Official Series Description


Lab Data Summary

Aggregate lab data for the LANTRY soil series. This aggregation is based on all pedons with a current taxon name of LANTRY, 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 LANTRY were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the LANTRY 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 LANTRY 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 LANTRY 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 LANTRY 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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Competing Series

Soil series competing with LANTRY 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 LANTRY 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 LANTRY 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 hills figure.

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 LANTRY, 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. SD-2012-03-16-05 | Ziebach County - March 1990

    Pattern of soils and parent material in the Trembles-Korchea-Banks and Lantry-Cabba-Rhoades associations (Soil Survey of Ziebach County, SD; 1990).

  2. SD-2012-03-16-06 | Ziebach County - March 1990

    Pattern of soils and parent material in the Reeder-Lantry association (Soil Survey of Ziebach County, SD; 1990).

Map Units

Map units containing LANTRY 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
Cabba-Lantry-Golva silt loams, 9 to 50 percent slopesE2709F174525635362r6tynd01119691:20000
Cabba-Lantry silt loams, 9 to 15 percent slopesE2743D162927597432r6tznd03319851:24000
Lantry-Cabba silt loams, 6 to 9 percent slopesE2745C26427597442r6v1nd03319851:24000
Cabba-Lantry-Golva silt loams, 9 to 50 percent slopesE2709F4127597402r6tynd03319851:24000
Cabba-Lantry silt loams, 9 to 15 percent slopesE2743D26727597202r6tznd05320031:24000
Cabba-Lantry complex, 25 to 40 percent slopesCbF263963541812v679sd04119721:24000
Morton-Lantry silt loams, 2 to 9 percent slopesMgB24737354212cwl6sd04119721:24000
Lantry-Morton silt loams, 6 to 15 percent slopesLmD13061354201cwkvsd04119721:24000
Cabba-Lantry complex, 15 to 25 percent slopesCbE74743541802v67bsd04119721:24000
Cabba-Lantry-Amor loams, 9 to 25 percent slopesCaD82363355725cy50sd06319841:24000
Reeder-Lantry loams, 2 to 9 percent slopesRcC109470354649cx19sd10519771:24000
Cabba-Lantry complex, 15 to 40 percent slopesCaE906383546192v677sd10519771:24000
Morton-Lantry loams, 2 to 9 percent slopesMdC79865354641cx11sd10519771:24000
Morton-Lantry loams, 6 to 15 percent slopesMdD73866354642cx12sd10519771:24000
Lantry-Cabba complex, 9 to 30 percent slopesLcD735343558532v678sd13719851:24000
Reeder-Lantry complex, 2 to 9 percent slopesRdC71255355871cy9qsd13719851:24000
Reeder-Rhoades-Lantry complex, 2 to 9 percent slopesReC30725355872cy9rsd13719851:24000
Cabba-Lantry complex, 25 to 40 percent slopesCaE205203558302v679sd13719851:24000
Lantry-Cabba-Rhoades complex, 9 to 30 percent slopesLdD17921355854cy95sd13719851:24000
Lantry-Korchea-Cabba complex, 1 to 25 percent slopesLeD1917355855cy96sd13719851:24000

Map of Series Extent

Approximate geographic distribution of the LANTRY 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 .