Official Series Description


Lab Data Summary

Aggregate lab data for the ARSON soil series. This aggregation is based on all pedons with a current taxon name of ARSON, 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 ARSON 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
43A04N1097S2004ID057015Arson6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.0029716,-116.8519135

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ARSON 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 ARSON 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 ARSON 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 ARSON 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 terrace figure.

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

Competing Series

Soil series competing with ARSON 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 ARSON 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 ARSON 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.

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 ARSON, 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 ARSON 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
Arson-Carlinton complex, 8 to 35 percent slopesAc15494644241pmczid05720131:24000
Arson-Carlinton complex, dry, 8 to 35 percent slopesAc23479644242pmd0id05720131:24000
Honeyjones-Arson-Chesley complex, 25 to 65 percent slopesHa2340114877021ly2did05720131:24000
Arson-Minaloosa complex, 25 to 60 percent slopesAn42453654988pzknid05720131:24000
Arson-Minaloosa complex, 5 to 25 percent slopesAn52430654989pzkpid05720131:24000
Arson ashy silt loam, 25 to 65 percent slopesAn12163644253pmdcid05720131:24000
Hugus-Chesley-Arson complex, 20 to 55 percent slopesHu876213875141hktjid05720131:24000
Arson-Lotuspoint complex, 8 to 40 percent slopes3406426629742v72tid60619761:24000
Sinkler-Arson complex, dry, 10 to 40 percent slopes3426326629842kp7vid60619761:24000
Arson-Carlinton complex, dry, 8 to 35 percent slopesAc21412663010pmd0id60819941:24000
Arson ashy silt loam, 25 to 65 percent slopesAn1822663012pmdcid60819941:24000
Sinkler-Arson complex, 10 to 40 percent slopes341420015431511nss2id62020131:24000
Arson-Lotuspoint complex, 8 to 40 percent slopes340258513898392v72tid62020131:24000
Sinkler-Arson complex, dry, 10 to 40 percent slopes342173523739132kp7vid62020131:24000
Arson-Carlinton complex, 8 to 35 percent slopesAc1462425117pmczid62020131:24000
Arson-Carlinton complex, dry, 8 to 35 percent slopesAc2412513911pmd0id62020131:24000
Arson-Minaloosa complex, 25 to 60 percent slopesAn442513912pzknid62020131:24000
Arson-Lotuspoint complex, 8 to 40 percent slopes934057122302272v72twa06320121:24000
Sinkler, dry-Arson, dry complex, 10 to 40 percent slopes934212724357642mrm1wa06320121:24000
Sinkler-Arson complex, 10 to 40 percent slopes934111524314652mm4cwa06320121:24000

Map of Series Extent

Approximate geographic distribution of the ARSON 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 .