Official Series Description


Lab Data Summary

Aggregate lab data for the ALTVAN soil series. This aggregation is based on all pedons with a current taxon name of ALTVAN, 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 ALTVAN 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
7240A2226S1957NE105011Altvan5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.3219452,-103.8925018
7240A2227S1957NE105012Altvan6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.3210907,-104.0188904

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ALTVAN 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 ALTVAN 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 ALTVAN 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 ALTVAN 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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Competing Series

Soil series competing with ALTVAN 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 ALTVAN 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 ALTVAN 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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There are insufficient data to create the 3D mountains figure.

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Click the image to view it full size.

Soil series sharing subgroup-level classification with ALTVAN, 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. NE-2012-02-13-46 | Kimball County - March 1962

    Typical soil pattern in the Altvan-Rosebud-Dix association: (1) deep Altvan loams; (2) Goshen loams; (3) moderately deep Altvan loams; (4) Gravelly land; (5) Bridgeport loams; and (6) Tripp loams (Soil Survey of Kimball County, Nebraska; March 1962).

  2. NE-2012-02-13-47 | Kimball County - March 1962

    Pattern of soils in valley of Lodgepole Creek: (1) Rosebud loams; (2) Bridgeport loams; (3) Tripp loams; (4) Parshall sandy loams; (5) Havre silt loam; (6) Vebar sandy loams; (7) Altvan loams; (8) Canyon complexes; (9) Gravelly land; and (10) Canyon-Rosebud loams (Soil Survey of Kimball County, Nebraska; March 1962).

  3. SD-2012-03-15-11 | Custer and Pennington Counties, Prairie Parts - May 1996

    Pattern of soils, topography, and underlying material in the Nunn-Satanta association (Soil Survey of Custer and Pennington Counties, Prairie Parts, SD; 1996).

Map Units

Map units containing ALTVAN 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
Dix-Altvan complex, 10 to 30 percent slopes2417225945042tlqbco07519741:24000
Wages-Altvan complex, 5 to 9 percent slopes121694194484359wco07519741:24000
Altvan-Eckley sandy loams, 3 to 5 percent slopes453479452135c2co07519741:24000
Altvan-Eckley sandy loams, 5 to 9 percent slopes548359453235cfco07519741:24000
Altvan fine sandy loam, 0 to 6 percent slopes1424689509935yqco61719801:24000
Peetz-Altvan complex, 0 to 20 percent slopes525646951463607co61719801:24000
Altvan fine sandy loam, 6 to 9 percent slopes242719511035z2co61719801:24000
Altvan-Dix complex, 6 to 10 percent slopes7844951772tlq8co61719801:24000
Altvan loam, 0 to 1 percent slopes11951995186361jco61819761:24000
Altvan loam, 1 to 3 percent slopes2205295197361wco61819761:24000
Altvan-Satanta loams, 3 to 9 percent slopes453210284jpwfco64319751:20000
Altvan loam, 0 to 3 percent slopes113066497634jptqco64419801:24000
Altvan loam, 3 to 9 percent slopes25246497665jpvqco64419801:24000
Altvan-Satanta loams, 0 to 3 percent slopes33689497676jpw2co64419801:24000
Altvan-Satanta loams, 3 to 9 percent slopes41732497687jpwfco64419801:24000
Satanta-Altvan complex, 3 to 6 percent slopes1820908216925081tt61ne00719881:20000
Altvan-Eckley complex, 3 to 9 percent slopes1508633816924552x2x5ne00719881:20000
Altvan-Satanta loams, 0 to 1 percent slopes151234122281412dskjne00719881:20000
Altvan loam, 3 to 6 percent slopes150333916924542v9gbne00719881:20000
Altvan fine sandy loam, 1 to 3 percent slopes15003622281392dskgne00719881:20000
Eckley and Altvan soils, 9 to 50 percent slopes15781922281422dskkne00719881:20000
Altvan-Satanta fine sandy loams, 1 to 3 percent slopes15111922281402dskhne00719881:20000
Altvan loam, 1 to 3 percent slopes1502249716990072x2x4ne02919801:20000
Altvan loam, 0 to 1 percent slopes1501222216990061v0ynne02919801:20000
Altvan loam, 3 to 6 percent slopes150359216990082v9gbne02919801:20000
Altvan-Dix complex, 3 to 9 percent slopes15061530616986552tlq7ne03319891:20000
Altvan loam, 1 to 3 percent slopes15021151416986532x2x4ne03319891:20000
Altvan loam, 3 to 6 percent slopes15031100316986542v9gbne03319891:20000
Blueridge-Altvan complex, 6 to 30 percent slopes592733522197022dhs9ne03319891:20000
Altvan-Eckley-Satanta complex, 3 to 9 percent slopes150927922196962dhs3ne03319891:20000
Altvan-Eckley complex, 3 to 9 percent slopes150825522196792x2x5ne03319891:20000
Altvan fine sandy loam, 1 to 3 percent slopes150017422196782dhrjne03319891:20000
Satanta-Johnstown-Altvan loams, 1 to 3 percent slopes182514422196972dhs4ne03319891:20000
Altvan-Eckley-Tassel complex, 3 to 9 percent slopes151011322196802dhrlne03319891:20000
Satanta-Altvan complex, 3 to 6 percent slopes18203522196892dhrwne03319891:20000
Eckley and Altvan soils, 9 to 50 percent slopes15781922196812dhrmne03319891:20000
Satanta-Johnstown-Altvan loams, 1 to 3 percent slopes18256167616988241v0rsne04920001:24000
Blueridge-Altvan complex, 6 to 30 percent slopes59272841816987971v0qxne04920001:24000
Altvan-Eckley-Satanta complex, 3 to 9 percent slopes15091963116987951v0qvne04920001:24000
Satanta-Altvan complex, 3 to 6 percent slopes18201528416988221v0rqne04920001:24000
Altvan-Dix complex, 6 to 30 percent slopes1507812516988702tlq9ne10119901:20000
Satanta-Johnstown-Altvan loams, 1 to 3 percent slopes182558122195802dhncne10119901:20000
Altvan loam, 1 to 3 percent slopes150238922195922x2x4ne10119901:20000
Altvan loam, 3 to 6 percent slopes150310322195932v9gbne10119901:20000
Blueridge-Altvan complex, 6 to 30 percent slopes59277722195852dhnjne10119901:20000
Altvan-Eckley-Satanta complex, 3 to 9 percent slopes15096222195782dhn9ne10119901:20000
Altvan-Eckley complex, 3 to 9 percent slopes15086005816925322x2x5ne10520041:24000
Altvan fine sandy loam, 1 to 3 percent slopes15003349716925311tt6sne10520041:24000
Altvan-Satanta fine sandy loams, 1 to 3 percent slopes15112605116925331tt6vne10520041:24000
Eckley and Altvan soils, 9 to 50 percent slopes15781750516925421tt74ne10520041:24000
Altvan-Satanta loams, 0 to 1 percent slopes15121683416925351tt6xne10520041:24000
Altvan-Eckley-Tassel complex, 3 to 9 percent slopes15101477616925341tt6wne10520041:24000
Tassel and Dix and Altvan soils, 9 to 30 percent slopes60231023416925591tt7pne10520041:24000
Altvan loam, 0 to 1 percent slopes1501397216925301tt6rne10520041:24000
Altvan-Dix complex, 3 to 9 percent slopes1506180916925752tlq7ne12319811:20000
Altvan loam, 1 to 3 percent slopes1502486116989522x2x4ne13519871:20000
Altvan loam, 3 to 6 percent slopes1503214816989532v9gbne13519871:20000
Altvan-Dix complex, 6 to 30 percent slopes1507121416989542tlq9ne13519871:20000
Satanta-Altvan complex, 3 to 6 percent slopes18203022195722dhn3ne13519871:20000
Altvan-Eckley-Satanta complex, 3 to 9 percent slopes1509322195712dhn2ne13519871:20000
Altvan-Dix complex, 3 to 9 percent slopes150620522276802tlq7ne15719651:20000
Altvan loam, 0 to 5 percent slopesAlB1513352719cv11sd00720041:20000
Altvan loam, 0 to 2 percent slopesAlA159227592352rd3xsd01919701:24000
Altvan loam, 2 to 6 percent slopesAlB31327592362rd3ysd01919701:24000
Altvan loam, 0 to 2 percent slopesAbA123127680422rd3xsd04719801:24000
Altvan loam, 2 to 6 percent slopesAbB67427680432rd3ysd04719801:24000
Altvan loam, 2 to 6 percent slopesP012B22527331142qt16sd04719801:24000
Altvan loam, 0 to 2 percent slopesP012A9527331132qt15sd04719801:24000
Altvan loam, 5 to 9 percent slopesAlC4997353341cvp3sd09519711:20000
Altvan loam, 0 to 2 percent slopesAlA1617352969cv93sd12119671:31680
Altvan loam, 2 to 5 percent slopesAlB477352970cv94sd12119671:31680
Altvan loam, 0 to 2 percent slopesAlA452027680532rd3xsd60019741:24000
Altvan loam, 2 to 6 percent slopesAlB447527680542rd3ysd60019741:24000
Altvan loam, moist, 2 to 6 percent slopesP014B122427334182qt18sd60019741:24000
Altvan loam, moist, 0 to 2 percent slopesP014A27027334172qt17sd60019741:24000
Altvan loam, 0 to 2 percent slopesAaA506227680642rd3xsd60620111:24000
Altvan loam, 2 to 6 percent slopesAaB168027680652rd3ysd60620111:24000
Altvan loam, 6 to 9 percent slopesAaC11902580865cyfzsd60620111:24000
Altvan sandy loam, 2 to 6 percent slopesAbB1122580995xgvrsd60620111:24000
Altvan sandy loam, 0 to 2 percent slopesAbA502580994xgvpsd60620111:24000
Altvan loam, 3 to 9 percent slopesAlC37442925508cv53sd61019651:20000
Altvan loam, 0 to 3 percent slopesAlA11042925502cv52sd61019651:20000
Richfield-Altvan silt loams, 0 to 3 percent slopesRaA37602582729cv4csd61320111:24000
Richfield-Altvan silt loams, 3 to 5 percent slopesRaB12222582730cv4dsd61320111:24000
Altvan loam, 0 to 3 percent slopes5804991048413j2zwy62119801:24000
Altvan loam, 3 to 6 percent slopes6470501048432v9gbwy62119801:24000
Altvan-Dix complex, 6 to 10 percent slopes7351991048442tlq8wy62119801:24000
Dix-Altvan complex, 10 to 30 percent slopes15213291048032tlqbwy62119801:24000
Altvan fine sandy loam, 6 to 9 percent slopes8041351047803j10wy62119801:24000
Altvan loam, 0 to 6 percent slopes6126151047733j0swy62119801:24000
Altvan fine sandy loam, 0 to 6 percent slopes791171047793j0zwy62119801:24000
Peetz-Altvan complex, 0 to 20 percent slopes69251047883j18wy62119801:24000
Altvan loam, 0 to 6 percent slopes101182341049023j4ywy72119941:24000
Altvan-Dix complex, 6 to 10 percent slopes102181311049032tlq8wy72119941:24000
Dix-Altvan complex, 10 to 30 percent slopes12994581049302tlqbwy72119941:24000
Urban land-Altvan complex, 0 to 6 percent slopes18327921049843j7lwy72119941:24000
Peetz-Altvan complex, 0 to 20 percent slopes1551231049563j6pwy72119941:24000

Map of Series Extent

Approximate geographic distribution of the ALTVAN 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 .