Official Series Description


Lab Data Summary

Aggregate lab data for the AIMELIIK soil series. This aggregation is based on all pedons with a current taxon name of AIMELIIK, 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 AIMELIIK were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
19303N0697S03PW002002Aimeliik7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties7.4318472,134.5229639
19303N0707S03PW002007Aimeliik7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties7.4320111,134.5232083
19305N0416S05PW212001Aimeliik7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties7.4961472,134.6291
19305N0418S05PW222001Aimeliik7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties7.5863472,134.5863889
19305N0419S05PW227001Aimeliik7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties7.5300028,134.5596028
19307N0080S06PW002001Aimeliik7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties7.5864111,134.5868972
19380P0146S79PB935003Aimeliik6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties7.3926917,134.5307528

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the AIMELIIK 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.

There are insufficient data to create the water balance bar figure.



There are insufficient data to create the water balance line figure.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the AIMELIIK series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the AIMELIIK series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the AIMELIIK 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 .

Click the image to view it full size.

Click the image to view it full size.

There are insufficient data to create the 3D mountains figure.

Click the image to view it full size.

Click the image to view it full size.

Competing Series

Soil series competing with AIMELIIK share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the AIMELIIK series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the AIMELIIK 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 .

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

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 AIMELIIK, 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 AIMELIIK 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
Aimeliik silt loam, 30 to 50 percent slopes60319888185924120dpjpw93520081:12000
Aimeliik silt loam, 50 to 75 percent slopes60412846185924020dphpw93520081:12000
Aimeliik silt loam, 12 to 30 percent slopes6029394185924220dpkpw93520081:12000
Aimeliik silt loam, volcanic bedded substratum, 30 to 50 percent slopes6082777185926020dq4pw93520081:12000
Aimeliik silt loam, bedded tuff substratum, 12 to 30 percent slopes6071900185925820dq2pw93520081:12000
Aimeliik silt loam, 6 to 12 percent slopes6011526185924320dplpw93520081:12000
Aimeliik-Ollei complex, 50 to 75 percent slopes6111286185926720dqcpw93520081:12000
Aimeliik silty clay loam, bedded tuff substratum, 50 to 75 percent slopes6091154185925920dq3pw93520081:12000
Aimeliik silt loam, bedded tuff substratum, 6 to 12 percent slopes606530185925720dq1pw93520081:12000
Aimeliik-Ollei complex, 30 to 50 percent slopes610450185926620dqbpw93520081:12000
Aimeliik silt loam, 2 to 6 percent slopes600325185924420dpmpw93520081:12000
Aimeliik silt loam, bedded tuff substratum, 2 to 6 percent slopes60518185925620dq0pw93520081:12000

Map of Series Extent

Approximate geographic distribution of the AIMELIIK 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 .