Official Series Description


Lab Data Summary

Aggregate lab data for the E22-MARITIME GLACIERS AND PERMANENT SNOWFIELDS soil series. This aggregation is based on all pedons with a current taxon name of E22-MARITIME GLACIERS AND PERMANENT SNOWFIELDS, 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 E22-MARITIME GLACIERS AND PERMANENT SNOWFIELDS 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 E22-MARITIME GLACIERS AND PERMANENT SNOWFIELDS 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.

There are insufficient data to create the water balance bar figure.



There are insufficient data to create the water balance line figure.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the E22-MARITIME GLACIERS AND PERMANENT SNOWFIELDS series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

There are insufficient data to create the sibling sketch figure.

Select annual climate data summaries for the E22-MARITIME GLACIERS AND PERMANENT SNOWFIELDS series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the E22-MARITIME GLACIERS AND PERMANENT SNOWFIELDS 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 .

There are insufficient data to create the 2D hillslope position figure.

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

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.

Competing Series

Soil series competing with E22-MARITIME GLACIERS AND PERMANENT SNOWFIELDS share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

There are insufficient data to create the competing sketch figure.

Select annual climate data summaries for the E22-MARITIME GLACIERS AND PERMANENT SNOWFIELDS series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the E22-MARITIME GLACIERS AND PERMANENT SNOWFIELDS 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 .

There are insufficient data to create the 2D hillslope position figure.

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

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 E22-MARITIME GLACIERS AND PERMANENT SNOWFIELDS, 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 .

This figure is not available.

Block Diagrams

No block diagrams are available.

Map Units

Map units containing E22-MARITIME GLACIERS AND PERMANENT SNOWFIELDS 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
Southern Alaska Coastal Mountains-Maritime Alpine-Barren MountainsE22M563933423299314kcak6231:63360
Southern Alaska Coastal Mountains-Maritime Alpine-Barren MountainsE22M51214443441857314kcak64419941:31680
Southern Alaska Coastal Mountains-Maritime Alpine-Barren MountainsE22M55512963441845314kcak64619921:31680
Southern Alaska Coastal Mountains-Maritime Alpine-Barren MountainsE22M52989113354704314kcak65920241:63360
Southern Alaska Coastal Mountains-Maritime Alpine-Barren MountainsE22M5623433423242314kcak69320191:63360
Southern Alaska Coastal Mountains-Maritime Alpine-Barren MountainsE22M5129583375340314kcak7061:250000
Southern Alaska Coastal Mountains-Maritime Alpine-Barren MountainsE22M512399493354725314kcak7071:250000
Southern Alaska Coastal Mountains-Maritime Alpine-Barren MountainsE22M57408263354912314kcak7081:250000
Southern Alaska Coastal Mountains-Maritime Alpine-Barren MountainsE22M57793503375356314kcak7091:250000
Southern Alaska Coastal Mountains-Maritime Alpine-Barren MountainsE22M5150993354834314kcak7701:250000
Southern Alaska Coastal Mountains-Maritime Alpine-Barren MountainsE22M51619543439033314kcak7721:250000
Southern Alaska Coastal Mountains-Maritime Alpine-Barren MountainsE22M52550873439083314kcak7731:250000
Southern Alaska Coastal Mountains-Maritime Alpine-Barren MountainsE22M5648233439055314kcak7741:250000
Southern Alaska Coastal Mountains-Maritime Alpine-Barren MountainsE22M521300513354870314kcak7751:250000
Southern Alaska Coastal Mountains-Maritime Alpine-Barren MountainsE22M576753439092314kcak7761:250000
Southern Alaska Coastal Mountains-Maritime Alpine-Barren MountainsE22M51065763439096314kcak7771:250000
Southern Alaska Coastal Mountains-Maritime Alpine-Barren MountainsE22M5690473439100314kcak7901:250000
Southern Alaska Coastal Mountains-Maritime Alpine-Barren MountainsE22M5192903439061314kcak7941:250000

Map of Series Extent

Approximate geographic distribution of the E22-MARITIME GLACIERS AND PERMANENT SNOWFIELDS 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 .