Official Series Description


Lab Data Summary

Aggregate lab data for the TANNA soil series. This aggregation is based on all pedons with a current taxon name of TANNA, 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 TANNA 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
43B89P044077MT077215Tanna5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.5023956,-112.726738
4491P094491MT093005Tanna5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.997776,-112.7166672

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the TANNA 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 TANNA 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 TANNA 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 TANNA 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 TANNA 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 TANNA 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 TANNA 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 TANNA, 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 TANNA 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
Tanna-Pinelli complex, 12 to 25 percent slopes1034392497932jq4bco65519841:24000
Tanna-Pinelli complex, 1 to 6 percent slopes1012572497930jq48co65519841:24000
Tanna-Pinelli complex, 6 to 12 percent slopes1021145497931jq49co65519841:24000
Tanna silty clay loam, 25 to 45 percent slopes643700496808jnz2co68319771:24000
Tanna-Ethridge silty clay loams, 2 to 8 percent slopes164C2097342937chvhmt01119921:24000
Tanna silty clay loam, 2 to 8 percent slopes64C1206343199cj3ymt01119921:24000
Tanna-Ethridge silty clay loams, 8 to 15 percent slopes164D817342938chvjmt01119921:24000
Tanna-Ethridge silty clay loams, 2 to 8 percent slopes164C3597342113cgzxmt02519911:24000
Tanna silty clay loam, 2 to 8 percent slopes64C2119342265ch4tmt02519911:24000
Tanna-Ethridge silty clay loams, 8 to 15 percent slopes164D1003342114cgzymt02519911:24000
Tanna-Ethridge silty clay loams, 3 to 6 percent slopesL1025B13632234952qk4bmt02519911:24000
Tanna-Abor complex, 2 to 8 percent slopes22315337342461chc4mt02719791:24000
Ernem-Delplain-Tanna complex, 4 to 25 percent slopes865776342590chh9mt02719791:24000
Tanna silty clay loam, 0 to 4 percent slopes2225423342460chc3mt02719791:24000
Tanna-Ethridge-Cabston complex, 8 to 25 percent slopes2242094342462chc5mt02719791:24000
Cabbart-Tanna loams, 4 to 15 percent slopes153D1269344488ckgjmt06519961:24000
Tanna loam, 1 to 6 percent slopes53A1127344597cgkjmt06519961:24000
Tanna-Cabbart loams, 2 to 8 percent slopes153C1112344487cghymt06519961:24000
Tanna clay loam, 1 to 6 percent slopes756229344746ckqvmt06919891:24000
Tanna-Weingart complex, 2 to 8 percent slopes765690344747ckqwmt06919891:24000
Tanna clay loam, 0 to 4 percent slopes13B2691345065cl24mt10119921:24000
Tanna clay loam, 4 to 8 percent slopes13C658345066cl25mt10119921:24000
Tanna-Beenom complex, 4 to 8 percent slopesFc15043454182zg53mt10319611:20000
Rentsac-Tanna complex, 2 to 15 percent slopes369D34419466641ndzcmt11119661:20000
Tanna loam, 1 to 6 percent slopes53A402396138cgkjmt11119661:20000
Tanna clay loam, 4 to 8 percent slopesTf86791469464xx6mt60019691:24000
Tanna-Wayden clay loams, rollingTh42621469484xx8mt60019691:24000
Tanna clay loam, 2 to 4 percent slopesTe28161469454xx5mt60019691:24000
Tanna-Absher clay loamsTg5131469474xx7mt60019691:24000
Tanna clay loam, 2 to 8 percent slopes19219627341859cgqqmt61319751:24000
Tanna clay loam, 0 to 2 percent slopes1913717341858cgqpmt61319751:24000
Tanna-Wabek complex, 2 to 10 percent slopes1941231341861cgqsmt61319751:24000
Tanna clay loam, 8 to 15 percent slopes193813341860cgqrmt61319751:24000
Tanna clay loam, 2 to 8 percent slopes13C928346596cmnjmt61519921:24000
Tanna loam, 8 to 15 percent slopes65D3791445444vdqmt62119971:24000
Tanna loam, 4 to 8 percent slopes65C2371445434vdpmt62119971:24000
Tanna-Boxwell loams, 4 to 8 percent slopes265C1041443014v4wmt62119971:24000
Tanna-Boxwell loams, 8 to 15 percent slopes265D861443024v4xmt62119971:24000
Tanna-Boxwell loams, 0 to 4 percent slopes265B411443004v4vmt62119971:24000
Tanna-Udecide complex, 15 to 35 percent slopes740E895155703570pmt62219971:24000
Tanna-Udecide complex, 8 to 15 percent slopes740D467155702570nmt62219971:24000
Tanna clay loam, 4 to 8 percent slopes40C21215546156rwmt62219971:24000
Marmarth, very stony-Marmarth-Tanna, very stony, 4 to 8 percent slopes136C577323844782l17nmt62420211:24000
Marmarth, very stony-Marmarth-Tanna, very stony, 8 to 15 percent slopes136D447723847982l1kzmt62420211:24000
Marmarth, very stony-Marmarth-Tanna, very stony, 15 to 35 percent slopes136F261523847992l1l0mt62420211:24000
Tanna-Cabbart complex, 2 to 8 percent slopes129C1266251344450psmt62420211:24000
Ethridge-Tanna clay loams, 2 to 8 percent slopes169C1221251367250s1mt62420211:24000
Marmarth, very stony-Marmarth-Tanna, very stony, 2 to 4 percent slopes136B119823839742l0qdmt62420211:24000
Tanna-Greybear-Cooers complex, 4 to 8 percent slopes126C112023932042lbb4mt62420211:24000
Tanna-Greybear-Cooers complex, 8 to 15 percent slopes126D108523932052lbb5mt62420211:24000
Tanna-Hinterland clay loams, 2 to 8 percent slopes130C813251344850pvmt62420211:24000
Tanna-Cabbart complex, 8 to 15 percent slopes129D726251344650ptmt62420211:24000
Tanna-Greybear-Cooers complex, 15 to 35 percent slopes126E69923938742lc0rmt62420211:24000
Rentsac-Tanna complex, 8 to 15 percent slopes440D5541914106227scmt62420211:24000
Cabbart-Tanna-Rock outcrop complex, 2 to 15 percent slopes242D385347396cnhbmt62420211:24000
Tanna-Greybear-Cooers complex, 2 to 4 percent slopes126B34623886322l5knmt62420211:24000
Tanna clay loam, 2 to 8 percent slopes, fan53C24419124202260zmt62420211:24000
Tanna loam, 1 to 6 percent slopes53A1103176856cgkjmt62420211:24000
Rentsac-Tanna complex, 15 to 35 percent slopes369E52513687510gmt62420211:24000
Tanna clay loam, 2 to 8 percent slopes142C2317685550qqmt62420211:24000
Tanna-Hinterland clay loams, 2 to 8 percent slopes130C1251914963250pvmt63920001:24000
Tanna-Cabbart complex, 2 to 8 percent slopes129C1174914963050psmt63920001:24000
Rentsac-Tanna complex, 2 to 15 percent slopes369D4182149929510fmt63920001:24000
Cabbart-Tanna complex, 2 to 8 percent slopes117C313114961650pbmt63920001:24000
Tanna, calcareous,-Rentsac complex, 2 to 8 percent slopes366C30231499245108mt63920001:24000
Tanna-Hinterland clay loams, 8 to 15 percent slopes130D266914963350pwmt63920001:24000
Rentsac-Tanna complex, 15 to 35 percent slopes369E1980149930510gmt63920001:24000
Tanna-Cabbart complex, 8 to 15 percent slopes129D195014963150ptmt63920001:24000
Rentsac-Tanna-Rock outcrop complex, 8 to 35 percent slopes368E1671149928510dmt63920001:24000
Tanna clay loam, 2 to 8 percent slopes142C149014965950qqmt63920001:24000
Tanna, calcareous,-Rentsac complex, 8 to 15 percent slopes366D14571499255109mt63920001:24000
Tanna-Yawdim complex, 2 to 8 percent slopes442C1001150008512zmt63920001:24000
Tanna-Boxwell, calcareous, complex, 2 to 8 percent slopes172C61814970450s5mt63920001:24000
Tanna-Boxwell, calcareous, complex, 8 to 15 percent slopes172D27914970550s6mt63920001:24000
Ethridge-Tanna clay loams, 2 to 8 percent slopes169C22714970050s1mt63920001:24000
Evanston-Tanna complex, 2 to 8 percent slopes445C2171500125133mt63920001:24000
Tanna-Boxwell loams, 4 to 8 percent slopes265C11521456284wjpmt64419951:24000
Tanna-Boxwell loams, 8 to 15 percent slopes265D7821456294wjqmt64419951:24000
Tanna loam, 4 to 8 percent slopes65C5731458534wrymt64419951:24000
Tanna loam, 8 to 15 percent slopes65D4871458544wrzmt64419951:24000
Tanna-Rentsac complex, 4 to 15 percent slopes56142724348189cp9xmt65519751:24000
Tanna clay loam, 2 to 8 percent slopes5346527348186cp9tmt65519751:24000
Tanna-Beenom complex, 4 to 8 percent slopes5532548348188cp9wmt65519751:24000
Tanna clay loam, 8 to 15 percent slopes544134348187cp9vmt65519751:24000
Tanna loam, 1 to 6 percent slopes53A407117125491vh1jmt65519751:24000
Tanna-Hinterland clay loams, 2 to 8 percent slopes130C715361434d435mt65519751:24000
Tanna-Cabbart complex, 2 to 8 percent slopes129C515361436d437mt65519751:24000
Tanna-Cabbart complex, 8 to 15 percent slopes129D229361435d436mt65519751:24000
Rentsac-Tanna complex, 2 to 15 percent slopes369D10417125691vh25mt65519751:24000
Tanna-Hinterland clay loams, 8 to 15 percent slopes130D20361433d434mt65519751:24000
Tanna-Cabbart loams, 2 to 8 percent slopes253C817125881vh2smt65519751:24000
Megonot-Tanna clay loams, 2 to 8 percent slopes270C11697348514cpndmt65719901:24000
Megonot-Richey-Tanna clay loams, 2 to 8 percent slopes148C11363348355cph8mt65719901:24000
Tanna clay loam, 0 to 4 percent slopes82B7030348809cpyxmt65719901:24000
Tanna-Cabbart complex, 2 to 8 percent slopes129C5887251344550psmt66620081:24000
Tanna loam, 1 to 6 percent slopes53A3994341698cgkjmt66620081:24000
Tanna-Cabbart loams, 2 to 8 percent slopes253C2973341649cghymt66620081:24000
Warhorse-Delplain-Tanna complex, 4 to 35 percent slopes165D155915318171ndzgmt66620081:24000
Tanna-Warhorse loams, 4 to 15 percent slopes164C144715318181ndzhmt66620081:24000
Rentsac-Tanna complex, 2 to 15 percent slopes369D130915318141ndzcmt66620081:24000
Tanna-Hinterland clay loams, 2 to 8 percent slopes130C290251344950pvmt66620081:24000
Rentsac-Tanna-Rock outcrop complex, 8 to 35 percent slopes368E20915318081ndz5mt66620081:24000
Ethridge-Tanna clay loams, 2 to 8 percent slopes169C112251367350s1mt66620081:24000
Tanna-Cabbart complex, 8 to 15 percent slopes129D61251344750ptmt66620081:24000
Tanna-Yawdim complex, 2 to 8 percent slopes442C5915318101ndz7mt66620081:24000
Reedpoint-Tanna-Ethridge complex, 4 to 35 percent slopes5502E8343156661580lmt6691:24000
Rentsac-Tanna-Cabbart complex, 4 to 35 percent slopes5518E2831699249rgmfmt6691:24000
Cabbart-Tanna-Rock outcrop complex, 25 to 60 percent slopes5601F2737156723582lmt6691:24000
Ethridge-Tanna-Reedpoint complex, 2 to 15 percent slopes5401D2718156719582gmt6691:24000
Cabbart-Tanna-Reedpoint complex, 2 to 15 percent slopes5305D1948636155pbz4mt6691:24000
Tanna-Janesburg, low precipitation-Scairt complex, 3 to 6 percent slopesL0654B17827071372qk41nd02519811:20000
Tanna-Ethridge silty clay loams, 3 to 6 percent slopesL1025B17627073192qk4bnd03319851:24000
Tanna-Janesburg, low precipitation-Scairt complex, 3 to 6 percent slopesL0654B19427158872qk41nd08719741:20000
Tanna-Ethridge silty clay loams, 3 to 6 percent slopesL1025B18527158922qk4bnd08719741:20000
Tanna silty clay loam, 2 to 9 percent slopesTnB5407355797cy7bsd06319841:24000
Tanna-Rhoades complex, 2 to 9 percent slopesToC3814355799cy7dsd06319841:24000
Tanna-Gerdrum complex, 0 to 3 percent slopesToA2376355798cy7csd06319841:24000
Tanna-Savo complex, 2 to 6 percent slopesTsB33011355471cxwtsd60119831:24000
Tanna-Delridge complex, 2 to 6 percent slopesTdB16640355469cxwrsd60119831:24000
Tanna-Delridge complex, 6 to 9 percent slopesTdC5188355470cxwssd60119831:24000
Tanna-Savo complex, 6 to 9 percent slopesTsC4425355472cxwvsd60119831:24000
Tanna-Savar-like-Potrio-like complex, 1 to 10 percent slopes5B07335835130zvywy6171:24000

Map of Series Extent

Approximate geographic distribution of the TANNA 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 .