Official Series Description


Lab Data Summary

Aggregate lab data for the KENNER soil series. This aggregation is based on all pedons with a current taxon name of KENNER, 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 KENNER 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
15140A4091S1971LA051001Kenner3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.8713551,-90.1661987
15140A4095S1971LA051005Kennern/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.8661118,-90.1616669
15140A4092S1971LA051006Kennern/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.8555565,-90.1591644

Water Balance

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

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Click the image to view it full size.

Competing Series

Soil series competing with KENNER 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 KENNER 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 KENNER 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 KENNER, 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. LA-2012-04-27-11 | Jefferson Parish - January 1983

    Transect showing relationship of soils to surface elevation from Mississippi River levee at Harahan (A) to Lake Pontchartrain at intersection of Clearview Parkway and Foise Street (B) (Soil Survey of Jefferson Parish, Louisiana; January 1983).

  2. LA-2012-04-27-13 | Plaquemines Parish - 2000

    Relationship of soils, landscape, parent materials, and marsh types of the Gulf Coastal Marshes in Plaquemines Parish (Soil Survey of Plaquemines Parish, Louisiana; 2000).

Map Units

Map units containing KENNER 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
Chowan, Brickyard, and Kenner soils, frequently flooded251998014770771ll0nfl03719901:20000
Brickyard, Chowan, and Kenner soils, frequently flooded412511414727621lfjgfl04519971:24000
Kenner muck, 0 to 1 percent slopes, very frequently floodedKE2183414134332qr73la05119811:24000
Kenner muck, drainedKa1055514134341jfsnla05119811:24000
Kenner muck, 0 to 1 percent slopes, very frequently floodedKE379198085202qr73la05719811:24000
Kenner muck drainedKe4499569889m40jla07119871:24000
Kenner muck, 0 to 1 percent slopes, very frequently floodedKE333315986642qr73la07519881:24000
Kenner muck, 0 to 1 percent slopes, very frequently floodedKE556633754732qr73la08919841:24000
Kenner muck, 0 to 1 percent slopes, very frequently floodedKe79625769692qr73la09520041:24000
Kenner muck, 0 to 1 percent slopes, very frequently floodedKEA409333784872qr73la10119991:24000
Kenner muckKE2895327003bz8hla10319851:24000
Kenner muckKE259115365131nkvyla10519851:24000
Kenner muck, 0 to 1 percent slopes, very frequently floodedKEA1164973936752qr73la10920011:24000

Map of Series Extent

Approximate geographic distribution of the KENNER 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 .