Official Series Description


Lab Data Summary

Aggregate lab data for the LATONIA soil series. This aggregation is based on all pedons with a current taxon name of LATONIA, 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 LATONIA 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
133B87P040387LA085002Latonia7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.7727776,-93.6055527

Water Balance

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

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

Soil series sharing subgroup-level classification with LATONIA, 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. ID-2011-06-01-22 | Teton Area, Idaho and Wyoming - 1969

    Relative positions of Ririe, Tetonia, and Latonia soils. The profile sketches show the effect of exposure on the formation of these soils (Soil Survey of Teton Area, Idaho and Wyoming; 1969).

  2. MS-2012-04-26-01 | Harrison County - June 1975

    Distribution and pattern of major soils in Eustis-Latonia-Lakeland association (Soil Survey of Harrison County, Mississippi; June 1975).

  3. MS-2012-04-26-03 | Harrison County - June 1975

    Distribution and pattern of major soils in Atmore-Harleston-Plummer association (Soil Survey of Harrison County, Mississippi; June 1975).

Map Units

Map units containing LATONIA 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
Latonia loamy sand, 0 to 2 percent slopes, rarely floodedLaA560328568c0wzal02319981:24000
Latonia loamy sand, 0 to 2 percent slopes, occasionally floodedLaA2300600101n4g3al02520041:24000
Latonia loamy fine sand, 0 to 2 percent slopes, rarely floodedLcA229026420952rjs3al12920131:24000
Latonia loamy fine sand, 2 to 5 percent slopes391354564913lyv0ar67019811:20000
Latonia fine sandy loam, 1 to 5 percent slopesLaC29045190304121w8fla08519911:24000
Latonia fine sandy loam, 0 to 2 percent slopesLt75613270062vy0pla10319851:24000
Latonia fine sandy loam, 0 to 2 percent slopesLt207317241422vy0pla11719891:24000
Latonia loamy sand, 0 to 5 percent slopesLaB2186567686m1qgms02919811:20000
Latonia-Trebloc association, occasionally floodedLT10201332220c4psms03519761:20000
Latonia fine sandy loam, 0 to 2 percent slopesLaA28063322212vy0pms03519761:20000
Latonia loamy fine sand, 0 to 2 percent slopes, rarely floodedLcA181226422002rryyms04120121:24000
Latonia loamy sandLt7924332434c4xpms04719711:20000
Latonia loamy sand, 0 to 2 percent slopes, occasionally flooded81452332602c533ms05919971:24000
Latonia loamy sand, 0 to 2 percent slopes3881221332614c53hms05919971:24000
Latonia fine sandy loam, 0 to 2 percent slopesLt22763328552vy0pms07319691:20000
Cahaba-Latonia association, occasionally floodedCL12231333054c5kpms08719771:20000
Latonia loamy sand, occasionally floodedLb3221333076c5ldms08719771:20000
Latonia loamy sandLa1982333075c5lcms08719771:20000
Latonia-Urban land complexLd490333077c5lfms08719771:20000
Latonia sandy loam, 0 to 2 percent slopesLaA9095333126c5n0ms09119831:20000
Latonia-Cahaba association, occasionally floodedLC1775333421c5yjms10319831:20000
Latonia fine sandy loam, occasionally floodedLa812333424c5ymms10319831:20000
Latonia fine sandy loam, 0 to 2 percent slopesLaA42713335412vy0pms10919801:20000
Cahaba, Latonia, and Bassfield soils, 0 to 2 percent slopes, occasionally floodedCLB7776333600c649ms11119971:20000
Latonia loamy sandy, 0 to 2 percent slopes, rarely floodedLaA5473333607c64jms11119971:20000
Latonia fine sandy loam, occasionally flooded141017334086c6mzms13119971:24000
Latonia loamy sand, 0 to 2 percent slopes, rarely floodedLaA116424034792lp0lms15320081:24000

Map of Series Extent

Approximate geographic distribution of the LATONIA 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 .