Official Series Description


Lab Data Summary

Aggregate lab data for the LAX soil series. This aggregation is based on all pedons with a current taxon name of LAX, 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 LAX 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
12298P03651998TN043001Lax6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.081192,-87.5354462
12207N04662007TN1615SLax7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.5943871,-87.9368896

Water Balance

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

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Competing Series

Soil series competing with LAX 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 LAX 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 LAX 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.

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 LAX, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. TN-2010-11-02-10 | Hickman County - 2008

    Typical pattern of soils and parent material in the Biffle-Lax general soil map unit (Soil Survey of Hickman County, Tennessee; 2008).

  2. TN-2010-11-02-13 | Lewis County - 2006

    Typical pattern of soils and parent material in the Biffle-Lax-Ironcity general soil map unit (Soil Survey of Lewis County, Tennessee; 2006).

  3. TN-2012-03-16-06 | Dickson County - 2002

    The relationship of soils, landscape, and parent material in the Saffell-Lax and the Armour-Humphreys-Sullivan general soil map units (Soil Survey of Dickson County, TN; 2002).

  4. TN-2012-03-19-35 | Wayne County - 2000

    Typical pattern of soils and parent material in the Brandon-Saffell-Lax and Humprheys-Ennis-Lobelville general soil map units (Soil Survey of Wayne County, TN; 2000).

Map Units

Map units containing LAX 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
Purchase-Lax-Brandon complex, 6 to 12 percent slopes, severely erodedPlC33222622325942dy65ky61019681:12000
Brandon-Purchase-Lax complex, 12 to 20 percent slopes, severely erodedBpD32164026234362qyk6ky61019681:12000
Lax-Loring-Feliciana complex, 2 to 12 percent slopes, erodedLlC22096022325952dy66ky61019681:12000
Purchase-Lax-Brandon complex, 6 to 12 percent slopes, erodedPlC2828226234422qykhky61019681:12000
Lax-Purchase-Providence complex, 6 to 12 percent slopes, severely erodedLpC3471922325882dy5zky61019681:12000
Purchase-Lax-Brandon complex, 4 to 6 percent slopes, severely erodedPlB3180726234382qyk7ky61019681:12000
Brandon-Purchase-Lax complex, 12 to 20 percent slopes, erodedBpD26226234352qyk5ky61019681:12000
Lax silt loam, 2 to 6 percent slopesLbB8900549472lfrxky62919791:20000
Lax silt loam, 6 to 12 percent slopesLbC8350549473lfryky62919791:20000
Lax silty clay loam, 6 to 12 percent slopes, severely erodedLcC31670549474lfrzky62919791:20000
Lax silt loam, 2 to 5 percent slopes, erodedLbB21410567687m1qhms02919811:20000
Lax silt loam, 5 to 12 percent slopes, erodedLaC22510125454012qsj0tn00520111:12000
Lax silt loam, 2 to 5 percent slopes, erodedLaB2318325453512qsgctn00520111:12000
Lax silty clay loam, 5 to 12 percent slopes, severely erodedLbC358625453522qsgftn00520111:12000
Lax silt loam, 5 to 12 percent slopesLaC9666527113kphntn04319931:24000
Lax silt loam, 2 to 5 percent slopesLaB3491527112kphmtn04319931:24000
Lax silt loam, 5 to 12 percent slopes, erodedLaC2166625452672qs8ctn07920121:12000
Lax silty clay loam, 5 to 12 percent slopes, severely erodedLbC3115725452682qs8dtn07920121:12000
Lax silt loam, 2 to 5 percent slopes, erodedLaB224325452662qs8btn07920121:12000
Lax silt loam, 5 to 12 percent slopesLaC10396527471kpw6tn08119971:24000
Lax silt loam, 2 to 5 percent slopesLaB812527470kpw5tn08119971:24000
Lax-Ironcity complex, 5 to 12 percent slopesLaC19266530866ktdqtn10119991:24000
Lax silt loam, 2 to 5 percent slopesLbB1401530867ktdrtn10119991:24000
Lax silt loam, 5 to 12 percent slopesLbC713530868ktdstn10119991:24000
Lax silt loam, 1 to 4 percent slopesLaB2049527986kqdttn12519721:15840
Lax silt loam, 4 to 8 percent slopesLaC1359527987kqdvtn12519721:15840
Lax-Ironcity complex, 5 to 12 percent slopesLaC3055560629ltcttn13520001:24000
Lax silt loam, 5 to 12 percent slopesLbC757560628ltcstn13520001:24000
Lax silt loam, 2 to 5 percent slopesLbB147560627ltcrtn13520001:24000
Lax silt loam, 5 to 12 percent slopesLaC956931604481kyz0tn16119531:20000
Lax silt loam, 5 to 12 percent slopes, erodedLb101323969212lg61tn16119531:20000
Lax silt loam, 12 to 20 percent slopesLaD70831604591ttx0tn16119531:20000
Lax silt loam, 2 to 5 percent slopesLc58623969222lg62tn16119531:20000
Lax silty clay loam, 5 to 12 percent slopes, severely erodedLe54123969242lg64tn16119531:20000
Lax-Brandon complex, 5 to 12 percent slopesLbC24131604601ttx5tn16119531:20000
Lax silt loam, 2 to 5 percent slopesLaB8960328019c0b8tn18119961:24000
Lax silt loam, 5 to 12 percent slopesLaC3945328020c0b9tn18119961:24000

Map of Series Extent

Approximate geographic distribution of the LAX 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 .