Official Series Description


Lab Data Summary

Aggregate lab data for the CANEYHEAD soil series. This aggregation is based on all pedons with a current taxon name of CANEYHEAD, 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 CANEYHEAD were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
152BS95TX199007S95TX199007Caneyhead5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.2959444,-94.13925

Water Balance

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

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Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the CANEYHEAD series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

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Select annual climate data summaries for the CANEYHEAD series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the CANEYHEAD 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 .

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

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

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

Competing Series

Soil series competing with CANEYHEAD share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

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Select annual climate data summaries for the CANEYHEAD series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the CANEYHEAD 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 .

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

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

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with CANEYHEAD, 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 .

Block Diagrams

No block diagrams are available.

Map Units

Map units containing CANEYHEAD 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
Spurger-Caneyhead frequently ponded complex, 0 to 1 percent slopesSpyA66727607201hctxtx07119691:24000
Kenefick-Caneyhead frequently ponded complex, 0 to 1 percent slopesKenA16026379686f748tx19919981:24000
Belrose-Caneyhead frequently ponded complex, 0 to 1 percent slopesBemA99822760765f73ytx19919981:24000
Spurger-Caneyhead frequently ponded complex, 0 to 1 percent slopesSpyA24127607741hctxtx19919981:24000
Kenefick-Caneyhead frequently ponded complex, 0 to 1 percent slopesKenA7592760802f748tx20119731:20000
Belrose-Caneyhead frequently ponded complex, 0 to 1 percent slopesBemA4712760799f73ytx20119731:20000
Spurger-Caneyhead frequently ponded complex, 0 to 1 percent slopesSpyA1229528883341hctxtx29119861:24000
Belrose-Caneyhead frequently ponded complex, 0 to 1 percent slopesBemA38222888265f73ytx29119861:24000
Kenefick-Caneyhead frequently ponded complex, 0 to 1 percent slopesKenA2022888272f748tx29119861:24000
Belrose-Caneyhead frequently ponded complex, 0 to 1 percent slopesBemA15142888342f73ytx33919671:20000
Kenefick-Caneyhead frequently ponded complex, 0 to 1 percent slopesKenA3042888345f748tx33919671:20000
Kenefick-Caneyhead frequently ponded complex, 0 to 1 percent slopesKenA97651479396f748tx45720071:24000
Belrose-Caneyhead frequently ponded complex, 0 to 1 percent slopesBemA93572888381f73ytx45720071:24000
Spurger-Caneyhead frequently ponded complex, 0 to 1 percent slopesSpyA263928883841hctxtx45720071:24000
Belrose-Caneyhead frequently ponded complex, 0 to 1 percent slopesBemA288322888389f73ytx61119801:20000
Spurger-Caneyhead frequently ponded complex, 0 to 1 percent slopesSpyA1253328884281hctxtx61119801:20000
Kenefick-Caneyhead frequently ponded complex, 0 to 1 percent slopesKenA85572888397f748tx61119801:20000
Kenefick-Caneyhead frequently ponded complex, 0 to 1 percent slopesKenA57162888437f748tx61719831:24000
Belrose-Caneyhead frequently ponded complex, 0 to 1 percent slopesBemA45192888434f73ytx61719831:24000
Spurger-Caneyhead frequently ponded complex, 0 to 1 percent slopesSpyA102928884551hctxtx61719831:24000
Spurger-Caneyhead frequently ponded complex, 0 to 1 percent slopesSpyA646128885141hctxtx62319961:24000
Belrose-Caneyhead frequently ponded complex, 0 to 1 percent slopesBemA31222888504f73ytx62319961:24000

Map of Series Extent

Approximate geographic distribution of the CANEYHEAD 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 .