Official Series Description


Lab Data Summary

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

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
43C04N033603OR023004Ateron6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.2194443,-119.5717239

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ATERON 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 ATERON 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 ATERON 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 ATERON 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 ATERON 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 ATERON 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 ATERON 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 ATERON, 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 ATERON 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
Snell-Ateron complex, 12 to 35 percent north slopes155D317916213922nhor60419881:24000
Ateron very stony loam, 2 to 12 percent slopes6C280496225122s3or60419881:24000
Ateron very stony loam, 12 to 35 percent south slopes7D241086226522skor60419881:24000
Snell-Ateron complex, 35 to 60 percent north slopes155E227936214022njor60419881:24000
Ateron very stony loam, 35 to 60 percent south slopes7E181296226622slor60419881:24000
Ateron-Roostercomb extremely gravelly clay loams, 12 to 35 percent south slopes9D167196229522tjor60419881:24000
Ateron-Roostercomb extremely gravelly clay loams, 35 to 60 percent south slopes9E129426229622tkor60419881:24000
Ateron-Roostercomb extremely gravelly clay loams, 2 to 12 percent slopes8C76166228222t3or60419881:24000
Ateron-Humarel complex, 0 to 15 percent slopes3482AO7031204681r07lor60720181:24000
Humarel-Ateron complex, 15 to 30 percent slopes3482BO6331204691r07mor60720181:24000
Ateron-Bingville complex, 2 to 20 percent slopes4011AO453120161nfqfor60720181:24000
Ateron gravelly loam, 2 to 20 percent slopes4401AO2643385426jggcor62620181:24000
Ateron-Bingville complex, 2 to 20 percent slopes4011AO2163385314nfqfor62620181:24000
Humarel-Ateron complex, 15 to 30 percent slopes3482BO18631222701r07mor62620181:24000
Anatone-Parsnip-Ateron complex, 0 to 15 percent slopes1722AO17231221302mszgor62620181:24000
Ateron-Humarel complex, 0 to 15 percent slopes3482AO12231222691r07lor62620181:24000
Ateron-Humarel complex, 30 to 60 percent slopes3482CO5231222711r07nor62620181:24000
Ateron-Maule complex, 15 to 40 percent slopes4337BO3433854211qklqor62620181:24000
Ateron-Snell complex, 20 to 50 percent south slopes4316NO283385478rcr2or62620181:24000
Ateron-Klicker complex, 20 to 50 percent south slopes4330NO1338541425xtqor62620181:24000
Merlin-Ateron-Rubble land complex, 2 to 20 percent slopes19627278490574jggzor62819971:24000
Merlin-Ateron-Ticino complex, 2 to 20 percent slopes1978597490575jgh0or62819971:24000
Ateron-Observation association, 5 to 30 percent slopes207895490581jgh6or62819971:24000
Ateron-Rubble land complex, 2 to 35 percent slopes196162490567jggror62819971:24000
Merlin-Ateron complex, 2 to 20 percent slopes1954991490573jggyor62819971:24000
Teguro-Ateron complex, 2 to 20 percent slopes3244741490749jgnmor62819971:24000
Ateron gravelly loam, 2 to 20 percent slopes182543490555jggcor62819971:24000
Gaib-Ateron complex, 2 to 15 percent slopes1272530490491jgd9or62819971:24000
Rubble land-Nuss-Ateron association, 20 to 60 percent slopes2942425490711jgmdor62819971:24000
Ateron-Carryback complex, 2 to 15 percent slopes502911932708842zgstor62819971:24000
Ateron very stony loam, 2 to 12 percent slopes4038AO516243756022s3or63120181:24000
Ateron very stony loam, 35 to 60 percent south slopes4038CS253243756222slor63120181:24000
Anatone-Parsnip-Ateron complex, 0 to 15 percent slopes1722AO9824370792mszgor63120181:24000
Ateron very stony loam, 12 to 35 percent south slopes4038BS9248680222skor63120181:24000
Snell-Ateron complex, 12 to 35 percent north slopes4040BN5248680422nhor63120181:24000
Ateron-Carryback complex, 2 to 15 percent slopes5029643332635462zgstor64420211:24000
Ateron-Carryback complex, 2 to 15 percent slopes50295330527222952sf3yor6451:24000
Anatone-Lambring-Ateron complex, 15 to 55 percent slopes90022752024851082pdysor6451:24000
Lambring-Ateron complex, 10 to 50 percent north slopes90132175925648372qxxkor6451:24000
Ginserly-Ateron complex, 15 to 60 percent slopes9028789427222732sf35or6451:24000
Bocker-Ateron-Rock outcrop complex, 8 to 45 percent south slopes9001242224847142pdk2or6451:24000
Ateron-Roostercomb complex, 15 to 35 percent south slopes9006164224821752p9x5or6451:24000
Sinker-Ateron complex, 8 to 35 percent north slopes901091024822282p9ywor6451:24000
Teguro-Anatone complex, 2 to 10 percent slopes253518185771020c34or6541:24000
Maule-Maucav-Anatone complex, dry, 2 to 30 percent south slopes423360185773020c3sor6541:24000
Observation-Ateron-Polkbutte complex, 0 to 35 percent slopes283253185771920c3for6541:24000
Erakatak-Ateron complex, 40 to 70 percent south slopes095224185764520c11or6541:24000
Maule-Maucav-Anatone complex, 2 to 30 percent south slopes433180185773220c3vor6541:24000
Ateron-Merlin, rubbly complex, 5 to 20 percent slopesX81083185777520c57or6541:24000
Observation-Bonnieview-Ateron complex, 0 to 50 percent slopesB45148185776920c51or6541:24000
Alding-Ateron complex, 10 to 40 percent slopesB74130185777020c52or6541:24000
Merlin-Ateron complex, 2 to 20 percent slopes195m19185769920c2sor6541:24000
Anatone-Ateron complex, 30 to 65 percent south slopes2482185770820c32or6541:24000

Map of Series Extent

Approximate geographic distribution of the ATERON 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 .