Official Series Description


Lab Data Summary

Aggregate lab data for the FLEAK soil series. This aggregation is based on all pedons with a current taxon name of FLEAK, 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 FLEAK 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 FLEAK 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 FLEAK 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 FLEAK 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 FLEAK 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 FLEAK 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 FLEAK series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the FLEAK 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 .

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Click the image to view it full size.

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 FLEAK, 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 FLEAK 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
Rhame-Fleak complex, 9 to 50 percent slopesL1425F324930404902qz6smt02519911:24000
Fleak-Badland complex, 9 to 70 percent slopesL3109F11242992076d353mt02519911:24000
Busby-Yamacall-Fleak complex, 15 to 45 percent slopes314F4754342735chmzmt03320021:24000
Busby-Twilight-Fleak complex, 8 to 15 percent slopes318D734342736chn0mt03320021:24000
Busby-Fleak complex, 15 to 45 percent slopes312F718342734chmymt03320021:24000
Gerdrum-Yawdim-Fleak complex, 0 to 8 percent slopes541C645339822cdm0mt03320021:24000
Yamacall-Twilight-Fleak complex, 8 to 15 percent slopes987D507342816chqlmt03320021:24000
Busby-Yamac-Fleak complex, 15 to 45 percent slopes2332392344384ckc5mt05519811:24000
Busby-Fleak complex, 15 to 45 percent slopes2026145344381ckc2mt05519811:24000
Busby-Twilight-Fleak complex, 8 to 15 percent slopes2214766344383ckc4mt05519811:24000
Hillon-Yamacall-Fleak complex, 15 to 45 percent slopes9511444344463ckfqmt05519811:24000
Yamacall-Twilight-Fleak complex, 8 to 15 percent slopes1638005344364ckbjmt05519811:24000
Gerdrum-Yawdim-Fleak complex, 8 to 45 percent slopes724081344438ckdxmt05519811:24000
Gerdrum-Yawdim-Fleak complex, 0 to 8 percent slopes711904344437ckdwmt05519811:24000
Fleak-Lihen fine sandy loams, 8 to 25 percent slopes651E202345237cl7pmt10119921:24000
Twilight-Fleak complex, 8 to 25 percent slopes661E7429346875cmyjmt61519921:24000
Fleak-Twilight-Rock outcrop complex, 25 to 70 percent slopes654F6744346873cmygmt61519921:24000
Fleak-Twilight-Yetull complex, 25 to 70 percent slopes653F4942346872cmyfmt61519921:24000
Rock outcrop-Fleak complex, 25 to 70 percent slopes4101284346763cmtxmt61519921:24000
Rhame-Fleak complex, 9 to 50 percent slopesL1425F1719527070372qz6snd00719981:24000
Rhame-Arikara-Fleak complex, 9 to 70 percent slopesL1661F415427070402qxhwnd00719981:24000
Fleak-Rhame complex, 3 to 15 percent slopesFnD747999282412b3lnd01119691:20000
Fleak-Tusler complex, 15 to 40 percent slopesFtE519099282612b3nnd01119691:20000
Rhame-Fleak fine sandy loams, 6 to 9 percent slopesRoC358999289012b5qnd01119691:20000
Rhame-Fleak complex, 9 to 50 percent slopesL1425F312725634682qz6snd01119691:20000
Fleak rocky complex, 15 to 50 percent slopesFoE288399282512b3mnd01119691:20000
Fleak-Rock outcrop-Tusler complex, 15 to 50 percent slopesL1475F259725634692q2mqnd01119691:20000
Tusler-Fleak-Chinook complex, 9 to 15 percent slopesL1405D238625634672qxhnnd01119691:20000
Fleak-Badland complex, 9 to 70 percent slopesL3109F22932758463d353nd01119691:20000
Rhame-Fleak fine sandy loams, 9 to 15 percent slopesRoD198199289112b5rnd01119691:20000
Tusler-Fleak-Telfer, low precipitation loamy fine sands, 6 to 15 percent slopesL1857D133725634732qxhynd01119691:20000
Rhame-Fleak complex, 9 to 50 percent slopesL1425F1921927071622qz6snd02519811:20000
Rhame-Arikara-Fleak complex, 9 to 70 percent slopesL1661F1479227071432qxhwnd02519811:20000
Tusler-Fleak-Telfer, low precipitation loamy fine sands, 6 to 15 percent slopesL1857D11327071442qxhynd02519811:20000
Rhame-Fleak complex, 9 to 50 percent slopesL1425F1357127073232qz6snd03319851:24000
Tusler-Fleak-Chinook complex, 9 to 15 percent slopesL1405D261127073222qxhnnd03319851:24000
Tusler-Fleak-Chinook complex, 3 to 9 percent slopesL1405C89227073212qxhmnd03319851:24000
Fleak-Badland complex, 9 to 70 percent slopesL3109F492759769d353nd03319851:24000
Rhame-Fleak complex, 9 to 50 percent slopesL1425F2511027151422qz6snd05320031:24000
Rhame-Arikara-Fleak complex, 9 to 70 percent slopesL1661F1922627151452qxhwnd05320031:24000
Fleak-Badland complex, 9 to 70 percent slopesL3109F102222715932d353nd08719741:20000
Rhame-Fleak complex, 9 to 50 percent slopesL1425F852827159002qz6snd08719741:20000
Tusler-Fleak-Chinook complex, 9 to 15 percent slopesL1405D675527158992qxhnnd08719741:20000
Tusler-Fleak-Telfer, low precipitation loamy fine sands, 6 to 15 percent slopesL1857D152427159032qxhynd08719741:20000
Fleak-Rock outcrop-Tusler complex, 15 to 50 percent slopesL1475F527585302q2mqnd08719741:20000
Trey-Fleak loamy fine sands, 2 to 15 percent slopesTtC15654355801cy7gsd06319841:24000
Fleak-Trey-Rock outcrop complex, 15 to 50 percent slopesFtE6127355740cy5hsd06319841:24000
Tusler-Galedor-Fleak complex, 1 to 8 percent slopes -- draft8402182426119282qst1wy7231:24000

Map of Series Extent

Approximate geographic distribution of the FLEAK 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 .