Official Series Description


Lab Data Summary

Aggregate lab data for the LANKTREE soil series. This aggregation is based on all pedons with a current taxon name of LANKTREE, 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 LANKTREE 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
1169C0136S1969ID075014Lanktree7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0791664,-116.6924973

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the LANKTREE 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 LANKTREE 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 LANKTREE 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 LANKTREE 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 hills figure.

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 LANKTREE 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 LANKTREE 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 LANKTREE 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.

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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 LANKTREE, 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 LANKTREE 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
Lanktree-Lankbush complex, 30 to 60 percent slopes1204679811192qdrid65619921:24000
Lanktree loam, 2 to 30 percent slopes1172920811152qdmid65619921:24000
Lanktree loam, 0 to 2 percent slopes116769811142qdlid65619921:24000
Lanktree very cobbly loam, 2 to 30 percent slopes119496811172qdpid65619921:24000
Lanktree clay loam, 4 to 8 percent slopes118347811162qdnid65619921:24000
Lanktree-Haw complex, 0 to 3 percent slopesLcB1568813532qn9id65919711:20000
Lanktree-Haw complex, 3 to 7 percent slopesLcC286813542qnbid65919711:20000
Lanktree and Chilcott loams, 7 to 12 percent slopesLmD5915805962pvwid66019621:15840
Lanktree loam, 12 to 30 percent slopesLfE3467805922pvrid66019621:15840
Lanktree and Chilcott loams, 12 to 30 percent slopesLmE3153805972pvxid66019621:15840
Lanktree sandy loam, 30 to 60 percent slopesLkF1879805942pvtid66019621:15840
Lanktree and Chilcott loams, 3 to 7 percent slopesLmC941805952pvvid66019621:15840
Lanktree sandy loam, 12 to 30 percent slopesLkE835805932pvsid66019621:15840
Lanktree and Chilcott sandy loams, 12 to 30 percent slopesLnE624805982pvyid66019621:15840
Lanktree gravelly loam, 12 to 30 percent slopesLdE315805882pvmid66019621:15840
Lanktree loam, 3 to 7 percent slopesLfC296805902pvpid66019621:15840
Lanktree gravelly sandy loam, 12 to 30 percent slopesLeE274805892pvnid66019621:15840
Lanktree loam, 7 to 12 percent slopesLfD167805912pvqid66019621:15840
Lanktree, Chilcott, and Sebree loams, 1 to 3 percent slopesLoB75805992pvzid66019621:15840
Lanktree-Chilcott loams, 0 to 12 percent slopes942954325196222r28id68520121:24000
Lankbush-Lanktree complex, 4 to 30 percent slopes91714825196192r25id68520121:24000
Lanktree loam, 0 to 4 percent slopes9348025196212r27id68520121:24000

Map of Series Extent

Approximate geographic distribution of the LANKTREE 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 .