Soil Data Explorer - CANA

Official Series Description

Lab Data Summary

Aggregate lab data for the CANA soil series. This aggregation is based on all pedons with a current taxon name of CANA, 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 CANA 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.

Pedons used in the lab summary:

MLRA	Lab ID	Pedon ID	Taxonname	CI	NSSL / NASIS Reports	Link To SoilWeb GMap
n/a	RO-058	1958-OH141-058	Cana	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	PY-029	1973-OH129-029	Cana	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	RO-095	YYYY-OH141-095	Cana	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 CANA 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 CANA series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-02) and snapshot of SC database (updated 2023-10-02).

Select annual climate data summaries for the CANA 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 2023-10-09).

Geomorphic description summaries for the CANA 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 2023-10-04).

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

Competing Series

Soil series competing with CANA share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-02) and snapshot of the SC database (updated 2023-10-02).

Select annual climate data summaries for the CANA 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 2023-10-09).

Geomorphic description summaries for the CANA 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 2023-10-04).

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 CANA, 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 2023-10-02).

Block Diagrams

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

1. OH-2010-09-29-23 | Ross County - 2003

   Typical pattern of soils and parent material in the Cruze-Rossmoyne-Shelocta general soil map unit (Soil Survey of Ross County, Ohio; 2003).

Map Units

Map units containing CANA 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
Cana silt loam, 2 to 6 percent slopes, moderately eroded	CaB2	64	169221	5p2r	oh047	1968	1:15840
Cana silt loam, 6 to 12 percent slopes, moderately eroded	CaC2	48	169222	5p2s	oh047	1968	1:15840
Cana silt loam, 12 to 18 percent slopes, moderately eroded	CaD2	469	1420383	1jp0t	oh071	1973	1:15840
Cana silt loam, 6 to 12 percent slopes, moderately eroded	CaC2	464	1420382	1jp0s	oh071	1973	1:15840
Cana silt loam, 18 to 35 percent slopes	CaF	261	1420384	1jp0v	oh071	1973	1:15840
Cana silt loam, 2 to 6 percent slopes	CaB	163	1420381	1jp0r	oh071	1973	1:15840
Cana silt loam, 2 to 6 percent slopes, moderately eroded	CaB2	5	1420697	1jpby	oh071	1973	1:15840
Cana silt loam, 12 to 20 percent slopes, eroded	CbD2	4	1398185	1hxxr	oh073	1986	1:15840
Cana silt loam, 20 to 35 percent slopes, eroded	CaE2	26	1688994	1tpjp	oh131	1984	1:15840
Cana silt loam, 12 to 20 percent slopes, eroded	CaD2	6745	170844	5qs3	oh141	1997	1:15840
Rossmoyne-Cana complex, 6 to 12 percent slopes, eroded	RsC2	5959	170957	5qwr	oh141	1997	1:15840
Cana silt loam, 6 to 12 percent slopes, eroded	CaC2	3031	170843	5qs2	oh141	1997	1:15840
Cana silt loam, 20 to 35 percent slopes, eroded	CaE2	2822	170845	5qs4	oh141	1997	1:15840
Cana silt loam, 2 to 6 percent slopes	CaB	668	170842	5qs1	oh141	1997	1:15840
Rossmoyne-Cana complex, 2 to 6 percent slopes	RsB	349	170956	5qwq	oh141	1997	1:15840

Map of Series Extent

Approximate geographic distribution of the CANA 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 2023-10-04).