Official Series Description


Lab Data Summary

Aggregate lab data for the ANVIK soil series. This aggregation is based on all pedons with a current taxon name of ANVIK, 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 ANVIK 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
48A92P081692CO033001Anvik7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.6966667,-108.2074966

Water Balance

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the ANVIK 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 ANVIK series and siblings. 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 ANVIK 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.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Competing Series

Soil series competing with ANVIK 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 ANVIK 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 ANVIK 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

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 ANVIK, 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 ANVIK 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
Anvik loam, 6 to 15 percent slopes03113177082jq1sco6451:24000
Anvik loam, 15 to 50 percent slopes49632497864jq24co64919771:24000
Anvik loam, 6 to 15 percent slopes33463497853jq1sco64919771:24000
Anvik-Skylick-Sawpit families complex, 5 to 40 percent slopes452B386114150301jhg4co6541:24000
Anvik-Skylick-Sligting association, 25 to 50 percent slopesAG11228114150751jhhlco6541:24000
Ansel-Anvik association, 25 to 45 percent slopesAG9113814150731jhhjco6541:24000
Anvik-Skylick-Sligting association, 10 to 25 percent slopesAG1052514150741jhhkco6541:24000
Anvik-Skylick-Sligting association, 25 to 50 percent slopes1130135497939jq4kco65519841:24000
Anvik-Skylick-Sligting association, 10 to 25 percent slopes1015776497928jq46co65519841:24000
Ansel-Anvik association, 25 to 45 percent slopes911374498035jq7nco65519841:24000
Ansel-Anvik association, 12 to 25 percent slopes81900498024jq79co65519841:24000
Anvik-Tuckerville complex, 10 to 45 percent slopes1603274507101k0p3co67220031:24000
Weminuche-Anvik complex, 15 to 60 percent slopes6033203507206k0shco67220031:24000
Peeler-Anvik, warm complex, 25 to 40 percent slopes9111939496938jp38co68419841:24000
Anvik, warm-Cochetopa-Passar complex, 3 to 25 percent slopes99926496936jp36co68419841:24000
Scout-Angostura-Anvik complex, 25 to 65 percent slopes1102793496834jnzxco68419841:24000
Scout-Angostura-Anvik complex, 5 to 25 percent slopes1091636496832jnzvco68419841:24000
Anvik loam, 15 to 35 percent slopes1F4750497301jpgzco69019741:24000
Anvik loam, 6 to 15 percent slopes1D525497300jpgyco69019741:24000
Anvik-Routt-Sedgway families, complex, 10 to 35 percent slopes56119425584422mnb5id71019681:24000
Davtone-Sedgway-Anvik families, complex, 10 to 35 percent slopes560471524326052mnb4id7131:24000
Anvik-Routt-Sedgway families, complex, 10 to 35 percent slopes561460424326062mnb5id7131:24000
Davtone-Sedgway-Anvik families, complex, 10 to 35 percent slopes5606331634252mnb4id7161:24000
Anvik-Routt-Sedgway families, complex, 10 to 35 percent slopes5615331634262mnb5id7161:24000

Map of Series Extent

Approximate geographic distribution of the ANVIK 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 .