Official Series Description


Lab Data Summary

Aggregate lab data for the EXCELSIOR soil series. This aggregation is based on all pedons with a current taxon name of EXCELSIOR, 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 EXCELSIOR 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
1587P022686CA019031Excelsior7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.6225014,-120.6633301
1788P027087CA019008Excelsior8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.7877769,-120.7786102
1788P097188CA107011EXCELSIOR5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.8666649,-119.5361099

Water Balance

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

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.

Competing Series

Soil series competing with EXCELSIOR 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 EXCELSIOR 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 EXCELSIOR 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.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with EXCELSIOR, 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. CA-2012-05-09-04 | Fresno County, Western Part - 2006

    Typical pattern of soils, landforms, and parent material on the western side of the San Joaquin Valley and the low hills and mountains of the California Coast Ranges (Soil Survey of Fresno County, California, Western Part; 2006).

  2. CA-2012-05-09-05 | Fresno County, Western Part - 2006

    Typical pattern of soils, landforms, and parent material on the hills and mountains of the California Coast Ranges near Coalinga. Geologic formations from Fowkes, 1982 (Soil Survey of Fresno County, California, Western Part; 2006).

Map Units

Map units containing EXCELSIOR 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
Excelsior sandy loam1128771461773hhhxca03119801:24000
Excelsior fine sandy loam, 0 to 1 percent slopes113tw3822182332dg7xca03119801:24000
Excelsior sandy loam, 0 to 2 percent slopes, MLRA 174453004127661192ss8vca65320001:24000
Excelsior sandy loam, sandy substratum, 0 to 2 percent slopes44720216467042hnzwca65320001:24000
Excelsior, sandy substratum-westhaven association, flooded, 0 to 2 percent slopes9609416467126hp2lca65320001:24000
Excelsior loamy sand, sandy substratum, 0 to 1 percent slopes, eroded4481010467043hnzxca65320001:24000
Excelsior sandy loam112ki2814870701lxf0ca65419661:24000
Excelsior fine sandy loam, 0 to 1 percent slopes1132030467185hp4hca65919991:24000
Excelsior sandy loam, 0 to 2 percent slopes, MLRA 17152620527661172ss8vca66619831:24000
Excelsior variant silt loam1531235463698hkj0ca66619831:24000
Excelsior sandy loam, 0 to 2 percent slopes, MLRA 171502049827661182ss8vca69120081:24000
Excelsior fine sandy loam, saline-sodic, 0 to 1 percent slopes1518618466456hnczca69120081:24000
Excelsior loam, 0 to 2 percent slopes1528345466457hnd0ca69120081:24000

Map of Series Extent

Approximate geographic distribution of the EXCELSIOR 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 .