Official Series Description


Lab Data Summary

Aggregate lab data for the DRANYON soil series. This aggregation is based on all pedons with a current taxon name of DRANYON, 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 DRANYON 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
43B07N0224S2006ID011001Dranyon7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.2103615,-111.6879425

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the DRANYON 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 DRANYON 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 DRANYON 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 DRANYON 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 DRANYON 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 DRANYON 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 DRANYON 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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Soil series sharing subgroup-level classification with DRANYON, 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. ID-2011-06-01-08 | Bingham Area - 1973

    Representative pattern of soils in association 8 (Soil Survey of Bingham Area, Idaho; 1973).

Map Units

Map units containing DRANYON 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
Dranyon loam, 3 to 20 percent slopes592855497236jpdwco68619921:31680
Greys-Dranyon complex, 12 to 30 percent slopes43B728134824282852mhtsid65020111:24000
Dranyon-Dra complex, 12 to 45 percent slopes43B72186024080482ltrzid65020111:24000
Dranyon silt loam, 2 to 25 percent slopes43B72570124282502mhsnid65020111:24000
Greys-Dranyon complex, 2 to 12 percent slopes43B73047724283432mhwnid65020111:24000
Kucera-Dranyon-Tetonia complex, 2 to 15 percent slopes1346342924278422mhchid65020111:24000
Dranyon-Dehana gravelly loams, 2 to 40 percent slopes52715486214j9ybid67519921:24000
Dranyon-Ricrest association, steep171875825902ry6id70919761:24000
Manila-Dranyon association, hilly341552826092rytid70919761:24000
Moohoo-Dranyon association, steepMHG6037827442s35id71019681:24000
Dranyon silt loam, rollingDRF3412827092s21id71019681:24000
Moohoo-Dranyon association, hillyMHF1335827432s34id71019681:24000
Dranyon-Hades-Hagenbarth complex, 10 to 35 percent slopes320051532389542pt1sid71019681:24000
Yago, very bouldery surface-Dranyon-Beaverdam complex, 5 to 30 percent slopes226014225584442pcynid71019681:24000
Camelback, very deep-Dranyon-Beehunt complex, 8 to 35 percent slopes2011932389512x3mxid71019681:24000
Pavohroo-Dranyon association, 10 to 30 percent slopesPDE1873238966n4c9id71119831:24000
Yago, very bouldery surface-Dranyon-Beaverdam complex, 5 to 30 percent slopes226011025584342pcynid71119831:24000
Dranyon-Hades-Hagenbarth complex, 10 to 35 percent slopes32002632389742pt1sid71119831:24000
Lag-Dranyon complex, 10 to 60 percent slopes126124331635032wd4wid71220081:24000
Dranyon silt loam, 10 to 40 percent slopes79103731634982wd4xid71220081:24000
Chokecherry-Dranyon complex, 15 to 60 percent slopes5233315450955s5id71220081:24000
Winnemucca, bouldery surface-Dranyon-Bailcreek family, extremely bouldery surface, complex, 10 to 30 percent slopes1046a20831732962wzzyid71220081:24000
Ezbin-Cluff family, bouldery surface-Dranyon complex, 8 to 25 percent slopes10603131732982x008id71220081:24000
Hondoho, very stony surface-Clegg-Dranyon complex, 25 to 60 percent slopes10352931732932w9rtid71220081:24000
Booneville-Dranyon-Zeebar family, very stony surface, complex, 15 to 40 percent slopes10582131732972x006id71220081:24000
Ezbin-Cluff family, bouldery surface-Dranyon complex, 8 to 25 percent slopes1060448729808462x008id7131:24000
Winnemucca, bouldery surface-Dranyon-Bailcreek family, extremely bouldery surface, complex, 10 to 30 percent slopes1046a363929808362wzzyid7131:24000
Booneville-Dranyon-Zeebar family, very stony surface, complex, 15 to 40 percent slopes1058282129808442x006id7131:24000
Ireland-Hondoho-Dranyon complex, 15 to 50 percent slopes2550170625202482pt1nid7131:24000
Booneville-Farlow family, very stony surface-Dranyon complex, 25 to 50 percent slopes1058a164629808452x007id7131:24000
Yago, very bouldery surface-Dranyon-Beaverdam complex, 5 to 30 percent slopes2260162025145972pcynid7131:24000
Kingmine family-Dranyon-Starley family, complex, 45 to 75 percent slopes986117329638872wv3gid7131:24000
Dranburn-Winnemucca-Booneville, complex, 15 to 35 percent slopes, MLRA 43B86186729842422x03nid7131:24000
Dranyon-Goodski family, complex, 25 to 55 percent slopes89469429638652wv2qid7131:24000
Hondoho, very stony surface-Clegg-Dranyon complex, 25 to 60 percent slopes103568829170362w9rtid7131:24000
Pavohroo-Lund-Dranyon complex, 12 to 40 percent slopes703251829810662yvfcid7131:24000
Lag-Dranyon complex, 10 to 60 percent slopes12636929170472wd4wid7131:24000
Ireland-Dranyon-Hagenbarth complex, 20 to 50 percent slopes708033930938852xxdqid7131:24000
Dranburn-Dranyon-Calpac complex, 15 to 50 percent slopes706017730938842xxdmid7131:24000
Dranyon-Booneville-Hagenbarth complex, 5 to 30 percent slopes700516729810672xxdjid7131:24000
Chokecherry-Dranyon complex, 15 to 60 percent slopes5287309389655s5id7131:24000
Dranyon silt loam, 10 to 40 percent slopes79-BL8329170482wd4xid7131:24000
Clegg-Drage-Dranyon complex, 12 to 50 percent slopes70857429810732xxdrid7131:24000
Booneville-Dranyon-Ireland complex, 20 to 55 percent slopes70102929809192xxdkid7131:24000
Chippy-Dranyon complex, 5 to 35 percent slopes70701529809182xxdsid7131:24000
Hagenbarth-Dranyon-Crystalbutte complex, 12 to 45 percent slopes7035632185622z43rid7131:24000
Mayhill-Dranyon complex, 10 to 35 percent slopes10301199824270682mgkjid7161:24000
Dranyon-Hades-Hagenbarth complex, 10 to 35 percent slopes3200936624954742pt1sid7161:24000
Dranyon-Ireland-Buist complex, 12 to 60 percent slopes500AA604124255162mdygid7161:24000
Dranburn-Dranyon-Calpac complex, 15 to 50 percent slopes7060412530740382xxdmid7161:24000
Booneville-Dranyon-Ireland complex, 20 to 55 percent slopes7010381630740362xxdkid7161:24000
Ireland-Hondoho-Dranyon complex, 15 to 50 percent slopes2550277424954702pt1nid7161:24000
Chippy-Dranyon complex, 5 to 35 percent slopes7070275530740432xxdsid7161:24000
Hagenbarth-Dranyon-Crystalbutte complex, 12 to 45 percent slopes7035252031756322z43rid7161:24000
Dranyon silt loam, 10 to 40 percent slopes79249831364332wd4xid7161:24000
Pavohroo-Lund-Dranyon complex, 12 to 40 percent slopes7032249531568312yvfcid7161:24000
Camelback, very deep-Dranyon-Beehunt complex, 8 to 35 percent slopes2011236229897342x3mxid7161:24000
Dranyon-Booneville-Hagenbarth complex, 5 to 30 percent slopes7005206930740352xxdjid7161:24000
Yago, very bouldery surface-Dranyon-Beaverdam complex, 5 to 30 percent slopes2260166724841432pcynid7161:24000
Cinderspring-Dranyon association, 5 to 40 percent slopes718760531364302ypjqid7161:24000
Dranyon-Goodski family, complex, 25 to 55 percent slopes89455531634582wv2qid7161:24000
Clegg-Drage-Dranyon complex, 12 to 50 percent slopes708554130740422xxdrid7161:24000
Ireland-Dranyon-Hagenbarth complex, 20 to 50 percent slopes708047330740412xxdqid7161:24000
Pavohroo-Dranyon association, 10 to 30 percent slopesPDE125600014n4c9id7161:24000
Greys-Dranyon complex, 12 to 30 percent slopes43B72891025185722qf5pid75819981:24000
Dranyon-Dra complex, 12 to 45 percent slopes43B72143425185692qf5lid75819981:24000
Dranyon silt loam, 2 to 25 percent slopes43B72525325185712qf5nid75819981:24000
Greys-Dranyon complex, 2 to 12 percent slopes43B7305225185732qf5qid75819981:24000
Dranyon silt loam, 4 to 45 percent slope, extremely stony915493842082tmdid76919781:24000
Dranyon silt loam, hillyDRF22399799052p4lid77019681:24000
Dranyon silt loam, steepDRG3841799062p4mid77019681:24000
Dranyon-Gilispie complex, hillyDSF1030799072p4nid77019681:24000
Dranyon-Hades-Hagenbarth complex, 10 to 35 percent slopes320049632389912pt1sid77019681:24000
Camelback, very deep-Dranyon-Beehunt complex, 8 to 35 percent slopes201110132389882x3mxid77019681:24000
Dranyon-Ireland-Buist complex, 12 to 60 percent slopes500AA7732389792mdygid77019681:24000
Dranyon-Tolman variant complex, 8 to 20 percent slopes214866553401vl5ut63319831:24000
Grassyhollow-Conwaycreek-Dranyon complex, 15 to 50 percent slopes5623324524870642pgzwwy6351:24000
Quakenasp-Philipsburg-Dranyon complex, 15 to 45 percent slopes811531696892y0ygwy7231:24000
Quakenasp-Philipsburg-Dranyon complex, 4 to 15 percent slopes811231696862y0ycwy7231:24000
Quietus-Swede-Dranyon complex, 15 to 45 percent slopes812131696922y0ykwy7231:24000
Quakenasp-Toponce-Dranyon complex, 15 to 35 percent slopes812031696982y0yrwy7231:24000
Grassyhollow-Conwaycreek-Dranyon complex, 15 to 50 percent slopes5623360325154342pgzwwy7231:24000

Map of Series Extent

Approximate geographic distribution of the DRANYON 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 .