Official Series Description


Lab Data Summary

Aggregate lab data for the PHILLIPS soil series. This aggregation is based on all pedons with a current taxon name of PHILLIPS, 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 PHILLIPS 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
5288P045388MT051005Phillips5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.1650009,-110.9338913
5288P077188MT051011Phillips7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.4515762,-111.005043
5288P077988MT051019Phillips7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.3935204,-111.0681
5288P078188MT051021Phillips7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.317688,-111.0119858
5288P078288MT051022Phillips6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.3824081,-111.1486588
5289P014489MT101001Phillips7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.7419434,-111.6936111
5290P109190MT071009Phillips7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.8675003,-107.8997192
5290P109290MT071010Phillips7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.8675003,-107.8997192
5240A3338S1962MT005007Phillips7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.8271484,-109.1980438
5240A3652S1967MT071001Phillips2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.5333328,-107.5
5240A3653S1967MT105002PHILLIPS2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.3333321,-106.1666641

Water Balance

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

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with PHILLIPS, 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 PHILLIPS 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
Phillips-Elloam complex, 0 to 4 percent slopes331B1638613439072sy7ymt04119941:24000
Phillips-Kevin complex, 0 to 4 percent slopes334B543883439102sy83mt04119941:24000
Phillips loam, 0 to 4 percent slopes33A99283439122sy7zmt04119941:24000
Phillips-Elloam complex, 0 to 4 percent slopes331B414143441832sy7ymt05119921:24000
Phillips-Kevin complex, 0 to 4 percent slopes332B640543451322sy83mt10119921:24000
Phillips-Elloam complex, 0 to 4 percent slopes331B157043451302sy7ymt10119921:24000
Phillips loam, 0 to 4 percent slopes33B42233451332sy7zmt10119921:24000
Phillips-Kevin complex, 2 to 8 percent slopes492892063455662vyr1mt10519761:24000
Phillips-Elloam complex, 2 to 8 percent slopes471836673455642vyr0mt10519761:24000
Phillips loam, 0 to 4 percent slopes461008103455632sy7zmt10519761:24000
Thoeny-Phillips complex, 1 to 5 percent slopes6997338345588clm0mt10519761:24000
Phillips-Telstad loams, 2 to 9 percent slopes5039350345568cllcmt10519761:24000
Phillips-Nobe-Absher complex, 1 to 5 percent slopes4820926345565cll8mt10519761:24000
Phillips-Thoeny loams, 0 to 2 percent slopes516955345569clldmt10519761:24000
Phillips-Elloam complex, 0 to 4 percent slopes972977563465762sy7ymt60819761:24000
Phillips-Kevin complex, 2 to 8 percent slopes100400343462422vyr1mt60819761:24000
Phillips-Elloam complex, 2 to 8 percent slopes98316953465792vyr0mt60819761:24000
Phillips-Kevin complex, 0 to 4 percent slopes99260343465832sy83mt60819761:24000
Phillips loam, 0 to 4 percent slopes95136533465732sy7zmt60819761:24000
Chinook-Phillips complex, 2 to 6 percent slopes331552346425cmh0mt60819761:24000
Phillips-Elloam complex, 0 to 4 percent slopes331B499553466942sy7ymt61519921:24000
Phillips loam, 0 to 4 percent slopes33A131893466972sy7zmt61519921:24000
Phillips-Elloam complex, 2 to 8 percent slopes331C75953466952vyr0mt61519921:24000
Phillips-Kevin complex, 0 to 4 percent slopes334B48263466962sy83mt61519921:24000
Kevin-Scobey-Phillips association, 2 to 15 percent slopes1441D132313347603cnq0mt64119941:24000
Phillips-Absher complex, 0 to 4 percent slopes331B89437347674cns9mt64119941:24000
Phillips-Elloam complex, 0 to 4 percent slopes332B871573476772sy7ymt64119941:24000
Scobey-Phillips complex, 0 to 4 percent slopes561B86567347750cnvrmt64119941:24000
Elloam-Phillips-Absher association, 0 to 8 percent slopes1523C74371347608cnq5mt64119941:24000
Phillips-Elloam complex, 2 to 8 percent slopes1332C552813475922vyr0mt64119941:24000
Phillips-Kevin complex, 2 to 8 percent slopes334C322703476792vyr1mt64119941:24000
Phillips-Absher complex, 4 to 8 percent slopes331C13735347675cnsbmt64119941:24000
Kevin-Phillips-Elloam association, 2 to 15 percent slopes1333C12719347593cnppmt64119941:24000
Phillips loam, 0 to 4 percent slopes33B20373476802sy7zmt64119941:24000
Phillips-Elloam complex, 2 to 8 percent slopes44168803482492vyr0mt66119821:24000

Map of Series Extent

Approximate geographic distribution of the PHILLIPS 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 .