Official Series Description


Lab Data Summary

Aggregate lab data for the PAYRAISE soil series. This aggregation is based on all pedons with a current taxon name of PAYRAISE, 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 PAYRAISE 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.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
43C93P0355S1992OR063006Payraise6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.2963905,-118.2455521

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the PAYRAISE 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 PAYRAISE 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 PAYRAISE 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 PAYRAISE 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 PAYRAISE 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 PAYRAISE 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 PAYRAISE 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 PAYRAISE, 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 PAYRAISE 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
Pinuscreek-Payraise-Dunstan complex, landslide, 15 to 30 percent slopes1356BL138231203941qzfhor60720181:24000
Pinuscreek-Payraise-Dunstan complex, landslide, 30 to 60 percent slopes1356CL93431207781v6b0or60720181:24000
Payraise-Slaughterhouse-Dunstan complex, landslide, 0 to 30 percent slopes1351NL48631207001sh59or60720181:24000
Pinuscreek-Payraise-Dunstan complex, landslide, 0 to 15 percent slopes1356AL29931203931qzfgor60720181:24000
Payraise-Lemoncreek complex, 30 to 60 percent slopes7312CO7331203261qy1vor60720181:24000
Hondu-Payraise complex, 30 to 60 percent north slopes7719CN6031206331sgdgor60720181:24000
Payraise-Lemoncreek complex, 30 to 60 percent slopes7312CO311931221621qy1vor62620181:24000
Kettlecreek-Payraise-Vogel complex, 30 to 60 percent slopes7753CO108631224251sgfhor62620181:24000
Uptmor-Payraise-Kingbolt complex, 30 to 60 percent slopes7344CO10631221181q70wor62620181:24000
Payraise-Lemoncreek complex, mass failure, 30 to 60 percent slopes7312CM3431223821sg99or62620181:24000
Payraise-Slaughterhouse complex, 15 to 30 percent north slopes7721BN2533854521sgdjor62620181:24000
Payraise-Slaughterhouse complex, 30 to 60 percent north slopes7721CN2533854531sgdkor62620181:24000
Payraise-Cotay complex, 30 to 60 percent slopes7340CO1131223961sg9vor62620181:24000
Hondu-Payraise complex, 30 to 60 percent north slopes7719CN233854511sgdgor62620181:24000
Pinuscreek-Payraise-Dunstan complex, 0 to 15 percent slopes, landslide1356AL118634295192kty6or6271:24000
Pinuscreek-Payraise-Dunstan complex, 15 to 30 percent slopes, landslide1356BL36834298012kty8or6271:24000
Payraise-Slaughterhouse complex, 15 to 30 percent north slopes7721BN17034319041sgdjor6271:24000
Payraise-Lemoncreek complex, 30 to 60 percent slopes7312CO11134319001qy1vor6271:24000
Payraise-Slaughterhouse complex, 30 to 60 percent north slopes7721CN510624868881sgdkor63120181:24000
Hondu-Payraise complex, 30 to 60 percent north slopes7719CN285424868851sgdgor63120181:24000
Payraise-Hondu complex, 60 to 90 percent north slopes7720DN118724868861sgdhor63120181:24000
Payraise-Lemoncreek complex, 30 to 60 percent slopes7312CO37824957361qy1vor63120181:24000
Payraise-Slaughterhouse complex, 15 to 30 percent north slopes7721BN36524868871sgdjor63120181:24000
Payraise-Cotay complex, 30 to 60 percent slopes7340CO8124868741sg9vor63120181:24000
Uptmor-Payraise-Kingbolt complex, 30 to 60 percent slopes7344CO1824868761q70wor63120181:24000
Payraise-Lemoncreek complex, mass failure, 30 to 60 percent slopes7312CM824868691sg99or63120181:24000
Payraise-Slaughterhouse complex, 30 to 60 percent north slopes90345927222912sf3tor6451:24000

Map of Series Extent

Approximate geographic distribution of the PAYRAISE 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 .