Official Series Description


Lab Data Summary

Aggregate lab data for the DIMMICK soil series. This aggregation is based on all pedons with a current taxon name of DIMMICK, 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 DIMMICK 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
5483ND04109183ND041091Dimmick5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.3861111,-102.9152778

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the DIMMICK 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 DIMMICK 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 DIMMICK 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 DIMMICK 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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Competing Series

Soil series competing with DIMMICK 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 DIMMICK 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 DIMMICK 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 hills figure.

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

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

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Soil series sharing subgroup-level classification with DIMMICK, 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. ND-2012-02-08-64 | Wells County - June 1970

    Parent material and position of soils in association 6 (Soil Survey of Wells County, North Dakota; June 1970).

Map Units

Map units containing DIMMICK 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
Dimmick clay, 0 to 1 percent slopes34A40693439142vys7mt04119941:24000
Dimmick silty clay561434344420ckdbmt05519811:24000
Dimmick clay, drained57918344421ckdcmt05519811:24000
Dimmick clay, 0 to 1 percent slopesDm43853488422vys8mt09119711:24000
Dimmick clay, 0 to 1 percent slopesDc10611467982vys7mt60019691:24000
Dimmick clayDw3321473494yb6mt60219631:20000
Dimmick clay, 0 to 1 percent slopes3956013464502vys7mt60819761:24000
Dimmick silty clay, 0 to 2 percent slopes204A119251367850tnmt62420211:24000
Dimmick silty clay, 0 to 2 percent slopes204A58014975050tnmt63920001:24000
Dimmick clay, 0 to 1 percent slopes170A70883476132vys7mt64119941:24000
Dimmick clay, 0 to 1 percent slopes1313103482152vys8mt66119821:24000
Dimmick silty clay, 0 to 1 percent slopesE4711A45925257621vzwgnd00119831:20000
Dimmick silty clay, 0 to 1 percent slopesC12A96925640962pwdvnd01519671:20000
Dimmick silty clay, 0 to 1 percent slopesE4711A224127072611vzwgnd02519811:20000
Dimmick clay, ponded, 0 to 1 percent slopesE4707A141727072602q64hnd02519811:20000
Dimmick silty clay, loamy substratum, 0 to 1 percent slopesE4713A72827073142r4ftnd03319851:24000
Dimmick silty clay, 0 to 1 percent slopesE4711A169525258281vzwgnd04119861:20000
Dimmick clay, ponded, 0 to 1 percent slopesE4707A4526618722q64hnd04719921:20000
Dimmick silty clay loam, 0 to 1 percent slopesE4715A8242699362d334nd05320031:24000
Dimmick silty clay, 0 to 1 percent slopesC12A18125666332pwdvnd05519741:20000
Dimmick silty clay, 0 to 1 percent slopesE4711A105826992521vzwgnd05719761:20000
Dimmick silty clay, 0 to 1 percent slopesE4711A107817183611vzwgnd05919981:20000
Dimmick silty clay, 0 to 1 percent slopesE4711A35625260081vzwgnd06519711:20000
Dimmick silty clay, loamy substratum, 0 to 1 percent slopesE4713A59726990782r4ftnd08519921:24000
Dimmick silty clay, 0 to 1 percent slopesE4711A169027158731vzwgnd08719741:20000
Dimmick silty clay, 0 to 1 percent slopesE4711A54617135811vzwgnd08919651:20000
Dimmick clay, 0 to 1 percent slopes142720123390192vys8nd10519931:24000
Dimmick and Heil soilsDb6367354624cx0hsd10519771:24000

Map of Series Extent

Approximate geographic distribution of the DIMMICK 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 .