Official Series Description


Lab Data Summary

Aggregate lab data for the ASHGROVE soil series. This aggregation is based on all pedons with a current taxon name of ASHGROVE, 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 ASHGROVE were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ASHGROVE 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 ASHGROVE 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 ASHGROVE 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 ASHGROVE 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.

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 ASHGROVE 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 ASHGROVE 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 ASHGROVE 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 .

Click the image to view it full size.

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 ASHGROVE, 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-2010-09-02-16 | Jefferson County - 1999

    Typical pattern of soils and parent material in the Clinton-Lindley-Ashgrove association (Soil Survey of Jefferson County, Iowa; 1999).

  2. IA-2010-09-02-18 | Jefferson County - 1999

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

  3. IA-2010-09-03-02 | Van Buren County - 2004

    Typical pattern of soils and parent material in the Weller-Lindley-Keswick association (Soil Survey of Van Buren County, Iowa; 2004).

  4. IA-2010-09-03-05 | Van Buren County - 2004

    Typical pattern of soils and parent material in the Lindley-Rathbun-Keswick association (Soil Survey of Van Buren County, Iowa; 2004).

  5. IA-2011-05-31-57 | Jefferson County - 1999

    Typical pattern of soils and parent material in the Clinton-Lindley-Ashgrove association (Soil Survey of Jefferson County, Iowa; 1999).

  6. IA-2011-05-31-60 | Jefferson County - 1999

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

Map Units

Map units containing ASHGROVE 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
Ashgrove silt loam, 5 to 9 percent slopes, moderately eroded795C24474027282wbd2ia00719701:15840
Ashgrove silt loam, 9 to 14 percent slopes, moderately eroded795D23494027292wbd3ia00719701:15840
Ashgrove silty clay loam, 9 to 14 percent slopes, moderately eroded795D22664047372wbd4ia05119881:15840
Ashgrove silty clay loam, 9 to 14 percent slopes, moderately eroded795D227340528331dnxia05719801:15840
Ashgrove silty clay loam, 9 to 14 percent slopes, moderately erodedS795D241930066402wbd4ia08719821:15840
Ashgrove silty clay loam, 9 to 14 percent slopes, moderately eroded795D215840690031dnxia08719821:15840
Ashgrove silty clay loam, 9 to 14 percent slopes, moderately erodedS795D2486230066412wbd4ia10119921:15840
Ashgrove silty clay loam, 9 to 14 percent slopes, moderately eroded795D2315040788331dnxia10119921:15840
Ashgrove silty clay loam, 5 to 9 percent slopes, moderately eroded795C2150240788131dnzia10119921:15840
Ashgrove silty clay loam, 9 to 14 percent slopes, moderately eroded795D2149944721831dnxia10719981:12000
Ashgrove silty clay loam, 5 to 9 percent slopes, moderately eroded795C21244721531dnzia10719981:12000
Ashgrove silt loam, 9 to 14 percent slopes, moderately eroded795D277364085092wbd3ia11119761:15840
Ashgrove silt loam, 5 to 9 percent slopes, moderately eroded795C238084085072wbd2ia11119761:15840
Ashgrove soils, 5 to 9 percent slopes, severely eroded795C3524408508fq2pia11119761:15840
Ashgrove soils, 9 to 14 percent slopes, severely eroded795D3503408510fq2ria11119761:15840
Ashgrove silty clay loam, 9 to 14 percent slopes, moderately eroded795D270540882331dnxia11519841:15840
Ashgrove silt loam, 9 to 14 percent slopes795D779409819frfzia13519821:15840
Ashgrove silty clay loam, 9 to 14 percent slopes, moderately eroded795D283044131682wbd4ia17719941:12000
Ashgrove silty clay loam, 5 to 9 percent slopes, moderately eroded795C21932413166fvxyia17719941:12000
Ashgrove silty clay loam, 9 to 14 percent slopes795D673413167fvxzia17719941:12000
Ashgrove silty clay loam, 9 to 14 percent slopes, moderately eroded795D25594118522wbd4ia17919781:15840
Ashgrove silty clay loam, 9 to 14 percent slopes, moderately eroded795D2108741210331dnxia18319831:15840

Map of Series Extent

Approximate geographic distribution of the ASHGROVE 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 .