Official Series Description


Lab Data Summary

Aggregate lab data for the FRIANT soil series. This aggregation is based on all pedons with a current taxon name of FRIANT, 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 FRIANT 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
5UCD715300371-CA-53-003xFRIANT3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6027107,-122.9056549

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the FRIANT 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 FRIANT 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 FRIANT 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 FRIANT 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 FRIANT 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 FRIANT 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 FRIANT 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 terrace figure.

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

Soil series sharing subgroup-level classification with FRIANT, 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 FRIANT 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
Friant rocky fine sandy loam, 30 to 70 percent slopesFxG29704456821hbc5ca63819671:24000
Friant rocky fine sandy loam, 9 to 30 percent slopesFxE8871456820hbc4ca63819671:24000
Friant fine sandy loam, 30 to 50 percent slopesFwF2642456819hbc3ca63819671:24000
Friant fine sandy loam, 30 to 45 percent slopesFyE1100464311hl4sca65419661:24000
Friant fine sandy loam, 9 to 30 percent slopesFyD539464310hl4rca65419661:24000
Friant-Rock outcrop complex, 15 to 75 percent slopes13036750463595hkdpca66019771:24000
Tollhouse-Sesame-Friant association, 30 to 60 percent slopes2825947467374hpblca66820071:24000
Friant-Rock outcrop complex, 15 to 75 percent slopes430324581328mhxjca66820071:24000
Arujo-Friant-Tunis complex, 50 to 75 percent slopes1087737463812hkmpca67019771:24000
Arujo-Friant-Tunis complex, 15 to 50 percent slopes1074766463811hkmnca67019771:24000
Friant sandy loam, 50 to 75 percent slopes1362687463840hknlca67019771:24000
Arujo-Friant-Tunis, 9 to 15 percent slopes106307463810hkmmca67019771:24000
Friant fine sandy loam, 50 to 75 percent slopes115680456017h9j7ca67619751:24000
Rock outcrop-Friant complex, 50 to 75 percent slopes125410456027h9jkca67619751:24000
Friant-Rock outcrop complexFr2270457957hcjtca67719721:24000
Cieneba-Friant sandy loams complexCp1060457951hcjmca67719721:24000
Friant fine sandy loam, 30 to 75 percent slopes15349740458054hcmyca67819741:24000
Friant rocky fine sandy loam, 25 to 50 percent slopes, erodedFyF230532458242hcv0ca67919671:15840
Friant rocky fine sandy loam, 8 to 25 percent slopes, e rodedFyE25708458241hctzca67919671:15840
Friant fine sandy loam, 5 to 25 percent slopes, erodedFwE22701458240hctyca67919671:15840
Friant fine sandy loam, 30 to 75 percent slopes153821729097sgp8ca67919671:15840
Friant-Geghus-Lithic Xerorthents complex, 30 to 60 percent slopes, thermic7202013628254p2r8ca69120081:24000

Map of Series Extent

Approximate geographic distribution of the FRIANT 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 .