Official Series Description


Lab Data Summary

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

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
58A83P072175MT087229Sagedale7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.3955574,-106.9069443

Water Balance

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

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

Click the image to view it full size.

Select annual climate data summaries for the SAGEDALE series and siblings. 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 SAGEDALE 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 .

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.

Click the image to view it full size.

Competing Series

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

Click the image to view it full size.

Select annual climate data summaries for the SAGEDALE 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 SAGEDALE 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.

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

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 SAGEDALE, 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 SAGEDALE 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
Sagedale clay loam, 3 to 20 percent slopes9211402502153jvjhco67519861:24000
Sagedale silty clay loam, 2 to 8 percent slopes52C4683343521cjgbmt01719951:24000
Sagedale silty clay loam, 0 to 2 percent slopes52A102343519cjg8mt01719951:24000
Sagedale-Midnot complex, 0 to 8 percent slopes652C32269465421pcxmt02719791:24000
Sagedale silty clay, 0 to 4 percent slopes323B575344179ck4kmt05119921:24000
Sagedale silty clay, 4 to 8 percent slopes323C448344180ck4lmt05119921:24000
Sagedale silty clay loam, 2 to 8 percent slopes323C672345127cl44mt10119921:24000
Wayden-Sagedale silty clay loams, 25 to 60 percent slopesWaF911474554yfmmt60219631:20000
Sagedale-Midnot complex, 0 to 8 percent slopes652C85269467321pcxmt60219631:20000
Sagedale clay loam, 0 to 8 percent slopes640C24269467221m3lmt60219631:20000
Sagedale-Narrows complex, 0 to 8 percent slopes118C3351484034zf6mt61220111:24000
Sagedale clay loam, 2 to 8 percent slopes18C2941484204zfrmt61220111:24000
Wayden-Sagedale silty clay loams, 25 to 60 percent slopes621F13895346862cmy3mt61519921:24000
Sagedale-Wayden silty clay loams, 8 to 25 percent slopes621E6560346861cmy2mt61519921:24000
Sagedale silty clay loam, 0 to 4 percent slopes323B5915346687cmrgmt61519921:24000
Sagedale silty clay loam, 4 to 8 percent slopes323C5196346688cmrhmt61519921:24000
Zahill-Sagedale-Wayden complex, 15 to 45 percent slopes722F5119346899cmz9mt61519921:24000
Sagedale clay loam, 0 to 8 percent slopes640C1485189520321m3lmt62420211:24000
Sagedale-Midnot complex, calcareous, 0 to 8 percent slopes651C526189557221mhhmt62420211:24000
Sagedale-Midnot complex, 0 to 8 percent slopes652C381189738321pcxmt62420211:24000
Sagedale-Windham complex, 8 to 45 percent slopes706E12624874142phc5mt62420211:24000
Sagedale clay loam, 0 to 8 percent slopes640C62261823021m3lmt6321:24000
Sagedale-Cabba complex, 2 to 8 percent slopes238C149414979750w5mt63920001:24000
Sagedale clay loam, 2 to 8 percent slopes265C58214982850x5mt63920001:24000
Sagedale clay loam, 8 to 15 percent slopes265D52114982950x6mt63920001:24000
Sagedale-Cabba complex, 8 to 35 percent slopes238F25114979850w6mt63920001:24000
Sagedale-Cabba-Wayden complex, 8 to 25 percent slopes1588791347984cp39mt64919851:24000
Shambo-Doney-Sagedale complex, 8 to 35 percent slopes1674933347994cp3mmt64919851:24000
Cabba-Wayden-Sagedale complex, 25 to 70 percent slopes534215348085cp6kmt64919851:24000
Sagedale silty clay loam, 4 to 15 percent slopes157728347983cp38mt64919851:24000
Fairfield, gravelly substratum-Tamaneen-Sagedale,calcareous surface, complex, 0 to 4 percent slopes448B3084156921588zmt6691:24000
Cabba-Doney-Sagedale complex, 15 to 45 percent slopes5639F450699344rgqhmt6691:24000
Bayerton-like-Sagedale, stony complex, 15 to 35 percent slopes581332504622zv6lwy6291:24000

Map of Series Extent

Approximate geographic distribution of the SAGEDALE 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 .