Official Series Description


Lab Data Summary

Aggregate lab data for the JACOB soil series. This aggregation is based on all pedons with a current taxon name of JACOB, 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 JACOB 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
11391P047089IL055022Jacob5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0208931,-88.96978
115B70IL0770031970IL077003Jacob5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.631729,-89.4287531
115B95P019193IL181035EJacob6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.5695106,-89.4486842
115B40A2802S1963IL077003Jacob7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.7427788,-89.5144424
120A95P020893IL087106EJacob6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.3136818,-88.9825582
n/a78IL1570491978IL157049Jacob3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a79IL1570871979IL157087Jacob3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a91P101991IL055025Jacob5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the JACOB 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 JACOB 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 JACOB 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 JACOB 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 hills figure.

There are insufficient data to create the 3D mountains figure.

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 JACOB 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 JACOB series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the JACOB 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 .

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

There are insufficient data to create the 3D mountains figure.

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 JACOB, 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. IL-2010-09-01-12 | Franklin and Jefferson Counties - 2003

    Typical pattern of soils and parent material in the Colp-Hurst-Okaw association (Soil Survey of Franklin and Jefferson Counties, Illinois; 2003).

  2. IL-2011-08-04-95 | Randolph County - 1988

    Pattern of soils and parent material in the Darwin-Fults association (Soil Survey of Randolph County, Illinois; 1988).

Map Units

Map units containing JACOB 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
Darwin and Jacob silty clays, undrained, 0 to 2 percent slopes, frequently flooded1845A2604602613n724il00320021:12000
Jacob silty clay, 0 to 2 percent slopes, occasionally flooded8085A433601841n687il00320021:12000
Jacob silty clay, 0 to 2 percent slopes, frequently flooded3085A2503809249w52til05520051:12000
Jacob silty clay, undrained, 0 to 2 percent slopes, frequently flooded1085A1119809231w527il05520051:12000
Jacob silty clay, 0 to 2 percent slopes, occasionally flooded8085A692715381051nmj9il07720061:12000
Darwin and Jacob silty clays, undrained, 0 to 2 percent slopes, frequently flooded1845A531015388101nn81il07720061:12000
Jacob silty clay, 0 to 2 percent slopes, frequently flooded3085A314915378741nm8vil07720061:12000
Jacob silty clay, undrained, 0 to 2 percent slopes, frequently flooded1085A3016119271r3bnil07720061:12000
Darwin and Jacob silty clays, undrained, 0 to 2 percent slopes, frequently flooded1845A361748937t4b8il15320041:12000
Jacob silty clay, 0 to 2 percent slopes, occasionally flooded8085A89749009t4dlil15320041:12000
Jacob silty clay, 0 to 2 percent slopes, occasionally flooded, long duration8085L18912005656qpvil15720011:12000
Jacob silty clay, 0 to 2 percent slopes, frequently flooded, long duration3085L3322005466qp7il15720011:12000
Jacob silty clay, 0 to 2 percent slopes, occasionally flooded8085A28031995396pmril18120011:12000
Jacob silty clay, 0 to 2 percent slopes, frequently flooded3085A110814780771lm1xil19920071:12000
Jacob silty clay, undrained, 0 to 2 percent slopes, frequently flooded1085A4014782271lm6ril19920071:12000

Map of Series Extent

Approximate geographic distribution of the JACOB 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 .