Soil Data Explorer - COLLINSTON

Official Series Description

Lab Data Summary

Aggregate lab data for the COLLINSTON soil series. This aggregation is based on all pedons with a current taxon name of COLLINSTON, 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 COLLINSTON were used in the calculation. Source: KSSL snapshot (updated 2020-03-13). 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 COLLINSTON 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 COLLINSTON 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 COLLINSTON 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 COLLINSTON 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).

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

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

Competing Series

Soil series competing with COLLINSTON 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 COLLINSTON 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 COLLINSTON 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 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 flats position figure.

Soil series sharing subgroup-level classification with COLLINSTON, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

1. ID-2010-08-30-06 | Franklin County Area - 2008

   Typical pattern of soils and underlying material in general soil map units 5 (Parleys-Ant Flat-Winwell) and 7 (Wheelon-Collinston-Winwell) (Soil Survey of Franklin County Area, Idaho; 2008).

Map Units

Map units containing COLLINSTON 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
Wheelon-Collinston complex, 4 to 12 percent slopes	149	6724	485241	j8xy	id714	1997	1:24000
Wheelon-Collinston complex, 12 to 20 percent slopes	150	3909	485243	j8y0	id714	1997	1:24000
Winwell-Collinston complex, 2 to 8 percent slopes	155	2037	485248	j8y5	id714	1997	1:24000
Wheelon-Collinston complex, 20 to 60 percent slopes	151	1305	485244	j8y1	id714	1997	1:24000
Collinston-Kearns complex, 2 to 12 percent slopes	23	1647	485615	j9b0	id715	1994	1:24000
Collinston silt loam, 0 to 2 percent slopes	22	827	485614	j99z	id715	1994	1:24000
Wheelon-Collinston silt loams, 10 to 30 percent slopes	WmE	3127	481521	j51y	ut602	1969	1:20000
Collinston-Wheelon silt loams, 6 to 10 percent slopes	CwD	1477	481338	j4w1	ut602	1969	1:20000
WHEELON-COLLINSTON COMPLEX, 10 TO 30 PERCENT SLOPES, ERODED	WlE2	9001	482858	j6g2	ut603	1968	1:20000
MENDON-COLLINSTON COMPLEX, 6 TO 30 PERCENT SLOPES,ERODED	MfE2	4853	482783	j6cn	ut603	1968	1:20000
MENDON-COLLINSTON COMPLEX, 1 TO 6 PERCENT SLOPES	MfB	1401	482782	j6cm	ut603	1968	1:20000
COLLINSTON LOAM, 10 TO 30 PERCENT SLOPES, ERODED	CmE2	1304	482696	j68v	ut603	1968	1:20000
AVON-COLLINSTON COMPLEX, 6 TO 10 PERCENT SLOPES	AsC	1274	482670	j680	ut603	1968	1:20000
AVON-COLLINSTON COMPLEX, 10 TO 30 PERCENT SLOPES	AsE	1123	482671	j681	ut603	1968	1:20000
COLLINSTON LOAM, 6 TO 10 PERCENT SLOPES	CmD	854	482695	j68t	ut603	1968	1:20000
COLLINSTON LOAM, 1 TO 6 PERCENT SLOPES	CmC	813	482694	j68s	ut603	1968	1:20000
COLLINSTON LOAMY FINE SAND, 0 TO 3 PERCENT SLOPES	ClA	468	482693	j68r	ut603	1968	1:20000
Hawkins-Collinston complex, 6 to 30 percent slopes	HcE	410	506556	k03j	ut609	1974	1:24000

Map of Series Extent

Approximate geographic distribution of the COLLINSTON 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).