Official Series Description


Lab Data Summary

Aggregate lab data for the BUCKNELL soil series. This aggregation is based on all pedons with a current taxon name of BUCKNELL, 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 BUCKNELL 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
108C95P0828S1995IA107011BUCKNELL7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.3211098,-91.984169
10995P0834S1995IA135002Bucknell7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.1116676,-93.0516663

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BUCKNELL 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 BUCKNELL 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 BUCKNELL 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 BUCKNELL 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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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with BUCKNELL 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 BUCKNELL 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 BUCKNELL 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.

Click the image to view it full size.

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

Soil series sharing subgroup-level classification with BUCKNELL, 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. IA-2010-09-02-15 | Jefferson County - 1999

    Typical pattern of soils and parent material in the Ladoga-Hedrick-Gara association (Soil Survey of Jefferson County, Iowa; 1999).

  2. IA-2010-09-09-01 | Adams County - 2008

    Typical pattern of soils and parent material in the Ladoga-Gara soil association (Soil Survey of Adams County, Iowa; 2008).

  3. IA-2011-05-31-56 | Jefferson County - 1999

    Typical pattern of soils and parent material in the Ladoga-Hedrick-Gara association (Soil Survey of Jefferson County, Iowa; 1999).

  4. IA-2011-06-01-16 | Lucas County - 1999

    Relationship of the major soils in Lucas County to parent material and to position on the landscape (Soil Survey of Lucas County, Iowa; 1999).

  5. IA-2011-06-01-20 | Montgomery County - 1989

    Typical pattern of soils and parent material in the Gara-Ladoga association (Soil Survey of Montgomery County, Iowa; 1989).

  6. IA-2011-06-01-42 | Ringgold County - 1992

    Relationship of the major soils in Ringgolg County to parent material and to position on the landscape (Soil Survey of Ringgold County, Iowa; 1992).

Map Units

Map units containing BUCKNELL 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
Gara-Bucknell complex, 9 to 14 percent slopes, moderately eroded421D2826519078592218via00320081:12000
Gara-Bucknell complex, 14 to 18 percent slopes, moderately eroded421E27541913039226nyia00320081:12000
Gara-Bucknell complex, 5 to 9 percent slopes, moderately eroded421C235622478482fg27ia00320081:12000
Bucknell-Hedrick complex, 14 to 18 percent slopes, severely eroded579E324722478502fg29ia00320081:12000
Bucknell silty clay loam, 9 to 14 percent slopes, moderately eroded423D240254041452tfz2ia03919871:15840
Bucknell silty clay loam, 9 to 14 percent slopes423D13164041442tfz0ia03919871:15840
Bucknell silty clay loam, 5 to 9 percent slopes, moderately eroded423C22864041432tfz1ia03919871:15840
Bucknell silty clay loam, 9 to 14 percent slopes, moderately eroded423D242484046842tfz2ia05119881:15840
Bucknell silty clay loam, 9 to 14 percent slopes, severely eroded423D3136404685fl3cia05119881:15840
Bucknell clay loam, 9 to 14 percent slopes, moderately eroded423D27631404798fl70ia05319861:15840
Bucknell clay loam, 5 to 9 percent slopes, moderately eroded423C2980404797fl6zia05319861:15840
Bucknell silty clay loam, 9 to 14 percent slopes, moderately eroded423D249124078062tfz2ia10119921:15840
Bucknell silty clay loam, 9 to 14 percent slopes, moderately eroded423D293614471012tfz2ia10719981:12000
Bucknell silty clay loam, 9 to 14 percent slopes, moderately eroded423D261594089372tfz2ia11719911:15840
Bucknell silty clay loam, 5 to 9 percent slopes, moderately eroded423C210304089342tfz1ia11719911:15840
Bucknell-Gara complex, 9 to 14 percent slopes, moderately eroded894D2439409055fqnbia11719911:15840
Bucknell silty clay loam, 9 to 14 percent slopes423D2684089362tfz0ia11719911:15840
Bucknell silty clay loam, 9 to 14 percent slopes, moderately eroded423D264064097832tfz2ia13519821:15840
Bucknell silty clay loam, 9 to 14 percent slopes, moderately eroded423D29004098652tfz2ia13719871:15840
Bucknell silty clay loam, 5 to 9 percent slopes, moderately eroded423C223234106972tfz1ia15919871:15840
Bucknell silty clay loam, 9 to 14 percent slopes, moderately eroded423D214844106992tfz2ia15919871:15840
Bucknell silty clay loam, 5 to 9 percent slopes423C5854106962yy81ia15919871:15840
Bucknell silty clay loam, 9 to 14 percent slopes423D4604106982tfz0ia15919871:15840
Bucknell silty clay loam, 9 to 14 percent slopes, moderately eroded423D214054116222tfz2ia17319891:15840
Bucknell silty clay loam, 5 to 9 percent slopes, moderately eroded423C212624116212tfz1ia17319891:15840
Bucknell silty clay loam, 9 to 14 percent slopes, moderately eroded423D236674130822tfz2ia17719941:12000
Bucknell silty clay loam, 9 to 14 percent slopes, moderately eroded423D250624225482tfz2ia18519661:15840

Map of Series Extent

Approximate geographic distribution of the BUCKNELL 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 .