Official Series Description


Lab Data Summary

Aggregate lab data for the SPRINGDALE soil series. This aggregation is based on all pedons with a current taxon name of SPRINGDALE, 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 SPRINGDALE 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
4440A1036S1957WA063008Springdale5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.8255539,-117.3563919
4440A1035S1957WA063009Springdale5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.7311096,-117.5002747

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SPRINGDALE 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 SPRINGDALE 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 SPRINGDALE 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 SPRINGDALE 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 SPRINGDALE 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 SPRINGDALE 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 SPRINGDALE 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 SPRINGDALE, 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 SPRINGDALE 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
Waterman-Springdale-Pacifico families complex, 30 to 70 percent slopes62112646465364hm7rca77619811:24000
Lithic Xerorthents, dry-Springdale families, dry-Rubble land association, 50 to 100 percent slopesJrG30779902v5k4ca77619811:24000
Springdale family-Lithic Xerorthents association, dry, 50 to 75 percent slopesFLG31330471645htscca77719811:24000
Lithic Xerorthents-Springdale family-Rubble land association, 50 to 100 percent slopesDhG25981471630htrwca77719811:24000
Springdale-Winthrop families complex, 50 to 75 percent slopesFhG9120471644htsbca77719811:24000
Springdale, dry-Olete families complex, 50 to 75 percent slopesJoG7615471653htsmca77719811:24000
Lithic Xerorthents, dry-Springdale families, dry-Rubble land association, 50 to 100 percent slopesJrG1570471654htsnca77719811:24000
Springdale gravelly ashy coarse sandy loam, 8 to 15 percent slopes31413526628852wg8id60619761:24000
Springdale gravelly sandy loam, 0 to 7 percent slopes7348996867329g8wa04319781:24000
Springdale cobbly ashy sandy loam, 0 to 15 percent slopes741487686742x1zkwa04319781:24000
Stutler-Springdale complex, 3 to 15 percent slopes31133126512802wglwa04319781:24000
Stutler-Springdale complex, 3 to 15 percent slopes311316691859812wglwa06320121:24000
Springdale gravelly ashy coarse sandy loam, 0 to 8 percent slopes314014409859292wdxwa06320121:24000
Urban land-Springdale, disturbed complex, 0 to 3 percent slopes7170354524252522mdnywa06320121:24000
Springdale gravelly ashy coarse sandy loam, 8 to 15 percent slopes31412946859712wg8wa06320121:24000
Urban land-Springdale, disturbed complex, 3 to 8 percent slopes7171165224252512mdnxwa06320121:24000
Urban land-Springdale, disturbed complex, 8 to 15 percent slopes717235924252502mdnwwa06320121:24000
Springdale gravelly ashy sandy loam, 0 to 15 percent slopes226174391581972x1zhwa06519781:24000
Springdale cobbly ashy sandy loam, 0 to 15 percent slopes22731701581982x1zkwa06519781:24000
Springdale sandy loam, 0 to 15 percent slopes225233315819659m3wa06519781:24000
Stutler-Springdale complex, 3 to 15 percent slopes311332126513532wglwa07519751:20000
Springdale stony sandy loam, 0 to 45 percent slopesSmE2259701802c0wwa61919681:24000
Springdale gravelly loam, 0 to 15 percent slopesSlC1978701792c0vwa61919681:24000
Springdale gravelly ashy sandy loam, dry, 0 to 15 percent slopes4491778705992x1zjwa64819871:24000
Springdale gravelly sandy loam, 30 to 65 percent slopes4511471706022cghwa64819871:24000
Springdale gravelly sandy loam, 15 to 30 percent slopes450596706012cggwa64819871:24000
Dart, warm-Springdale complex, 30 to 65 percent slopes111384702252c2bwa64819871:24000
Dart, warm-Springdale complex, 5 to 30 percent slopes110317702242c29wa64819871:24000
Springdale-Rock outcrop complex, 35 to 65 percent slopes342820757972jw2wa74920051:24000
Springdale cobbly ashy coarse sandy loam, 15 to 35 percent slopes341729757962jw1wa74920051:24000

Map of Series Extent

Approximate geographic distribution of the SPRINGDALE 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 .