Official Series Description


Lab Data Summary

Aggregate lab data for the HIKO SPRINGS soil series. This aggregation is based on all pedons with a current taxon name of HIKO SPRINGS, 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 HIKO SPRINGS 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
28A40A0953S1966UT027001Hiko Springs8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6202774,-113.8555527
28A40A0954S1966UT027002Hiko Springs8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.621067,-113.8580475
28A40A0955S1966UT027003Hiko Springs7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6161118,-113.8763885
28A40A0956S1966UT027004Hiko Springs8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6163902,-113.8766632
28A68C0051S1968UT001005Hiko Springs5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5472221,-113.7586136
28A68C0053S1968UT001006Hiko Springs5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5327797,-113.7586136

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HIKO SPRINGS 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 HIKO SPRINGS 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 HIKO SPRINGS 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 HIKO SPRINGS 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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Competing Series

Soil series competing with HIKO SPRINGS 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 HIKO SPRINGS 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 HIKO SPRINGS 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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Soil series sharing subgroup-level classification with HIKO SPRINGS, 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 HIKO SPRINGS 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
Hiko Springs-Summermute association40403146480117j3lnnv77920041:24000
Hiko Springs fine sandy loam, 0 to 2 percent slopes1042494505367jyw5ut04719991:24000
Hiko Springs-Okrist association, 1 to 8 percent slopes4018649481249j4s5ut60119851:24000
Hiko Springs-Summermute association791462713897191hn3nut61119921:24000
Hiko Springs gravelly sandy loam, 2 to 4 percent slopes256487482129j5pkut61119921:24000
Sanpete-Hiko Springs-Penoyer families association, 0 to 15 percent slopes715021631838992x4gxut6171:24000
Hiko Springs-Lynndyl families association, 0 to 8 percent slopes352796131838592whryut6171:24000
Siltcliffe-Hiko Springs-Dera complex, 0 to 3 percent slopes183593222205052djm6ut6261:24000
Hiko Springs-Lynndyl complex, 0 to 2 percent slopes178291222205002djm1ut6261:24000
Hiko Springs sandy loam, 3 to 10 percent slopes, erodedHKC219065482396j5z5ut63219701:20000
Hiko Springs very gravelly loam, hardpan variant, 3 to 10 percent slopesHLC1735482397j5z6ut63219701:20000

Map of Series Extent

Approximate geographic distribution of the HIKO SPRINGS 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 .