Official Series Description


Lab Data Summary

Aggregate lab data for the ABSHER soil series. This aggregation is based on all pedons with a current taxon name of ABSHER, 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 ABSHER 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
34A40A3271S1975CO107005ABSHER7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.4535828,-107.2937088
5290P070190MT071004Absher5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.8277779,-107.9041672
5290P109090MT071008Absher8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.8277779,-107.9041672
5240A3711S1971MT013005ABSHER7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.3985138,-111.6411591
58A40A3485S1952MT111026Absher6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.9493713,-108.2615814

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ABSHER 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 ABSHER 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 ABSHER 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 ABSHER 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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Click the image to view it full size.

Competing Series

Soil series competing with ABSHER 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 ABSHER 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 ABSHER 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 ABSHER, 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. ND-2012-02-07-41 | Golden Valley County - July 1989

    Typical pattern of soils and parent material in the Absher-Belfield association (Soil Survey of Golden Valley County, North Dakota; July 1989).

Map Units

Map units containing ABSHER 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
Absher loam, 3 to 8 percent slopes41864496990jp4yco68519791:24000
Absher loam, 0 to 3 percent slopes31660496979jp4lco68519791:24000
Gerdrum-Absher complex, 2 to 8 percent slopes165C607173429412wbxxmt01119921:24000
Archin-Absher complex, 2 to 8 percent slopes75C452073432322yk0nmt01119921:24000
Absher-Gerdrum complex, 0 to 4 percent slopes168B345073429492zg6fmt01119921:24000
Gerdrum-Absher complex, 0 to 2 percent slopes165A22655342940chvlmt01119921:24000
Creed-Absher complex, 2 to 8 percent slopes154C19258342913chtqmt01119921:24000
Archin-Absher complex, 0 to 2 percent slopes75A88113432312yk0mmt01119921:24000
Gerdrum-Absher complex, warm, 3 to 9 percent slopes611D304343170cj30mt01119921:24000
Gerdrum-Absher complex, warm, 0 to 3 percent slopes611B261343169cj2zmt01119921:24000
Pinehill-Absher complex, 2 to 15 percent slopes641D4674343601cjjxmt01719951:24000
Creed-Absher complex, 2 to 8 percent slopes813C1652343695cjmymt01719951:24000
Absher silty clay loam, 0 to 8 percent slopes112C12523433032zg67mt01719951:24000
Absher loam, 0 to 8 percent slopesAb41263419932zg69mt02119711:24000
Gerdrum-Absher complex, 2 to 8 percent slopes165C182403421162wbxxmt02519911:24000
Archin-Absher complex, 2 to 8 percent slopes75C162843422852yk0nmt02519911:24000
Absher-Gerdrum complex, 0 to 4 percent slopes168B36603421202zg6gmt02519911:24000
Archin-Absher complex, 0 to 2 percent slopes75A21473422842yk0mmt02519911:24000
Gerdrum-Absher complex, 0 to 2 percent slopes165A1752342115cgzzmt02519911:24000
Creed-Absher complex, 2 to 8 percent slopes154C1419342098cgzfmt02519911:24000
Thebo-Weingart-Absher clays, 4 to 15 percent slopes23545546342474chckmt02719791:24000
Absher-Nobe complex, 0 to 4 percent slopes9267513425942zg6bmt02719791:24000
Gerdrum-Absher complex, 2 to 8 percent slopes11316032342339ch76mt02719791:24000
Gerdrum-Absher complex, 0 to 2 percent slopes11213502342338ch75mt02719791:24000
Absher clay loam, 0 to 4 percent slopes852853425832zg66mt02719791:24000
Weingart-Absher clays, 0 to 4 percent slopes2602518342502chdgmt02719791:24000
Gerdrum-Absher clay loams, 0 to 8 percent slopes559C843339753cdjsmt03320021:24000
Absher silty clay loam, 0 to 8 percent slopes21C813426172zg67mt03320021:24000
Thoeny-Elloam-Absher complex, 0 to 4 percent slopes115B152223438472vyr6mt04119941:24000
Gerdrum-Absher-Creed complex, 0 to 2 percent slopes402A6223343949cjx4mt04119941:24000
Elloam-Absher complex, 0 to 4 percent slopes522A27383439782sy7rmt04119941:24000
Absher-Gerdrum complex, 0 to 2 percent slopes262A2121343889cjv6mt04119941:24000
Thoeny-Elloam-Absher complex, 0 to 4 percent slopes115B61583441342vyr6mt05119921:24000
Elloam-Absher complex, 0 to 4 percent slopes521C28523442212sy7rmt05119921:24000
Gerdrum-Absher clay loams, 0 to 8 percent slopes7012455344436ckdvmt05519811:24000
Thoeny-Absher complex, 2 to 8 percent slopes1382633344336ck9mmt05519811:24000
Absher clay loam, 8 to 15 percent slopes11889344293ck87mt05519811:24000
Adger-Absher complex, 0 to 8 percent slopes31339344391ckcdmt05519811:24000
Nobe-Absher complex, 0 to 4 percent slopes22B5515344507cgjcmt06519961:24000
Nobe-Absher silty clays, 0 to 4 percent slopes719108344742ckqqmt06919891:24000
Creed-Gerdrum-Absher complex, 0 to 4 percent slopes311B19921345123cl40mt10119921:24000
Gerdrum-Absher complex, 0 to 2 percent slopes402A15053345161cl57mt10119921:24000
Absher-Nobe complex, 0 to 2 percent slopes261A4263345109cl3kmt10119921:24000
Elloam-Absher complex, 0 to 4 percent slopes521B30123452112sy7rmt10119921:24000
Absher clay, 0 to 4 percent slopes26B1622345110cl3lmt10119921:24000
Elloam-Absher complex, 0 to 4 percent slopes7771073455892sy7rmt10519761:24000
Absher-Vaeda complex, 1 to 5 percent slopes140110345523cljxmt10519761:24000
Phillips-Nobe-Absher complex, 1 to 5 percent slopes4820926345565cll8mt10519761:24000
Nobe-Absher complex, 0 to 3 percent slopes448262345561cll4mt10519761:24000
Absher complexAc243441467554xq1mt60019691:24000
Ethridge-Absher clay loams, 0 to 2 percent slopesEm116591468044xrmmt60019691:24000
Wayden-Absher complex, undulatingWc33091469694xxymt60019691:24000
Tanna-Absher clay loamsTg5131469474xx7mt60019691:24000
Absher-Nobe complex, 1 to 4 percent slopesAn67053458582zg6dmt60719701:24000
Thoeny-Elloam-Absher complex, 0 to 4 percent slopes1231168653462742vyr6mt60819761:24000
Elloam-Absher complex, 0 to 4 percent slopes40270533464582sy7rmt60819761:24000
Absher-Nobe complex, 0 to 4 percent slopes149053462392zg6bmt60819761:24000
Absher-Nobe complex, 0 to 5 percent slopes1020183341757cgmfmt61319751:24000
Assinniboine-Absher complex, 0 to 2 percent slopes175184341834cgpxmt61319751:24000
Absher complex, 0 to 2 percent slopes91887341978cgvkmt61319751:24000
Virgelle-Absher complex, 0 to 3 percent slopes2121429341882cgrgmt61319751:24000
Fergus-Absher silty clay loams, 0 to 2 percent slopes811326341969cgv8mt61319751:24000
Gerdrum-Absher-Creed complex, 0 to 2 percent slopes402A9155346756cmtpmt61519921:24000
Thoeny-Elloam-Absher complex, 0 to 4 percent slopes521B75313468152vyr6mt61519921:24000
Absher-Nobe complex, 0 to 4 percent slopes261B2444346651cmq9mt61519921:24000
Absher-Gerdrum complex, 0 to 4 percent slopes265B9823466542zg6gmt61519921:24000
Nobe-Absher silty clays, 0 to 4 percent slopes22B4562347372cngkmt62420211:24000
Absher clay loam, 0 to 8 percent slopes163C1304347282cncnmt62420211:24000
Ledger, rarely flooded-Absher complex, 0 to 4 percent slopes622B837189814521q5hmt62420211:24000
Nobe-Absher complex, 0 to 4 percent slopes922B502513695cgjcmt62420211:24000
Absher-Bigsag families, clays, 0 to 4 percent slopes257B47251368450wxmt62420211:24000
Absher-Bigsag families, clays, 0 to 4 percent slopes257B381814982050wxmt63920001:24000
Absher clay, 0 to 8 percent slopes163C11281496912zg68mt63920001:24000
Soapcreek-Absher family complex, 0 to 4 percent slopes461B60714962150phmt63920001:24000
Thibadeau, saline-Absher family complex, 0 to 8 percent slopes255B22814981750wtmt63920001:24000
Thoeny-Elloam-Absher complex, 0 to 4 percent slopes211B991333476322vyr6mt64119941:24000
Phillips-Absher complex, 0 to 4 percent slopes331B89437347674cns9mt64119941:24000
Elloam-Absher complex, 0 to 4 percent slopes521B835933477462sy7rmt64119941:24000
Elloam-Phillips-Absher association, 0 to 8 percent slopes1523C74371347608cnq5mt64119941:24000
Gerdrum-Absher complex, 0 to 4 percent slopes402B20744347704cnt8mt64119941:24000
Phillips-Absher complex, 4 to 8 percent slopes331C13735347675cnsbmt64119941:24000
Scobey-Elloam-Absher gravelly clay loams, 2 to 8 percent slopes567C12232347757cnvzmt64119941:24000
Creed-Absher complex, 0 to 4 percent slopes391B9460347701cnt5mt64119941:24000
Telstad-Absher complex, 2 to 8 percent slopes504C6389347739cnvdmt64119941:24000
Creed-Gerdrum-Absher association, 0 to 4 percent slopes1392B6297347596cnpsmt64119941:24000
Ferd-Absher complex, 0 to 4 percent slopes312B5366347667cns2mt64119941:24000
Absher-Nobe clays, 0 to 4 percent slopes1261B1269347587cnphmt64119941:24000
Absher-Nobe complex, 0 to 4 percent slopes557363480812zg6cmt64919851:24000
Absher silty clay loam, 0 to 8 percent slopes7136943482042zg67mt65519751:24000
Nobe-Absher complex, 0 to 4 percent22B26917125771vh2fmt65519751:24000
Gerdrum-Absher clay loams, 0 to 2 percent slopes114A4356348301cpfjmt65719901:24000
Creed-Absher complex, 0 to 4 percent slopes137B3017348344cpgxmt65719901:24000
Absher clay loam, wet, 0 to 2 percent slopes214A2642348440cpl0mt65719901:24000
Nobe-Absher complex, 0 to 4 percent slopes22B7014341662cgjcmt66620081:24000
Absher clay, 0 to 8 percent slopes163C202824171wnm5mt6691:24000
Rhoades-Absher complex, 2 to 6 percent slopesRrB1622699289312b5tnd01119691:20000
Rhoades-Absher complex, 0 to 2 percent slopesRrA514099289212b5snd01119691:20000
Absher-Slickspots complex, 0 to 9 percent slopesAeB55246353136cvghsd01919701:24000
Absher-Loburn fine sandy loams, 3 to 9 percent slopesAbB13074353135cvggsd01919701:24000
Absher-Loburn fine sandy loams, 0 to 3 percent slopesAbA374333336302zj56sd01919701:24000
Absher-Slickspots complex, 2 to 6 percent slopesAlB26510355417cxv2sd60119831:24000
Absher loam, 0 to 3 percent slopes1012638502179jvkbwy62519851:24000
Absher-Forelle complex, 3 to 15 percent slopes -- draft3951363124379832mtxmwy6301:24000
Absher-Stylite complex, 1 to 7 percent slopes -- draft4231046625160432qftdwy6301:24000
Absher variant silty clay loam, 1 to 5 percent slopes -- draft416671424554782nf3zwy6301:24000
Absher-Elkol-Havre complex, 0 to 6 percent slopes0601275915758158z8wy6471:24000
Havre-Absher-Forelle loams, 0 to 6 percent slopes033833515753258xpwy6471:24000
Abston-Absher complex, 0 to 6 percent slopes020707715743158tfwy6471:24000
Havre-Absher-Forelle loams, 0 to 6 percent slopes541387190155621tqjwy67719751:24000
Absher-Elkol complex, 0 to 4 percent slopes62586190154521tq5wy67719751:24000
Havre-Absher-Forelle loams, 0 to 6 percent slopes15757390503022jwfjwy71319861:24000
Countryman-Absher complex, 0 to 3 percent slopes13310886502998jwdrwy71319861:24000
Absher-Elkol complex, 0 to 4 percent slopes1007033502957jwcfwy71319861:24000
Tisworth-Absher-Forelle complex, 0 to 6 percent slopes2125353503088jwhnwy71319861:24000
Venapass-Uhl-Absher loams, 1 to 6 percent slopes2185174503097jwhywy71319861:24000
Absher-Poposhia-Sinkson complex, 1 to 10 percent slopes1012685502959jwchwy71319861:24000
Absher variant-Absher complex, 0 to 6 percent slopes1022167502961jwckwy71319861:24000
Absher-Bearbou complex, 0 to 3 percent slopes1001418826119752qsvnwy7231:24000

Map of Series Extent

Approximate geographic distribution of the ABSHER 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 .