Official Series Description


Lab Data Summary

Aggregate lab data for the LITTLEJOE soil series. This aggregation is based on all pedons with a current taxon name of LITTLEJOE, 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 LITTLEJOE 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
13699P044799VA141010LITTLEJOE6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.7641678,-80.0888901

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the LITTLEJOE 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 LITTLEJOE 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 LITTLEJOE 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 LITTLEJOE 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 LITTLEJOE 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 LITTLEJOE 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 LITTLEJOE 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 .

Click the image to view it full size.

Click the image to view it full size.

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.

Soil series sharing subgroup-level classification with LITTLEJOE, 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 LITTLEJOE 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
Littlejoe silt loam, 2 to 7 percent slopes80B37305164732v7k2va00319811:15840
Littlejoe silt loam, 7 to 15 percent slopes80C11005164742v7k3va00319811:15840
Bugley-Littlejoe complex, 25 to 60 percent slopes2E96681366734l6tva00920041:24000
Littlejoe silt loam, 7 to 15 percent slopes21C41151367304l8nva00920041:24000
Bugley-Littlejoe complex, 15 to 25 percent slopes2D22621366724l6sva00920041:24000
Littlejoe silt loam, 15 to 25 percent slopes21D8921367314l8pva00920041:24000
Littlejoe silt loam, 2 to 7 percent slopes21B7331367294l8mva00920041:24000
Bugley-Littlejoe complex, 7 to 15 percent slopes2C7161366744l6vva00920041:24000
Littlejoe gravelly loam, 7 to 15 percent slopes30C63751359702xx6yva01919851:24000
Littlejoe gravelly loam, 15 to 25 percent slopes30D31621359712xx6zva01919851:24000
Littlejoe gravelly loam, 2 to 7 percent slopes30B8241359692xx6xva01919851:24000
Littlejoe silt loam, 2 to 7 percent slopes23B2927024794162p715va02920101:24000
Littlejoe silt loam, 7 to 15 percent slopes23C2043824794172p716va02920101:24000
Littlejoe-Bentley complex, 7 to 15 percent slopes25C344424794202p719va02920101:24000
Littlejoe-Appomattox complex, 7 to 15 percent slopes24C189524794182p717va02920101:24000
Appomattox-Littlejoe complex, 7 to 15 percent slopes2C120424793392p6ypva02920101:24000
Appomattox-Littlejoe complex, 15 to 25 percent slopes2D63124793412p6yrva02920101:24000
Appomattox-Littlejoe complex, 2 to 7 percent slopes2B30524793372p6ymva02920101:24000
Littlejoe-Strawfield-Penhook complex, 8 to 15 percent slopes26C4623582008mjmgva06720041:24000
Littlejoe-Strawfield-Penhook complex, 15 to 25 percent slopes26D2528582009mjmhva06720041:24000
Littlejoe-Penhook-Goblintown complex, 8 to 15 percent slopes25C189582002mjm8va06720041:24000
Littlejoe-Penhook-Goblintown complex, 15 to 25 percent slopes25D150582004mjmbva06720041:24000
Littlejoe silt loam, 7 to 15 percent slopes12C1139122305438bva08919951:24000
Littlejoe silt loam, 15 to 25 percent slopes12D812122307438dva08919951:24000
Littlejoe silt loam, 7 to 15 percent slopes31C39661370344llgva12519921:24000
Littlejoe silt loam, 2 to 7 percent slopes31B17131370334llfva12519921:24000
Littlejoe silt loam, 2 to 7 percent slopes, moderately erodedTsB2141031199242zhgqva13719661:15840
Littlejoe silt loam, 7 to 15 percent slopes, moderately erodedTsC248621199262zhgsva13719661:15840
Littlejoe loam, 2 to 7 percent slopes, moderately erodedTaB229531199212zhgmva13719661:15840
Littlejoe silt loam, 2 to 7 percent slopesTsB28461199232zhgpva13719661:15840
Littlejoe loam, 7 to 15 percent slopes, moderately erodedTaC217921199222zhgnva13719661:15840
Littlejoe silty clay loam, 7 to 15 percent slopes, severely erodedTtC316281199282zhgvva13719661:15840
Littlejoe silty clay loam 2 to 7 percent slopes, severely erodedTtB32581199272zhgtva13719661:15840
Littlejoe silt loam, 7 to 15 percent slopesTsC2311199252zhgrva13719661:15840
Fairystone-Littlejoe complex, 25 to 45 percent slopes, rocky25E22252027585261vzva14120081:24000
Fairystone-Littlejoe complex, 8 to 15 percent slopes23C1448210867528s7sva14120081:24000
Bugley-Littlejoe complex, 45 to 75 percent slopes, very rocky6F431210866628s7hva14120081:24000
Fairystone-Littlejoe complex, 15 to 25 percent slopes, stony24D4052027584261vyva14120081:24000
Littlejoe gravelly loam, 15 to 25 percent slopes37D19791200032yzt8va14319891:24000
Littlejoe gravelly loam, 2 to 7 percent slopes37B13701200012yzt6va14319891:24000
Littlejoe gravelly loam, 7 to 15 percent slopes37C13671200022yzt7va14319891:24000
Littlejoe gravelly loam, 25 to 45 percent slopes37E10611200042yzt9va14319891:24000
Bugley-Littlejoe complex, 7 to 15 percent slopes14C3991199562yzrzva14319891:24000

Map of Series Extent

Approximate geographic distribution of the LITTLEJOE 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 .