Official Series Description


Lab Data Summary

Aggregate lab data for the CARMODY soil series. This aggregation is based on all pedons with a current taxon name of CARMODY, 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 CARMODY were used in the calculation. Source: KSSL snapshot . 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 CARMODY 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 CARMODY 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 CARMODY 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 CARMODY 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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Competing Series

Soil series competing with CARMODY 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 CARMODY series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the CARMODY 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

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

Soil series sharing subgroup-level classification with CARMODY, 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

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

  1. WY-2012-03-23-01 | Fremont County, East Part and Dubois Area - July 1993

    Soils and their landscape positions as they relate to parent material, precipitation zones, and temperature regimes (Soil Survey of Fremont County, East Part and Dubois Area, WY; 1993).

Map Units

Map units containing CARMODY 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
Carmody-Rock River-Crestman complex, 6 to 15 percent slopes3012812497205jpcwco68619921:31680
Carmody-Ryan Park fine sandy loams, 6 to 15 percent slopes13612395501672jv0zwy60119911:24000
Carmody-Edlin fine sandy loams, 15 to 45 percent slopes1351964501671jv0ywy60119911:24000
Carmody-Blackhall complex, 6 to 45 percent slopes -- Draft47215258353s1wy6291:24000
Blackhall-Carmody-Rock outcrop complex, 3 to 50 percent slopes -- draft3031413623778622ktc7wy6301:24000
McFadden-Carmody complex, 0 to 15 percent slopes -- draft3431096423785522kv2hwy6301:24000
Carmody-Cushool-Rock outcrop complex, 3 to 15 percent slopes -- draft388816526092322r854wy6301:24000
Carmody-Blackhall sandy loams, 2 to 15 percent slopes -- draft410539324210182m88cwy6301:24000
Elk Mountain-Carmody complex, 6 to 30 percent slopes -- draft411389224210192m88dwy6301:24000
Poposhia, alkali-Carmody loams, 0 to 6 percent slopes -- draft372165424210022m87vwy6301:24000
Carmody-Ryan Park fine sandy loams, 6 to 15 percent slopes45155625730312x8pgwy6301:24000
Cragosen-Carmody-Blazon complex, 6 to 40 percent slopes0253494215754058xywy6471:24000
Blackhall-Carmody association, 5 to 45 percent slopes0232543515754258y0wy6471:24000
Poposhia-Blazon-Carmody complex, 3 to 45 percent slopes0452412615757458z1wy6471:24000
Rentsac-Carmody complex, 2 to 40 percent slopes0471107315757258yzwy6471:24000
Blazon-Rock outcrop-Carmody complex, 2 to 40 percent slopes419220185908420djgwy6471:24000
Blackhall-Carmody association2141841590595bhywy67719751:24000
Blazon-Rock outcrop-Carmody complex, hilly602919190154921tq9wy67719751:24000
Poposhia-Blazon-Carmody complex, hilly552055190157121tr0wy67719751:24000
Blackhall-Carmody association, hilly59966190154821tq8wy67719751:24000
Rentsac-Carmody complex, hilly64211190157221tr1wy67719751:24000
Cragosen-Carmody-Blazon complex, hilly6743190155221tqdwy67719751:24000
Blackhall-Carmody association, hilly11760449502982jwd7wy71319861:24000
Cragosen-Carmody-Blazon complex, hilly13659156503001jwdvwy71319861:24000
Blazon-Rock outcrop-Carmody complex, hilly11853053502983jwd8wy71319861:24000
Poposhia-Blazon-Carmody complex, hilly18647347503051jwggwy71319861:24000
Cragosen-Rock outcrop-Carmody complex, hilly13739676503002jwdwwy71319861:24000
Ryan Park-Carmody association, 1 to 15 percent slopes20329404503072jwh4wy71319861:24000
Rentsac-Carmody complex, hilly19110038503056jwgmwy71319861:24000
Forelle-Redgap-Carmody, rubbly surface, complex, 2 to 25 percent slopes4225322235030j6hwy7371:24000
Carmody-Cushool-Rock outcrop complex, 3 to 15 percent slopes -- draft738820526119102r854wy7371:24000

Map of Series Extent

Approximate geographic distribution of the CARMODY 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 .