Official Series Description


Lab Data Summary

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

Competing Series

Soil series competing with DRAGE 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 DRAGE 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 DRAGE 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

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

Soil series sharing subgroup-level classification with DRAGE, 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 DRAGE 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
Drage gravelly loam, cool, 2 to 15 percent slopes309843793152njkid68019851:24000
Drage very gravelly loam, cool, 0 to 3 percent slopes311641793162njlid68019851:24000
Drage gravelly loam, 4 to 8 percent slopes28972793122njgid68019851:24000
Drage gravelly loam, 8 to 12 percent slopes29375793132njhid68019851:24000
Justesen-Drage complex, 2 to 15 percent slopes98-CL7531736092smvid7031:24000
Drage-Vitale, stony surface-Broadhead association, 5 to 30 percent slopesDGF93238965n4bkid71119831:24000
Cedarhill-Clegg-Drage complex, 5 to 55 percent slopes47729331634922dvl1id71220081:24000
Ireland, extremely stony surface-Drage family, complex, 15 to 35 percent slopes106969731733002x00did71220081:24000
Drage-Causey-Lilcan complex, 10 to 35 percent slopes74581784243vb25id71220081:24000
Drage family-Geemore family-Laschance complex, 10 to 35 percent slopes202149031733132x01fid71220081:24000
Ireland, extremely stony surface-Drage family, complex, 35 to 65 percent slopes100913931732912w9rmid71220081:24000
Remainder-Thatcher-Drage complex, 4 to 15 percent slopes35431129844062xyfnid71220081:24000
Ireland, extremely stony surface-Drage family, complex, 35 to 65 percent slopes10091014029170302w9rmid7131:24000
Ireland, extremely stony surface-Drage family, complex, 15 to 35 percent slopes1069530029808502x00did7131:24000
Drage family-Geemore family-Laschance complex, 10 to 35 percent slopes2021259429808822x01fid7131:24000
Cedarhill-Clegg-Drage complex, 5 to 55 percent slopes47-BL7629657182dvl1id7131:24000
Clegg-Drage-Dranyon complex, 12 to 50 percent slopes70857429810732xxdrid7131:24000
Ireland, extremely stony surface-Drage family, complex, 35 to 65 percent slopes10093631733492w9rmid71419971:24000
Bezzant-Watkins Ridge-Drage complex, 12 to 50 percent slopes5520162131365442ypjvid7161:24000
Cedarhill-Clegg-Drage complex, 5 to 55 percent slopes47157022300792dvl1id7161:24000
Drage-Vitale, stony surface-Broadhead association, 5 to 30 percent slopesDGF594599991n4bkid7161:24000
Clegg-Drage-Dranyon complex, 12 to 50 percent slopes708554130740422xxdrid7161:24000
Justesen-Drage complex, 2 to 15 percent slopes983701832612smvid75219991:24000
Justesen-Drage complex, 1 to 20 percent slopes474473790572n87id76319981:24000
Drage gravelly loam, cool, 2 to 15 percent slopes14980633312p80fid76319981:24000
Drage gravelly loam, cool, 2 to 15 percent slopes1352514870431lxd4id78019981:24000
Justesen-Drage complex, 1 to 20 percent slopes2714115314091ndk9id78019981:24000
Drage very gravelly loam, cool, 0 to 3 percent slopes14315902561qcslid78019981:24000
Cedarhill-Clegg-Drage complex, 5 to 55 percent slopes471623962492lfhcut60419801:24000
Remainder-Thatcher-Drage complex, 4 to 15 percent slopes354329253012xyfnwy7231:24000
Drage-Vicking complex, 2 to 15 percent slopes375029253142xyfvwy7231:24000
Drage-Bruner, very stony surface-Clegg complex, 15 to 60 percent slopes380231608882yx30wy7231:24000

Map of Series Extent

Approximate geographic distribution of the DRAGE 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 .