Soil Data Explorer - TYPIC CRYAQUODS

Official Series Description

Lab Data Summary

Aggregate lab data for the TYPIC CRYAQUODS soil series. This aggregation is based on all pedons with a current taxon name of TYPIC CRYAQUODS, 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 TYPIC CRYAQUODS were used in the calculation. Source: KSSL snapshot (updated 2020-03-13). 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 TYPIC CRYAQUODS 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 TYPIC CRYAQUODS series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-10-24), parsed OSD records (updated 2024-10-23) and snapshot of SC database (updated 2024-10-23).

There are insufficient data to create the sibling sketch figure.

Select annual climate data summaries for the TYPIC CRYAQUODS 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 2024-10-23).

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the TYPIC CRYAQUODS 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 2024-10-23).

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.

Competing Series

Soil series competing with TYPIC CRYAQUODS share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2024-10-23) and snapshot of the SC database (updated 2024-10-23).

There are insufficient data to create the competing sketch figure.

Select annual climate data summaries for the TYPIC CRYAQUODS 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 2024-10-23).

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the TYPIC CRYAQUODS 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 2024-10-23).

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 TYPIC CRYAQUODS, 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 2024-10-23).

This figure is not available.

Block Diagrams

No block diagrams are available.

Map Units

Map units containing TYPIC CRYAQUODS 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
Typic Cryaquods, 0 to 20 percent slopes	143	317	51732	1qts	ak641	1985	1:31680
Cryohemists-Typic Cryaquods association, rolling lowlands, 6 to percent slopes	63T	12885	50153	1p5v	ak646	1992	1:31680
Typic Cryaquods-Typic Humicryods assocation, rolling hills, 36 to 55 percent slopes	42KC	10275	50061	1p2w	ak646	1992	1:31680
Typic Humicryods-Typic Cryaquods complex, 6 to 35 percent slopes	51K	5999	50102	1p46	ak646	1992	1:31680
Typic Cryaquods-Typic Humicryods association, broken, 36 to 55 percent slopes	36KC	5859	50033	1p1z	ak646	1992	1:31680
Typic Cryaquods-Typic Humicryods-McGilvery association, broken, 56 to 75 percent slopes	36KD	4043	50034	1p20	ak646	1992	1:31680
Typic Cryaquods-Typic Humicryods-McGilvery association, smooth, 56 to 75 percent slopes	35KD	3788	49963	1nzq	ak646	1992	1:31680
Typic Cryaquods-Typic Humicryods association, smooth hills, 36 to 55 percent slopes	44KC	3467	50088	1p3r	ak646	1992	1:31680
Cryohemists-Typic Cryaquods association, sloping lowlands, 6 to 35 percent slopes	61T	3309	50144	1p5k	ak646	1992	1:31680
Typic Cryaquods-Typic Humicryods-McGilvery association, shallowly incised, 56 to 75 percent slopes	32KD	2990	49918	1ny8	ak646	1992	1:31680
Cryohemists-Typic Cryaquods association, dissected footslopes, 6 35 percent slopes	52T	2371	50119	1p4r	ak646	1992	1:31680
Typic Cryaquods-Typic Humicryods association, deeply incised, 36 to 55 percent slopes	31KC	1839	49876	1nwx	ak646	1992	1:31680
Typic Cryaquods-Typic Humicryods association, smooth, 36 to 55 percent slopes	35KC	1590	49962	1nzp	ak646	1992	1:31680
Typic Cryaquods-Typic Humicryods-McGilvery association, deeply incised, 56 to 75 percent slopes	31KD	1420	49877	1nwy	ak646	1992	1:31680
Typic Cryaquods-Typic Humicryods association, shallowly incised, 36 to 55 percent slopes	32KC	1189	49917	1ny7	ak646	1992	1:31680
Typic Cryaquods-Typic Humicryods-McGilvery association, rolling hills, 56 to 75 percent slopes	42KD	1179	50062	1p2x	ak646	1992	1:31680
Typic Cryaquods-Typic Humicryods-McGilvery association, smooth hills, 56 to 75 percent slopes	44KD	1176	50089	1p3s	ak646	1992	1:31680
Typic Cryaquods-Typic Humicryods-McGilvery association, 76 to 120 percent slopes	31KE	968	49878	1nwz	ak646	1992	1:31680
Cryohemists-Typic Cryaquods association, footslopes, 6 to 35 percent slopes	51T	797	50103	1p47	ak646	1992	1:31680
Typic Cryaquods-Histic Cryaquepts association, flat lowlands, 0 to 5 percent slopes	6231A	10699	2805087	2tpt4	ak693	2019	1:63360
Typic Cryosaprists-Typic Cryaquods complex, glacial topography, 0 to 5 percent slopes	6375B	5497	2805099	2tptj	ak693	2019	1:63360
Oxyaquic Haplocryods-Typic Cryaquods association, rolling hills, 6 to 35 percent slopes	4213B	3547	2805072	2tpsp	ak693	2019	1:63360
Typic Cryaquods-Typic Humicryods-McGilvery association, deeply incised, 76 to 120 percent slopes	3100KE	269	2805122	2tpvm	ak693	2019	1:63360

Map of Series Extent

Approximate geographic distribution of the TYPIC CRYAQUODS 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 2024-10-30).