Official Series Description


Lab Data Summary

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

Soil series competing with DEAMA 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 DEAMA 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 DEAMA 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.

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

Soil series sharing subgroup-level classification with DEAMA, 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. AZ-2011-05-27-07 | Coconino County Area, Central Part - 1983

    Soil-landscape profile in an area north of Seligman (Soil Survey of Coconino County Area, Arizona, Central Part; 1983).

  2. AZ-2011-05-27-21 | Hualapai-Havasupai Area - 1999

    Typical pattern of soils and parent material in the Deama-Toqui and Natank-Disterheff-Yumtheska general soil map units. The landscape is controlled by the underlying limestone, and soil components vary mainly in depth to rock and slope (Soil Survey of Hualapai-Havasupai Area, Arizona; 1999).

Map Units

Map units containing DEAMA 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
Deama-Rock outcrop complex, 8 to 30 percent slopes1261398526431rs5az63119801:24000
Deama gravelly loam, 2 to 15 percent slopes1055806526411rs3az63119801:24000
Deama stony loam, 1 to 15 percent slopes1135541526421rs4az63119801:24000
Daze-Deama association, moderately steep935533527111rvcaz63119801:24000
Deama-Tovar association, steep1423773526451rs7az63119801:24000
Deama-Toqui complex, 0 to 8 percent slopes136941526441rs6az63119801:24000
Deama-Rock outcrop complex, 1 to 20 percent slopes1518400541851tcxaz63319941:24000
Rock outcrop-Deama complex, 20 to 60 percent slopes534690542281tf9az63319941:24000
Deama family very gravelly loam, 1 to 8 percent slopes143750541841tcwaz63319941:24000
Deama-Rock outcrop complex, 25 to 55 percent slopes1035500545141tqjaz69919931:24000
Deama-Rock outcrop complex, 25 to 55 percent slopes33965615920nnxdaz70120011:24000
Deama-Darvey association, 1 to 10 percent slopes695703376307dmkynm01119831:48000
Deama cobbly loam, 3 to 25 percent slopes589982375879dm44nm01919881:48000
Deama-Laporte association, steepDL844557841w1hnm61219701:24000
Deama-Rock outcrop association, very steep14271885375571dlt6nm63219811:63360
Deama-Pastura association, moderately sloping13262839375570dlt5nm63219811:63360
Deama very cobbly loam, moderately sloping11193213375568dlt3nm63219811:63360
Deama-Pastura association, moderately undulating1235495375569dlt4nm63219811:63360
Rock outcrop-Stroupe-Deama association, extremely steep7326973375636dlw9nm63219811:63360
Deama very stony loam, 12 to 55 percent slopesDE69904566621wytnm63619701:31680
Deama very stony loam, 1 to 12 percent slopesDA39353566611wysnm63619701:31680
Limestone rock landLM3337566711wz3nm63619701:31680
Deama-Darvey-Rock outcrop association, moderately rollingDDC31701375750dlzznm64419811:24000
Deama-Pastura association, moderately rollingDPC20813375751dm00nm64419811:24000
Deama-Rock outcrop-Threadgill complex, hillyDRD19297375752dm01nm64419811:24000
Deama-Rock outcrop complex, 50 to 150 percent slopesDRG36415635639pbfhnm64619761:24000
Deama gravelly loam, 5 to 30 percent slopesDEF26759635637pbffnm64619761:24000
Deama-Rock outcrop complex, 20 to 50 percent slopesDRF21978635638pbfgnm64619761:24000
Rock outcrop-Deama complex, 40 to 150 percent slopesRPG20194635704pbhlnm64619761:24000
Deama-Rock outcrop-Holloman variant complex, 15 to 65 percent slopesDSF16368635640pbfjnm64619761:24000
Tortugas-Deama association, moderately steepTPE9886635718pbj1nm64619761:24000
Tortugas-Deama association, very steepTPG9070635719pbj2nm64619761:24000
Deama gravelly loam, 0 to 5 percent slopesDEB7133635636pbfdnm64619761:24000
Deama-Elpedro-Rock outcrop complex, 10 to 55 percent slopes3585329564101wppnm65619871:24000
Deama-Elpedro association, 5 to 30 percent slopes582525564471wqwnm65619871:24000
Rock outcrop-Deama association, extremely steep7234999565171wt4nm66019811:48000
Deama-Rock outcrop complex, 3 to 40 percent slopes84053630572071xjdnm66419841:24000
Cuate-Deama-Tanbark complex, 15 to 60 percent slopes83040437572021xj7nm66419841:24000
Deama dry-Rock outcrop complex, 10 to 55 percent slopes48217136571251xfrnm66419841:24000
Deama-Rock outcrop complexDe175456559521w6xnm66619741:24000
Deama-Remunda associationDR6856559501w6vnm66619741:24000
Deama-Elpedro-Rock outcrop complex, 10 to 55 percent slopesDaE29629344662whk9nm6781:24000
Deama-Rock outcrop complex, 30 to 90 percent slopes2311365624402002mx74nm68820141:24000
Deama-Penagua-Rock outcrop complex, 35 to 90 percent slopes227284024402102mx7gnm68820141:24000
Deama-Rock outcrop complex, 35 to 65 percent slopes7716055581761yjnnm71920001:24000
Deama-Penalto-Rock outcrop complex, 15 to 35 percent slopes795435581781yjqnm71920001:24000
Deama-Rock outcrop complex, 15 to 35 percent slopes763660581751yjmnm71920001:24000
Deama-Penalto-Rock outcrop complex, 35 to 65 percent slopes802567581791yjrnm71920001:24000
Deama-Penalto-Rock outcrop complex, 5 to 15 percent slopes781597581771yjpnm71920001:24000
Deama-Rock outcrop complex, 5 to 15 percent slopes75678581741yjlnm71920001:24000

Map of Series Extent

Approximate geographic distribution of the DEAMA 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 .