Official Series Description


Lab Data Summary

Aggregate lab data for the FELTON soil series. This aggregation is based on all pedons with a current taxon name of FELTON, 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 FELTON 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
2040A3038S1961CA073001Felton5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.0177765,-116.6380539

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the FELTON 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 FELTON 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 FELTON 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 FELTON 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 FELTON 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 FELTON 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 FELTON 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 flats position figure.

Soil series sharing subgroup-level classification with FELTON, 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 FELTON 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
Felton loam, 50 to 75 percent slopesFaG845455793h990ca01319731:24000
Felton variant-Soulajule complex, 30 to 50 percent slopes1252410459417hf1xca04119791:24000
Felton variant-Soulajule complex, 50 to 75 percent slopes1261115459418hf1yca04119791:24000
Felton variant-Soulajule complex, 15 to 30 percent slopes1241010459416hf1wca04119791:24000
Felton variant-Soulajule complex, 9 to 15 percent slopes123790459415hf1vca04119791:24000
Felton gravelly loam, 30 to 50 percent slopes1365340458960hdl5ca05519741:24000
Lodo-Maymen-Felton association, 30 to 75 percent slopes1574815458981hdlvca05519741:24000
Felton gravelly loam, 50 to 75 percent slopes1372510458961hdl6ca05519741:24000
Felton gravelly loam, 15 to 30 percent slopes135455458959hdl4ca05519741:24000
Ben Lomond-Felton complex, 50 to 75 percent slopes11520079455891h9d5ca08719761:24000
Lompico-Felton complex, 50 to 75 percent slopes, MLRA 4B144159974559202tb7rca08719761:24000
Lompico-Felton complex, 30 to 50 percent slopes, MLRA 4B143142454559192tb7tca08719761:24000
Lompico-Felton complex, 5 to 30 percent slopes1429807455918h9f1ca08719761:24000
Ben Lomond-Felton complex, 30 to 50 percent slopes1144753455890h9d4ca08719761:24000
Felton sandy loam, 5 to 9 percent slopes1381007455914h9dxca08719761:24000
Ben Lomond-Felton complex, 30 to 75 percent slopes519scl3524838322pcmmca08719761:24000
Felton silt loam, 50 to 75 percent slopesFaGes6700551rhzfca08719761:24000
Felton loam, 50 to 75 percent slopesFaGcc801710vx7mca60919631:20000
Felton fine sandy loam, 30 to 50 percent slopes525scl1224838242pcmcca63719581:15000
Felton fine sandy loam, 30 to 50 percent slopes52518416744211t6clca64120091:24000
Ben Lomond-Felton complex, 30 to 75 percent slopes5197723908622l7wlca64120091:24000
Lompico-Felton complex, 5 to 30 percent slopes142sc2224838392pcmvca64120091:24000
Lompico-Felton complex, 30 to 50 percent slopes, MLRA 4B143sc824838402tb7tca64120091:24000
Felton silt loam, 50 to 75 percent slopesFaG2946456989hbjlca64619671:24000
Felton silt loam, 30 to 50 percent slopesFaF259456988hbjkca64619671:24000
Lompico-Felton complex, 30 to 50 percent slopes, MLRA 4B143sc1566996932tb7tca64619671:24000
Felton silt loam, 15 to 30 percent slopesFaE96456987hbjjca64619671:24000
Lompico-Felton complex, 50 to 75 percent slopes, MLRA 4B144sc56996942tb7rca64619671:24000
Green Bluff-Waterman-Felton families complex, 30 to 70 percent slopes.1849319471193ht9sca71319841:24000
Felton-Waterman families-Rock outcrop complex, 2 to 60 percent slopes.1561058471165ht8wca71319841:24000

Map of Series Extent

Approximate geographic distribution of the FELTON 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 .