Official Series Description


Lab Data Summary

Aggregate lab data for the MERCER soil series. This aggregation is based on all pedons with a current taxon name of MERCER, 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 MERCER 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
n/a66KY-211-00166KY-211-001Mercer4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a68KY-067-00268KY-067-002Mercer3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MERCER 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 MERCER 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 MERCER 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 MERCER 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 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 MERCER 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 MERCER 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 MERCER 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 MERCER, 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. KY-2012-01-27-36 | Clark County - 1964

    Major soil series in soil association 3, their relationship to the landscape, and the parent rocks from which the soils formed (Soil Survey of Clark County, Kentucky; 1964).

  2. KY-2012-01-27-45 | Clark County - 1964

    Geolgic cross section of Clark County, showing some of the principal soils and their relation to the rock formations (Soil Survey of Clark County, Kentucky; 1964).

  3. KY-2012-01-27-67 | Fayette County - February 1968

    Relationship of soils to topography and underlying material in association 2. Unshaded areas represent caverns or sinkholes in the limestone bedrock (Soil Survey of Fayette County, Kentucky; February 1968).

  4. KY-2012-01-30-11 | Harrison County - April 1968

    Major and minor soils in association 1, their relationship to the landscape, and the parent material from which the soils formed (Soil Survey of Harrison County, Kentucky; April 1968).

  5. KY-2012-02-01-07 | Madison County - March 1973

    Relationship of soils to topography and underlying material in the Shelbyville-Mercer-Nicholson association (Soil Survey of Madison County, Kentucky; March 1973).

  6. KY-2012-02-01-08 | Madison County - March 1973

    Relationship of soils to topography and underlying material in the Lawrence-Mercer-Robertsville association (Soil Survey of Madison County, Kentucky; March 1973).

Map Units

Map units containing MERCER 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
Mercer silt loam, 2 to 6 percent slopesMmB16185501992wlv9ky04919621:15840
Mercer silt loam, 6 to 12 percent slopes, erodedMmC27115502022wh3xky04919621:15840
Mercer silt loam, 6 to 12 percent slopesMmC4885502012wv4pky04919621:15840
Mercer silt loam, 2 to 6 percent slopes, erodedMmB22085502002wh3wky04919621:15840
Mercer silt loam, 2 to 6 percent slopesMtB6635518222wlv9ky09719651:15840
Mercer silt loam, 2 to 6 percent slopesMuB942413978912wlv9ky15119681:20000
Mercer silt loam, 6 to 12 percent slopesMuC611513978922wv4pky15119681:20000
Mercer silt loam, 0 to 2 percent slopesMuA146813978902wh5hky15119681:20000
Mercer silty clay loam, 6 to 12 percent slopes, severely erodedMvC317513978932wh5jky15119681:20000
Mercer silt loam, 2 to 6 percent slopesMuB593513988922wlv9ky64319651:15840
Mercer silt loam, 6 to 12 percent slopesMuC147513988942wv4pky64319651:15840
Mercer silt loam, 6 to 12 percent slopes, erodedMuC2129613988952wh3xky64319651:15840
Mercer silt loam, 2 to 6 percent slopes, erodedMuB224113988932wh3wky64319651:15840
Mercer silt loam, 0 to 2 percent slopesMuA9813988912wh5hky64319651:15840

Map of Series Extent

Approximate geographic distribution of the MERCER 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 .