Official Series Description


Lab Data Summary

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

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
23140A0610S1956AK090001FAIRBANKS5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties64.8844452,-147.789444
23140A0611S1956AK090002FAIRBANKS4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties64.9097214,-147.6261139
23140A0612S1959AK090001FAIRBANKS5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties64.9097214,-147.6261139
23140A0613S1959AK090002FAIRBANKS5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties64.7941666,-147.9894409
23140A0614S1959AK090003FAIRBANKS5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties64.8905563,-147.3230591
23140A0616S1960AK090001FAIRBANKS6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties64.9097214,-147.6261139
23140A0615S1960AK090003FAIRBANKS6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties64.8905563,-147.3230591
23104N0278S2003AK090008Fairbanks6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties64.8666687,-147.8666687
23104N0281S2003AK090010Fairbanks6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties64.8039474,-148.3311462

Water Balance

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

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Select annual climate data summaries for the FAIRBANKS 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 FAIRBANKS 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.

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

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Select annual climate data summaries for the FAIRBANKS 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 FAIRBANKS 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.

Click the image to view it full size.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with FAIRBANKS, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. AK-2011-05-27-01 | Fairbanks Area - 1959

    Diagram of a landscape showing relationship of soil series, underlying material, and permafrost. Adapted from Pewe (Soil Survey of Fairbanks Area, Alaska; 1959).

Map Units

Map units containing FAIRBANKS 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
Fairbanks silt loam, 12 to 20 percent slopes1189824692878r7zxak61020031:25000
Fairbanks silt loam, 7 to 12 percent slopes1175883692876r7zvak61020031:25000
Fairbanks silt loam, 20 to 30 percent slopes1193653692879r7zyak61020031:25000
Fairbanks silt loam, 3 to 7 percent slopes1161291692875r7ztak61020031:25000
Fairbanks silt loams, strongly sloping and steep121755692877r7zwak61020031:25000
Fairbanks-Steese complex, 20 to 30 percent slopes123695692918r816ak61020031:25000
Fairbanks silt loam, 30 to 45 percent slopes120458692880r7zzak61020031:25000
Fairbanks-Steese complex, 12 to 20 percent slopes122178692917r815ak61020031:25000
Saulich-Fairbanks complex, 3 to 12 percent slopes13310929517691qvzak64219901:24000
Fairbanks silt loam, 7 to 12 percent slopes1084209517441qv5ak64219901:24000
Fairbanks silt loam, 12 to 20 percent slopes1091786517451qv6ak64219901:24000
Fairbanks silt loam, 3 to 7 percent slopes107341517431qv4ak64219901:24000
Fairbanks silt loam, 12 to 20 percent slopes42D1033510631q46ak65020061:24000
Fairbanks silt loams, strongly sloping and steep42CG776510621q45ak65020061:24000
Fairbanks silt loam, 3 to 7 percent slopes42B638510601q43ak65020061:24000
Fairbanks-Steese complex, 12 to 20 percent slopes421D629511151q5wak65020061:24000
Fairbanks silt loam, 7 to 12 percent slopes42C551510611q44ak65020061:24000
Fairbanks and Steese silt loams, 15 to 45 percent slopes89X514520101r3rak65020061:24000
Fairbanks silt loam, 20 to 30 percent slopes42E136510641q47ak65020061:24000
Fairbanks silt loam, 12 to 20 percent slopes31FA0318547202556725zrwak65520071:25000
Fairbanks silt loams, gullied, 7 to 70 percent slopes31FA075474202557125zs0ak65520071:25000
Fairbanks-Steese complex, 20 to 30 percent slopes31FA112741202557525zs4ak65520071:25000
Fairbanks-Steese complex, 12 to 20 percent slopes31FA102020202557425zs3ak65520071:25000
Fairbanks silt loam, 30 to 45 percent slopes31FA051618202556925zryak65520071:25000
Fairbanks silt loam, 3 to 7 percent slopes31FA011376202556525zrtak65520071:25000
Fairbanks-Steese complex, 30 to 45 percent slopes31FA12811202557625zs5ak65520071:25000
Fairbanks-Steese complex, 7 to 12 percent slopes31FA09676202557325zs2ak65520071:25000
Fairbanks-Steese complex, 3 to 7 percent slopes31FA08393202557225zs1ak65520071:25000
Fairbanks silt loam, 45 to 70 percent slopes31FA06287202557025zrzak65520071:25000

Map of Series Extent

Approximate geographic distribution of the FAIRBANKS 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 .