Official Series Description


Lab Data Summary

Aggregate lab data for the KINNEY soil series. This aggregation is based on all pedons with a current taxon name of KINNEY, 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 KINNEY 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
340A0925S1960OR047001KINNEY4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.830555,-122.6136093
340A0926S1960OR047002Kinney4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.834446,-122.644165
311N0317S2010OR043001kinney7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.5566673,-122.5419464

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the KINNEY 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 KINNEY 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 KINNEY 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 KINNEY 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 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.

Competing Series

Soil series competing with KINNEY 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 KINNEY 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 KINNEY 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.

Click the image to view it full size.

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 KINNEY, 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 KINNEY 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
Klickitat-Kinney complex, 5 to 30 percent slopes52D1371161674225hor61019821:20000
Kinney cobbly loam, 3 to 20 percent slopes47C11579616632254or61019821:20000
Kinney cobbly loam, 20 to 50 percent slopes47E1888616642255or61019821:20000
Kinney cobbly loam, slump, 3 to 30 percent slopes69E1428262726238for63719811:20000
Kinney cobbly loam, 50 to 70 percent north slopes67G1396362723238bor63719811:20000
Kinney cobbly loam, 20 to 50 percent south slopes68F1152762724238cor63719811:20000
Kinney cobbly loam, 20 to 50 percent north slopes67F7756627222389or63719811:20000
Kinney cobbly loam, 50 to 70 percent south slopes68G699962725238dor63719811:20000
Kinney cobbly loam, 3 to 20 percent slopes66D6082627212388or63719811:20000
Dutchoven-Kinney complex, 45 to 90 percent slopes, south-facing33171273734394662xptmor63719811:20000
Dutchoven-Kinney complex, 45 to 90 percent slopes33172172134394652xptlor63719811:20000
Kinney, moist-Mooseridge complex, 0 to 30 percent slopes33271122634394722xpt2or63719811:20000
Kinney-Westfir-Dutchoven complex, 45 to 90 percent slopes, south-facing3517176734394862z4rbor63719811:20000
Kinney gravelly loam, 30 to 55 percent slopes3517358834394852z4r7or63719811:20000
Kinney gravelly loam, 2 to 30 percent slopes3377157534394842z9pcor63719811:20000
Kinney-Dutchoven, moist-Westfir, moist complex, 45 to 90 percent slopes3517243834394822z4rcor63719811:20000
Kinney-Mooseridge complex, low precipitation, 0 to 30 percent slopes41271381343949130k8jor63719811:20000
Kinney-Klickitat complex, 50 to 70 percent south slopes59G106556434624ypor63919831:20000
Kinney cobbly loam, 20 to 50 percent north slopes55F97956433824yfor63919831:20000
Kinney cobbly loam, 50 to 70 percent north slopes55G95856433924ygor63919831:20000
Kinney cobbly loam, 20 to 50 percent south slopes56F92006434024yhor63919831:20000
Kinney cobbly loam, 3 to 20 percent slopes54D86306433724ydor63919831:20000
Kinney-Klickitat complex, 50 to 70 percent north slopes58G68856434424ymor63919831:20000
Kinney cobbly loam, 50 to 70 percent south slopes56G30056434124yjor63919831:20000
Kinney cobbly loam, slump, 3 to 30 percent slopes57E23006434224ykor63919831:20000
Kinney-Klickitat complex, 20 to 50 percent north slopes58F17956434324ylor63919831:20000
Kinney-Klickitat complex, 20 to 50 percent south slopes59F16906434524ynor63919831:20000
Kinney-Westfir-Dutchoven complex, 45 to 90 percent slopes, south-facing35171155334395242z4rbor63919831:20000
Kinney, moist-Mooseridge complex, 0 to 30 percent slopes3327199734395232xpt2or63919831:20000
Kinney-Dutchoven, moist-Westfir, moist complex, 45 to 90 percent slopes3517283134395182z4rcor63919831:20000
Dutchoven-Kinney complex, 45 to 90 percent slopes3317252134395072xptlor63919831:20000
Dutchoven-Kinney complex, 45 to 90 percent slopes, south-facing3317136834395082xptmor63919831:20000
Kinney gravelly loam, 30 to 55 percent slopes3517318234395222z4r7or63919831:20000
Kinney gravelly loam, 2 to 30 percent slopes337711434395212z9pcor63919831:20000
Kinney cobbly loam, 20 to 50 percent slopesKCF231606411024q2or64319661:20000
Kinney cobbly loam, 2 to 20 percent slopesKCD124886410924q1or64319661:20000
Kinney cobbly loam, 50 to 70 percent slopesKCG26486411124q3or64319661:20000
Dutchoven-Kinney complex, 45 to 90 percent slopes3317227834395362xptlor64319661:20000
Klickitat-Kinney complex, 30 to 60 percent slopes126F24817663162707or64919941:24000
Kinney-Klickitat complex, 3 to 30 percent slopes122E28516629426zjor64919941:24000
Kinney-Mooseridge complex, low precipitation, 0 to 30 percent slopes4127135562338561630k8jor6571:24000
Dutchoven-Kinney complex, 45 to 90 percent slopes, south-facing331713490033854822xptmor6571:24000
Dutchoven-Kinney complex, 45 to 90 percent slopes331723187233854812xptlor6571:24000
Kinney-Dutchoven, moist-Westfir, moist complex, 45 to 90 percent slopes351722336733854972z4rcor6571:24000
Kinney, moist-Mooseridge complex, 0 to 30 percent slopes332712221133855102xpt2or6571:24000
Kinney-Westfir-Dutchoven complex, 45 to 90 percent slopes, south-facing351712182633855122z4rbor6571:24000
Kinney gravelly loam, 30 to 55 percent slopes351731733333855092z4r7or6571:24000
Kinney gravelly loam, 2 to 30 percent slopes33771619433855082z9pcor6571:24000
Kinney silt loam, 30 to 50 percent slopesKeF12690720152dy2wa01119721:20000
Kinney silt loam, 15 to 30 percent slopesKeE5780720142dy1wa01119721:20000
Kinney silt loam, 3 to 15 percent slopesKeC3470720132dy0wa01119721:20000
Kinney cobbly silt loam, 30 to 60 percent slopesKnF2270720162dy3wa01119721:20000
Kinney loam, 30 to 65 percent slopes58833513855811hht5wa65919871:24000
Kinney loam, 5 to 30 percent slopes57223013855801hht4wa65919871:24000
Kinney loam, 30 to 65 percent east slopes59129013855821hht6wa65919871:24000

Map of Series Extent

Approximate geographic distribution of the KINNEY 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 .