Official Series Description


Lab Data Summary

Aggregate lab data for the KINGMINE soil series. This aggregation is based on all pedons with a current taxon name of KINGMINE, 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 KINGMINE 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 KINGMINE 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 KINGMINE 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 KINGMINE 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 KINGMINE 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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Competing Series

Soil series competing with KINGMINE 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 KINGMINE 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 KINGMINE 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 KINGMINE, 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 KINGMINE 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
Kingmine-Gralic families, complex, 40 to 65 percent slopes9766131732802wv33id71220081:24000
Kingmine family, stony surface-Zeebar family-Rubble land complex, 40 to 70 percent slopes9883931732822wv3mid71220081:24000
Toze, stony surface-Kingmine, stony surface-Spearhead families, complex 25 to 65 percent slopes9673131732862wxbnid71220081:24000
Gralic-Kingmine families, complex, 15 to 40 percent slopes993631732812wv3jid71220081:24000
Gralic, very stony surface-Kingmine-Sponsor families, complex, 25 to 55 percent slopes8741994727334862slsdid7131:24000
Kingmine family, 30 to 55 percent slopes922751027335062slt2id7131:24000
Davtone-Kingmine families, complex, 30 to 65 percent slopes915705727335002slswid7131:24000
Kingmine family-Jumpstart-Dranburn complex, 15 to 40 percent slopes949632929638542wv1xid7131:24000
Kingmine family-Ezbin-Stringam complex, 25 to 65 percent slopes955622429638562wv1zid7131:24000
Mayhill-Kingmine family, complex, 5 to 35 percent slopes923604827335072slt3id7131:24000
Nieman-Kingmine-Groomer families, complex, 5 to 35 percent slopes881404327334932slsmid7131:24000
Kingmine-Kingmine, low effective precipitation families, complex, 30 to 70 percent slopes927361527335112slt7id7131:24000
Kingmine family, stony surface-Woodhurst family-Stringam, stony surface, complex, 30 to 65 percent slopes963349629682352wxbjid7131:24000
Pavohroo-Kingmine family, stony surface-Sparky, stony surface, complex, 15 to 45 percent slopes965333729682342wxbgid7131:24000
Kingmine-Kingmine, moderately deep, families, complex, 15 to 35 percent slopes918328227335032slszid7131:24000
Mikesell-Kingmine family, very stony surface, complex, 5 to 40 percent slopes970302529682412wxbrid7131:24000
Kingmine family-Ercan family-Moonlight complex, 20 to 45 percent slopes971254429682492wxbsid7131:24000
Tigeron-Kingmine families, complex, 35 to 70 percent slopes890213329841642x03jid7131:24000
Toze, stony surface-Kingmine, stony surface-Spearhead families, complex 25 to 65 percent slopes967194129682392wxbnid7131:24000
Moonlight-Kingmine family-Stringam complex, 25 to 70 percent slopes991190629638732wv2zid7131:24000
Kingmine-Gralic families, complex, 40 to 65 percent slopes976181529638772wv33id7131:24000
Ercan-Kingmine families, complex, 5 to 25 percent slopes917178227335022slsyid7131:24000
Kingmine family-Dranburn complex, 50 to 75 percent slopes903177529638712wv2wid7131:24000
Kingmine family-Daisypeak-Cavemountain complex, 25 to 65 percent slopes2011176529808722x013id7131:24000
Kingmine family-Stringam complex, 20 to 60 percent slopes2018165429808792x01bid7131:24000
Stringam-Jumpstart-Kingmine family, complex, 15 to 50 percent slopes2004138029808662x00xid7131:24000
Kingmine family-Dranyon-Starley family, complex, 45 to 75 percent slopes986117229638872wv3gid7131:24000
Kingmine family, stony surface-Zeebar family-Rubble land complex, 40 to 70 percent slopes988110029638912wv3mid7131:24000
Kingmine family-Hagenbarth-Trapper family, complex, 20 to 55 percent slopes887108829841602x03did7131:24000
Wayan-Kingmine family-Groomer family, complex, 15 to 45 percent slopes201263229808732x014id7131:24000
Ericson-Kingmine-Sambrito families, complex, 5 to 30 percent slopes95851929638632wv2jid7131:24000
Gralic-Kingmine families, complex, 15 to 40 percent slopes99329429638892wv3jid7131:24000
Trapper-Kingmine families, 5 to 20 percent slopes88627829841672x03mid7131:24000
Gralic, very stony surface-Kingmine-Sponsor families, complex, 25 to 55 percent slopes874121931634452slsdid7161:24000
Mayhill-Kingmine family, complex, 5 to 35 percent slopes923102031634702slt3id7161:24000
Davtone-Kingmine families, complex, 30 to 65 percent slopes91580731634662slswid7161:24000
Kingmine family, 30 to 55 percent slopes92244231634692slt2id7161:24000
Kingmine-Kingmine, moderately deep, families, complex, 15 to 35 percent slopes91831331733962slszid7161:24000
Kingmine family-Dranburn complex, 50 to 75 percent slopes90315631634782wv2wid7161:24000
Kingmine-Kingmine, low effective precipitation families, complex, 30 to 70 percent slopes927031634742slt7id7161:24000
Kingmine-Bumper-Longridge complex, 15 to 70 percent slopesANF215769629586402wrfzut0131:24000
Kingmine, extremely stony-Banjo association, 20 to 60 percent slopesDNG622614804811lpkgut0131:24000
Kingmine-Northorn-Angostura complex, 30 to 80 percent slopes081192116505481sdjhut62320111:24000
Frisco, extremely stony-Kingmine-Trout Creek families association, 8 to 45 percent slopes488281724042942lpvwut6471:24000
Kingmine family-Hagenbarth-Trapper family, complex, 20 to 55 percent slopes88725330834752x03dwy62319711:20000
Gralic, very stony surface-Kingmine-Sponsor families, complex, 25 to 55 percent slopes87423030834642slsdwy62319711:20000
Trapper-Kingmine families, 5 to 20 percent slopes88617030834782x03mwy62319711:20000
Kingmine family-Ezbin-Stringam complex, 25 to 65 percent slopes9559430834852wv1zwy62319711:20000
Kingmine-Kingmine, moderately deep, families, complex, 15 to 35 percent slopes9185330834722slszwy62319711:20000
Mayhill-Kingmine family, complex, 5 to 35 percent slopes9234430834742slt3wy62319711:20000
Kingmine family, 30 to 55 percent slopes9221830834732slt2wy62319711:20000
Nieman-Kingmine-Groomer families, complex, 5 to 35 percent slopes8811430834672slsmwy62319711:20000
Davtone-Kingmine families, complex, 30 to 65 percent slopes915430834712slswwy62319711:20000
Sedimentary Till-Mantled Sideslopes (West), Subalpine Fir Complex364877761518735314wy66219981:24000
Sedimentary Sideslopes, Tall Forb-Subalpine Fir Complex365724511518785319wy66219981:24000
Storm family-Kingmine family-Rubble land complex, 40 to 90 percent slopes3564003152018535twy66320121:24000
Needleton-Kingmine-Cluff families, complex, 10 to 40 percent slopes3232429152003535bwy66320121:24000
Kingmine family-Ezbin-Stringam complex, 25 to 65 percent slopes9557930834552wv1zwy66320121:24000

Map of Series Extent

Approximate geographic distribution of the KINGMINE 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 .