Official Series Description


Lab Data Summary

Aggregate lab data for the MINAM soil series. This aggregation is based on all pedons with a current taxon name of MINAM, 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 MINAM 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
940A0831S1964OR063008Minam6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.3744431,-117.3038864
940A0832S1964OR063009MINAM5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.2994461,-117.1338882

Water Balance

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

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Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the MINAM 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 MINAM series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the MINAM 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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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with MINAM 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 MINAM series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the MINAM 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 .

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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 MINAM, 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. OR-2010-09-30-01 | Wallowa County -

Map Units

Map units containing MINAM 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
Keerins-Minam complex, 5 to 50 percent slopesV51057934346462mtqor6181:24000
Anatone-Minam-Rock outcrop association, 2 to 50 percent slopes11m6634346812mp1or6181:24000
Minam-Welch, frequently flooded complex, 0 to 3 percent slopes210m3034346782mszor6181:24000
Minam silt loam, 0 to 2 percent slopes4339AO113385423jghmor62620181:24000
Keerins-Minam complex, 5 to 50 percent slopesV5105734346302mtqor6271:24000
Anatone-Minam-Rock outcrop association, 2 to 50 percent slopes111455490471jgcnor62819971:24000
Minam silt loam, 0 to 2 percent slopes2091411490594jghmor62819971:24000
Minam-Welch complex, 0 to 3 percent slopes210354490597jghqor62819971:24000
Minam loam, 2 to 8 percent slopes2055610845832v0hor67019991:24000
Minam gravelly loam, 8 to 15 percent slopes2081918845862v0lor67019991:24000
Minam loam, 8 to 15 percent slopes2061175845842v0jor67019991:24000
Minam gravelly loam, 2 to 8 percent slopes2071138845852v0kor67019991:24000
Minam cobbly loam, 2 to 15 percent slopes209668845872v0mor67019991:24000
Minam-Endoaquepts complex, 2 to 8 percent slopes212592845912v0ror67019991:24000
Minam stony loam, 8 to 15 percent slopes211421845902v0qor67019991:24000
Minam-Endoaquepts complex, 8 to 15 percent slopes213176845922v0sor67019991:24000
Minam stony loam, 2 to 8 percent slopes21048845882v0nor67019991:24000

Map of Series Extent

Approximate geographic distribution of the MINAM 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 .