Official Series Description


Lab Data Summary

Aggregate lab data for the CARFALL soil series. This aggregation is based on all pedons with a current taxon name of CARFALL, 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 CARFALL 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 CARFALL 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 CARFALL 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 CARFALL 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 CARFALL 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 CARFALL 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 CARFALL 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 CARFALL 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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Soil series sharing subgroup-level classification with CARFALL, 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 CARFALL 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
Carfall-Assinniboine complex, 2 to 8 percent slopes114C9832342841chrdmt01119921:24000
Carfall-Assinniboine complex, 8 to 15 percent slopes114D5344342842chrfmt01119921:24000
Carfall loam, 2 to 8 percent slopes14C4090342901chtbmt01119921:24000
Carfall fine sandy loam, 2 to 8 percent slopes214C2483343027chydmt01119921:24000
Carfall fine sandy loam, 8 to 15 percent slopes214D1283343028chyfmt01119921:24000
Carfall-Assinniboine complex, 2 to 8 percent slopes114C1526342070cgyjmt02519911:24000
Carfall loam, 2 to 8 percent slopes14C1272342093cgz8mt02519911:24000
Carfall-Assinniboine complex, 8 to 15 percent slopes114D1004342071cgykmt02519911:24000
Kunz family, moist-Carfall family complex, 2 to 40 percent slopes2121613512421k66qut6461:24000
Sheckle family-Carfall family complex, cool, moist, 0 to 40 percent slopes218236512418k66mut6461:24000
Birney, stony-Bondoe-Carfall complex, 1 to 50 percent slopes9C01335665130z8fwy6171:24000
Southbaldy-Sharrot-Carfall, stony complex, 3 to 50 percent slopes5D43335832930zv7wy6171:24000
Raghorn-like-Carfall complex, 3 to 20 percent slopes2C07335833430zvdwy6171:24000
Carfall-Pachel complex, 8 to 25 percent slopes236532534242ztlkwy6291:24000
Carfall, very stony-Zillman, extremely stony-Reicess-like, stony complex, 25 to 60 percent slopes250632504392zv5vwy6291:24000
Carfall-Norbert-Cabba-like complex, 6 to 50 percent slopes555731709902z20pwy6291:24000
Clasoil-Carfall, very stony-Bonjea-like, very stony complex, 25 to 70 percent slopes752032504422zv5ywy6291:24000
Carfall, very stony-Zillman, extremely stony-Reicess-like, stony complex, 25 to 60 percent slopes250632505182zv5vwy65620081:24000
Clasoil-Carfall, very stony-Bonjea-like, very stony complex, 25 to 70 percent slopes752033028902zv5ywy65620081:24000

Map of Series Extent

Approximate geographic distribution of the CARFALL 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 .