Official Series Description


Lab Data Summary

Aggregate lab data for the LEVENGOOD soil series. This aggregation is based on all pedons with a current taxon name of LEVENGOOD, 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 LEVENGOOD 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 LEVENGOOD 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 LEVENGOOD 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 LEVENGOOD 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 LEVENGOOD 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 flats position figure.

Competing Series

Soil series competing with LEVENGOOD 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 LEVENGOOD series and competing. 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 LEVENGOOD 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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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.

Soil series sharing subgroup-level classification with LEVENGOOD, 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 LEVENGOOD 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
Benteen-Levengood-Maciver families, complex, moderately steep mountain slopes534C516202405325y61id75819981:24000
Levengood-Rooset-Whitore families, complex, landslide deposits706C45202407025y6lid75819981:24000
Tibson-Levengood families, complex, gentle mountain slopes526C27202404625y5tid75819981:24000
Levengood-Slagamelt-Houlihan families, complex, 2 to 15 percent slopes1112D9229952472qc01mt02719791:24000
Dutchhollow, occasionally flooded-Crookedrun-Levengood families, complex, 1 to 8 percent slopes1117C1429952412qbz3mt02719791:24000
Skaggs-Farlin, stony-Levengood complex, 8 to 25 percent slopes164E1953039571pd3qmt60219631:20000
Levengood-Maciver-Tetonville, occasionally flooded families, complex, 2 to 12 percent slopes1116D3330396822qbzymt60219631:20000
Levengood-Slagamelt-Houlihan families, complex, 2 to 15 percent slopes1112D2930396832qc01mt60219631:20000
Dutchhollow, occasionally flooded-Crookedrun-Levengood families, complex, 1 to 8 percent slopes1117C130396562qbz3mt60219631:20000
Hanson-Bridger-Levengood families, complex, eroded mountain tops906C80961487874ztlmt60520071:24000
Levengood-Rooset-Whitore families, complex, landslide deposits706C56831487704zt1mt60520071:24000
Benteen-Levengood-Maciver families, complex, moderately steep mountain slopes534C45951486454zp0mt60520071:24000
Adel-Levengood-Groomer families, complex, gentle mountain slopes524C39621486064zmrmt60520071:24000
Groomer-Levengood-Whitore families, complex, landslide deposits706T32751487724zt3mt60520071:24000
Tibson-Levengood families, complex, gentle mountain slopes526C27861486184zn4mt60520071:24000
Hardhart, very stony, Levengood, stony-Rock outcrop complex, 8 to 35 percent slopes904E181924038152lpcfmt60520071:24000
Maciver, very stony-Levengood complex, 20 to 50 percent slopes908F144826334642pp9hmt60520071:24000
Levengood-Benteen-Wetopa families, complex, valley bottoms646G105614931850cqmt60520071:24000
Hanson-Levengood-Elve families, complex, alluvial fans686E9531487494zscmt60520071:24000
Rockisland, stony-Levengood-Cheadle, very stony complex, 15 to 35 percent slopes914E41025980212ppbcmt60520071:24000
Tibson, stony-Levengood complex, 15 to 50 percent slopes185F34024038052lpc3mt60520071:24000
Philipsburg, extremely stony-Levengood, extremely stony-Tropal, rubbly complex, 8 to 45 percent slopes, landslides128F4326334342m78xmt60520071:24000
Hardhart, very stony, Levengood, stony-Rock outcrop complex, 8 to 35 percent slopes904E4792185995920ffpmt61220111:24000
Rockisland, stony-Levengood complex, 15 to 50 percent slopes185F284722203152djf2mt61220111:24000
Levengood, very stony-Raynesford, very stony-Tropal, extremely stony complex, 8 to 35 percent slopes410E175924251682mdl7mt61220111:24000
Philipsburg, extremely stony-Levengood, extremely stony-Tropal, rubbly complex, 8 to 45 percent slopes, landslides128F78624200742m78xmt61220111:24000
Maciver, very stony-Levengood complex, 20 to 50 percent slopes908F425976402pp9hmt61220111:24000
Levengood-Benteen-Wetopa families, complex, valley bottoms646G4259777250cqmt61220111:24000
Dutchhollow, occasionally flooded-Crookedrun-Levengood families, complex, 1 to 8 percent slopes1117C55430397062qbz3mt61319751:24000
Levengood-Jonescreek, occasionally flooded families, complex, 2 to 35 percent slopes, very stony1111E630397142r6ygmt61319751:24000
Maciver, very stony-Levengood complex, 20 to 50 percent slopes908F230424929562pp9hmt61420121:24000
Raynesford-Nikat-Levengood complex, 8 to 35 percent slopes954E222624866062pgj3mt61420121:24000
Ratiopeak-Tiban, very stony-Levengood complex, 2 to 8 percent slopes927C78225187142pp9ymt61420121:24000
Rockisland, stony-Levengood-Cheadle, very stony complex, 15 to 35 percent slopes914E58425187282ppbcmt61420121:24000
Rockisland, very bouldery-Levengood-Farlin, very stony complex, 4 to 15 percent slopes883D33225187382ppbmmt61420121:24000
Philipsburg, extremely stony-Levengood, extremely stony-Tropal, rubbly complex, 8 to 45 percent slopes, landslides128F8431628322m78xmt61420121:24000
Tibson-Levengood gravelly loams, 8 to 15 percent slopes176D37915461555wlmt61620031:24000
Tibson-Levengood gravelly loams, 35 to 60 percent slopes176F8415461755wnmt61620031:24000
Tibson-Levengood gravelly loams, 15 to 35 percent slopes176E37261442394v2wmt62119971:24000
Tibson-Levengood gravelly loams, 8 to 15 percent slopes176D7111442384v2vmt62119971:24000
Tibson-Levengood gravelly loams, 35 to 60 percent slopes176F831442404v2xmt62119971:24000
Tibson-Levengood gravelly loams, 4 to 8 percent slopes176C611442374v2tmt62119971:24000
Levengood-Raynesford complex, 8 to 35 percent slopes526E14824870202pgygmt62420211:24000
Levengood-Slagamelt-Houlihan families, complex, 2 to 15 percent slopes1112D10930940962qc01mt63019911:24000
Tiban-Hanson-Levengood families complex, low relief mountain slopes and ridges75CH37217035371v5ntmt63119881:24000
Findon, stony-Farlin, very stony-Levengood families, complex, 8 to 35 percent slopes, landslides2105E604626274322rf1smt6321:24000
Skaggs-Farlin, stony-Levengood complex, 8 to 25 percent slopes164E421223927802l9wgmt6321:24000
Levengood-Jonescreek, occasionally flooded families, complex, 2 to 35 percent slopes, very stony1111E304426044822r6ygmt6321:24000
Levengood-Maciver-Tetonville, occasionally flooded families, complex, 2 to 12 percent slopes1116D253826322672qbzymt6321:24000
Dutchhollow, occasionally flooded-Crookedrun-Levengood families, complex, 1 to 8 percent slopes1117C246625128822qbz3mt6321:24000
Farlin, stony-Levengood-Skaggs complex, 15 to 45 percent slopes364F175723928082l9xcmt6321:24000
Levengood-Slagamelt-Houlihan families, complex, 2 to 15 percent slopes1112D47526322702qc01mt6321:24000
Levengood-Poso families, complex, 0 to 15 percent slopes2150D3384035316l7mt6331:24000
Tiban-Hanson-Levengood families, complex, low relief mountain slopes and ridges75CH3175514951250kzmt63520061:24000
Levengood-Benteen-Wetopa families, complex, valley bottoms3053117101621vdkjmt63619831:24000
Farlin, stony-Levengood-Skaggs complex, 15 to 45 percent slopes364F5746637167pd0smt63720141:24000
Skaggs-Farlin, stony-Levengood complex, 8 to 25 percent slopes164E5020637258pd3qmt63720141:24000
Skaggs, very stony-Levengood complex, 35 to 60 percent slopes156F279324244042mcslmt63720141:24000
Levengood-Skaggs, very stony-Raynesford complex, 15 to 35 percent slopes156E244624259712mff4mt63720141:24000
Skaggs, very stony-Levengood, stony-Rock outcrop complex, 60 to 90 percent slopes156G164824244052mcsmmt63720141:24000
Farlin, stony-Roxal-Levengood complex, 8 to 35 percent slopes458E442780870v6kcmt63720141:24000
Dutchhollow, occasionally flooded-Crookedrun-Levengood families, complex, 1 to 8 percent slopes1117C2829796502qbz3mt63720141:24000
Dutchhollow, occasionally flooded-Crookedrun-Levengood families, complex, 1 to 8 percent slopes1117C99829952562qbz3mt66620081:24000
Levengood-Slagamelt-Houlihan families, complex, 2 to 15 percent slopes1112D6329952602qc01mt66620081:24000

Map of Series Extent

Approximate geographic distribution of the LEVENGOOD 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 .