Official Series Description


Lab Data Summary

Aggregate lab data for the SANPETE soil series. This aggregation is based on all pedons with a current taxon name of SANPETE, 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 SANPETE 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
28A40A377075UT041007Sanpete8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.0316277,-111.9207764
28A85P094685UT045004Sanpete7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.2625008,-112.234726

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SANPETE 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 SANPETE 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 SANPETE 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 SANPETE 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 SANPETE 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 SANPETE series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the SANPETE 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.

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

Soil series sharing subgroup-level classification with SANPETE, 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 SANPETE 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
Sanpete-Theriot families complex, 5 to 60 percent slopes.15927609471575htq3ca76319841:24000
Sanpete-Theriot families-Rock outcrop, limestone association, 60 to 80 percent slopes.1609697471576htq4ca76319841:24000
Sanpete gravelly silt loam, high rainfall, 10 to 30 percent slopesSlE16583481485j50sut60219691:20000
Sanpete gravelly silt loam, high rainfall, 6 to 10 percent slopesSlD14380481484j50rut60219691:20000
Sanpete gravelly silt loam, high rainfall, 1 to 6 percent slopesSlB10725481483j50qut60219691:20000
Sanpete gravelly silt loam, high rainfall, 30 to 50 percent slopesSlG3089481486j50tut60219691:20000
Sanpete gravelly silt loam, 6 to 30 percent slopesSkE1928481482j50put60219691:20000
Sanpete gravelly fine sandy loam, 4 to 15 percent slopesScD6491482607j65zut60819811:24000
Sanpete gravelly fine sandy loam, 15 to 40 percent slopesScF2852482608j660ut60819811:24000
Dera-Sanpete families association, 1 to 10 percent slopes1810909431838412whrbut6171:24000
Sanpete-Dera-Spager families association, 2 to 15 percent slopes199364931838422whrcut6171:24000
Sanpete-Amtoft families associtation, 2 to 25 percent slopes706092231838982x4gwut6171:24000
Sanpete-Spager families association, 2 to 15 percent slopes725489131839002x4gyut6171:24000
Sanpete-Hiko Springs-Penoyer families association, 0 to 15 percent slopes715021631838992x4gxut6171:24000
Biddleman-Sanpete-Broncho families association, 2 to 15 percent slopes62689531838862x4ghut6171:24000
Sanpete-Amtoft association, 15 to 60 percent slopesSRG286524540142nclrut61819951:24000
Denmark-Sanpete complex, 2 to 10 percent slopesMMD62024540192nclxut61819951:24000
Sanpete stony fine sandy loam, 5 to 30 percent slopes, erodedSCE222055482334j5x5ut62719711:24000
Sanpete very cobbly sandy loam, 8 to 30 percent slopesSNF2907024539642nck4ut62719711:24000
Sanpete cobbly fine sandy loam, 5 to 10 percent slopes, erodedSbD25300482333j5x4ut62719711:24000
Sanpete gravelly fine sandy loam, 2 to 5 percent slopesSaC3870482332j5x3ut62719711:24000
Lisade-Sanpete complex, 2 to 5 percent slopes, erodedLFC23325482281j5vgut62719711:24000
Sanpete-Amtoft association, 15 to 60 percent slopesSRG286524539632nck3ut62719711:24000
Sanpete-Lisade association, 2 to 15 percent slopesSMD231324539902nckzut62719711:24000
Sanpete very cobbly sandy loam, 8 to 30 percent slopes1987737483599j76zut6281:24000
Sanpete-Lisade association, 2 to 15 percent slopes2007295483598j76yut6281:24000
Sanpete-Amtoft, moist association, 15 to 60 percent slopes1994213483603j773ut6281:24000
Sanpete-Lisade complex, 2 to 5 percent slopes2012449483607j777ut6281:24000
Sanpete very cobbly sandy loam, 4 to 15 percent slopes, rubbly1972420483605j775ut6281:24000
Hiko Peak-Pibler-Sanpete association, 2 to 30 percent slopes1431410483606j776ut6281:24000
Denmark-Sanpete complex, 2 to 10 percent slopes1221218483553j75hut6281:24000
Sanpete cobbly fine sandy loam, 5 to 10 percent slopes, eroded1953724539492ncjnut6281:24000
Sanpete stony fine sandy loam, 5 to 30 percent slopes, eroded1961724539892nckyut6281:24000
Sanpete, extremely stony-Pibler, very stony complex, 4 to 35 percent slopesUp9145428102662trdsut6291:24000
Sanpete extremely cobbly loam, 8 to 25 percent slopes4716075484012j7n9ut63419971:24000

Map of Series Extent

Approximate geographic distribution of the SANPETE 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 .