Official Series Description


Lab Data Summary

Aggregate lab data for the KLACKING soil series. This aggregation is based on all pedons with a current taxon name of KLACKING, 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 KLACKING 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
94AS78MI-85-2S1978MI085002Klacking5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.99625,-85.8807778

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the KLACKING 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 KLACKING 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 KLACKING 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 KLACKING 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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Competing Series

Soil series competing with KLACKING 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 KLACKING 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 KLACKING 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 KLACKING, 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. MI-2010-09-07-23 | Montmorency County - 2003

    Typical pattern of soils and underlying material in the Rubicon-Grayling-Tawas and Millersburg-Klacking-Horsehead associations (Soil Survey of Montmorency County, Michigan; 2003).

  2. MI-2012-02-06-03 | Alcona County - 1998

    Typical pattern of soils and parent material in the McGinn-Hoist-Klacking, Grayling-Graycalm-Typic Udipsamments, and Glennie-Bamfield-Lupton associations (Soil Survey of Alcona County, Michigan; 1998).

  3. MI-2012-02-06-04 | Alcona County - 1998

    Typical pattern of soils and parent material in the Klacking-McGinn association (adjacent to the Lupton-Tawas-Leafriver association) (Soil Survey of Alcona County, Michigan; 1998).

Map Units

Map units containing KLACKING 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
Klacking-McGinn loamy sands, 8 to 50 percent slopes, dissected94F247371903856d3gmi00119931:20000
Klacking loamy sand, 6 to 12 percent slopes31C101201903146d15mi00119931:20000
Klacking loamy sand, 0 to 6 percent slopes31B61301903136d14mi00119931:20000
Klacking loamy sand, 12 to 18 percent slopes31D41211903156d16mi00119931:20000
Klacking-McGinn loamy sands, 0 to 6 percent slopes92B24481903836d3dmi00119931:20000
Klacking loamy sand, 18 to 35 percent slopes31E2481903166d17mi00119931:20000
Klacking loamy sand, 0 to 6 percent slopes31B35941912676f0xmi00719981:12000
Klacking loamy sand, 6 to 12 percent slopes31C27091912686f0ymi00719981:12000
Klacking loamy sand, 18 to 35 percent slopes31E23211913256f2smi00719981:12000
Klacking-McGinn loamy sands, 8 to 50 percent slopes, dissected94F22731913136f2dmi00719981:12000
Klacking loamy sand, 12 to 18 percent slopes31D11501912696f0zmi00719981:12000
Klacking-McGinn loamy sands, 6 to 12 percent slopes92C3711913546f3qmi00719981:12000
Klacking-McGinn loamy sands, 0 to 6 percent slopes92B2421913486f3jmi00719981:12000
Graycalm-Klacking complex, 0 to 6 percent slopes21B117031896786ccnmi03919931:15840
Klacking loamy sand, 0 to 6 percent slopes31B49811897106cdpmi03919931:15840
Graycalm-Klacking complex, 6 to 18 percent slopes21D12291896796ccpmi03919931:15840
Graycalm-Klacking complex, 8 to 45 percent slopes21F3091896806ccqmi03919931:15840
Klacking sand, 6 to 18 percent slopes123D171917046fh0mi06919951:15840
Graycalm-Klacking complex, 0 to 6 percent slopes21B73181906386dcmmi07919981:12000
Graycalm-Klacking complex, 6 to 18 percent slopes21D10661906396dcnmi07919981:12000
Graycalm-Klacking complex, 18 to 45 percent slopes21F2341906956dfgmi07919981:12000
Millersburg-Klacking-Graycalm complex, 0 to 6 percent slopes388B107551922726g2bmi11919971:12000
Millersburg-Klacking-Graycalm complex, 6 to 18 slopes388D92471922736g2cmi11919971:12000
Klacking sand, 0 to 6 percent slopes307B86051922366g15mi11919971:12000
Klacking sand, 6 to 18 percent slopes123D83871921796fzbmi11919971:12000
Millersburg-Klacking-Graycalm complex, 18 to 35 percent slopes388E30381922746g2dmi11919971:12000
Klacking sand, 18 to 35 percent slopes307E19641922376g16mi11919971:12000
Klacking-McGinn loamy sands, 8 to 50 percent slopes, dissected94F1661923456g4pmi11919971:12000
Klacking sand, 35 to 70 percent slopes307F1291922386g17mi11919971:12000
Klacking sand, 0 to 6 percent slopes18B50311898806cl5mi12919871:15840
Klacking sand, 6 to 18 percent slopes18C43351898816cl6mi12919871:15840
Klacking sand, 18 to 35 percent slopes18E12401898826cl7mi12919871:15840
Klacking-Isabella complex, 12 to 18 percent slopes93D11661899646cnwmi12919871:15840
Klacking-Isabella complex, 6 to 12 percent slopes93C7771899636cnvmi12919871:15840
Klacking-Isabella complex, 18 to 25 percent slopes93E7191899656cnxmi12919871:15840
Graycalm-Klacking sands, 6 to 18 percent slopes475D1267720906670k2mi13520031:12000
Graycalm-Klacking sands, 0 to 6 percent slopes475B1189820906570k1mi13520031:12000
Millersburg-Klacking-Graycalm complex, 0 to 6 percent slopes388B502020904370jbmi13520031:12000
Millersburg-Klacking-Graycalm complex, 6 to 18 percent slopes388D453520904470jcmi13520031:12000
Klacking sand, 0 to 6 percent slopes307B2975241420836rmi13520031:12000
Klacking-Perecheney sands, 0 to 6 percent slopes476B26242684019093mi13520031:12000
Graycalm-Klacking sands, 18 to 35 percent slopes475E164020906970k5mi13520031:12000
Millersburg-Klacking-Graycalm complex, 18 to 35 percent slopes388E77320904570jdmi13520031:12000
Klacking sand, 6 to 18 percent slopes123D4242414288370mi13520031:12000
Klacking-Perecheney sands, 6 to 18 percent slopes476D378628182p2nymi13520031:12000
Klacking sand, 18 to 35 percent slopes307E8620903870j5mi13520031:12000
Klacking loamy sand, 0 to 6 percent slopes31B55241355834nmi13520031:12000
Klacking loamy sand, 6 to 12 percent slopes31C17241356834pmi13520031:12000
Klacking loamy sand, 12 to 18 percent slopes31D16241357834qmi13520031:12000
Klacking-McGinn loamy sands, 8 to 50 percent slopes, dissected94F152413718355mi13520031:12000
Graycalm-Klacking complex, 6 to 18 percent slopes21D8241386835nmi13520031:12000
Klacking sand, 0 to 6 percent slopes4B35961909046dn6mi14119891:15840
Klacking sand, 6 to 12 percent slopes4C13821909056dn7mi14119891:15840
Graycalm-Klacking sands, 0 to 6 percent slopes475B136551910256ds3mi14319991:12000
Klacking sand, 0 to 6 percent slopes307B62611910156drsmi14319991:12000
Graycalm-Klacking sands, 6 to 18 percent slopes475D50071910266ds4mi14319991:12000
Klacking-Perecheney sands, 0 to 6 percent slopes476B32841909776dqkmi14319991:12000
Graycalm-Klacking sands, 18 to 35 percent slopes475E13291910276ds5mi14319991:12000
Klacking-Perecheney sands, 6 to 18 percent slopes476D9821910406dslmi14319991:12000
Klacking sand, 6 to 18 percent slopes123D8321910116drnmi14319991:12000
Klacking sand, 18 to 35 percent slopes307E3941910166drtmi14319991:12000

Map of Series Extent

Approximate geographic distribution of the KLACKING 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 .