Official Series Description


Lab Data Summary

Aggregate lab data for the MACK soil series. This aggregation is based on all pedons with a current taxon name of MACK, 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 MACK 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
3580P037180CO083002Mack7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.2636108,-108.9466629

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MACK 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 MACK 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 MACK 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 MACK 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 mountains figure.

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Competing Series

Soil series competing with MACK 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 MACK 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 MACK 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 mountains figure.

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

Soil series sharing subgroup-level classification with MACK, 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 MACK 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
Mack fine sandy loam, 1 to 3 percent slopes562261594071ztcco67020051:24000
Mack fine sandy loam, 0 to 6 percent slopes551070594461zvmco67020051:24000
Mack fine sandy loam, 3 to 6 percent slopes571039594081ztdco67020051:24000
Mack fine sandy loam, 0 to 6 percent slopes705407576971y16co67119971:24000
Mack clay loam, 0 to 2 percent slopes7612164508793k2fpco67720181:24000
Mack loam, 2 to 5 percent slopes766948800782vw8pco67720181:24000
Mack-Utaline, sodic complex, 3 to 12 percent slopes, very stonyMC485533170497k09lco67919761:24000
Mack loam, 2 to 5 percent slopes766422990929vw8pco67919761:24000
Mack-Avalon complex, moist, 3 to 12 percent slopes715303506763k0b6co68019701:31680
Avalon-Mack-Skumpah complex, 2 to 25 percent slopes793122506770k0bfco68019701:31680
Mack-Utaline, sodic complex, 3 to 12 percent slopes, very stony482787506744k09lco68019701:31680
Mack-Gyprockmesa complex, 1 to 5 percent slopes1311652506832k0dfco68019701:31680
Mack loam, 0 to 2 percent slopesMa609506810k0cqco68019701:31680
Mack-Avalon complex, moist, 3 to 12 percent slopesMC7133170528k0b6co68219861:24000
Avalon-Mack complex, 1 to 12 percent slopes64945497237jpdxco68619921:31680
Mack-Mesa fine sandy loams, 1 to 4 percent slopes2108412573731xprnm71719931:24000
Mack fine sandy loam, 1 to 3 percent slopes5285565574581xshnm71719931:24000
Mack loam, 2 to 6 percent slopes2816958504521jxzwut62419851:24000
Mack-Sagers complex297272504522jxzxut62419851:24000
Avalon-Mack-Skumpah complex, 2 to 25 percent slopes6791942990970k0bfut62419851:24000
Moffat-Seeg, warm-Mack, moist complex, 2 to 15 percent slopes5047406359792206sut68620041:24000
Moffat-Mack, moist complex, 1 to 5 percent slopes5049371159811207dut68620041:24000
Mack sandy loam, 1 to 4 percent slopes211631708722w7kdwy6031:24000
Mack sandy loam, 1 to 4 percent slopes211629119372w7kdwy6291:24000

Map of Series Extent

Approximate geographic distribution of the MACK 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 .