Official Series Description


Lab Data Summary

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

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
111CJR80261980IN073026Lucas3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.04325,-86.9560306
99DF-0271974-OH039-027Lucas3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.1732483,-84.3389816

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the LUCAS 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 LUCAS 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 LUCAS 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 LUCAS 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.

There are insufficient data to create the 3D mountains figure.

Click the image to view it full size.

Click the image to view it full size.

Competing Series

Soil series competing with LUCAS 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 LUCAS 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 LUCAS 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.

There are insufficient data to create the 3D mountains figure.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with LUCAS, 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. OH-2012-02-16-31 | Henry County - November 1974

    Relationship of soils to relief and underlying material in the central part of the county (Soil Survey of Henry County, Ohio; November 1974).

  2. OH-2012-02-16-37 | Sandusky County - July 1987

    Typical pattern of soils and parent material in the Toledo-Fulton association (Soil Survey of Sandusky County, Ohio; July 1987).

Map Units

Map units containing LUCAS 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
Lucas silty clay loam, 2 to 6 percent slopes, erodedLuB23191613595dx4in07319851:15840
Lucas silty clay loam, 2 to 6 percent slopesLwB115397861np8joh03919811:15840
Lucas silty clay loam, 6 to 12 percent slopes, moderately erodedLwC2115397871np8koh03919811:15840
Lucas silty clay loam, 12 to 18 percent slopes, moderately erodedLwD2115397881np8loh03919811:15840
Lucas silty clay loam, 2 to 6 percent slopes, erodedLuB247644417pmknoh06319971:12000
Lucas silty clay, 12 to 45 percent slopes, severely erodedLxE34811690145nw2oh06919681:15840
Lucas silty clay, 6 to 12 percent slopes, severely erodedLxC33731690135nw1oh06919681:15840
Lucas silty clay loam, 6 to 12 percent slopes, moderately erodedLwC21731690125nw0oh06919681:15840
Lucas silty clay loam, 2 to 6 percent slopes, moderately erodedLwB21331690115nvzoh06919681:15840
Lucas silt loam, loamy substratum, 0 to 2 percent slopesLtA63024457786hloh12519931:12000
Lucas silty clay loam, loamy substratum, 2 to 6 percent slopes, erodedLuB238724457886hmoh12519931:12000
Lucas silty clay loam, loamy substratum, 6 to 12 percent slopes, erodedLuC222524457986hnoh12519931:12000
Lucas silty clay loam, 2 to 6 percent slopesLwB7921706545qkzoh13719711:20000
Lucas silty clay loam, 6 to 12 percent slopes, moderately erodedLwC25511706555ql0oh13719711:20000
Lucas silty clay loam, 12 to 18 percent slopes, moderately erodedLwD22151706565ql1oh13719711:20000
Lucas silty clay loam, 2 to 6 percent slopes, erodedLwB2215291581nb6poh13719711:20000
Lucas silty clay loam, loamy substratum, 2 to 6 percent slopes, erodedLuB2215291791nb7coh13719711:20000
Lucas silty clay, 2 to 6 percent slopesLuB5621695695pfzoh14319831:15840
Lucas silty clay loam, 12 to 25 percent slopes, moderately erodedLuD27901681745mzzoh17119751:15840
Lucas silty clay loam, 6 to 12 percent slopes, moderately erodedLuC25001681735mzyoh17119751:15840
Lucas silty clay loam, 2 to 6 percent slopes, moderately erodedLuB22741681725mzxoh17119751:15840
Lucas silty clay, 6 to 12 percent slopes, severely erodedLwC31414141351jgj8oh17119751:15840
Lucas silty clay, 12 to 45 percent slopes, severely erodedLwE31114141361jgj9oh17119751:15840

Map of Series Extent

Approximate geographic distribution of the LUCAS 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 .