Official Series Description


Lab Data Summary

Aggregate lab data for the SHEETIRON soil series. This aggregation is based on all pedons with a current taxon name of SHEETIRON, 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 SHEETIRON 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
5UCD521702352-CA-17-023xSHEETIRON2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.5020523,-122.7437744
5UCD541101654-CA-11-016SHEETIRON2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.6608772,-122.713562
5UCD585202358-CA-52-023SHEETIRON2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9117546,-122.7415771
5UCD601200760-CA-12-007xSHEETIRON3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.1019859,-123.6386719
5UCD714516971-CA-45-169xSHEETIRON2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7930641,-122.5494919
5UCD744711574-CA-47-115xSHEETIRON2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.2314529,-122.2048874
585P004584CA105005Sheetiron6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5423508,-122.8261032
581P0048S1980CA033010SHEETIRON5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.5686111,-122.8380585
581P0049S1980CA033013Sheetiron4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4852791,-122.7327805
n/a82P0205S1981CA103301Sheetiron6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SHEETIRON 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 SHEETIRON 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 SHEETIRON 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 SHEETIRON 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 terrace figure.

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

Competing Series

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

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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 SHEETIRON, 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 SHEETIRON 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
Neuns-Sheetiron-Goulding complex, 30 to 50 percent slopes591691461651hhczca01119991:24000
Neuns-Goulding-Sheetiron complex, 50 to 75 percent slopes59228461652hhd0ca01119991:24000
Sheetiron gravelly loam, 30 to 50 percent slopes, MLRA 5SkE514114588512ty1hca02119611:20000
Sheetiron gravelly loam, shallow, 30 to 50 percent slopesSlE19793458855hdgsca02119611:20000
Sheetiron gravelly loam, 50 to 65 percent slopesSkF7062458852hdgpca02119611:20000
Sheetiron gravelly loam, shallow, 50 to 65 percent slopesSlF6065458857hdgvca02119611:20000
Sheetiron gravelly loam, 10 to 30 percent slopesSkD2570458850hdgmca02119611:20000
Sheetiron gravelly loam, shallow, 10 to 30 percent slopesSlD2057458853hdgqca02119611:20000
Josephine-Sheetiron gravelly loams, 30 to 50 percent slopesJsE1499458669hd8sca02119611:20000
Sheetiron-Rock outcrop complex, 10 to 50 percent slopes330mnf86425048732q42cca02119611:20000
Sheetiron gravelly loam, shallow, 30 to 50 percent slopes, erodedSlE2752458856hdgtca02119611:20000
Sheetiron gravelly loam, shallow, 10 to 30 percent slopes, erodedSlD2623458854hdgrca02119611:20000
Sheetiron gravelly loam, shallow, 50 to 65 percent slopes, erodedSlF2222458858hdgwca02119611:20000
Sheetiron very gravelly loam, 50 to 75 percent slopes329mnf3325048722q42bca02119611:20000
Sheetiron-Deadwood association, 50 to 75 percent slopes20515064459608hf82ca03319851:24000
Sheetiron-Deadwood association, 30 to 50 percent slopes2049598459607hf81ca03319851:24000
Neuns-Sheetiron-Deadwood complex, 30 to 50 percent slopes1896086459592hf7kca03319851:24000
Neuns-Sheetiron-Deadwood complex, 50 to 75 percent slopes1904048459593hf7lca03319851:24000
Deadwood-Sheetiron association, 50 to 75 percent slopes1303152459533hf5nca03319851:24000
Sheetiron-Rock outcrop complex, 10 to 50 percent slopes330mnf29225048602q41yca03319851:24000
Sheetiron very gravelly loam, 50 to 75 percent slopes329mnf4525048672q425ca03319851:24000
Sheetiron very gravelly loam, 30 to 50 percent slopes328mnf725048662q424ca03319851:24000
SHEETIRON-BARPEAK COMPLEX, 50 TO 90 PERCENT SLOPES1917944466090hn05ca60619901:24000
BARPEAK-SHEETIRON COMPLEX, 50 TO 90 PERCENT SLOPES1096597466005hmxfca60619901:24000
SHEETIRON VARIANT-DEDRICK COMPLEX, 50 TO 75 PERCENT SLOPES192839466091hn06ca60619901:24000
SHEETIRON EXTREMELY GRAVELLY LOAM, 75 TO 90 PERCENT SLOPES190193466089hn04ca60619901:24000
Sheetiron very stony loam, 50 to 75 percent slopesSgF6394460123hfspca60719671:20000
Sheetiron very stony loam, 75 to 90 percent slopesSgG1520460124hfsqca60719671:20000
Josephine-Sheetiron complex, 50 to 70 percent slopesJsF1461460023hfpgca60719671:20000
Sheetiron very stony loam, 30 to 50 percent slopesSgE602460122hfsnca60719671:20000
Sheetiron gravelly loam, 30 to 50 percent slopesSnE87664460927hgmmca64519611:20000
Sheetiron gravelly loam, 50 to 65 percent slopesSnF26237460928hgmnca64519611:20000
Josephine-Sheetiron gravelly loams, 30 to 50 percent slopesJsE11827460788hgh4ca64519611:20000
Sheetiron gravelly loam, 10 to 30 percent slopesSnD3573460926hgmlca64519611:20000
Sheetiron very gravelly loam, 50 to 75 percent slopes329mnf233125048562q41sca64519611:20000
Josephine-Sheetiron gravelly loams, 10 to 30 percent slopesJsD2143460787hgh3ca64519611:20000
Sheetiron rocky loam, 30 to 50 percent slopesSrE970460929hgmpca64519611:20000
Sheetiron rocky loam, 50 to 65 percent slopesSrF839460930hgmqca64519611:20000
Sheetiron very gravelly loam, 30 to 50 percent slopes328mnf8825048552q41rca64519611:20000
Sheetiron very stony loam, 50 to 75 percent slopesSgFsh409186845620q8sca70719831:24000
Sheetiron very gravelly loam, 30 to 50 percent slopes328mnf23125048772q42gca70719831:24000
Barpeak-Sheetiron complex, 50 to 90 percent slopes109tw164186872720qkjca70719831:24000
Sheetiron very stony loam, 75 to 90 percent slopesSgGsh123186845820q8vca70719831:24000
Sheetiron very gravelly loam, 50 to 75 percent slopes329mnf2425048782q42hca70719831:24000
Sheetiron very stony loam, 30 to 50 percent slopesSgEsh19186845420q8qca70719831:24000
Sheetiron very gravelly loam, 30 to 50 percent slopes3283207027478112q1z4ca70920101:24000
Sheetiron very gravelly loam, 50 to 75 percent slopes3293078427478122q1z5ca70920101:24000
Sheetiron-Rock outcrop complex, 10 to 50 percent slopes3302706327478132q1z6ca70920101:24000
Sheetiron-Rock outcrop, sedimentary, complex, 30 to 50 percent slopes333196627478142q1z7ca70920101:24000
Sheetiron gravelly loam, 30 to 50 percent slopesSnEte14412747892hgmmca70920101:24000
Sheetiron gravelly loam, 30 to 50 percent slopesSkEgl97227479062q41lca70920101:24000
Neuns-Sheetiron-Deadwood complex, 30 to 50 percent slopes189la35227478722q3rdca70920101:24000
Sheetiron gravelly loam, shallow, 50 to 65 percent slopesSlFgl19727479082q41nca70920101:24000
Neuns-Sheetiron-Deadwood complex, 50 to 75 percent slopes190la8727478732q3rfca70920101:24000
Josephine-Sheetiron gravelly loams, 30 to 50 percent sl opesJsEte927478892q3rzca70920101:24000
Sheetiron gravelly loam, 50 to 65 percent slopesSkFgl427479072q41mca70920101:24000
Sheetiron gravelly loam, 10 to 30 percent slopesSkDgl227479052q41kca70920101:24000

Map of Series Extent

Approximate geographic distribution of the SHEETIRON 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 .