Official Series Description


Lab Data Summary

Aggregate lab data for the MOUNTIRELAND soil series. This aggregation is based on all pedons with a current taxon name of MOUNTIRELAND, 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 MOUNTIRELAND 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
43C03N092303WA013001Mountireland6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.1199989,-117.8499985

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MOUNTIRELAND 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 MOUNTIRELAND 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 MOUNTIRELAND 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 MOUNTIRELAND 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 terrace figure.

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

Competing Series

Soil series competing with MOUNTIRELAND 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 MOUNTIRELAND 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 MOUNTIRELAND 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 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 MOUNTIRELAND, 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 MOUNTIRELAND 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
Mountemily-Mountireland complex, 0 to 15 percent slopes3304AO1317531207021sh5qor60720181:24000
Mountireland-Mountemily-McNamee complex, 15 to 30 percent slopes1838BO287431204111r005or60720181:24000
Troutmeadows-Mountireland-Pinuscreek complex, 2 to 25 percent slopes1819NO269231207811v6bxor60720181:24000
Mountireland-Mountemily-Balloontree complex, 0 to 15 percent slopes3300AW263931207962mh5qor60720181:24000
Troutmeadows-Mountireland-Mountemily complex, 0 to 15 percent slopes1740AO232031204021qzt1or60720181:24000
Mountemily-Troutmeadows-Mountireland complex, 15 to 30 percent slopes1814BO156131204051qzzror60720181:24000
Troutmeadows-Mountireland-Mountemily complex, 15 to 30 percent slopes1740BO131731202391nxz4or60720181:24000
Mountemily-Mountireland complex, 15 to 30 percent slopes3304BO54131207031sh5ror60720181:24000
Mountireland-Mountemily-McNamee complex, 0 to 15 percent slopes1838AO22831204101r004or60720181:24000
Mountireland-Deardorf complex, 15 to 30 percent slopes3476BO6431207111shrwor60720181:24000
Mountireland-Deardorf complex, 0 to 15 percent slopes3476AO92331224761shrvor62620181:24000
Troutmeadows-Mountireland-Mountemily complex, 0 to 15 percent slopes1740AO76531222141qzt1or62620181:24000
Mountireland-Mountemily-Downeygulch complex, 0 to 15 percent slopes4984AO50531223261r19tor62620181:24000
Mountireland-Deardorf complex, 15 to 30 percent slopes3476BO16831224771shrwor62620181:24000
Mountemily-Troutmeadows-Mountireland complex, 15 to 30 percent slopes1814BO1431222231qzzror62620181:24000
Troutmeadows-Mountireland-Mountemily complex, 15 to 30 percent slopes1740BO1431220961nxz4or62620181:24000
Mountireland-Mountemily-McNamee complex, 15 to 30 percent slopes1838BO122424864771r005or63120181:24000
Mountemily-Mountireland complex, 15 to 30 percent slopes3304BO120824864791sh5ror63120181:24000
Mountireland-Mountemily-McNamee complex, 0 to 15 percent slopes1838AO108924864761r004or63120181:24000
Troutmeadows-Mountireland-Mountemily complex, 15 to 30 percent slopes1740BO61624864721nxz4or63120181:24000
Mountemily-Mountireland complex, 0 to 15 percent slopes3304AO26124864781sh5qor63120181:24000
Troutmeadows-Mountireland-Mountemily complex, 0 to 15 percent slopes1740AO4324864691qzt1or63120181:24000
Mountemily-Troutmeadows-Mountireland complex, 15 to 30 percent slopes1814BO3924370841qzzror63120181:24000
Mountemily-Mountireland complex, 0 to 15 percent slopes3304AO125031214811sh5qor66719841:20000
Mountireland-Mountemily-Balloontree complex, 0 to 15 percent slopes3300AW831214932mh5qor66719841:20000
Mountemily-Mountireland complex, 15 to 30 percent slopes3304BO83031144942ygddwa71420181:24000
Mountemily-Mountireland complex, 0 to 15 percent slopes3304AO16231144932ygdcwa71420181:24000

Map of Series Extent

Approximate geographic distribution of the MOUNTIRELAND 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 .