Official Series Description


Lab Data Summary

Aggregate lab data for the KETTENBACH soil series. This aggregation is based on all pedons with a current taxon name of KETTENBACH, 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 KETTENBACH 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
43A82P04321982ID035002Kettenbach6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.4166889,-116.1772194
43A82P04351982ID057005Kettenbach6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.5661125,-116.7233353
43A82P04331982ID061003Kettenbach6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.4385167,-116.3887667
882P04341982ID069400Kettenbach6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.49545,-116.7235611

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the KETTENBACH 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 KETTENBACH 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 KETTENBACH 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 KETTENBACH 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 KETTENBACH 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 KETTENBACH 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 KETTENBACH 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 mountains figure.

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

Soil series sharing subgroup-level classification with KETTENBACH, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. ID-2010-08-30-12 | Lewis and Nez Perce Counties - 2004

    Typical pattern of soils in general soil map unit 11 (Soil Survey of Lewis and Nez Perce Counties, Idaho; 2004).

  2. ID-2010-08-30-18 | Lewis and Nez Perce Counties - 2004

    Idealized sequence of soils and vegetation types on north- and south-facing slopes of basalta canyonsides (Soil Survey of Lewis and Nez Perce Counties, Idaho; 2004).

Map Units

Map units containing KETTENBACH 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
Kettenbach-Gwin-Kettenbach, moist complex, 30 to 75 percent slopes5760367796702y6tpid61119941:24000
Linville-Kettenbach association, 45 to 75 percent slopes8123721796972nxwid61119941:24000
Kettenbach-Rock outcrop complex, 45 to 90 percent slopes595754796722nx2id61119941:24000
Kettenbach-Keuterville association, 35 to 75 percent slopes583172796712nx1id61119941:24000
Gwin-Kettenbach complex, very rocky, 35 to 75 percent slopes57j964679209qsrzid61119941:24000
Klickson-Rock outcrop-Kettenbach complex, 35 to 85 percent slopes67j35679210qss0id61119941:24000
Klickson-Rock outcrop-Kettenbach complex, 35 to 85 percent slopes1484296777314qss0id61220031:24000
Kettenbach-Keuterville association, 35 to 75 percent slopes14041457755902nx1id61220031:24000
Gwin-Kettenbach complex, 35 to 75 percent slopes1003593775589v120id61220031:24000
Kettenbach-Gwin-Rock outcrop complex, 45 to 75 percent slopes1392444777366v2xbid61220031:24000
Klickson-Kettenbach association, 35 to 90 percent slopes1471674777312v2vlid61220031:24000
Gwin-Kettenbach-Keuterville complex, 10 to 25 percent slopes101342777365v2x9id61220031:24000
Kettenbach-Gwin-Kettenbach, moist complex, 30 to 75 percent slopes2y6tp279630989052y6tpid61819651:24000
Lickskillet-Kettenbach-Rockly complex, 60 to 90 percent slopes4907DO277831203191qy0vor60720181:24000
Gwin-Klickson-Kettenbach complex, 60 to 90 percent slopes6121DO263531207952mtd0or60720181:24000
Gwin-Kettenbach-Rock outcrop complex, 60 to 90 percent south slopes6060DS19093120192nj36or60720181:24000
Gwin-Kettenbach-Rock outcrop complex, 30 to 60 percent south slopes6060CS283120191nj34or60720181:24000
Gwinly-Mallory-Kettenbach complex, 60 to 90 percent south slopes85F1966404524mzor62519791:20000
Gwinly-Mallory-Kettenbach complex, 30 to 60 percent south slopes85E1556404624n0or62519791:20000
Gwinly-Kettenbach-Rock outcrop complex, 60 to 90 percent south slopes86F406404724n1or62519791:20000
Gwinly-Mallory-Kettenbach complex, 15 to 30 percent south slopes85D186404324mxor62519791:20000
Gwin-Kettenbach-Rock outcrop complex, 60 to 90 percent south slopes84F26404224mwor62519791:20000
Gwinly-Kettenbach-Mallory complex, 60 to 90 percent south slopes5867DO97312437384nj3nor63120181:24000
Gwinly-Kettenbach-Mallory complex, 30 to 60 percent south slopes5867CO44432437383nj3lor63120181:24000
Gwin-Kettenbach-Rock outcrop complex, 60 to 90 percent south slopes6060DS8992437448nj36or63120181:24000
Gwin-Kettenbach-Rock outcrop complex, 30 to 60 percent south slopes6060CS3632437447nj34or63120181:24000
Gwinly-Kettenbach-Rock outcrop complex, 60 to 90 percent south slopes6078DS2572437458nj3bor63120181:24000
Gwinly-Kettenbach-Mallory complex, 15 to 30 percent south slopes5867BO2262437382nj3jor63120181:24000
Gwin-Klickson-Kettenbach complex, 60 to 90 percent slopes6121DO324374682mtd0or63120181:24000
Gwinly-Mallory-Kettenbach complex, 30 to 60 percent south slopes10117118844722twxor67019991:24000
Gwin-Kettenbach-Rock outcrop complex, 60 to 90 percent south slopes9515720848242v88or67019991:24000
Gwinly-Kettenbach-Rock outcrop complex, 60 to 90 percent south slopes979473848262v8bor67019991:24000
Gwin-Kettenbach-Rock outcrop complex, 30 to 60 percent south slopes948151848232v87or67019991:24000
Gwinly-Mallory-Kettenbach complex, 60 to 90 percent south slopes1026394844732twyor67019991:24000
Gwinly-Mallory-Kettenbach complex, 15 to 30 percent south slopes1002502844712twwor67019991:24000
Gwin-Klickson-Kettenbach association, 60 to 90 percent slopes96459848252v89or67019991:24000
Gwin-Klickson-Kettenbach complex, 60 to 90 percent slopes6121DO25531225712ygdxwa60319841:24000
Gwin-Klickson-Kettenbach complex, 60 to 90 percent slopes6121DO207231145052ygdxwa71420181:24000

Map of Series Extent

Approximate geographic distribution of the KETTENBACH 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 .