Official Series Description


Lab Data Summary

Aggregate lab data for the ARCHIN soil series. This aggregation is based on all pedons with a current taxon name of ARCHIN, 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 ARCHIN 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
5240A3654S1967MT005002Archin2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.6666679,-109
58A40A3484S1952MT111025Archin5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.9477043,-108.2615814
58D83P002682SD063005Archin8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.7427788,-103.980835

Water Balance

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

Soil series sharing subgroup-level classification with ARCHIN, 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 ARCHIN 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
Archin-Absher complex, 2 to 8 percent slopes75C452073432322yk0nmt01119921:24000
Archin loam, 2 to 8 percent slopes175C426683429682wby1mt01119921:24000
Archin-Absher complex, 0 to 2 percent slopes75A88113432312yk0mmt01119921:24000
Eapa-Archin loams, 2 to 8 percent slopes184C7468342988chx4mt01119921:24000
Archin, gullied-Delpoint complex, 4 to 15 percent slopes275D64433430642yk0pmt01119921:24000
Chinook-Archin complex, 2 to 8 percent slopes283C56153430682yk0tmt01119921:24000
Archin loam, 0 to 2 percent slopes175A55723429672yk0lmt01119921:24000
Archin-Ynot complex, 2 to 8 percent slopes375C47803430962yk0rmt01119921:24000
Archin-Gerdrum loams, 2 to 8 percent slopes191C213533433302yk0qmt01719951:24000
Archin loam, 2 to 8 percent slopes19C157593433322wby1mt01719951:24000
Archin-Davidell-Bullock complex, 2 to 8 percent slopes192C34583433312yk0smt01719951:24000
Archin loam, 2 to 8 percent slopes175C259503421322wby1mt02519911:24000
Archin-Absher complex, 2 to 8 percent slopes75C162843422852yk0nmt02519911:24000
Chinook-Archin complex, 2 to 8 percent slopes283C107633421892yk0tmt02519911:24000
Archin-Ynot complex, 2 to 8 percent slopes375C34023422162yk0rmt02519911:24000
Archin loam, 0 to 2 percent slopes175A25953421312yk0lmt02519911:24000
Archin, gullied-Delpoint complex, 4 to 15 percent slopes275D24023421832yk0pmt02519911:24000
Archin-Absher complex, 0 to 2 percent slopes75A21473422842yk0mmt02519911:24000
Archin loam, 2 to 8 percent slopes86C79003427042wby1mt03320021:24000
Archin-Gerdrum loams, 2 to 8 percent slopes861C36033427032yk0qmt03320021:24000
Rhame-Kremlin-Archin complex, 6 to 15 percent slopesL2335D626327070472qxkfnd00719981:24000
Rhame-Kremlin-Archin complex, 0 to 6 percent slopesL2335B88527070462qz9hnd00719981:24000
Archin-Zeona-Ladner complex, 0 to 6 percent slopesL1237B91925634622qk4dnd01119691:20000
Archin-Desart, low precipitation fine sandy loams, 0 to 6 percent slopesL1235B65825634612qk4cnd01119691:20000
Tusler, severely eroded-Ladner-Archin complex, 0 to 6 percent slopesL1249B26625634642qk4gnd01119691:20000
Archin-Ladner fine sandy loams, 6 to 15 percent slopesL1241D16425634632qk4fnd01119691:20000
Rhame-Kremlin-Archin complex, 6 to 15 percent slopesL2335D260027151502qxkfnd05320031:24000
Rhame-Kremlin-Archin complex, 0 to 6 percent slopesL2335B5027151492qz9hnd05320031:24000
Archin-Zeona-Ladner complex, 0 to 6 percent slopesL1237B141227158942qk4dnd08719741:20000
Archin-Ladner fine sandy loams, 6 to 15 percent slopesL1241D52827158952qk4fnd08719741:20000
Rhame-Kremlin-Archin complex, 0 to 6 percent slopesL2335B11427585322qz9hnd08719741:20000
Rhame-Kremlin-Archin complex, 6 to 15 percent slopesL2335D7927585332qxkfnd08719741:20000
Archin-Desart, low precipitation fine sandy loams, 0 to 6 percent slopesL1235B2527158932qk4cnd08719741:20000
Archin-Slickspots complex, 0 to 3 percent slopesAnA118743531412zj4bsd01919701:24000
Archin-Bullock fine sandy loams, 0 to 4 percent slopesAkA401713557122y6djsd06319841:24000
Chinook-Archin fine sandy loams, 0 to 3 percent slopesCnA17919355731cy56sd06319841:24000
Assinniboine-Archin fine sandy loams, 0 to 3 percent slopesAtA113983557162zj4ssd06319841:24000
Eapa-Archin complex, 0 to 3 percent slopesEcA68793557382zj50sd06319841:24000
Korchea-Archin complexKm6801355758cy62sd06319841:24000
Kremlin-Archin complex, 0 to 3 percent slopesKrA4387355760cy64sd06319841:24000
Glendive-Archin fine sandy loams, 2 to 6 percent slopesGhB2184355743cy5lsd06319841:24000
Archin-Foreleft complex, 2 to 8 percent slopes, frequently flooded122131709782z209wy6291:24000
Foreleft-Archin-Kremlin-like complex, 4 to 25 percent slopes943131710062zt95wy6291:24000

Map of Series Extent

Approximate geographic distribution of the ARCHIN 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 .