Official Series Description


Lab Data Summary

Aggregate lab data for the KINGBOLT soil series. This aggregation is based on all pedons with a current taxon name of KINGBOLT, 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 KINGBOLT 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
43C91P032590OR001102Kingbolt6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.7866669,-118.2019424
43C97P0542S1997OR023003Kingbolt6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.585556,-118.7052765

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the KINGBOLT 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 KINGBOLT 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 KINGBOLT 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 KINGBOLT 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 terrace figure.

There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with KINGBOLT 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 KINGBOLT 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 KINGBOLT 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.

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 KINGBOLT, 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 KINGBOLT 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
Analulu-Vogel-Kingbolt complex, 15 to 30 percent south slopes7712BS123624978291sgd1or60419881:24000
Gutridge-McWillar-Kingbolt complex, 30 to 60 percent slopes7804CO1181531206691sghpor60720181:24000
Analulu-McWillar-Kingbolt complex, 30 to 60 percent slopes1309CO1035731206982pf8zor60720181:24000
Kingbolt-McWillar complex, 15 to 30 percent slopes1342BO678031203901qzf9or60720181:24000
Kingbolt-Analulu-Gutridge complex, 0 to 30 percent slopes7803NO505131206681sghnor60720181:24000
Kingbolt-Threecent complex, 0 to 15 percent slopes1335AO475431203871qzf5or60720181:24000
McWillar-Kingbolt complex, 15 to 30 percent slopes7793BO312731206611sghcor60720181:24000
Gutridge-Threecent-Kingbolt complex, sandstone substratum, 30 to 60 percent slopes2009CO299631203221qy10or60720181:24000
Kingbolt-Threecent complex, sandstone substratum, 15 to 30 percent slopes2006BO206731203351qy6zor60720181:24000
McWillar-Kingbolt complex, sandstone substratum, 15 to 30 percent slopes2005BO199131204191r00gor60720181:24000
Kingbolt-Analulu complex, 30 to 60 percent slopes1344CO194931203921qzfcor60720181:24000
McWillar-Kingbolt complex, 30 to 60 percent slopes7793CO128531206621sghfor60720181:24000
Kingbolt-McWillar complex, 0 to 15 percent slopes7792AO96431206601sghbor60720181:24000
Kingbolt-Analulu-McWillar complex, sandstone substratum, 30 to 60 percent slope2004CO96331204171r00dor60720181:24000
McWillar-Kingbolt complex, sandstone substratum, 30 to 60 percent slopes2005CO83031204201r00hor60720181:24000
Kingbolt-Analulu-McWillar complex, 30 to 60 percent slopes1341CO67731203891qzf8or60720181:24000
McWillar-Kingbolt complex, without serpentine, 0 to 15 percent slopes7554AO40631206171sgbxor60720181:24000
McWillar-Kingbolt complex, sandstone substratum, 0 to 15 percent slopes2005AO32231204181r00for60720181:24000
Kingbolt-Threecent complex, sandstone substratum, 0 to 15 percent slopes2006AO30131204211r00jor60720181:24000
Kingbolt-Lemoncreek complex, 0 to 15 percent slopes7360AO20231206111sgbgor60720181:24000
Gutridge-McWillar-Kingbolt complex, 0 to 30 percent slopes7804NO16931207871v6m7or60720181:24000
Vogel-Kingbolt complex, 15 to 30 percent slopes7757BO14731206441sgfnor60720181:24000
Analulu-Vogel-Kingbolt complex, 15 to 30 percent south slopes7712BS14031206281sgd1or60720181:24000
Blackgulch-Kingbolt complex, 0 to 15 percent slopes7329AO4031206041sg9por60720181:24000
Slaughterhouse-Kingbolt-Lemoncreek complex, 30 to 60 percent slopes7326CO3231206021sg9mor60720181:24000
Kingbolt-Slaughterhouse-Blackgulch complex, 15 to 30 percent slopes7324BO1731206011sg9kor60720181:24000
Analulu-Kingbolt complex, 15 to 30 percent slopes7749BO1731206422pgtcor60720181:24000
Kingbolt-Slaughterhouse-Blackgulch complex, 15 to 30 percent slopes7324BO257531223881sg9kor62620181:24000
Vogel-Kingbolt complex, 15 to 30 percent slopes7757BO105331224281sgfnor62620181:24000
Analulu-Kingbolt complex, 15 to 30 percent slopes7749BO46831224232pgtcor62620181:24000
Slaughterhouse-Kingbolt-Lemoncreek complex, 30 to 60 percent slopes7326CO32731223901sg9mor62620181:24000
Lemoncreek-Kingbolt-Rock outcrop complex, 15 to 30 percent slopes7302BO26531223771sg8yor62620181:24000
Vogel-Kingbolt complex, 0 to 15 percent slopes7757AO21131224271sgfmor62620181:24000
Gutridge-McWillar-Kingbolt complex, frost basin, 0 to 30 percent slopes7804NF18633854582tz1hor62620181:24000
Analulu-Kingbolt complex, 0 to 15 percent slopes7749AO16131225162pgtbor62620181:24000
Kingbolt-McWillar complex, 0 to 15 percent slopes7792AO11531224391sghbor62620181:24000
Uptmor-Payraise-Kingbolt complex, 30 to 60 percent slopes7344CO10631221181q70wor62620181:24000
Blackgulch-Kingbolt complex, 0 to 15 percent slopes7329AO6631223921sg9por62620181:24000
McWillar-Kingbolt complex, 15 to 30 percent slopes7793BO4233854561sghcor62620181:24000
Kingbolt-Lemoncreek complex, 0 to 15 percent slopes7360AO2931224021sgbgor62620181:24000
Analulu-McWillar-Kingbolt complex, 30 to 60 percent slopes1309CO431224652pf8zor62620181:24000
Analulu-Vogel-Kingbolt complex, 15 to 30 percent south slopes7712BS1123524374781sgd1or63120181:24000
Analulu-McWillar-Kingbolt complex, 30 to 60 percent slopes1309CO93424854242pf8zor63120181:24000
McWillar-Kingbolt complex, 15 to 30 percent slopes7793BO67624869021sghcor63120181:24000
Kingbolt-Threecent complex, 0 to 15 percent slopes1335AO36124861871qzf5or63120181:24000
Kingbolt-Hondu complex, 0 to 15 percent slopes7733AO26624374901sgdwor63120181:24000
Kingbolt-McWillar complex, 15 to 30 percent slopes1342BO10524861891qzf9or63120181:24000
Vogel-Kingbolt complex, 0 to 15 percent slopes7757AO4131225401sgfmor63120181:24000
Analulu-Kingbolt complex, 15 to 30 percent slopes7749BO2324868932pgtcor63120181:24000
Uptmor-Payraise-Kingbolt complex, 30 to 60 percent slopes7344CO1824868761q70wor63120181:24000
Analulu-Kingbolt complex, 0 to 15 percent slopes7749AO1424868922pgtbor63120181:24000
Gutridge-Threecent-Kingbolt complex, sandstone substratum, 30 to 60 percent slopes2009CO89031215061qy10or64819771:24000
McWillar-Kingbolt complex, sandstone substratum, 15 to 30 percent slopes2005BO31831215171r00gor64819771:24000
Kingbolt-Threecent complex, sandstone substratum, 15 to 30 percent slopes2006BO21631215081qy6zor64819771:24000
McWillar-Kingbolt complex, sandstone substratum, 30 to 60 percent slopes2005CO9031215181r00hor64819771:24000
Kingbolt-Analulu-McWillar complex, sandstone substratum, 30 to 60 percent slope2004CO5331215161r00dor64819771:24000
Analulu-McWillar-Kingbolt complex, 30 to 60 percent slopes1309CO16031214802pf8zor66719841:20000
Kingbolt-Analulu complex, 30 to 60 percent slopes1344CO10931214571qzfcor66719841:20000

Map of Series Extent

Approximate geographic distribution of the KINGBOLT 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 .