Official Series Description


Lab Data Summary

Aggregate lab data for the MACMEAL soil series. This aggregation is based on all pedons with a current taxon name of MACMEAL, 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 MACMEAL 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
43B97P045196MT081007Macmeal5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.9294434,-114.1833344

Water Balance

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

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Soil series sharing subgroup-level classification with MACMEAL, 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 MACMEAL 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
Macmeal-Rock outcrop complex, 4 to 35 percent slopes250E543344523ckhnmt06519961:24000
Macmeal association, steep846195346549cmm0mt60819761:24000
Silverchief-Whitecow-Macmeal association, steep1152697346262cm9rmt60819761:24000
Silverchief-Whitecow-Macmeal complex, 15 to 60 percent slopes115F2513347578cnp6mt64119941:24000
Macmeal complex, 25 to 60 percent slopes84F1258347788cnwzmt64119941:24000
Macmeal-Kadygulch-Tolman families, complex, dissected mountain slopes31B703936633771p8h7mt64520131:12000
Totelake-Macmeal-Sharrott families, complex, dissected mountain slopes31B152906242380451bymt64520131:12000
Macmeal-Totelake-Sharrott families, complex, moderately steep mountain slopes32B30237113895541hmybmt64520131:12000
Macmeal-Kadygulch families, complex, steep mountain slopes30B31207124238012mc54mt64520131:12000
Macmeal-Haugan families, complex, fan remnants17B321273754411tb0vmt64520131:12000
Totelake-Sharrott-Macmeal families, complex, steep mountain slopes30B33759757659tfdmmt64520131:12000
Totelake-Macmeal-Sharrott families, complex, dissected mountain slopes31B152837615025551bymt64720071:24000
Macmeal-Kadygulch-Tolman families, complex, dissected mountain slopes31B702147115026051c3mt64720071:24000
Macmeal-Totelake-Sharrott families, complex, moderately steep mountain slopes32B301033115027951cqmt64720071:24000
Macmeal-Kadygulch families, complex, steep mountain slopes30B31789615022751b1mt64720071:24000
Totelake-Sharrott-Macmeal families, complex, steep mountain slopes30B33497615022951b3mt64720071:24000
Macmeal-Haugan families, complex, fan remnants17B323445150220519tmt64720071:24000
Totelake-Macmeal families, complex, landslides50B16282415038051gzmt64720071:24000
Macmeal-Rock outcrop complex, 4 to 35 percent slopes250E61215316501ndt2mt66620081:24000
Broback, stony-Macmeal, very bouldery-Rock outcrop complex, 30 to 70 percent slopes460532090382zdq2wy6291:24000
Macmeal, bouldery-Holter, stony-Rock outcrop complex, 45 to 70 percent slopes460432090372zdq1wy6291:24000
Macmeal, very stony-Foreleft complex, 6 to 30 percent slopes543929119142w7jnwy6291:24000
Broback, stony-Macmeal, very bouldery-Rock outcrop complex, 30 to 70 percent slopes460532505242zdq2wy65620081:24000

Map of Series Extent

Approximate geographic distribution of the MACMEAL 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 .