Soil Data Explorer - ANVIK

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 (updated 2020-03-18). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Pedons used in the lab summary:

MLRA	Lab ID	Pedon ID	Taxonname	CI	NSSL / NASIS Reports	Link To SoilWeb GMap
48A	92P0816	92CO033001	Anvik	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	37.6966667,-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.

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 (updated 2024-02-21), parsed OSD records (updated 2023-10-06) and snapshot of SC database (updated 2023-10-02).

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 (updated 2023-10-09).

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 (updated 2023-10-04).

Competing Series

Soil series competing with ANVIK share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-06) and snapshot of the SC database (updated 2023-10-02).

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 (updated 2023-10-09).

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 (updated 2023-10-04).

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 (updated 2023-10-02).

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 slopes	03		3177082	jq1s	co645		1:24000
Anvik loam, 15 to 50 percent slopes	4	9632	497864	jq24	co649	1977	1:24000
Anvik loam, 6 to 15 percent slopes	3	3463	497853	jq1s	co649	1977	1:24000
Anvik-Skylick-Sawpit families complex, 5 to 40 percent slopes	452B	3861	1415030	1jhg4	co654		1:24000
Anvik-Skylick-Sligting association, 25 to 50 percent slopes	AG11	2281	1415075	1jhhl	co654		1:24000
Ansel-Anvik association, 25 to 45 percent slopes	AG9	1138	1415073	1jhhj	co654		1:24000
Anvik-Skylick-Sligting association, 10 to 25 percent slopes	AG10	525	1415074	1jhhk	co654		1:24000
Anvik-Skylick-Sligting association, 25 to 50 percent slopes	11	30135	497939	jq4k	co655	1984	1:24000
Anvik-Skylick-Sligting association, 10 to 25 percent slopes	10	15776	497928	jq46	co655	1984	1:24000
Ansel-Anvik association, 25 to 45 percent slopes	9	11374	498035	jq7n	co655	1984	1:24000
Ansel-Anvik association, 12 to 25 percent slopes	8	1900	498024	jq79	co655	1984	1:24000
Anvik-Tuckerville complex, 10 to 45 percent slopes	160	3274	507101	k0p3	co672	2003	1:24000
Weminuche-Anvik complex, 15 to 60 percent slopes	603	3203	507206	k0sh	co672	2003	1:24000
Peeler-Anvik, warm complex, 25 to 40 percent slopes	91	11939	496938	jp38	co684	1984	1:24000
Anvik, warm-Cochetopa-Passar complex, 3 to 25 percent slopes	9	9926	496936	jp36	co684	1984	1:24000
Scout-Angostura-Anvik complex, 25 to 65 percent slopes	110	2793	496834	jnzx	co684	1984	1:24000
Scout-Angostura-Anvik complex, 5 to 25 percent slopes	109	1636	496832	jnzv	co684	1984	1:24000
Anvik loam, 15 to 35 percent slopes	1F	4750	497301	jpgz	co690	1974	1:24000
Anvik loam, 6 to 15 percent slopes	1D	525	497300	jpgy	co690	1974	1:24000
Anvik-Routt-Sedgway families, complex, 10 to 35 percent slopes	561	194	2558442	2mnb5	id710	1968	1:24000
Davtone-Sedgway-Anvik families, complex, 10 to 35 percent slopes	560	4716	2432605	2mnb4	id713		1:24000
Anvik-Routt-Sedgway families, complex, 10 to 35 percent slopes	561	4605	2432606	2mnb5	id713		1:24000
Davtone-Sedgway-Anvik families, complex, 10 to 35 percent slopes	560	63	3163425	2mnb4	id716		1:24000
Anvik-Routt-Sedgway families, complex, 10 to 35 percent slopes	561	53	3163426	2mnb5	id716		1:24000

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 (updated 2023-10-04).