Official Series Description


Lab Data Summary

Aggregate lab data for the DICKEY soil series. This aggregation is based on all pedons with a current taxon name of DICKEY, 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 DICKEY 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
102AUMN2259S1976MN0272259Dickey3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.0779381,-96.3112411
56UMN3174S1979MN167022 (3174)Dickey2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.2371292,-96.3693924

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the DICKEY 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 DICKEY 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 DICKEY 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 DICKEY 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 DICKEY 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 DICKEY 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 DICKEY 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 mountains figure.

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

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Soil series sharing subgroup-level classification with DICKEY, 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

No block diagrams are available.

Map Units

Map units containing DICKEY 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
Dickey loamy fine sand, 1 to 5 percent slopes609B504435877gmkkmn11119961:20000
Dickey-Esmond-Embden complex, 3 to 9 percent slopesF750C93125877322q5m9nd0051:12000
Dickey-Esmond-Embden complex, 3 to 9 percent slopesG750C15825737372q60dnd0051:12000
Dickey-Buse-Embden complex, 3 to 9 percent slopesG738C3725737892q5wynd0051:12000
Dickey-Buse-Embden complex, 3 to 9 percent slopesF738C225876602q5m3nd0051:12000
Towner-Dickey loamy fine sands, 3 to 6 percent slopesF735B36325860472q5m0nd00919811:20000
Dickey-Esmond-Embden complex, 3 to 9 percent slopesG750C84025763552q60dnd0271:12000
Dickey-Buse-Embden complex, 3 to 9 percent slopesG738C4925763512q5wynd0271:12000
Dickey-Buse-Embden complex, 3 to 9 percent slopesG738C161525764722q5wynd03119901:20000
Dickey-Buse-Embden complex, 6 to 15 percent slopesG738D112325764732q5wznd03119901:20000
Dickey-Esmond-Embden complex, 6 to 15 percent slopesG750D64225764792q60fnd03119901:20000
Towner-Dickey loamy fine sands, 3 to 6 percent slopesG735B48125764692q5wvnd03119901:20000
Dickey-Esmond-Embden complex, 3 to 9 percent slopesG750C29825764782q60dnd03119901:20000
Dickey-Buse-Embden complex, 6 to 25 percent slopesG738E625764742q5x0nd03119901:20000
Dickey-Esmond-Embden complex, 6 to 25 percent slopesG750E325882462q60gnd03119901:20000
Dickey-Esmond-Embden complex, 6 to 15 percent slopesG750D198325766752q60fnd03919911:24000
Towner-Dickey loamy fine sands, 3 to 6 percent slopesG735B60825766692q5wvnd03919911:24000
Dickey-Buse-Embden complex, 6 to 15 percent slopesG738D53225766722q5wznd03919911:24000
Dickey-Esmond-Embden complex, 6 to 25 percent slopesG750E1125766762q60gnd03919911:24000
Dickey-Buse-Embden complex, 6 to 15 percent slopesG738D7125771292q5wznd04519661:20000
Dickey-Buse-Embden complex, 3 to 9 percent slopesG738C916025714112q5wynd04919871:20000
Towner-Dickey loamy fine sands, 3 to 6 percent slopesG735B677625714082q5wvnd04919871:20000
Dickey-Buse-Embden complex, 6 to 25 percent slopesG738E604225714132q5x0nd04919871:20000
Towner-Dickey loamy fine sands, 3 to 6 percent slopesF735B498825857642q5m0nd04919871:20000
Dickey-Buse-Embden complex, 6 to 25 percent slopesF738E357225857672q5m4nd04919871:20000
Dickey-Buse-Embden complex, 3 to 9 percent slopesF738C153625856452q5m3nd04919871:20000
Dickey-Esmond-Embden complex, 6 to 25 percent slopesF750E43125856402q5mcnd04919871:20000
Dickey-Esmond-Embden complex, 3 to 9 percent slopesF750C33525857492q5m9nd04919871:20000
Dickey-Esmond-Embden complex, 3 to 9 percent slopesG750C1125714152q60dnd04919871:20000
Dickey-Buse-Embden complex, 6 to 15 percent slopesG738D925714122q5wznd04919871:20000
Towner-Dickey loamy fine sands, 3 to 6 percent slopesG735B7025771892q5wvnd05519741:20000
Dickey-Buse-Embden complex, 6 to 15 percent slopesG738D5325772202q5wznd05519741:20000
Dickey-Buse-Embden complex, 6 to 25 percent slopesG738E61125773782q5x0nd0631:12000
Dickey-Esmond-Embden complex, 6 to 25 percent slopesG750E46125773802q60gnd0631:12000
Dickey-Buse-Embden complex, 3 to 9 percent slopesG738C14025773772q5wynd0631:12000
Dickey-Buse-Embden complex, 6 to 25 percent slopesF738E7225873732q5m4nd0631:12000
Towner-Dickey loamy fine sands, 3 to 6 percent slopesG735B655825823322q5wvnd06919751:20000
Dickey-Esmond-Embden complex, 6 to 15 percent slopesG750D427725823362q60fnd06919751:20000
Towner-Dickey loamy fine sands, 3 to 6 percent slopesF735B149225872792q5m0nd06919751:20000
Dickey-Esmond-Embden complex, 6 to 25 percent slopesF750E26425872162q5mcnd06919751:20000
Dickey-Esmond-Embden complex, 3 to 9 percent slopesF750C12825872692q5m9nd06919751:20000
Dickey-Buse-Embden complex, 6 to 15 percent slopesG738D1225823332q5wznd06919751:20000
Dickey-Esmond-Embden complex, 3 to 9 percent slopesG750C325823352q60dnd06919751:20000
Dickey-Buse-Embden complex, 3 to 9 percent slopesF738C225025871602q5m3nd07119841:12000
Dickey-Foldahl fine sandy loams, 3 to 6 percent slopesI267B75126410651nyv0nd07720051:12000
Dickey-Esmond-Embden complex, 3 to 9 percent slopesF750C461725881752q5m9nd07919901:24000
Dickey-Buse-Embden complex, 3 to 9 percent slopesF738C199725880772q5m3nd07919901:24000
Towner-Dickey loamy fine sands, 3 to 6 percent slopesF735B194725881892q5m0nd07919901:24000
Dickey-Esmond-Embden complex, 6 to 25 percent slopesF750E170125880722q5mcnd07919901:24000
Dickey-Buse-Embden complex, 6 to 25 percent slopesF738E94025881912q5m4nd07919901:24000
Dickey-Buse-Embden complex, 3 to 9 percent slopesG738C54025795262q5wynd08119591:12000
Dickey-Esmond-Embden complex, 3 to 9 percent slopesG750C41525794812q60dnd08119591:12000
Dickey-Towner fine sandy loams, 3 to 6 percent slopesI326B39826412571vh7xnd08119591:12000
Dickey-Esmond-Embden complex, 6 to 25 percent slopesG750E825882472q60gnd08119591:12000
Dickey-Buse-Embden complex, 3 to 9 percent slopesG738C208125820142q5wynd08319901:20000
Dickey-Esmond-Embden complex, 3 to 9 percent slopesG750C172225820182q60dnd08319901:20000
Dickey-Esmond-Embden complex, 6 to 25 percent slopesG750E42225820192q60gnd08319901:20000
Dickey-Buse-Embden complex, 6 to 25 percent slopesG738E29525820152q5x0nd08319901:20000
Towner-Dickey loamy fine sands, 3 to 6 percent slopesG735B9525820112q5wvnd08319901:20000
Dickey-Esmond-Embden complex, 6 to 15 percent slopesG750D65025797852q60fnd09119911:20000
Dickey-Buse-Embden complex, 6 to 15 percent slopesG738D25225797842q5wznd09119911:20000
Dickey-Buse-Embden complex, 6 to 15 percent slopesG738D325882482q5wznd09319901:24000
Towner-Dickey loamy fine sands, 3 to 6 percent slopesF735B21125852722q5m0nd10119671:20000
Dickey-Buse-Embden complex, 6 to 15 percent slopesG738D2027988242q5wzsd08919801:20000
Dickey-Buse-Embden complex, 3 to 9 percent slopesG738C132227993172q5wysd09119701:20000
Dickey fine sandy loam, 2 to 6 percent slopesDcB1346417810g0rrsd10919771:20000
Dickey fine sandy loam, 0 to 2 percent slopesDcA820417809g0rqsd10919771:20000
Dickey-Towner fine sandy loams, 3 to 6 percent slopesI326B12628002101vh7xsd10919771:20000

Map of Series Extent

Approximate geographic distribution of the DICKEY 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 .