Official Series Description


Lab Data Summary

Aggregate lab data for the HAUBSTADT soil series. This aggregation is based on all pedons with a current taxon name of HAUBSTADT, 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 HAUBSTADT 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
114A92P0921S1992IN119005Haubstadt7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2741661,-86.726387
114BJN77021977IN071002Haubstadt2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.8198194,-85.8421028
114BJN78141978IN071014Haubstadt2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.8420194,-85.9828194
114B90P004389IN143016Haubstadt5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7852783,-85.7791672
115APK81031981IN125003Haubstadt2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4162944,-87.2278139
n/aAT-S011954-OH009-S01Haubstadt4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aHY-0531966-OH071-053Haubstadt4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aHY-0711983-OH071-071Haubstadt4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aRO-0991990-OH141-099Haubstadt4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HAUBSTADT 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 HAUBSTADT 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 HAUBSTADT 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 HAUBSTADT 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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Click the image to view it full size.

Competing Series

Soil series competing with HAUBSTADT 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 HAUBSTADT 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 HAUBSTADT 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.

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 HAUBSTADT, 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. IN-2010-09-24-25 | Scott County -

    Typical pattern of soils and parent material in the Haubstadt-Dubois-Peoga association (Soil Survey of Scott County, Indiana).

  2. IN-2012-01-19-28 | Jackson County - October 1990

    Typical pattern of soils and parent material in the Dubois-Peoga-Haubstadt association (Soil Survey of Jackson County, Indiana; 1990).

Map Units

Map units containing HAUBSTADT 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
Haubstadt silt loam, 2 to 6 percent slopes, erodedHccB21821851332vzcbin01920011:12000
Haubstadt-Shircliff silt loams, 6 to 15 percent slopes, erodedHcdC22613951nlvwin01920011:12000
Haubstadt-Shircliff complex, 6 to 15 percent slopes, severely erodedHceC31613952nlvxin01920011:12000
Haubstadt silt loam, 2 to 6 percent slopes, erodedHccB21369419070592vzcbin07119851:15840
Haubstadt silt loam, 0 to 2 percent slopesHccA22031907058220g0in07119851:15840
Urban land-Haubstadt complex, 2 to 6 percent slopesUusB12019076722212tin07119851:15840
Haubstadt silt loam, 2 to 6 percent slopes, erodedHdB2269754002vzcbin07719821:15840
Haubstadt-Shircliff complex, 6 to 15 percent slopes, severely erodedHeC31297540711qzrin07719821:15840
Haubstadt-Shircliff silt loams, 6 to 15 percent slopes, erodedHeC21097540611qzqin07719821:15840
Haubstadt silt loam, 2 to 6 percent slopes, erodedHccB237117091352vzcbin07920101:12000
Haubstadt silt loam, 2 to 6 percent slopes, erodedHccB252417081332vzcbin10119841:15840
Haubstadt silt loam, 6 to 15 percent slopes, severely erodedHdbC316217081371vbg6in10119841:15840
Haubstadt silt loam, 6 to 15 percent slopes, erodedHdbC215817081361vbg5in10119841:15840
Haubstadt silt loam, 2 to 6 percent slopes, erodedHccB253881660462vzcbin11919971:12000
Haubstadt silt loam, 6 to 12 percent slopes, severely erodedHccC35911660475kscin11919971:12000
Haubstadt silt loam, 0 to 2 percent slopesHccA4421660455ks9in11919971:12000
Haubstadt silt loam, 1 to 6 percent slopesHbB60821619085fgvin12519831:15840
Haubstadt silt loam, 2 to 6 percent slopes, erodedHccB237711656782vzcbin14319951:12000
Haubstadt-Shircliff complex, 6 to 15 percent slopes, severely erodedHceC312821656805kdjin14319951:12000
Haubstadt silt loam, 0 to 2 percent slopesHccA8601656775kdfin14319951:12000
Haubstadt-Urban land complex, 2 to 6 percent slopesHcfB7661656815kdkin14319951:12000
Haubstadt-Shircliff silt loams, 6 to 15 percent slopes, erodedHcdC27561656795kdhin14319951:12000
Haubstadt silt loam, 2 to 6 percent slopesHhB7095354902w0w4in17519841:15840
Haubstadt silt loam, 0 to 2 percent slopesHhA314690451l9nkin17519841:15840
Haubstadt silt loam, 2 to 6 percent slopesHbB1218714204282w0w4oh07119731:15840
Haubstadt silt loam, 6 to 12 percent slopes, moderately erodedHbC2481814204291jp29oh07119731:15840
Haubstadt silt loam, 0 to 2 percent slopesHbA73014204271jp27oh07119731:15840
Haubstadt silt loam, 12 to 18 percent slopes, moderately erodedHbD250714204311jp2coh07119731:15840
Haubstadt silt loam, 6 to 12 percent slopes, severely erodedHbC337214204301jp2boh07119731:15840
Haubstadt silt loam, 12 to 18 percent slopes, severely erodedHbD330014204321jp2doh07119731:15840
Haubstadt-Urban land complex, gently slopingHcB14514204331jp2foh07119731:15840
Haubstadt-Urban land complex, slopingHcC5214204341jp2goh07119731:15840
Haubstadt silt loam, 6 to 12 percent slopes, erodedHaC25461708825qtboh14119971:15840
Haubstadt silt loam, 2 to 6 percent slopesHaB3761708812w0w4oh14119971:15840

Map of Series Extent

Approximate geographic distribution of the HAUBSTADT 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 .