Official Series Description


Lab Data Summary

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


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the AITS 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 AITS series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

There are insufficient data to create the sibling sketch figure.

Select annual climate data summaries for the AITS 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 AITS 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 .

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 AITS 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 AITS 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 AITS 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.

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 AITS, 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 AITS 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
Aits stony loam, 0 to 40 percent slopes95371815829359q7wa06519781:24000
Aits stony loam, 40 to 65 percent slopes103264315805759gmwa06519781:24000
Aits loam, 40 to 65 percent slopes82869015828259pwwa06519781:24000
Aits-Rock outcrop complex, 40 to 65 percent slopes122281915807959hbwa06519781:24000
Aits loam, 25 to 40 percent slopes72064815827159pjwa06519781:24000
Aits-Rock outcrop complex, 0 to 40 percent slopes111916115806859gzwa06519781:24000
Aits loam, 15 to 25 percent slopes61854615826059p5wa06519781:24000
Aits loam, 0 to 15 percent slopes51378215824959ntwa06519781:24000
Rock outcrop-Aits complex, 30 to 65 percent slopes189778515815559kswa06519781:24000
Aits loam, 15 to 35 percent slopesAlE7418700342bw5wa61919681:24000
Aits-Rock land complex, 15 to 50 percent slopesAoE2585700372bw8wa61919681:24000
Aits silt loam, dry, 5 to 20 percent slopes64043706972ckkwa64819871:24000
Aits silt loam, dry, 20 to 40 percent slopes72289707082ckxwa64819871:24000
Aits silt loam, sandy substratum, 0 to 8 percent slopes8211707192cl8wa64819871:24000
Aits ashy loam, 15 to 35 percent slopes20230194950623fm9wa64920081:24000
Aits loam, high precipitation, 15 to 25 percent slopes5810515841259v2wa65119811:24000
Aits loam, high precipitation, 25 to 40 percent slopes6615715842359vfwa65119811:24000
Aits loam, high precipitation, 0 to 15 percent slopes4566915840159tqwa65119811:24000
Aits loam, high precipitation, 40 to 65 percent slopes7557215843459vswa65119811:24000
Aits stony loam, high precipitation, 0 to 40 percent slopes8443215844559w4wa65119811:24000
Aits, high precipitation-Rock outcrop complex, 0 to 40 percent slopes10198815830659qnwa65119811:24000
Aits stony loam, high precipitation, 40 to 65 percent slopes9159115845659whwa65119811:24000
Aits, high precipitation-Rock outcrop complex, 40 to 65 percent slopes11151815831759r0wa65119811:24000
Rock outcrop-Aits, high precipitation, complex, 30 to 65 percent slopes11440415832259r5wa65119811:24000
Aits ashy loam, 15 to 35 percent slopes100350612985nkvqwa74920051:24000

Map of Series Extent

Approximate geographic distribution of the AITS 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 .