Official Series Description


Lab Data Summary

Aggregate lab data for the SOPER soil series. This aggregation is based on all pedons with a current taxon name of SOPER, 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 SOPER 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
15UCD541701454-CA-17-014xSOPER4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.0315819,-122.565094
1874C0011S1974CA029011SOPER6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.1847229,-118.4347229

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SOPER 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 SOPER 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 SOPER 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 SOPER 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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Competing Series

Soil series competing with SOPER 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 SOPER 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 SOPER 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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Soil series sharing subgroup-level classification with SOPER, 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 SOPER 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
Soper gravelly loam, 15 to 30 percent slopes, erodedSlE22864456290h9t1ca06919651:20000
Soper sandy loam, 15 to 30 percent slopes, erodedSmE22586456293h9t4ca06919651:20000
Soper gravelly loam, 30 to 50 percent slopes, eroded, cool MAAT, MLRA 15SlF220114562912wv8bca06919651:20000
Soper gravelly loam, 9 to 15 percent slopesSlD1331456289h9t0ca06919651:20000
Soper sandy loam, 30 to 50 percent slopes, erodedSmF2888456294h9t5ca06919651:20000
Soper sandy loam, 9 to 15 percent slopesSmD180456292h9t3ca06919651:20000
Soper gravelly loam, 30 to 50 percent slopes, eroded, MLRA 20SvF2146124577792wv8cca67419681:24000
Soper loam, 15 to 30 percent slopes, erodedSsE22321457778hcc1ca67419681:24000
Soper gravelly sandy loam, 15 to 30 percent slopes132870456034h9jsca67619751:24000
Soper gravelly sandy loam, 30 to 50 percent slopes133289456035h9jtca67619751:24000
Anaheim-Soper complex, 20 to 55 percent slopes1164LA29117822w62yca67719721:24000
Soper gravelly loam, 30 to 50 percent slopes, MLRA 20SrF5504579912wv8fca67719721:24000
Soper gravelly loam, 15 to 30 percent slopes, MLRA 20SrE3804579902wv8dca67719721:24000
Soper gravelly loam, 30 to 50 percent slopes, MLRA 2020234454581032wv8fca67819741:24000
Soper-Rock outcrop complex, 30 to 75 percent slopes2041590458105hcplca67819741:24000
Soper loam, 30 to 50 percent slopes2001405458101hcpgca67819741:24000
Soper cobbly loam, 15 to 50 percent slopes2031170458104hcpkca67819741:24000
Soper gravelly loam, 15 to 30 percent slopes, MLRA 2020110454581022wv8dca67819741:24000
Soper loam, 15 to 30 percent slopes199735458100hcpfca67819741:24000
Soper cobbly loam, 25 to 50 percent slopes, erodedSuF2366458372hcz6ca67919671:15840
Soper loam, 15 to 35 percent slopes, erodedStF2229458371hcz5ca67919671:15840
Soper gravelly loam, 30 to 50 percent slopes, MLRA 20SrF827291172wv8fca67919671:15840
Urban land-Dapplegray-Soper complex, 20 to 55 percent slopes1242305728333622tb7vca69620161:24000
Soper-Pachic Haploxerolls-Boades complex, 25 to 75 percent slopes1143248925137212pt47ca69620161:24000
Anaheim-Soper complex, 20 to 55 percent slopes116472629117762w62yca69620161:24000
Soper-Buzzpeak association, 35 to 75 percent slopes114459625137222pt48ca69620161:24000
Soper gravelly sandy loam, 15 to 30 percent slopes132sf32670251h9jsca69620161:24000

Map of Series Extent

Approximate geographic distribution of the SOPER 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 .