Official Series Description


Lab Data Summary

Aggregate lab data for the MCKAMIE soil series. This aggregation is based on all pedons with a current taxon name of MCKAMIE, 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 MCKAMIE 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
131C01N0368S2000LA015003McKamie7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.5883217,-93.619606

Water Balance

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

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Click the image to view it full size.

Competing Series

Soil series competing with MCKAMIE 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 MCKAMIE 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 MCKAMIE 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 MCKAMIE, 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-2012-02-01-01 | Bossier Parish - August 1962

    Physiographic relationships of general soil areas in the northwestern part of Bossier Parish. The area represented is about 12 miles square (Soil Survey of Bossier Parish, Louisiana; August 1962).

  2. LA-2012-04-27-05 | Avoyelles Parish - September 1986

    Pattern of soils, topography, and underlying material in General Soil Map Units 13 and 14 (Soil Survey of Avoyelles Parish, Louisiana; September 1986).

Map Units

Map units containing MCKAMIE 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
McKamie silt loam, 3 to 8 percent slopes192105565385lzb7ar02919771:20000
McKamie silt loam, 8 to 12 percent slopes20772565387lzb9ar02919771:20000
McKamie silt loam, 1 to 3 percent slopes18597565384lzb6ar02919771:20000
McKamie silty clay loam, 3 to 8 percent slopes, severely eroded15762565490lzfmar04519751:20000
McKamie silt loam, 3 to 8 percent slopesMkC688565569lzj5ar04719671:20000
McKamie silty clay loam, 3 to 8 percent slopes, eroded227063565647lzlpar05719761:20000
McKamie fine sandy loam, 8 to 12 percent slopes232101565648lzlqar05719761:20000
McKamie silt loam, 3 to 8 percent slopesMcC1684565847lzt4ar07119731:24000
McKamie silt loam, 3 to 8 percent slopes191222565882lzv8ar08319771:20000
McKamie silt loam, 3 to 8 percent slopes202090566092m021ar10519801:20000
McKamie very fine sandy loam, 3 to 8 percent slopes212202566126m034ar11519781:20000
McKamie silt loam, 3 to 8 percent slopesMkC1444566383m0cfar13119711:20000
McKamie silt loam, 3 to 8 percent slopes, eroded303066564989lyxgar14919851:20000
McKamie silt loam, 2 to 5 percent slopes4116703564916lyv3ar67019811:20000
McKamie silt loam, 5 to 20 percent slopes423405564917lyv4ar67019811:20000
Immanuel-McKamie complex, 8 to 20 percent slopes23140175643062ry5war68019801:20000
McKamie silt loam, 5 to 12 percent slopesMa445217119431vgdzla00919811:24000
McKamie very fine sandy loam, 5 to 15 percent slopesMcF2746315922401qfvlla01520051:24000
McKamie very fine sandy loam, 1 to 5 percent slopesMcC161315922391qfvkla01520051:24000
McKamie very fine sandy loam, 5 to 15 percent slopesMcF137628057242ssxgla01720131:24000
McKamie soils, 8 to 30 percent slopesMcE132141017139134dyla03919701:24000
McKamie very fine sandy loam, 5 to 12 percent slopesMcD1849569970m434la07919731:24000
McKamie very fine sandy loam, 1 to 5 percent slopesMcC838569969m433la07919731:24000
Gore-McKamie association, slopingGSC514817206661vrhcla08119731:24000
McKamie loam, 3 to 5 percent slopes37887571421m5lyok07919811:24000
McKamie loam, 5 to 12 percent slopes, eroded38305571422m5lzok07919811:24000
McKamie loam, 5 to 12 percent slopesMkE2175571898m63bok13519661:24000
McKamie loam, 5 to 12 percent slopes1910684575263m9lwtx03719781:20000
McKamie loam, 1 to 5 percent slopes186613575262m9lvtx03719781:20000
McKamie loam, 5 to 12 percent slopesMcE7709371451dgj9tx38719721:24000
McKamie loam, 1 to 5 percent slopesMcC2949371450dgj8tx38719721:24000

Map of Series Extent

Approximate geographic distribution of the MCKAMIE 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 .