Official Series Description


Lab Data Summary

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the GELKIE series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the GELKIE series and siblings. 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 GELKIE 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

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

Competing Series

Soil series competing with GELKIE share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the GELKIE 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 GELKIE 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

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

Soil series sharing subgroup-level classification with GELKIE, 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 GELKIE 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
Gelkie sandy loam, 3 to 15 percent slopes205714496455jnlpco62719801:24000
Gelkie sandy loam, 15 to 30 percent slopes212423496456jnlqco62719801:24000
Bushvalley-Gelkie-Rock outcrop complex, 3 to 65 percent slopes1027921498440jqnqco63319811:24000
Gelkie loam, 3 to 25 percent slopes274737498458jqp9co63319811:24000
Clayburn-Gelkie-Bowen families complex, 2 to 30 percent slopes815G1815500989jt9yco6341:24000
Bowen-Gelkie families association, 2 to 40 percent slopes645M740500975jt9hco6341:24000
Gelkie sandy loam, 1 to 10 percent slopes1212360498375jqlmco63519791:24000
Gelkie sandy loam, 2 to 15 percent slopesGeD14360497784jpzkco64619731:24000
Gelkie sandy loam, moderately deep variant, 0 to 25 percent slopesGkE962497785jpzlco64619731:24000
Youga-Gelkie-Clayburn, warm complex, 25 to 45 percent slopes, extremely bouldery221673106836jpchco6481:24000
Gelkie fine sandy loam, 2 to 7 percent slopes14332024536832nc82co66419871:24000
Youga-Gelkie-Clayburn, warm complex, 25 to 45 percent slopes, extremely bouldery2216538497193jpchco68619921:31680
Gelkie-Goosepeak families-Rock outcrop complex, 15 to 55 percent slopes, extremely stony1623253333597mwy6291:24000
Brushfire-Gelkie-Reinecker complex, 0 to 4 percent slopes3202564316536091shq7wy6351:24000
Jaycox-Burtswell-Gelkie complex, 2 to 12 percent slopes3404421016760051t80pwy6351:24000
Gelkie-Goosepeak families-Rock outcrop complex, 15 to 55 percent slopes, extremely stony1626186157840597mwy65620081:24000
Hoodle-Gelkie association, 2 to 15 percent slopes163D18815792559bcwy65620081:24000
Lymanson-Abston-Gelkie association, hilly7187190156721tqwwy67719751:24000
Uhl-Gelkie loams, 1 to 8 percent slopes6846190157921tr8wy67719751:24000
Hoodle-Gelkie association, 2 to 15 percent slopes16379241503028jwfqwy71319861:24000
Uhl-Gelkie loams, 1 to 8 percent slopes21720098503095jwhwwy71319861:24000
Lymanson-Abston-Gelkie association, hilly17116638503036jwfzwy71319861:24000
Gelkie variant-Barrett variant association, undulating1523336503017jwfcwy71319861:24000

Map of Series Extent

Approximate geographic distribution of the GELKIE 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 .