Official Series Description


Lab Data Summary

Aggregate lab data for the GRABLE soil series. This aggregation is based on all pedons with a current taxon name of GRABLE, 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 GRABLE 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
107BM87195211987MO195021mGrable3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3666649,-93.1258316
107BM87195231987MO195023mGrable3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3666649,-93.1244431
107BM87195311987MO195031mGrable4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2392041,-92.9899114
107BM09195022009MO195002Grable4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2635556,-93.4279167
107BM09195032009MO195003Grable4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2630833,-93.4246944
107BM09195082009MO195008Grable4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2574167,-93.4173611
115BM87195341987MO195034mGrable4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.0894444,-92.9338889
115BM89053051989MO053005Grable4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672644,-92.3451678
115BM91041041991MO041004Grable4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM07027322007MO027032GRABLE4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6268889,-91.9151667
115BM07027362007MO027036GRABLE4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6832222,-91.8296944
115BM07139032007MO139003GRABLE4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6878333,-91.5421389
115BM07151052007MO151005GRABLE4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6963889,-91.6486111
115BM09183092009MO183009Grable4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.8326111,-90.1590278

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the GRABLE 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 GRABLE 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 GRABLE 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 GRABLE 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 GRABLE 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 GRABLE 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 GRABLE 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 GRABLE, 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. IA-2010-09-02-23 | Monona County - 2003

    Typical pattern of soils and parent material in the Albaton-Percival-Sarpy and Albaton-Onawa-Forney associations (Soil Survey of Monona County, Iowa; 2003).

  2. MO-2010-09-08-03 | Holt County - 1997

    Typical pattern of soils and parent material in the Leta-Grable-Haynie association (Soil Survey of Holt County, Missouri; 1997).

  3. NE-2012-02-10-04 | Cedar County - October 1985

    Typical pattern of soils in the Sarpy-Blake-Albaton association and the relationship of the soils to topography and parent material (Soil Survey of Cedar County, Nebraska; October 1985).

Map Units

Map units containing GRABLE 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
Grable silt loam5142265406149fmmlia07119681:20000
Grable silt loam514820406773fn8qia08519711:15840
Grable silt loam, 0 to 2 percent slopes5142025409579fr67ia12919791:15840
Grable silt loam, 0 to 2 percent slopes, rarely flooded5141899447381h0jnia13319941:12000
Grable silt loam, 0 to 2 percent slopes, occasionally flooded15141315447415h0kria13319941:12000
Grable silt loam, 0 to 2 percent slopes5141577410503fs51ia15519861:15840
Grable-Morconick complex, 0 to 2 percent slopes, rarely flooded3513769741615swq2ia19320031:12000
Grable-Morconick complex, 0 to 2 percent slopes, occasionally flooded1513512741613swq0ia19320031:12000
Grable very fine sandy loam, 0 to 2 percent slopes, rarely flooded13521112525283832qmtlmo02119841:24000
Grable silt loam, 0 to 2 percent slopes, occasionally flooded13519204888510ytkmmo04119921:24000
Grable silt loam, loamy substratum, 0 to 2 percent slopes, frequently flooded6611918824281132mhn7mo05319931:24000
Grable silt loam, loamy substratum, 0 to 2 percent slopes, occasionally flooded66094119887189ys60mo05319931:24000
Grable-Leta complex, 0 to 2 percent slopes, rarely flooded135227027887498yshzmo08719921:24000
Grable very fine sandy loam, 0 to 2 percent slopes, rarely flooded13521320525283822qmtlmo08719921:24000
Kenmoor-Grable complex, 0 to 2 percent slopes, rarely flooded13538817887507ysj8mo08719921:24000
Grable very fine sandy loam, 0 to 2 percent slopes, frequently flooded13520648887497yshymo08719921:24000
Grable very fine sandy loam, loamy substratum, 0 to 2 percent slopes, rarely flooded136042183888249yt96mo19519891:24000
Sarpy-Grable variant complex, occasionally flooded78573158427861gc6zne02119781:20000
Grable silt loam, occasionally flooded77031368427820gc5nne02119781:20000
Grable silt loam, rarely flooded77071912427104gbfkne02719821:20000
Grable very fine sandy loam, occasionally flooded77043128426732gb1kne04319721:20000
Grable very fine sandy loam, rarely flooded77051722170422df0hne04319721:20000
Grable very fine sandy loam, rarely flooded77051922426671g9zlne05119751:20000
Grable very fine sandy loam, occasionally flooded7704105616916581ts9mne12719831:20000
Grable silt loam, occasionally flooded7703551395536f8l7ne17720001:12000
Haynie-Grable silt loams, 0 to 2 percent slopesHg1513445577gyngsd02719951:24000
Haynie-Lossing-Grable complex, 0 to 2 percent slopesHn1416445578gynhsd02719951:24000
Grable-Ticonic-Vore complex, 0 to 2 percent slopesGt1375445574gyncsd02719951:24000
Ticonic-Grable complex, 0 to 2 percent slopesTr983445616gypqsd02719951:24000
Grable-Vore-Haynie complex, 0 to 3 percent slopesGv963445575gyndsd02719951:24000
Grable silt loam, 0 to 2 percent slopesGa416445573gynbsd02719951:24000
Grable silt loamGa2907453697h73dsd12719741:20000
Sardak-Grable complex, 0 to 4 percent slopesSeA1810418105g128sd13519771:20000
Grable silt loamGa1500418087g11psd13519771:20000

Map of Series Extent

Approximate geographic distribution of the GRABLE 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 .