Official Series Description


Lab Data Summary

Aggregate lab data for the KILGORE soil series. This aggregation is based on all pedons with a current taxon name of KILGORE, 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 KILGORE 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 KILGORE 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 KILGORE 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 KILGORE 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 KILGORE 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 KILGORE 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 KILGORE 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 KILGORE 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 KILGORE, 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 KILGORE 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
Handran-Kilgore, frequently flooded families complex, 2 to 30 percent slopes5F2233500961jt91co6341:24000
Kilgore silt loam, 1 to 5 percent slopesAG692514150941jhj6co6541:24000
Kilgore silt loam693307498012jq6xco65519841:24000
Kilgore loam, 1 to 3 percent slopes63352496907jp28co68419841:24000
Idmonton-Kilgore-Alex complex, 0 to 4 percent slopes1312054428093652pxf8id75819981:24000
Alex-Fourme-Kilgore complex, 0 to 4 percent slopes1312133928093662pxfcid75819981:24000
Idmonton-Kilgore-Alex complex, 0 to 4 percent slopes131201355524976822pxf8id76120181:24000
Alex-Fourme-Kilgore complex, 0 to 4 percent slopes13121836424976852pxfcid76120181:24000
Alex-Kilgore complex, 0 to 4 percent slopes1312648324976942pxfpid76120181:24000
Foxgulch, rarely flooded-Kilgore, occasionally flooded complex, 0 to 4 percent slopes, very stony936B30185973720f6jmt60520071:24000
Kilgore-Mooseflat complex, 0 to 2 percent slopes914A13185958920f1rmt60520071:24000
Kilgore-Mooseflat complex, 0 to 2 percent slopes914A54415303341ncfmmt61020051:24000
Kilgore-Mooseflat-Water complex, 0 to 2 percent slopes414A23115312091ndbvmt61020051:24000
Kilgore-Foolhen-Mooseflat complex, 0 to 2 percent slopes314A87715469555z5mt61620031:24000
Kilgore-Mooseflat complex, 0 to 2 percent slopes914A58615514456fnmt61620031:24000
Kilgore-Foolhen-Mooseflat complex, 0 to 2 percent slopes, moderately impacted1314A397612104njy9mt61620031:24000
Kilgore-Foolhen-Philipsburg complex, 2 to 12 percent slopes597C2517031961v59tmt63520061:24000
Kilgore-Danielvil complex, 2 to 8 percent slopes28C2317031221v57fmt63520061:24000
Kilgore-Foxgulch complex, 0 to 4 percent slopes612A1517031971v59vmt63520061:24000
Kilgore, occasionally flooded-Danielvil complex, 1 to 4 percent slopes2509216975041tzd6mt63619831:24000
Kilgore-Foxgulch complex, 0 to 4 percent slopes2514616975051tzd7mt63619831:24000
Foolhen-Kilgore complex, 0 to 4 percent slopes175B104014246701jth3mt67020071:24000
Work, stony-Adel-Kilgore, rarely flooded complex, 2 to 15 percent slopes25D872320259br7ymt67020071:24000
Kilgore, occasionally flooded-Foolhen, rarely flooded-Philipsburg complex, 2 to 12 percent slopes21C626320247br7kmt67020071:24000
Kilgore-Foolhen-Philipsburg complex, 2 to 12 percent slopes597C59414247561jtkwmt67020071:24000
Nissler-Kilgore-Pappascreek, very stony complex, 2 to 15 percent slopes601D59314247541jtktmt67020071:24000
Kilgore, frequently flooded-Foxgulch, rarely flooded complex, 0 to 4 percent slopes612A59214247471jtklmt67020071:24000
Kilgore-Foolhen-Monaberg complex, 0 to 4 percent slopes166B56214246791jthdmt67020071:24000
Kilgore, rarely flooded-Mooseflat, occasionally flooded-Philipsburg complex, 0 to 6 percent slopes24B460320241br7cmt67020071:24000
Kilgore-Danielvil complex, 2 to 8 percent slopes28C384320249br7mmt67020071:24000
Foxgulch, rarely flooded-Kilgore, occasionally flooded complex, 0 to 4 percent slopes, very stony936B32514248371jtnhmt67020071:24000
Philipsburg-Monaberg-Kilgore, occasionally flooded complex, 0 to 15 percent slopes82D19714246461jtgbmt67020071:24000
Kilgore, occasionally flooded-Danielvil complex, 1 to 4 percent slopes32B184320245br7hmt67020071:24000
Mooseflat, occasionally flooded-Bridger-Kilgore, rarely flooded complex, 0 to 8 percent slopes26C150320248br7lmt67020071:24000
Foolhen-Monaberg-Kilgore, occasionally flooded complex, 0 to 6 percent slopes47B11514246221jtfkmt67020071:24000
Dranburn-Kilgore complex, 2 to 40 percent slopes625467325314422qmg9wy6301:24000
Foolhen-Kilgore-Toddhole, extremely bouldery complex, 1 to 4 percent slopes1204305016859801tldgwy6351:24000
Foolhen-Kilgore-Toddhole, extremely bouldery complex, 1 to 4 percent slopes12049225143911tldgwy66219981:24000

Map of Series Extent

Approximate geographic distribution of the KILGORE 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 .