Official Series Description


Lab Data Summary

Aggregate lab data for the ERICSON soil series. This aggregation is based on all pedons with a current taxon name of ERICSON, 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 ERICSON 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 ERICSON 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 ERICSON 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 ERICSON 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 ERICSON 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 ERICSON 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 ERICSON 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 ERICSON 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 ERICSON, 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 ERICSON 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
Jughandle-Ericson association582252686334558tid60919891:24000
Ericson-Rock outcrop complex3610226863295581id60919891:24000
Ericson loam, 4 to 25 percent slopes34552686328557zid60919891:24000
Jughandle-Ericson association583051154033558tid61719761:24000
Ericson loam, 4 to 25 percent slopes342109154007557zid61719761:24000
Ericson loam, 25 to 40 percent slopes3515361540085580id61719761:24000
Ericson-Rock outcrop complex3611841540095581id61719761:24000
Ericson, high effective precipitation-Ericson-Namela families, complex, 5 to 55 percent slopes978109229638842wv3cid7131:24000
Ericson-Kingmine-Sambrito families, complex, 5 to 30 percent slopes95852029638632wv2jid7131:24000
Crossley-Nielsen-Ericson family, complex, 5 to 40 percent slopes93432029638942wv3qid7131:24000
Mikesell-Ericson-Odark, stony families, complex, 4 to 15 percent slopes201D444430051172v7zxmt60019691:24000
Ericson family, very stony-Leighcan family-Ipasha, occasionally flooded complex, 0 to 15 percent slopes282D16030051072v804mt60019691:24000
Mikesell-Ericson-Odark, stony families, complex, 4 to 15 percent slopes201D15929110992v7zxmt6321:24000
Ericson family, very stony-Leighcan family-Ipasha, occasionally flooded complex, 0 to 15 percent slopes282D850428518502v804mt66320171:24000
Mikesell-Ericson-Odark, stony families, complex, 4 to 15 percent slopes201D779628518412v7zxmt66320171:24000
Ericson-Nooney-Bigcoulee families, association, 8 to 35 percent slopes, Broadly Defined1890272620349ntj8wy66119851:24000
Ericson-Nooney families, association, 15 to 60 percent slopes, Broadly Defined586935620333nthrwy66119851:24000
Ericson-Currycreek-Nooney families, association, 8 to 60 percent slopes, Broadly Defined1063386620335nthtwy66119851:24000
Ericson-Midfork-Nooney families, association, 15 to 70 percent slopes, Broadly Defined1244280620336nthvwy66119851:24000
Ericson-Bigcoulee families, association, 8 to 35 percent slopes, Broadly Defined729532620334nthswy66119851:24000

Map of Series Extent

Approximate geographic distribution of the ERICSON 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 .