Official Series Description


Lab Data Summary

Aggregate lab data for the DAY soil series. This aggregation is based on all pedons with a current taxon name of DAY, 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 DAY 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
1098P0221S1997OR023011DAY6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.6105537,-119.6333313
1099P0246S1998OR069011DAY7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.6500015,-120.2836075
n/a74C0166S1974OR065003Day8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the DAY 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 DAY 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 DAY 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 DAY 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 DAY 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 DAY series and competing. 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 DAY 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 .

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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 DAY, 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 DAY 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
Karcal-Day-Rock outcrop complex, 2 to 15 percent slopes87883425196142r20id68520121:24000
Chilcott-Day-Rock outcrop complex, 2 to 15 percent slopes26368625195472qzvid68520121:24000
Day-Simas complex, 1 to 12 percent slopes047280834350232mqhor6181:24000
Twickenham-Day-Badland complex, 30 to 60 percent south slopes123E168342516726hkor6271:24000
Simas-Day complex, 15 to 40 percent north slopes358D673425037269lor6271:24000
Twickenham-Day-Badland complex, 15 to 30 percent south slopes123D41342506526hlor6271:24000
Day clay, 8 to 40 percent slopesDaE48506288823fnor66619701:31680
Day complex, 8 to 40 percent slopes2131926318423r6or67419931:24000
Day clay, 0 to 12 percent slopes2010876317723qzor67419931:24000
Day-Antoken complex, 30 to 55 percent slopes227856319323rhor67419931:24000
Simas-Day complex, 3 to 15 percent slopes358C25303421814269mor6771:24000
Simas-Day complex, 15 to 40 percent north slopes358D19463421862269lor6771:24000
Simas-Day complex, 15 to 40 percent south slopes359D14953421915269sor6771:24000
Twickenham-Day-Badland complex, 15 to 30 percent south slopes123D867342199826hlor6771:24000
Day-Sorf complex, 3 to 20 percent slopes241E549342450126cwor6771:24000
Badland-Day complex, 2 to 45 percent slopes352E43434245622696or6771:24000
Day-Drewsey complex, 1 to 5 percent slopes343B16434247262691or6771:24000
Day-Simas complex, 0 to 3 percent slopes357A1473424749269nor6771:24000
Twickenham-Day-Badland complex, 30 to 60 percent south slopes123E66342479126hkor6771:24000

Map of Series Extent

Approximate geographic distribution of the DAY 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 .