Official Series Description


Lab Data Summary

Aggregate lab data for the GOLDSTREAM soil series. This aggregation is based on all pedons with a current taxon name of GOLDSTREAM, 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 GOLDSTREAM 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
23104N0279S2003AK090006Goldstream6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties64.8668518,-147.8747406

Water Balance

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

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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.

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Competing Series

Soil series competing with GOLDSTREAM 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 GOLDSTREAM 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 GOLDSTREAM 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 GOLDSTREAM, 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 GOLDSTREAM 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
Goldstream peat, 0 to 3 percent slopes13311523692858r7z8ak61020031:25000
Chatanika-Goldstream complex1078081692905r80sak61020031:25000
Goldstream peat, 3 to 7 percent slopes1341394692859r7z9ak61020031:25000
Goldstream-Histels complex, 0 to 3 percent slopes135159692906r80tak61020031:25000
Goldstream and Histosols, 0 to 3 percent slopes30824217494331nfmak64019861:24000
Goldstream peat, 0 to 3 percent slopes30420065494291nfhak64019861:24000
Goldstream-Tanana complex, 0 to 3 percent slopes3078290494321nflak64019861:24000
Goldstream peat, 3 to 7 percent slopes3053593494301nfjak64019861:24000
Tanana, moderately wet-Goldstream complex, 0 to 3 percent slopes3262847494511ng6ak64019861:24000
Goodpaster variant-Goldstream complex, 0 to 3 percent slopes3092661494341nfnak64019861:24000
Goldstream peat, 7 to 12 percent slopes3062412494311nfkak64019861:24000
Tanana, moderately wet-Goldstream complex, 3 to 7 percent slopes3271329494521ng7ak64019861:24000
Goldstream-Pergelic Cryohemists complex, 0 to 2 percent slopes11767220517531qvgak64219901:24000
Goldstream peat, 0 to 3 percent slopes1156378517511qvdak64219901:24000
Goldstream peat, 3 to 7 percent slopes1166025517521qvfak64219901:24000
Goldstream-Histels complex, 0 to 3 percent slopes21212606510921q54ak65020061:24000
Chatanika-Goldstream complex, 0 to 5 percent slopes2116528510911q53ak65020061:24000
Goldstream peat, 0 to 3 percent slopes21A4597510451q3mak65020061:24000
Goldstream peat, 3 to 7 percent slopes21B1566510461q3nak65020061:24000
Chatanika-Goldstream complex, 0 to 5 percent slopes31CH0412468202556125zrpak65520071:25000
Goldstream peat, 0 to 3 percent31GD015195202557725zs6ak65520071:25000
Goldstream peat, 3 to 7 percent slopes31GD021593202557825zs7ak65520071:25000

Map of Series Extent

Approximate geographic distribution of the GOLDSTREAM 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 .