Soil Data Explorer - COLOCKUM

Official Series Description

Lab Data Summary

Aggregate lab data for the COLOCKUM soil series. This aggregation is based on all pedons with a current taxon name of COLOCKUM, 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 COLOCKUM 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
8	88P0442	88WA037007	Colockum	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	46.6811104,-120.1530533

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the COLOCKUM 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 COLOCKUM 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 COLOCKUM 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 COLOCKUM 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 terrace figure.

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

Competing Series

Soil series competing with COLOCKUM 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 COLOCKUM 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 COLOCKUM 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 COLOCKUM, 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 COLOCKUM 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
Colockum bouldery silt loam, 25 to 45 percent slopes	CtE	4040	73333	2g9l	wa607	1969	1:20000
Colockum silt loam, 25 to 45 percent slopes	CrE	1949	73329	2g9g	wa607	1969	1:20000
Colockum silt loam, 8 to 15 percent slopes	CrC	1860	73327	2g9d	wa607	1969	1:20000
Colockum silt loam, 15 to 25 percent slopes	CrD	1525	73328	2g9f	wa607	1969	1:20000
Colockum silt loam, 3 to 8 percent slopes	CrB	1244	73326	2g9c	wa607	1969	1:20000
Colockum cobbly silt loam 25 to 45 percent slopes	CsE	620	73332	2g9k	wa607	1969	1:20000
Colockum cobbly silt loam, 8 to 15 percent slopes	CsC	403	73330	2g9h	wa607	1969	1:20000
Colockum cobbly silt loam, 15 to 25 percent slopes	CsD	273	73331	2g9j	wa607	1969	1:20000
Colockum-Cheviot complex, 15 to 30 percent slopes	1010	2390	76123	2k6l	wa639	2003	1:24000
Colockum-Cheviot complex, 30 to 60 percent slopes	1011	2385	76124	2k6m	wa639	2003	1:24000
Broadax-Colockum-Tronsen complex, 5 to 15 percent slopes	391	1390	76318	2kdw	wa639	2003	1:24000
Oreoke-Colockum complex, 30 to 60 percent slopes	43	574	76336	2kfg	wa639	2003	1:24000
Colockum stony loam, 3 to 25 percent slopes	91	1181	70732	2clp	wa648	1987	1:24000
Colockum loam, 8 to 15 percent slopes	90	587	70731	2cln	wa648	1987	1:24000
Colockum bouldery loam, 25 to 65 percent slopes	92	325	70733	2clq	wa648	1987	1:24000
Colockum silt loam, 10 to 15 percent slopes	49	2065	70956	2ctx	wa681	1994	1:24000
Colockum silt loam, 5 to 10 percent slopes	48	1612	70951	2ctr	wa681	1994	1:24000
Colockum silt loam, 15 to 30 percent slopes	50	1080	70966	2cv7	wa681	1994	1:24000
Camaspatch-Colockum complex, 15 to 30 percent slopes	39	592	70887	2crp	wa681	1994	1:24000
Colockum-Tronsen complex, 3 to 15 percent slopes	51	253	70977	2cvl	wa681	1994	1:24000

Map of Series Extent

Approximate geographic distribution of the COLOCKUM 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).