Official Series Description


Lab Data Summary

Aggregate lab data for the INKLER soil series. This aggregation is based on all pedons with a current taxon name of INKLER, 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 INKLER 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 INKLER 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 INKLER 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 INKLER 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 INKLER 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 INKLER 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 INKLER 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 INKLER 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 terrace figure.

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

Soil series sharing subgroup-level classification with INKLER, 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 INKLER 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
Inkler very gravelly loam, 50 to 70 percent north slopes83F58266227222ssor60419881:24000
Inkler very gravelly loam, 35 to 50 percent north slopes83E48756227122sror60419881:24000
Inkler very gravelly loam, 2 to 35 percent north slopes83D30206227022sqor60419881:24000
Antelopepeak-Inkler complex, 15 to 30 percent slopes0829BO32325938502mswror60419881:24000
Inkler-Twocolor complex, 15 to 30 percent slopes0803BS24425938441qs60or60419881:24000
Antelopepeak-Inkler complex, 0 to 15 percent slopes0829AO19025938491qydfor60419881:24000
Bigelk-Inkler-Twocolor complex, 60 to 90 percent south slopes0807DS15425938451qyb6or60419881:24000
Inkler-Twocolor complex, 30 to 60 percent south slopes0803CS25231202751qcr9or60720181:24000
Inkler-Twocolor complex, 15 to 30 percent slopes0803BS2431202941qs60or60720181:24000
Inkler-Twocolor complex, 30 to 60 percent south slopes0803CS144931221251qcr9or62620181:24000
Inkler-Twocolor complex, 15 to 30 percent slopes0803BS87831221361qs60or62620181:24000
Bigelk-Inkler-Twocolor complex, 60 to 90 percent south slopes0807DS13133852641qyb6or62620181:24000
Bigelk-Inkler complex, 0 to 15 percent slopes0805AO731220981q6sgor62620181:24000
Inkler-Twocolor complex, 30 to 60 percent south slopes0803CS221424369721qcr9or63120181:24000
Inkler-Twocolor complex, 15 to 30 percent slopes0803BS194324369711qs60or63120181:24000
Antelopepeak-Inkler complex, 0 to 15 percent slopes0829AO174124369941qydfor63120181:24000
Bigelk-Inkler-Twocolor complex, 60 to 90 percent south slopes0807DS150024369741qyb6or63120181:24000
Antelopepeak-Inkler complex, 15 to 30 percent slopes0829BO53524369952mswror63120181:24000
Bigelk-Inkler complex, 0 to 15 percent slopes0805AO42224369731q6sgor63120181:24000
Inkler-Rock outcrop complex, 40 to 65 percent slopes11489881580732v740wa06519781:24000
Inkler-Rock outcrop complex, 5 to 40 percent slopes11358661580722v73zwa06519781:24000
Rock outcrop-Inkler complex, 30 to 65 percent slopes192158415815959kxwa06519781:24000
Inkler gravelly ashy silt loam, 40 to 65 percent slopes11212511580712v743wa06519781:24000
Inkler gravelly ashy silt loam, 20 to 40 percent slopes11110571580702v73ywa06519781:24000
Inkler silt loam, 0 to 20 percent slopes11098715806959h0wa06519781:24000
Inkler stony fine sandy loam, 30 to 60 percent slopes142908467440285hwa60819951:24000
Kloochman-Inkler-Rock outcrop association, 45 to 75 percent slopes*156767674632867wa60819951:24000
Kloochman-Inkler association, 30 to 60 percent slopes*155210674622866wa60819951:24000
Tillmont-Inkler association, 30 to 60 percent slopes*3241606789228n2wa60819951:24000
Inkler gravelly ashy silt loam, dry, 20 to 40 percentInE5766700912v741wa61919681:24000
Inkler gravelly ashy silt loam, dry, 40 to 65 percentInF2259700922v742wa61919681:24000
Inkler-Rock land complex, 15 to 50 percent slopesIrE2248700932by2wa61919681:24000
Inkler gravelly ashy silt loam, dry, 20 to 40 percent22311665703492v741wa64819871:24000
Inkler gravelly ashy silt loam, dry, 40 to 65 percent2246905703502v742wa64819871:24000
Inkler, dry-Rock outcrop complex, 20 to 40 percent slopes2276718703532c6gwa64819871:24000
Inkler, dry-Baldknob-Rock outcrop complex, 5 to 30 percent slopes2255047703512c6dwa64819871:24000
Inkler gravelly silt loam, dry, 5 to 20 percent slopes2224720703482c69wa64819871:24000
Inkler, dry-Baldknob-Rock outcrop complex, 30 to 65 percent slopes2264182703522c6fwa64819871:24000
Inkler, dry-Rock outcrop complex, 40 to 65 percent slopes2283983703542c6hwa64819871:24000
Inkler-Rock outcrop complex, 40 to 65 percent slopes5980081584222v740wa65119811:24000
Inkler-Rock outcrop complex, 5 to 40 percent slopes5832861584212v73zwa65119811:24000
Inkler gravelly ashy silt loam, 20 to 40 percent slopes5632131584192v73ywa65119811:24000
Inkler gravelly ashy silt loam, 40 to 65 percent slopes5719011584202v743wa65119811:24000
Inkler gravelly silt loam, 0 to 20 percent slopes55138815841859v8wa65119811:24000
Inkler gravelly ashy silt loam, 15 to 35 percent slopes18311612981nkvlwa74920051:24000

Map of Series Extent

Approximate geographic distribution of the INKLER 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 .