Official Series Description


Lab Data Summary

Aggregate lab data for the ZION soil series. This aggregation is based on all pedons with a current taxon name of ZION, 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 ZION 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/a93P036693NC151001Zion6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

Soil series competing with ZION 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 ZION 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 ZION 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 ZION, 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 ZION 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
Wynott-Zion-Wilkes complex, 15 to 35 percent slopesWzF6735126986484bga15919971:24000
Wilkes-Zion complex, 6 to 15 percent slopesWkD44201269854849ga15919971:24000
Zion gravelly loam, 10 to 15 percent slopesZnD82512491245zfga22119841:20000
Zion gravelly loam, 2 to 10 percent slopesZnC80012491145zdga22119841:20000
Zion gravelly loam, 15 to 25 percent slopesZnE57012491345zgga22119841:20000
Zion silt loam, 10 to 25 percent slopesZnE69701271354894ga64519951:12000
Zion silt loam, 2 to 10 percent slopesZnC67351271344893ga64519951:12000
Rasalo-Zion complex, 2 to 6 percent slopesRaB7424313262mlzwnc03519691:15840
Siloam-Zion complex, 15 to 25 percent slopesSzE9624328412mnkrnc05719851:24000
Siloam-Zion complex, 8 to 15 percent slopesSzD2324328402mnkqnc05719851:24000
Siloam-Zion complex, 25 to 45 percent slopesSzF1624328432mnktnc05719851:24000
Siloam-Zion complex, 2 to 8 percent slopesSzB1224328392mnkpnc05719851:24000
Rasalo-Zion complex, 6 to 10 percent slopesRaC2924246832md2lnc09720111:12000
Rasalo-Zion complex, 2 to 6 percent slopesRaB1924246822md2knc09720111:12000
Zion-Siloam complex, 8 to 15 percent slopesZwC110523890252l5zbnc16919921:24000
Siloam-Zion complex, 15 to 45 percent slopesSrE44314276971jxmrnc17120051:24000
Siloam-Zion complex, 6 to 15 percent slopesSrC41912754748qfnc17120051:24000
Siloam-Zion complex, 10 to 15 percent slopesSoD35523982082lhjknc19719601:15840
Siloam-Zion complex, 10 to 15 percent slopes, moderately erodedSoD222223982092lhjlnc19719601:15840
Zion silt loam, undulating phaseZa18212185042snva06519501:15840
Zion loam, 2 to 7 percent slopes, erodedZoB21858119439408wva10919721:15840
Zion loam, 7 to 15 percent slopes, erodedZoC2610119440408xva10919721:15840
Zion loam, 2 to 7 percent slopesZoB577119438408vva10919721:15840
Zion silt loam, 2 to 7 percent slopesZoB305517068kc1mva11319671:15840
Zion silt loam, 7 to 15 percent slopesZoC258517069kc1nva11319671:15840
Zion silt loam, 2 to 7 percent slopesZoB38611994740t8va13719661:15840
Zion silt loam, 7 to 15 percent slopes, moderately erodedZoC21611199482zhhfva13719661:15840
Iredell-Zion fine sandy loams, undulating phasesIb14581202574148va14719501:20000
Iredell-Zion fine sandy loams, rolling phasesIa6001202564147va14719501:20000
Zion loam, deep variant, 2 to 6 percent slopesZlB34912058841gyva17919701:15840
Zion loam, deep variant, 6 to 10 percent slopes, erodedZlC227912058941gzva17919701:15840

Map of Series Extent

Approximate geographic distribution of the ZION 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 .