Official Series Description


Lab Data Summary

Aggregate lab data for the FRUITHURST soil series. This aggregation is based on all pedons with a current taxon name of FRUITHURST, 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 FRUITHURST 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
136S72AL-029-972AL029009-pgmFruithurst2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.6447296142578,-85.4111175537109
136S96AL-123-2S1996AL123002Fruithurst3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.8258333,-85.8466667
136S97AL-123-1S1997AL123001Fruithurst2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.7803778,-85.8481694

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the FRUITHURST 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 FRUITHURST 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 FRUITHURST 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 FRUITHURST 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 mountains figure.

There are insufficient data to create the 3D terrace figure.

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

Competing Series

Soil series competing with FRUITHURST 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 FRUITHURST 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 FRUITHURST 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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Click the image to view it full size.

Click the image to view it full size.

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

Soil series sharing subgroup-level classification with FRUITHURST, 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 FRUITHURST 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
Tallapoosa-Fruithurst complex, 2 to 10 percent slopes, moderately erodedTfC691932601362zs7wal02719711:20000
Tatum-Fruithurst association, hillyTFH9765312281043smal02919741:24000
Tatum-Tallapoosa-Fruithurst association, steepTTS8614412281143snal02919741:24000
Tatum-Fruithurst complex, 6 to 10 percent slopesTfC2490812281243spal02919741:24000
Tallapoosa-Badin-Fruithurst complex, 6 to 15 percent slopes, moderately erodedTaD23569518957392rrtjal03720061:24000
Tallapoosa-Fruithurst complex, 15 to 40 percent slopes, moderately erodedTfE23551018957402xn6wal03720061:24000
Badin-Tallapoosa-Fruithurst complex, 3 to 10 percent slopesBfC9620189571121mmzal03720061:24000
Tallapoosa-Fruithurst complex, 15 to 40 percent slopes, moderately erodedRf381953292892xn6wal05119481:20000
Tallapoosa-Fruithurst complex, 15 to 40 percent slopes, moderately erodedTfE22157014764462xn6wal12320051:24000
Tallapoosa-Badin-Fruithurst complex, 6 to 15 percent slopes, moderately erodedTbD21778814764452rrtjal12320051:24000
Badin-Tallapoosa-Fruithurst complex, 3 to 10 percent slopesBfC578014764471lkcbal12320051:24000
Tallapoosa-Fruithurst complex, 25 to 60 percent slopesTaF367724819042p9mfga01520131:12000
Fruithurst-Tallapoosa complex, 15 to 25 percent slopesFtE2535114875717kcpga01520131:12000
Fruithurst-Braswell complex, 6 to 15 percent slopesFrD169016117261r345ga01520131:12000
Fruithurst-Braswell complex, 15 to 25 percent slopesFrE30116117271r346ga01520131:12000
Tallapoosa-Fruithurst complex, 25 to 60 percent slopesTaF151902511201try5ga22320101:12000
Fruithurst-Braswell complex, 15 to 25 percent slopesFrE1060025112972q0krga22320101:12000
Fruithurst-Braswell complex, 6 to 15 percent slopesFrD1003025112962q0ksga22320101:12000
Fruithurst-Tallapoosa complex, 15 to 25 percent slopesFtE44025112852p7k8ga22320101:12000

Map of Series Extent

Approximate geographic distribution of the FRUITHURST 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 .