Official Series Description


Lab Data Summary

Aggregate lab data for the LOCANE soil series. This aggregation is based on all pedons with a current taxon name of LOCANE, 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 LOCANE 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 LOCANE 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.

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the LOCANE series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the LOCANE series and siblings. 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 LOCANE 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Competing Series

Soil series competing with LOCANE share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the LOCANE 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 LOCANE 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

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 LOCANE, 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 LOCANE 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
Labshaft-Locane association, very steepLAF6766477947j1bnnv62119711:24000
Labshaft-Locane association, steepLAE3209477946j1bmnv62119711:24000
Locane very cobbly loam, 4 to 30 percent slopes5352323474756hy0qnv76019941:24000
Reluctan-Locane-Itca association345315785479228j2nznv76819851:63360
Locane-Coztur-Punchbowl association356214370479236j2p7nv76819851:63360
Punchbowl-Jung-Locane association208911490479098j2jsnv76819851:63360
Punchbowl-Locane-Nobuck association20969525479105j2k0nv76819851:63360
Robson-Locane-Softscrabble association31534970479199j2n1nv76819851:63360
Locane-Muni association35634565479237j2p8nv76819851:63360
Robson-Locane-Rock outcrop association31543555479200j2n2nv76819851:63360
Buffaran-Spasprey-Locane association25463055479130j2ktnv76819851:63360
Locane-Rock outcrop association15106147475225hyhvnv76919861:24000
Locane-Sumine-Glean association35616350479637j335nv77519851:24000
Wiskan-Locane association12154170479438j2wrnv77519851:24000
Locane-Zoesta-Bucan association35643585479638j336nv77519851:24000
Locane-Robson-Bregar association35603025479636j334nv77519851:24000
Punchbowl-Jung-Locane association20941625479527j2zmnv77519851:24000
Reluctan-Locane-Itca association3453615479634j332nv77519851:24000
Locane very cobbly loam, 8 to 30 percent slopes15401085475565hyvtnv77719931:24000
Locane very cobbly loam, 5 to 25 percent slopes174728490548jgg4or62819971:24000
Locane-Deseed complex, 2 to 20 percent slopes417593016899221tqhmor63520061:24000
Locane-Anawalt complex, 2 to 15 percent slopes416210516899211tqhlor63520061:24000
Locane cobbly clay loam, 2 to 8 percent slopes41530316899201tqhkor63520061:24000
Locane-Anawalt complex, 2 to 15 percent slopes140C5207488946jdsgor63619911:24000
Locane cobbly clay loam, 2 to 8 percent slopes139B3941488941jds9or63619911:24000
Locane-Anawalt complex, 15 to 30 percent slopes140E912488948jdsjor63619911:24000

Map of Series Extent

Approximate geographic distribution of the LOCANE 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 .