Soil Data Explorer - CORDESTON

Official Series Description

Lab Data Summary

Aggregate lab data for the CORDESTON soil series. This aggregation is based on all pedons with a current taxon name of CORDESTON, 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 CORDESTON were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). 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
62	05N0373	S02SD081001B	Cordeston	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.1928222,-103.7195722

Water Balance

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

Soil series sharing subgroup-level classification with CORDESTON, 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 CORDESTON 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
Cordeston-Rapidcreek, rarely flooded complex, dry, 2 to 9 percent slopes	Q0620C	18	2516997	2krlh	sd047	1980	1:24000
Cordeston-Marshbrook loams, 0 to 6 percent slopes, flooded	Q0206B	4856	2375701	2kr3j	sd081	2007	1:24000
Bullflat, moist-Cordeston silt loams, 2 to 9 percent slopes	Q0502C	678	2375731	2kr4h	sd081	2007	1:24000
Heely-Cordeston complex, 2 to 15 percent slopes	Q0209D	665	2375670	2kr2j	sd081	2007	1:24000
Marshbrook-Cordeston loams, 2 to 9 percent slopes, flooded	Q0217C	618	2375685	2kr30	sd081	2007	1:24000
Cordeston loam, 1 to 6 percent slopes, flooded	Q0518B	616	2513756	2mv3f	sd081	2007	1:24000
Cordeston-Rapidcreek, rarely flooded complex, 2 to 9 percent slopes	Q0520C	277	2375752	2kr55	sd081	2007	1:24000
Cordeston loam, 6 to 10 percent slopes	Q0518C	255	2427154	2mgn9	sd081	2007	1:24000
Bullflat, moist-Cordeston silt loams, 2 to 9 percent slopes	Q0502C	174	2513958	2kr4h	sd600	1974	1:24000
Marshbrook-Cordeston loams, 2 to 9 percent slopes, flooded	Q0217C	94	2514525	2kr30	sd600	1974	1:24000
Cordeston-Rapidcreek, rarely flooded complex, 2 to 9 percent slopes	Q0520C	87	2513965	2kr55	sd600	1974	1:24000
Cordeston loam, 1 to 6 percent slopes, flooded	Q0518B	59	2513758	2mv3f	sd600	1974	1:24000
Cordeston-Rapidcreek, rarely flooded complex, dry, 2 to 9 percent slopes	Q0620C	54	2516996	2krlh	sd600	1974	1:24000
Cordeston loam, 6 to 10 percent slopes	Q0518C	48	2513943	2mgn9	sd600	1974	1:24000
Bullflat-Cordeston, dry silt loams, high mica, 2 to 9 percent slopes	Q0300C	6899	2586606	2krjf	sd607	2011	1:24000
Cordeston-Marshbrook loams, 0 to 6 percent slopes, flooded	Q0206B	6600	2586634	2kr3j	sd607	2011	1:24000
Heely-Cordeston complex, 2 to 15 percent slopes	Q0209D	6064	2586551	2kr2j	sd607	2011	1:24000
Bullflat-Cordeston, dry silt loams, 2 to 9 percent slopes	Q0609C	5774	2586417	2mhnl	sd607	2011	1:24000
Cordeston-Rapidcreek, rarely flooded complex, dry, 2 to 9 percent slopes	Q0620C	4656	2586442	2krlh	sd607	2011	1:24000
Cordeston loams, dry, high mica, 2 to 10 percent slopes, flooded	Q0306C	4386	2586580	2krjw	sd607	2011	1:24000
Cordeston, dry-Marshbrook loams, 0 to 6 percent slopes, flooded	Q0307B	4260	2586448	2krjx	sd607	2011	1:24000
Cordeston loam, high mica, 2 to 10 percent slopes, flooded	Q0205C	3993	2586630	2kr8s	sd607	2011	1:24000
Heely-Cordeston complex, dry, 6 to 15 percent slopes	Q0310D	3684	2586462	2krk0	sd607	2011	1:24000
Bullflat, moist-Cordeston silt loams, 2 to 9 percent slopes	Q0502C	1814	2586591	2kr4h	sd607	2011	1:24000
Bullflat, moist-Cordeston silt loams, high mica, 2 to 9 percent slopes	Q0200C	1492	2586612	2kr29	sd607	2011	1:24000
Cordeston loam, dry, 2 to 10 percent slopes	Q0619C	904	2586450	2mhx2	sd607	2011	1:24000
Cordeston-Rapidcreek, rarely flooded complex, 2 to 9 percent slopes	Q0520C	753	2586412	2kr55	sd607	2011	1:24000
Cordeston loam, 1 to 6 percent slopes, flooded	Q0518B	8306	2513757	2mv3f	wy011	1978	1:24000
Cordeston-Hickok loams, 2 to 6 percent slopes	Q0519B	2489	2438907	2mvwf	wy011	1978	1:24000
Cordeston loam, 6 to 10 percent slopes	Q0518C	945	2513942	2mgn9	wy011	1978	1:24000
Cordeston silt loams, 0 to 3 percent slopes, flooded	Q0813A	621	2439233	2mw6y	wy011	1978	1:24000
Nunnston, thick surface-Cordeston loams, 1 to 6 percent slopes	Q0913B	338	2441286	2myc5	wy011	1978	1:24000
Cordeston, warm-Lakoa loams, 2 to 6 percent slopes	P094B	202	2768171	2rwdw	wy011	1978	1:24000
Cordeston loam, high mica, 2 to 10 percent slopes, flooded	Q0205C	65	2516983	2kr8s	wy011	1978	1:24000
Cordeston loam, dry, 0 to 6 percent slopes	P092B	43	2768174	2rxtn	wy011	1978	1:24000
Cordeston loam, 1 to 6 percent slopes, flooded	Q0518B	1777	2438163	2mv3f	wy045	1984	1:24000
Cordeston loam, dry, 0 to 6 percent slopes	P092B	1737	2745971	2rxtn	wy045	1984	1:24000
Cordeston loam, 6 to 10 percent slopes	Q0518C	25	2513941	2mgn9	wy045	1984	1:24000

Map of Series Extent

Approximate geographic distribution of the CORDESTON 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).