Official Series Description


Lab Data Summary

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

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with ARCIA, 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 ARCIA 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
Arcia complex, 15 to 35 percent slopes210734861292fhl2id67519921:24000
Chen-Arcia complex, 15 to 50 percent slopes2383932709392dh24id67519921:24000
Chen-Arcia-Cleavage association1880829626339712rhgtnv61219681:24000
Chen-Cotant-Arcia association1879224625179212qhm3nv61219681:24000
Leevan-Cleavage-Arcia association700382526339902rhhgnv62119711:24000
Chen-Quarz-Arcia association187415990477140j0hmnv76319861:24000
Chen-Chen, steep-Arcia association18761920477142j0hpnv76319861:24000
Quarz-Quarz, very steep-Arcia association1723111625177002q90knv76420211:24000
Cleavage-Arcia-Lerrow association7527680475110hyd4nv76519861:24000
Shalcleav-Graley-Arcia association2245390474951hy70nv76519861:24000
Shalcleav-Cleavage-Arcia association2205145474947hy6wnv76519861:24000
Graley-Chen-Arcia association4623455475037hy9snv76519861:24000
Amtoft-Arcia-Kram association30251845474991hy89nv76519861:24000
Gollaher-Arcia-Vitale association7991350475130hydsnv76519861:24000
Quarz, steep-Quarz-Arcia association2821150474972hy7pnv76519861:24000
Shalcleav-Arcia association2191020474946hy6vnv76519861:24000
Chen-Arcia-Cleavage association188011662478799j274nv76719861:24000
Leevan-Cleavage-Arcia association7008510478983j2f2nv76719861:24000
Arcia-Tusel-Hackwood association6405057478975j2dtnv76719861:24000
Chen-Cotant-Arcia association18793723478798j273nv76719861:24000
Quarz-Quarz, sloping-Arcia association17213019478769j265nv76719861:24000
Chen-McIvey-Arcia association18892663478808j27fnv76719861:24000
Quarz-Quarz, very steep-Arcia association1723190932709002q90knv76719861:24000
Doyn-Arcia association, 2 to 30 percent slopes8227909490959jgwdor62819971:24000
Ninemile-Arcia complex, 2 to 15 percent slopes481391616899831tqklor63520061:24000
Chen-Arcia complex, 15 to 50 percent slopes2381991622190152dh24or64420211:24000
Erakatak-Boost-Arcia complex, 2 to 60 percent slopes4581346129868612x2m1or64420211:24000
Chen-Arcia complex, 0 to 8 percent slopes468852630598612wz67or64420211:24000
Boost-Arcia complex, 2 to 15 percent slopes214341722190132dh22or64420211:24000
Erakatak-Arcia-Rock outcrop complex, 30 to 60 percent slopes451190929868462wbjwor64420211:24000
Arcia complex, 15 to 35 percent slopes210155122493002fhl2or64420211:24000

Map of Series Extent

Approximate geographic distribution of the ARCIA 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 .