Official Series Description


Lab Data Summary

Aggregate lab data for the LACKEY soil series. This aggregation is based on all pedons with a current taxon name of LACKEY, 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 LACKEY were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

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

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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 LACKEY 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 LACKEY 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 LACKEY 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 LACKEY, 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

No block diagrams are available.

Map Units

Map units containing LACKEY 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
Lackey, cool-Rock outcrop, granitic-Tuohy, steep complex, 15 to 100 percent slopes313054532310402twpqca74019961:24000
Rock outcrop, granitic-Dorst-Lackey complex, 45 to 125 percent slopes313428532310392twpwca74019961:24000
Lackey, moraine-Tuohy complex, 2 to 30 percent slopes312425732310452r1c3ca74019961:24000
Lackey-Hockett complex, 2 to 30 percent slopes322725132920442t8znca74019961:24000
Lackey, cool-Dorst complex, 15 to 60 percent slopes314022932310422tbffca74019961:24000
Lackey-Windowpeak, warm-Halstead complex, 6 to 45 percent slopes31207732310522wcjvca74019961:24000
Mineralking, warm-Lackey-Typic Xerorthents complex, 30 to 60 percent slopes31427532920412wcjwca74019961:24000
Pigchute, cool-Lackey-Tuohy complex, 15 to 60 percent slopes31375332920432r1c9ca74019961:24000
Lackey, cool-Dorst complex, 15 to 60 percent slopes3140144532310832tbffca76019811:24000
Lackey, cool-Rock outcrop, granitic-Tuohy, steep complex, 15 to 100 percent slopes313096232310812twpqca76019811:24000
Mineralking, warm-Lackey-Typic Xerorthents complex, 30 to 60 percent slopes314257732310942wcjwca76019811:24000
Lackey-Doncecil complex, 30 to 60 percent slopes314330132311032x28pca76019811:24000
Lackey-Hockett complex, 2 to 30 percent slopes32274532920312t8znca76019811:24000
Lackey-Cahoon complex, 2 to 30 percent slopes31501032310852twpkca76019811:24000
Rock outcrop, granitic-Dorst-Lackey complex, 45 to 125 percent slopes31342159827668572twpwca79220181:24000
Lackey, cool-Dorst complex, 15 to 60 percent slopes31401772627668602tbffca79220181:24000
Lackey, cool-Rock outcrop, granitic-Tuohy, steep complex, 15 to 100 percent slopes31301440327668582twpqca79220181:24000
Lackey-Doncecil complex, 30 to 60 percent slopes31431166129246862x28pca79220181:24000
Mineralking, warm-Lackey-Typic Xerorthents complex, 30 to 60 percent slopes31421086629246362wcjwca79220181:24000
Lackey-Cahoon complex, 2 to 30 percent slopes3150870627668622twpkca79220181:24000
Lackey-Windowpeak, warm-Halstead complex, 6 to 45 percent slopes3120735529246352wcjvca79220181:24000
Lackey, moraine-Tuohy complex, 2 to 30 percent slopes3124569827772362r1c3ca79220181:24000
Pigchute, cool-Lackey-Tuohy complex, 15 to 60 percent slopes3137505927772352r1c9ca79220181:24000
Doncecil-Lackey complex, 3 to 45 percent slopes3127121032310312zm37ca79220181:24000
Lackey-Hockett complex, 2 to 30 percent slopes322795929246372t8znca79220181:24000

Map of Series Extent

Approximate geographic distribution of the LACKEY 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 .