very stony	6D	3555	283518	9j0r	vt019	2005	1:20000
Vershire-Lombard complex, 15 to 25 percent slopes, rocky	3D	1742	283475	9hzc	vt019	2005	1:20000
Vershire-Lombard complex, 3 to 8 percent slopes, very stony	6B	1126	283516	9j0p	vt019	2005	1:20000
Glover-Vershire complex, 15 to 35 percent slopes, very rocky	67D	20418	282729	9h69	vt023	1996	1:20000
Vershire-Dummerston complex, 8 to 15 percent slopes, rocky	66C	15198	282724	9h64	vt023	1996	1:20000
Vershire-Dummerston complex, 15 to 25 percent slopes, rocky	66D	13215	282725	9h65	vt023	1996	1:20000
Glover-Vershire complex, 35 to 60 percent slopes, very rocky	67E	7313	282730	9h6b	vt023	1996	1:20000
Glover-Vershire complex, 8 to 15 percent slopes, very rocky	67C	7061	282728	9h68	vt023	1996	1:20000
Vershire-Dummerston complex, 25 to 60 percent slopes, rocky	66E	2305	282726	9h66	vt023	1996	1:20000
Vershire-Dummerston complex, 3 to 8 percent slopes, rocky	66B	1604	282723	9h63	vt023	1996	1:20000
Glover-Vershire complex, 15 to 35 percent slopes, very rocky	20D	39767	283153	9hmz	vt027	2000	1:20000
Vershire-Dummerston complex, 15 to 25 percent slopes, rocky	19D	33409	283145	9hmq	vt027	2000	1:20000
Glover-Vershire complex, 35 to 60 percent slopes, very rocky	20E	25223	283154	9hn0	vt027	2000	1:20000
Glover-Vershire complex, 3 to 15 percent slopes, very rocky	20C	19104	283152	9hmy	vt027	2000	1:20000
Vershire-Dummerston complex, 8 to 15 percent slopes, rocky	19C	15010	283144	9hmp	vt027	2000	1:20000
Vershire-Dummerston complex, 25 to 60 percent slopes, rocky	19E	14444	283146	9hmr	vt027	2000	1:20000
Vershire-Buckland complex, 8 to 15 percent slopes	49C	1676	283219	9hq3	vt027	2000	1:20000
Vershire-Buckland complex, 15 to 25 percent slopes	49D	1342	283220	9hq4	vt027	2000	1:20000
Vershire-Dummerston complex, 3 to 8 percent slopes, rocky	19B	949	283143	9hmn	vt027	2000	1:20000
Vershire-Buckland complex, 3 to 8 percent slopes	49B	159	283218	9hq2	vt027	2000	1:20000

Map of Series Extent

Approximate geographic distribution of the VERSHIRE 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).