Official Series Description


Lab Data Summary

Aggregate lab data for the DEAN soil series. This aggregation is based on all pedons with a current taxon name of DEAN, 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 DEAN 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 DEAN 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 DEAN 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 DEAN 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 DEAN 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 DEAN 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 DEAN 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 DEAN 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.

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 DEAN, 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 DEAN 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
Rolie-Dean complex, 2 to 20 percent slopes1282310798508vsxbaz69720051:24000
Rolie-Dean complex, 2 to 20 percent slopes4025460545301tr1az69919931:24000
Harvey-Dean loams, 3 to 15 percent slopes8516263375895dm4nnm01919881:48000
Dean soils, 0 to 9 percent slopesDd20880376338dmlynm02119681:31680
Campus-Dean association, gently slopingCN19606376321dmldnm02119681:31680
Campus-Dean association, warm, 0 to 9 percent slopesCNwD1164731561842xxwdnm02119681:31680
Dean soils, 0 to 9 percent slopesDE4912376333dmlsnm02119681:31680
Dean soils, warm, 0 to 9 percent slopesDEwD118931561852xxwmnm02119681:31680
Dean-Pinon association, gently slopingDP1140557851w1jnm61219701:24000
Tapia-Dean association, undulatingTD51161375555dlspnm63019771:48000
Dioxice-Dean association, undulatingDA1218375517dlrgnm63019771:48000
Harvey-Dean association, 1 to 9 percent slopes73863395571831xhmnm66419841:24000
Harvey-Dean complex, 1 to 7 percent slopes44641510571131xfcnm66419841:24000
Ildecarb-Dean gravelly loams, 1 to 10 percent slopes74918414571841xhnnm66419841:24000
Tapia-Dean loams, 0 to 5 percent slopesTd10930814739791lgsqnm67419651:24000
Harvey-Dean loams, 1 to 9 percent slopesHh10453514739141lgqmnm67419651:24000
Dean loam, 1 to 9 percent slopesDe5211614739021lgq7nm67419651:24000
Hagerman-Dean complex, 1 to 5 percent slopesHd4494414739101lgqhnm67419651:24000
Harvey and Dean soils, erodedHm2420414739151lgqnnm67419651:24000
Tapia and Dean soils, erodedTe977914739801lgsrnm67419651:24000
Clovis-Dean loams, 0 to 5 percent slopesCp863714738991lgq4nm67419651:24000
Penistaja-Dean fine sandy loams, 1 to 5 percent slopesPo779114739561lgrznm67419651:24000
Penistaja-Dean complex, 1 to 5 percent slopesPn728314739551lgrynm67419651:24000
Tapia-Dean association, moist,1 to 5 percent slopesTDC12129424732wl56nm6781:24000

Map of Series Extent

Approximate geographic distribution of the DEAN 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 .