Official Series Description


Lab Data Summary

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

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
200P0855S2000OR003004Philomath6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.5997238,-123.2861099
201N0511S2000OR039001Philomath6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.9742584,-122.8208847
201N0512S2000OR039002Philomath6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0798111,-122.9428329
201N0514S2001OR043001Philomath6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.5195312,-122.797287

Water Balance

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

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Sibling Summary

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

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

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Geomorphic description summaries for the PHILOMATH 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 .

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

Competing Series

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

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Select annual climate data summaries for the PHILOMATH 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 PHILOMATH 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 PHILOMATH, 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 PHILOMATH 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
Philomath silty clay loam, 3 to 12 percent slopes131399852452vpvor00320041:24000
Philomath silty clay, 12 to 45 percent slopes57E1096239122xmor05319771:20000
Philomath silty clay, 3 to 12 percent slopes56C686239022xlor05319771:20000
Dixonville-Philomath-Hazelair complex, 12 to 35 percent slopes43E1994762680236yor63719811:20000
Dixonville-Philomath-Hazelair complex, 3 to 12 percent slopes43C1033662679236xor63719811:20000
Philomath cobbly silty clay, 12 to 45 percent slopes108F678662576233lor63719811:20000
Philomath silty clay, 3 to 12 percent slopes107C231262574233jor63719811:20000
Philomath cobbly silty clay, 3 to 12 percent slopes108C208962575233kor63719811:20000
Philomath-Urban land complex, 12 to 45 percent slopes109F24062577233mor63719811:20000
Philomath cobbly silty clay, 12 to 45 percent slopes79F66006437624znor63919831:20000
Dixonville-Philomath-Hazelair complex, 12 to 35 percent slopes35E52156430124x7or63919831:20000
Dixonville-Philomath-Hazelair complex, 3 to 12 percent slopes35C39356430024x6or63919831:20000
Philomath cobbly silty clay, 3 to 12 percent slopes79C29406437524zmor63919831:20000
Philomath silty clay, 3 to 12 percent slopes78C12056437424zlor63919831:20000
Philomath-Dixonville complex, 30 to 70 percent slopes189F2488466514276mor64919941:24000
Philomath-Edenbower complex, 30 to 60 percent slopes190F1418666520276tor64919941:24000
Philomath-Dixonville complex, 3 to 30 percent slopes189E1102566513276lor64919941:24000
Philomath-Edenbower complex, 12 to 30 percent slopes190E212066519276sor64919941:24000

Map of Series Extent

Approximate geographic distribution of the PHILOMATH 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 .