Official Series Description


Lab Data Summary

Aggregate lab data for the DATEMAN soil series. This aggregation is based on all pedons with a current taxon name of DATEMAN, 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 DATEMAN 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 DATEMAN 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 DATEMAN 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 DATEMAN 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 DATEMAN 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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Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

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

Competing Series

Soil series competing with DATEMAN 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 DATEMAN series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the DATEMAN 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 .

There are insufficient data to create the 2D hillslope position figure.

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 DATEMAN, 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. UT-2012-03-22-17 | Tooele Area - 2000

    Typical pattern of soils and parent material in the Lodar-Reywat-Lundy and Dateman-Podmor-Rock outcrop general soil map units (adjacent to the Borvant-Abela-Kapod general soil map unit). (Soil Survey of Tooele Area, Utah; Tooele County and Parts of Box Elder, Davis, and Juab Counties, Utah, and Parts of White Pine and Elko Counties, Nevada; 2000).

Map Units

Map units containing DATEMAN 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
Dateman gravelly loam, 30 to 50 percent slopes229600496762jnxlco68319771:24000
Dateman, cool-Sapphire-Secondset loams, 3 to 25 percent slopes3528144496876jp18co68419841:24000
Farlow-Dateman-Rock outcrop complex, 8 to 25 percent slopes4225948496884jp1jco68419841:24000
Nimerick-Clinetop-Dateman-Cool loams, 1 to 25 percent slopes818653496927jp2xco68419841:24000
Dateman, cool-Secondset-Nimerick loams, 3 to 35 percent slopes375510496878jp1bco68419841:24000
Dateman, cool-Sapphire-Secondset loams, 25 to 65 percent slopes364474496877jp19co68419841:24000
Ireland, extremely stony surface-Dateman-Pavohroo association, 20 to 60 percent slopes60839231635412v05lid71119831:24000
Pavohroo-Broad Canyon-Dateman complex, 20 to 55 percent slopes2560182232389732pt1pid71119831:24000
Ricafied-Dateman-Pavohroo association, 20 to 60 percent slopes420F2723238964n465id71119831:24000
Pavohroo-Broad Canyon-Dateman complex, 20 to 55 percent slopes2560139929170552pt1pid7131:24000
Ireland, extremely stony surface-Dateman-Pavohroo association, 20 to 60 percent slopes6080725145852v05lid7131:24000
Ricafied-Dateman-Pavohroo association, 20 to 60 percent slopes420F3842917056n465id7131:24000
Ricafied-Dateman-Pavohroo association, 20 to 60 percent slopes420F173173332n465id71419971:24000
Pavohroo-Broad Canyon-Dateman complex, 20 to 55 percent slopes2560389424954712pt1pid7161:24000
Mayhill-Booneville-Dateman complex, 15 to 60 percent slopes7030239229897292x3mrid7161:24000
Ricafied-Dateman-Pavohroo association, 20 to 60 percent slopes420F2153599855n465id7161:24000
Mayhill-Booneville-Dateman complex, 15 to 60 percent slopes70309532389962x3mrid77019681:24000
Parkay-Dateman families association, 20 to 60 percent slopes5816146481268j4ssut60119851:24000
AGASSIZ-DATEMAN ASSOCIATION, ERODEDADG214318482657j67lut60319681:20000
DATEMAN EXTREMELY ROCKY SILT LOAM, 40 TO 80 PERCENT SLOPESDEG7950482703j692ut60319681:20000
DATEMAN-BRADSHAW ASSOCIATIONDHG3258482704j693ut60319681:20000
PICAYUNE-SMARTS ASSOCIATIONPRG877482795j6d1ut60319681:20000
Dateman gravelly loam, 40 to 70 percent slopesDAG178482890j6h3ut61219671:20000
Flygare-Dateman families-Rock outcrop association, 25 to 80 percent slopes222753331838462whrhut6171:24000
Dateman, moist-Croydon families complex, 30 to 60 percent slopes14532432832zsd1ut6451:24000
Dateman, extremely stony-Adel families complex, 15 to 60 percent slopesmt546768331484130hl4ut6451:24000
Dateman-Bradshaw families association, 30 to 70 percent slopesR3630623905ny6zut6471:24000

Map of Series Extent

Approximate geographic distribution of the DATEMAN 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 .