Official Series Description


Lab Data Summary

Aggregate lab data for the D36-WESTERN MARITIME TUSSOCK SCRUB LOAMY EOLIAN SLOPES soil series. This aggregation is based on all pedons with a current taxon name of D36-WESTERN MARITIME TUSSOCK SCRUB LOAMY EOLIAN SLOPES, 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 D36-WESTERN MARITIME TUSSOCK SCRUB LOAMY EOLIAN SLOPES 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 D36-WESTERN MARITIME TUSSOCK SCRUB LOAMY EOLIAN SLOPES 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 D36-WESTERN MARITIME TUSSOCK SCRUB LOAMY EOLIAN SLOPES 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 D36-WESTERN MARITIME TUSSOCK SCRUB LOAMY EOLIAN SLOPES 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 D36-WESTERN MARITIME TUSSOCK SCRUB LOAMY EOLIAN SLOPES 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 D36-WESTERN MARITIME TUSSOCK SCRUB LOAMY EOLIAN SLOPES 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 D36-WESTERN MARITIME TUSSOCK SCRUB LOAMY EOLIAN SLOPES 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 D36-WESTERN MARITIME TUSSOCK SCRUB LOAMY EOLIAN SLOPES 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 D36-WESTERN MARITIME TUSSOCK SCRUB LOAMY EOLIAN SLOPES, 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 D36-WESTERN MARITIME TUSSOCK SCRUB LOAMY EOLIAN SLOPES 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
Western Maritime Eolian Plains with Common Permafrost, Very WetD36PNE58309226614972rpx0ak63620151:63360
Western Maritime Glaciated Plains and Flood Plains, WetD36PNS25932726615112rpx9ak63620151:63360
Western Maritime Eolian Plains and Flood Plains with Common Permafrost, WetD36PNZ22130626615182rpx1ak63620151:63360
Western Maritime Organic and Glaciated PlainsD36PNH19373726615002rpwwak63620151:63360
Western Maritime Eolian Plains, Very WetD36PNB18955926615242rpwxak63620151:63360
Western Maritime Eolian Hills and Plains, CoolD36HIE11463426614902pz3sak63620151:63360
Western Maritime Eolian Hills and Plains with Common PermafrostD36HIC9639526614892pz3pak63620151:63360
Western Maritime Eolian Plains, WetD36PND8086226614962rpx4ak63620151:63360
Western Maritime Glaciated Plains, RollingD36PNI6320826615012rpx7ak63620151:63360
Western Maritime Eolian Plains with Common Permafrost, WetD36PNC5712126614952rpx2ak63620151:63360
Western Maritime Plains, WetD36PNY5426726615172rpxdak63620151:63360
Western Maritime Glaciated and Eolian Plains, WetD36PNL4954426615042rpx5ak63620151:63360
Western Maritime Eolian PlainsD36PNU4369026615132rpwzak63620151:63360
Western Maritime Plains with Common PermafrostD36PNK3308026615032rpx8ak63620151:63360

Map of Series Extent

Approximate geographic distribution of the D36-WESTERN MARITIME TUSSOCK SCRUB LOAMY EOLIAN SLOPES 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 .