Official Series Description


Lab Data Summary

Aggregate lab data for the FLORENCE soil series. This aggregation is based on all pedons with a current taxon name of FLORENCE, 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 FLORENCE 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
7488KS06113988KS061139Florence2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.0600319,-96.5386353
7640A183763KS017004Florence5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1369438,-96.5830536
7687P045187KS161004FLORENCE7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.0963898,-96.5774994
7697KS16104897KS161048Florence3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.218029,-96.6269989
7640A5192S1963KS017002Florence6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1611557,-96.5775223

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the FLORENCE 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 FLORENCE 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 FLORENCE 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 FLORENCE 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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Click the image to view it full size.

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 FLORENCE 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 FLORENCE series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the FLORENCE 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 .

There are insufficient data to create the 2D hillslope position figure.

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.

Soil series sharing subgroup-level classification with FLORENCE, 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. KS-2012-01-20-10 | Chase County - June 1974

    Pattern of soils in the Florence-Labette association (Soil Survey of Chase County, Kansas; 1974).

  2. KS-2012-01-20-54 | Elk County - November 1986

    Typical pattern of soils and underlying material in the Florence-Martin association (Soil Survey of Elk County, Kansas; 1986).

  3. KS-2012-01-23-06 | Geary County - February 1960

    Diagram showing the relationship of the soils in the southeastern part of Geary County (Soil Survey of Geary County, Kansas; 1960).

  4. KS-2012-01-24-15 | Morris County - November 1974

    Typical pattern of soils and underlying material in association 1 (Soil Survey of Morris County, Kansas; 1974).

  5. KS-2012-01-24-18 | Morris County - November 1974

    Typical pattern of soils and underlying material in association 4. In many places Florence and Labette soils, closely intermingled and mapped together, border soils of this association (Soil Survey of Morris County, Kansas; 1974).

  6. KS-2012-01-25-09 | Pottawatomie County - December 1987

    Pattern of soils and parent material in the Clime-Tully-Benfield association (Soil Survey of Pottawatomie County, Kansas; 1987).

  7. KS-2012-01-26-19 | Wabaunsee County - May 1991

    Typical pattern of soils and parent material in the Florence-Irwin-Labette association (Soil Survey of Wabaunsee County, Kansas; 1991).

Map Units

Map units containing FLORENCE 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
Florence cherty silt loam, 5 to 15 percent slopes46455408213828672tt4rks01519701:24000
Florence-Martin complex, 2 to 12 percent slopes4660202913828692tt4tks01519701:24000
Florence-Labette complex, 2 to 12 percent slopes4655196613828682tt4mks01519701:24000
Florence-Labette complex, 2 to 12 percent slopes46553682113828212tt4mks01719671:24000
Florence-Matfield cherty silt loams, 1 to 15 percent slopes46653128013828222tt4vks01719671:24000
Florence silt loam, 2 to 15 percent slopes4650138613828202tt4sks01719671:24000
Florence cherty silt loam, 5 to 15 percent slopes464583513828192tt4rks01719671:24000
Florence cherty silt loam, 5 to 15 percent slopes46453607613829302tt4rks03519771:24000
Martin-Florence complex, 2 to 12 percent slopes73123071413829462tt4wks03519771:24000
Florence-Martin complex, 2 to 12 percent slopes4660192113829312tt4tks03519771:24000
Florence-Martin complex, 2 to 12 percent slopes4660940214533032tt4tks04919841:24000
Florence cherty silt loam, 5 to 15 percent slopes4645214533022tt4rks04919841:24000
Benfield-Florence complex, 5 to 30 percent slopes45304131913871812tt4qks06119911:24000
Florence-Labette complex, 2 to 12 percent slopes46551883914536462tt4mks07319811:24000
Florence-Martin complex, 2 to 12 percent slopes466066814536472tt4tks07319811:24000
Florence-Labette complex, 2 to 12 percent slopes46551118114537062tt4mks11119771:24000
Florence silt loam, 2 to 15 percent slopes4650438613827722tt4sks11519811:24000
Benfield-Florence complex, 5 to 30 percent slopes453074214570682tt4qks11719771:24000
Florence-Labette complex, 2 to 12 percent slopes46552633214544982tt4mks12719701:24000
Florence cherty silt loam, 5 to 15 percent slopes46452350514544972tt4rks12719701:24000
Benfield-Florence complex, 5 to 30 percent slopes45308914544942tt4qks12719701:24000
Benfield-Florence complex, 5 to 30 percent slopes45304444614806912tt4qks14919841:24000
Benfield-Florence complex, 5 to 30 percent slopes45303117114723052tt4qks16119701:24000
Florence-Labette complex, 2 to 12 percent slopes465573114723112tt4mks16119701:24000
Florence-Labette complex, 2 to 12 percent slopes46555319014721422tt4mks19719881:24000
Benfield-Florence complex, 5 to 30 percent slopes4530651714721382tt4qks19719881:24000

Map of Series Extent

Approximate geographic distribution of the FLORENCE 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 .