Official Series Description


Lab Data Summary

Aggregate lab data for the ARMSTER soil series. This aggregation is based on all pedons with a current taxon name of ARMSTER, 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 ARMSTER 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
10605KS10304605KS103046Armster3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2253876,-95.0548859
10605KS10314505KS103145Armster1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2254906,-95.0546799
10607KS00500507KS005005Armster3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4400673,-95.1803436
10607KS10302307KS103023Armster1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2035675,-94.976944
10608KS10307108KS103071Armster3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.1715851,-94.9531937
10606N0843S2006KS103105Armster7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.1639709,-94.9806366
109M06199032006MO199003ARMSTER4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5853333,-92.0296389
109M06199052006MO199005ARMSTER4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5281722,-91.9756444
109M06199092006MO199009ARMSTER4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.4046389,-91.9921667
109M06199332006MO199033ARMSTER4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.3431944,-92.2652222
109M06199352006MO199035Armster4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.3503333,-92.2659444
109M06199372006MO199037Armster4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.4403611,-92.23275
109M07047022007MO047002Armster4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4441681,-94.2505569
109M07199022007MO199002Armster4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.58275,-92.2643611
109M07199032007MO199003ARMSTER4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5802222,-92.2626111
109M07199062007MO199006ARMSTER4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5128611,-92.2881667
109M07199072007MO199007Armster4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5122778,-92.2902222
109M07199082007MO199008Armster4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5145556,-92.0778889
109M07199112007MO199011Armster4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5153056,-92.0786667
109M07199142007MO199014Armster4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.4343056,-92.1075
109M07199152007MO199015Armster4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.4378333,-92.1084444
113M05139602005MO139060ARMSTER4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9,-91.3666667
113M05139612005MO139061ARMSTER4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9833333,-91.4833333
113M05139642005MO139064ARMSTER4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9666667,-91.35
113M05219592005MO219059ARMSTER4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.8963889,-91.2644444
113M06139562006MO139056ARMSTER4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9848611,-91.5408889
113M08027652008MO027065ARMSTER4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9210278,-91.7620278
115CM03219052003MO219005Armster4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.840525,-91.0697056
115CM05139632005MO139063ARMSTER4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9333333,-91.2666667
115CM05139652005MO139065ARMSTER4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9833333,-91.2833333
115CM05219662005MO219066Armster4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9783333,-91.2263889
115CM06199392006MO199039ARMSTER4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5006944,-91.9953056
115CM06199402006MO199040Armster4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.4975,-91.9951944
n/a97KS005004L97KS005004LArmster3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ARMSTER 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 ARMSTER 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 ARMSTER 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 ARMSTER 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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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with ARMSTER 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 ARMSTER 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 ARMSTER 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 .

Click the image to view it full size.

Click the image to view it full size.

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 ARMSTER, 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. KS-2012-01-20-04 | Atchison County - February 1984

    Typical pattern of soils in the Knox-Armster-Gosport association (Soil Survey of Atchison County, Kansas; 1984).

  2. MO-2012-02-06-24 | Clay and Ray Counties - January 1986

    Pattern of soils and parent material in the Snead-Ladoga association (Soil Survey of Clay and Ray Counties, Missouri; January 1986).

Map Units

Map units containing ARMSTER 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
Armster clay loam, 12 to 20 percent slopes7912917514753901lj87ks00519981:24000
Armster clay loam, 6 to 12 percent slopes7910662414753891lj86ks00519981:24000
Armster clay loam, 8 to 12 percent slopes, eroded7907259824203472m7kqks00519981:24000
Armster clay loam, 12 to 20 percent slopes, eroded791360424201112m7b3ks00519981:24000
Armster clay loam, 3 to 8 percent slopes, eroded790615724203462m7kpks00519981:24000
Armster clay loam, 8 to 12 percent slopes, eroded790737524801782p7trks04319771:24000
Armster clay loam, 12 to 20 percent slopes, eroded791386747150t2gmks04319771:24000
Armster clay loam, 8 to 12 percent slopes, eroded79072224203452m7knks08719741:24000
Armster clay loam, 8 to 12 percent slopes, eroded7907710224203442m7kmks10319731:24000
Armster clay loam, 3 to 8 percent slopes, eroded7906275724203432m7klks10319731:24000
Armster clay loam, 12 to 20 percent slopes, eroded791345824206082m7v4ks10319731:24000
Armster clay loam, 6 to 12 percent slopes791072186241020hzrks10319731:24000
Armster clay loam, 8 to 12 percent slopes, eroded7907329024203422m7kkks20919731:24000
Armster clay loam, 3 to 8 percent slopes, eroded7906175624203412m7kjks20919731:24000
Armster silt loam, 2 to 7 percent slopes50054126882782y8cnmo00719901:24000
Armster silt loam, 9 to 14 percent slopes10007135425210332qkxtmo02119841:24000
Armster silty clay loam, 5 to 9 percent slopes, eroded300201436325285392wbfnmo02519671:24000
Armster loam, 9 to 14 percent slopes, eroded30024878325285492qmw0mo02519671:24000
Armster clay loam, 9 to 14 percent slopes, severely eroded30014202225285272qmvtmo02519671:24000
Armster loam, 5 to 9 percent slopes30019169025285372qmvymo02519671:24000
Armster loam, 14 to 20 percent slopes, eroded30017154525285332qmvwmo02519671:24000
Armster clay loam, 5 to 9 percent slopes, severely eroded30013152425285202qmvsmo02519671:24000
Armster loam, 9 to 14 percent slopes300231339887967yt03mo02519671:24000
Armster loam, 2 to 5 percent slopes30018125825285342qmvxmo02519671:24000
Armster cobbly loam, 5 to 14 percent slopes, stony500174602885954yqx5mo02719861:24000
Armster silt loam, 2 to 7 percent slopes50054247125285402y8cnmo02719861:24000
Armster cobbly loam, 14 to 30 percent slopes, stony500161181885955yqx6mo02719861:24000
Armster loam, 9 to 14 percent slopes, eroded3002457925285502qmw0mo02719861:24000
Armster loam, 5 to 9 percent slopes300192783025285362qmvymo03319881:24000
Armster clay loam, 5 to 9 percent slopes, eroded300124932908875zhrkmo03319881:24000
Armster clay loam, 9 to 14 percent slopes, severely eroded30014285025285262qmvtmo03319881:24000
Armster silty clay loam, 5 to 9 percent slopes, eroded3002069725285412wbfnmo03319881:24000
Armster loam, 2 to 5 percent slopes3001840125285352qmvxmo03319881:24000
Armster clay loam, 9 to 20 percent slopes, severely eroded300162825285292qmvvmo03319881:24000
Armster silty clay loam, 5 to 9 percent slopes, eroded30020999325285452wbfnmo04719821:24000
Armster loam, 9 to 14 percent slopes, eroded30024881925285542qmw0mo04719821:24000
Armster clay loam, 5 to 9 percent slopes, severely eroded3001350025285222qmvsmo04719821:24000
Armster clay loam, 9 to 20 percent slopes, severely eroded3001642425285312qmvvmo04719821:24000
Armster silty clay loam, 5 to 9 percent slopes, eroded3002050325285422wbfnmo04919811:24000
Armster loam, 9 to 14 percent slopes, eroded3002418225285512qmw0mo04919811:24000
Armster clay loam, 9 to 20 percent slopes, severely eroded30016125285302qmvvmo04919811:24000
Armster silty clay loam, 5 to 9 percent slopes, eroded3002014625285432wbfnmo06119521:24000
Armster loam, 9 to 14 percent slopes, eroded300248925285522qmw0mo06119521:24000
Armster silty clay loam, 5 to 9 percent slopes, eroded300206025285442wbfnmo06319741:24000
Armster loam, 14 to 20 percent slopes, eroded300172425285322qmvwmo06319741:24000
Armster clay loam, 5 to 9 percent slopes, severely eroded30013725285212qmvsmo06319741:24000
Armster silt loam, 2 to 7 percent slopes500543509225285462y8cnmo13919751:24000
Armster clay loam, 5 to 9 percent slopes, severely eroded30013437825285232qmvsmo13919751:24000
Armster loam, 9 to 14 percent slopes, eroded300241100025285532qmw0mo16519821:24000
Armster silt loam, 9 to 14 percent slopes100071625210342qkxtmo16519821:24000
Armster silty clay loam, 5 to 9 percent slopes, eroded300201718825285472wbfnmo17719791:24000
Armster loam, 9 to 14 percent slopes, eroded30024661225285482qmw0mo17719791:24000
Armster clay loam, 9 to 20 percent slopes, severely eroded30016323925285282qmvvmo17719791:24000
Armster clay loam, 5 to 9 percent slopes, severely eroded30013295525285242qmvsmo17719791:24000
Armster clay loam, 9 to 14 percent slopes, severely eroded300142925285252qmvtmo17719791:24000
Armster silt loam, 2 to 7 percent slopes500541968325327402y8cnmo18319791:24000
Armster silt loam, 2 to 7 percent slopes500541439525285382y8cnmo21919751:24000
Armster clay loam, 5 to 9 percent slopes, severely eroded3001318225285192qmvsmo21919751:24000

Map of Series Extent

Approximate geographic distribution of the ARMSTER 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 .