Official Series Description


Lab Data Summary

Aggregate lab data for the LEONI soil series. This aggregation is based on all pedons with a current taxon name of LEONI, 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 LEONI 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
111B40A1900S1975MI075003Leoni7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.2900085,-84.3957367

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the LEONI 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 LEONI 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 LEONI 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 LEONI 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 LEONI 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 LEONI 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 LEONI 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 LEONI, 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 LEONI 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
Leoni gravelly sandy loam, 0 to 6 percent slopes30B218818697868kkmi02319841:15840
Leoni gravelly loam, 0 to 6 percent slopes21B26291886896bbrmi02519931:15840
Leoni gravelly loam, 6 to 12 percent slopes21C9131886906bbsmi02519931:15840
Leoni gravelly sandy loam, 1 to 6 percent slopes44B23331886566b9pmi05919911:15840
Leoni very gravelly sandy loam, 6 to 12 percent slopes, eroded44C215021886576b9qmi05919911:15840
Leoni very gravelly sandy loam, 12 to 18 percent slopes, eroded44D22941886586b9rmi05919911:15840
Boyer-Leoni complex, 18 to 40 percent slopes11E47061887476bdmmi07519791:15840
Leoni gravelly sandy loam, 2 to 6 percent slopes44B45821887736bfgmi07519791:15840
Oshtemo-Leoni complex, 1 to 6 percent slopes68B43051888046bggmi07519791:15840
Leoni gravelly sandy loam, 6 to 12 percent slopes44C29861887746bfhmi07519791:15840
Riddles-Leoni complex, 10 to 20 percent slopes56D15981887896bfzmi07519791:15840
Oshtemo-Leoni complex, 6 to 12 percent slopes68C15851888056bghmi07519791:15840
Leoni gravelly sandy loam, 12 to 18 percent slopes44D12611887756bfjmi07519791:15840
Leoni gravelly sandy loam, 0 to 6 percent slopes51B252018776069csmi10719821:15840
Leoni gravelly sandy loam, 6 to 12 percent slopes51C132918776169ctmi10719821:15840
Leoni gravelly sandy loam, 12 to 18 percent slopes51D83018776269cvmi10719821:15840
Leoni gravelly sandy loam, 1 to 6 percent slopes51B7831888616bj9mi12519801:15840
Leoni gravelly sandy loam, 6 to 12 percent slopes51C5761888626bjbmi12519801:15840
Leoni gravelly loam, 12 to 25 percent slopesLeE701720605s1boh04119971:12000

Map of Series Extent

Approximate geographic distribution of the LEONI 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 .