Official Series Description


Lab Data Summary

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

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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 STARMAN, 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. CO-2011-05-31-02 | Rio Blanco Area - 1982

    Typical pattern of soils in general map unit 11 (Soil Survey of Rio Blanco Area, Colorado; 1982).

  2. CO-2012-05-09-07 | Rio Blanco County Area - May 1982

    Typical pattern of soils in general map unit 11 (Soil Survey of Rio Blanco County Area, Colorado; May 1982).

Map Units

Map units containing STARMAN 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
Starley-Starman very channery loams, 3 to 25 percent slopes1002364497929jq47co65519841:24000
Irigul-Starman channery loams, 5 to 35 percent slopes503526496713jnw0co68219861:24000
Irigul-Starman channery loams, 5 to 50 percent slopes384700496779jny4co68319771:24000
Starman-Vandamore complex, 5 to 40 percent slopes8713912497042jp6mco68519791:24000
Rubble land-Midfork-Starman association396112194975423fw9id75819981:24000
Rock outcrop-Sheege-Starman association352331194975123fw6id75819981:24000
Starman-Owlcan association46-A53194975523fwbid75819981:24000
Rubble land-Rock outcrop-Starman family, very rubbly, complex, 20 to 70 percent slopes5100G82729952442r88cmt02719791:24000
Rubble land-Rock outcrop-Starman family, very rubbly, complex, 20 to 70 percent slopes5100G8230396662r88cmt60219631:20000
Garlet, very stony-Broad Canyon, very stony-Starman, extremely stony families, complex, 25 to 60 percent slopes6312F57530941012tymhmt63019911:24000
Starman, extremely stony-Rock outcrop-Garlet, very rubbly families, complex, 35 to 70 percent slopes6310G43930940992tym9mt63019911:24000
Rock outcrop-Starman, family, very rubbly-Rubble land, complex, 4 to 30 percent slopes6311E2530941032tymrmt63019911:24000
Starman, extremely stony-Rock outcrop-Garlet, very rubbly families, complex, 35 to 70 percent slopes6310G1804428268342tym9mt6321:24000
Rubble land-Rock outcrop-Starman family, very rubbly, complex, 20 to 70 percent slopes5100G1075226098322r88cmt6321:24000
Rock outcrop-Starman, very rubbly-Oorang, very rubbly families, complex, 45 to 70 percent slopes6414G1023328268322tym7mt6321:24000
Garlet, very stony-Broad Canyon, very stony-Starman, extremely stony families, complex, 25 to 60 percent slopes6312F775328268402tymhmt6321:24000
Helmville, extremely stony-Starman, very rubbly-Lingshire, stony families, complex, 4 to 50 percent slopes6315F704728268422tymkmt6321:24000
Ouselfal, very stony-Garlet, very rubbly-Starman, rubbly families, complex, 15 to 60 percent slopes, landslides6314F429528268382tymfmt6321:24000
Starman, rubbly-Garlet, extremely bouldery families-Rock outcrop complex, 25 to 60 percent slopes6414F288328268442tymmmt6321:24000
Rock outcrop-Starman, family, very rubbly-Rubble land, complex, 4 to 30 percent slopes6311E173528268472tymrmt6321:24000
Helmville, extremely stony-Starman, very rubbly-Lingshire, stony families, complex, 4 to 50 percent slopes6315F1530941292tymkmt65719901:24000
Amesmont-Vandamore-Starman families complex, 40 to 80 percent slopes2083240512423k66sut6461:24000
Rock outcrop-Starman complex, 6 to 45 percent slopes6327109152110538swy04319761:24000
Starley-Starman extremely gravelly-Rock outcrop complex, 6 to 60 percent slopes -- Draft8061000015226553fswy6031:24000
Rock outcrop-Starman complex, 20 to 50 percent slopes403800015219653ckwy6031:24000
Rock outcrop-Starman complex, 6 to 45 percent slopes635816479wdm1wy61919711:24000
Cundick-Starman complex, 15 to 40 percent slopes, stony56930054402x7fpwy6301:24000
Cundick-Lymanson-Starman complex, 3 to 25 percent slopes5101587724554792nf40wy6301:24000
Shineberger-Starman complex, 3 to 20 percent slopes552909328284302tz4bwy6301:24000
Rock outcrop-Starman variant association, 10 to 70 percent slopes2431393360733d3ckwy63319871:24000
Rock outcrop-Starman association, 15 to 45 percent slopes242528360989d3mtwy63319871:24000
Vertic Haplocryalfs-Sudduth family-Starman family, complex, 0 to 60 percent slopes205422554761533swy6351:24000
Woosley-Decross-Starman complex, 2 to 20 percent slopes22125148637780pdnkwy6471:24000
Starman-Rock outcrop-Woosley complex, 10 to 40 percent slopes30025079637537pddqwy6471:24000
Starman-Cloud Peak-Rock outcrop complex, 2 to 60 percent slopes1061908215759358znwy6471:24000
Sawcreek-Starman-Indart complex, 4 to 60 percent slopes122188415760158zxwy6471:24000
Farlow-Nathrop-Starman complex, 10 to 50 percent slopes173123733699smgqwy6471:24000
Starman-Starley association, 2 to 30 percent slopes393232115805059gdwy65019821:24000
Rock outcrop-Starman association, 5 to 70 percent slopes34440115804559g7wy65019821:24000
Surdal-Starman-Spearhead families, complex, 15 to 60 percent slopes22024061577915961wy65620081:24000
Woosley-Decross-Starman association, 2 to 20 percent slopes221D122815793859bswy65620081:24000
Farlow family-Nathrop family-Starman complex, 10 to 50 percent slopes173D11981884372217v6wy65620081:24000
Starman-Rock outcrop-Woosley complex, 10 to 40 percent slopes209D44315793559bpwy65620081:24000
Starman-Midfork families, complex, 40 to 90 percent slopes26616843151981534mwy66320121:24000
Vertic Haplocryalfs-Sudduth family-Starman family, complex, 0 to 60 percent slopes2059683151955533swy66320121:24000
Starman-Kamack families, complex, 20 to 60 percent slopes -- draft4353075152043536mwy66320121:24000
Lymanson-Starman, extremely stony-Billycanyon, very stony, complex, 15 to 45 percent slopes651032830833112wdjnwy66320121:24000
Rubble land-Midfork-Starman association *391320115328854hswy66619781:24000
Starman-Owlcan association *461077415329654j1wy66619781:24000
Rock outcrop-Sheege-Starman association *35467315328454hnwy66619781:24000
Starman-Rock outcrop-Woosley complex, 10 to 40 percent slopes77194190175521txywy67719751:24000
Starman-Rock outcrop-Woosley complex, 10 to 40 percent slopes20912573503085jwhkwy71319861:24000
Woosley-Decross-Starman association, rolling2218098503100jwj1wy71319861:24000
Midelight variant-Winada variant-Starman gravelly loams, steep1734275503038jwg1wy71319861:24000
Lymanson-Starman, extremely stony-Billycanyon, very stony, complex, 15 to 45 percent slopes651029251402wdjnwy7231:24000
Starman-Kamack families, complex, 20 to 60 percent slopes -- draft43572612003536mwy7231:24000

Map of Series Extent

Approximate geographic distribution of the STARMAN 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 .