Official Series Description


Lab Data Summary

Aggregate lab data for the KECKO soil series. This aggregation is based on all pedons with a current taxon name of KECKO, 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 KECKO 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
n/a90P002089ID063010Kecko5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

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

Competing Series

Soil series competing with KECKO 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 KECKO 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 KECKO 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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Click the image to view it full size.

Soil series sharing subgroup-level classification with KECKO, 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-2010-08-31-13 | Wood River Area, Gooding County and Parts of Blaine, Lincoln, and Minidoka Counties - 2005

    Typical pattern of soils and underlying material in general soil map unit 10 (Soil Survey of Wood River Area, Idaho; 2005).

Map Units

Map units containing KECKO 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
Vining-Kecko-Rock outcrop complex, 2 to 12 percent slopes20674448819442r8cid68119931:24000
Jestrick-Kecko-Rock outcrop complex, 2 to 12 percent slopes9224950821472rgxid68119931:24000
Vining-Kecko-Starbuck complex, 2 to 12 percent slopes20715360819452r8did68119931:24000
Quincy-Kecko complex, 1 to 4 percent slopes1552095818872r6jid68119931:24000
Kecko fine sandy loam, 2 to 4 percent slopes971810821522rh2id68119931:24000
Kecko fine sandy loam, 0 to 2 percent slopes961765821512rh1id68119931:24000
Kecko-Snowmore complex, 2 to 20 percent slopes1001520818262r4kid68119931:24000
Kecko-Vining-Rock outcrop complex, 2 to 15 percent slopes1011515818272r4lid68119931:24000
Jestrick-Starbuck-Kecko complex, 1 to 6 percent slopes93970821482rgyid68119931:24000
Kecko loamy fine sand, 1 to 4 percent slopes94945821492rgzid68119931:24000
Jestrick-Kecko complex, 2 to 8 percent slopes91890821462rgwid68119931:24000
Ackelton-Kecko complex, 1 to 5 percent slopes4700820082rbfid68119931:24000
Kecko loamy fine sand, 4 to 8 percent slopes95670821502rh0id68119931:24000
Kecko fine sandy loam, 4 to 8 percent slopes98415821532rh3id68119931:24000
Kecko fine sandy loam, hardpan substratum, 2 to 4 percent slopes99400821542rh4id68119931:24000
Taunton-Kecko complex, 1 to 4 percent slopes190355819262r7sid68119931:24000
Vining-Kecko-Rock outcrop complex, 1 to 8 percent slopes4616284801032pbzid70219991:24000
Kecko fine sandy loam, 1 to 4 percent slopes172813800742pb1id70219991:24000
Kecko fine sandy loam, 1 to 4 percent slopes588788802642pj5id70419921:24000
Kecko-Emberton complex, 1 to 6 percent slopes605429802672pj8id70419921:24000
Quincy-Kecko complex, 1 to 6 percent slopes974142803072pkkid70419921:24000
Jestrick-Kecko complex, 1 to 8 percent slopes563529802622pj3id70419921:24000
Kecko fine sandy loam, 4 to 8 percent slopes591192802652pj6id70419921:24000
Kecko-Escalante complex, 2 to 4 percent slopes255625825992ryhid70919761:24000
Kecko-Clems-Vining association, undulating243085825982rygid70919761:24000
Kecko-Escalante complex, 8 to 12 percent slopes271483826012rykid70919761:24000
Kecko-Escalante complex, 4 to 8 percent slopes26838826002ryjid70919761:24000
Vining-Kecko-Rock outcrop complex, 2 to 12 percent slopes118591692148r77cid70919761:24000
Vining-Kecko-Rock outcrop complex, 2 to 12 percent slopes82384315326761nfw5id78019981:24000
Kecko loamy fine sand, 2 to 8 percent slopes2915423324860642pfymor6451:24000

Map of Series Extent

Approximate geographic distribution of the KECKO 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 .