Official Series Description


Lab Data Summary

Aggregate lab data for the HOBACKER soil series. This aggregation is based on all pedons with a current taxon name of HOBACKER, 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 HOBACKER 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
43B69C0118S1969WY023005Hobacker6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.7291679,-110.9358368
43B69C0119S1969WY023006Hobacker3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.6369438,-110.9430542
43B89P0766TSW4/89BHobacker6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.6228167,-110.5153972

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HOBACKER 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 HOBACKER 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 HOBACKER 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 HOBACKER 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 flats position figure.

Competing Series

Soil series competing with HOBACKER 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 HOBACKER 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 HOBACKER 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 flats position figure.

Soil series sharing subgroup-level classification with HOBACKER, 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. WA-2012-05-11-50 | Star Valley Area - March 1976

    Generalized cross-section of Star Valley Area showing the relative position of the four soil associations: 1. Hobacker-Greyback-Leavittville association; 2. Turson-Dipman association; 3. Robana-Buckskin-Cowdrey association; and 4. Paulson-Lail-Stony rock land association (Soil Survey of Star Valley Area Wyoming-Idaho; Parts of Lincoln County, Wyoming, and Bonneville and Caribou Counties, Idaho; March 1976).

Map Units

Map units containing HOBACKER 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
Hobacker loam, 3 to 25 percent slopes592590496902jp23co68419841:24000
Hobacker gravelly sandy loamHb52202391425y1kid75819981:24000
Hobacker gravelly loam, 0 to 4 percent slopes124857841572tkrid76919781:24000
Hobacker gravelly loam, 4 to 10 percent slopes13777841582tksid76919781:24000
Hobacker family-Clayey-skeletal pachic haplocryolls-Midfork family complex, 5 to 25 percent slopes413331287530gwnut6451:24000
Hobacker-Gralic families-Rock outcrop complex, 30 to 80 percent slopes8331487030hm0ut6451:24000
Hobacker-Clayey-skeletal Pachic Haplocryolls families complex, 5 to 30 percent slopes628A331486230hlmut6451:24000
Hobacker, stony-Baird Hollow-Becks, frequently flooded families complex, 0 to 30 percent slopes628331486130hlnut6451:24000
Gralic-Merino-Hobacker families complex, 30 to 80 percent slopes46331288230gwwut6451:24000
Clayey-skeletal pachic haplocryolls-Hobacker family complex, 5 to 30 percent slopes415331287730gwqut6451:24000
Hobacker-Castino families-Rock outcrop complex, 15 to 60 percent slopes281209331285830gw2ut6451:24000
Hobacker gravelly loamHc749715270353wxwy62319711:20000
Greyback and Hobacker soils, 0 to 30 percent slopesGHE326115269653wpwy62319711:20000
Hobacker cobbly loamHd175415270453wywy62319711:20000
Hobacker gravelly sandy loamHb115115270253wwwy62319711:20000
Hobacker-Osmund gravelly loams, 6 to 20 percent slopesHgD93915270553wzwy62319711:20000
Hobacker-Osmund gravelly loams, 20 to 30 percent slopesHOE27615270153wvwy62319711:20000
Hobacker-Arrowpeak families-Rubble land complex2546191515794459bzwy65620081:24000
Rock outcrop-Rubble land-Hobacker family, complex522Y63715794559c0wy65620081:24000
Rock outcrop-Rubble land-Badwater family, complex529434115794659c1wy65620081:24000
Hobacker family-Cumulic Haplocryolls-Tonsina family, complex, 0 to 15 percent slopes1311114151947533jwy66320121:24000
Arrowpeak-Hobacker families-Rock outcrop, complex25466544830565312xtsjwy66519961:62500
Hobacker-Kegsprings families-Typic Cryaquolls, complex21673390230565232xts3wy66519961:62500
Hobacker-Libeg-Greyback families, complex29242569830565432xtsrwy66519961:62500
Rock outcrop-Rubble land-Hobacker family, complex52941682930565362xtt0wy66519961:62500
Hobacker-Greyback-Shadow families, complex22131466730565222xts6wy66519961:62500
Hobacker-Elkpeak-Kegsprings families, complex29151025230565322xtspwy66519961:62500
Rock outcrop-Hobacker family-Rubble land, complex522736330564902xtr6wy66519961:62500
Hobacker-Teedown-Pineisle families, complex2975419030565422xtswwy66519961:62500
Hobacker-Adel-Bearmouth families, complex2222231830565212xts8wy66519961:62500
Hobacker family2025202030565112xtrzwy66519961:62500
Midfork, stony-Hobacker-Adel families, complex, 15 to 60 percent slopes4152729804452wqqwwy6671:24000

Map of Series Extent

Approximate geographic distribution of the HOBACKER 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 .