Official Series Description


Lab Data Summary

Aggregate lab data for the MCMULLIN soil series. This aggregation is based on all pedons with a current taxon name of MCMULLIN, 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 MCMULLIN were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MCMULLIN 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 MCMULLIN 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 MCMULLIN 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 MCMULLIN 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 MCMULLIN 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 MCMULLIN series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the MCMULLIN 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 MCMULLIN, 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 MCMULLIN 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
Tocaloma-McMullin complex, 50 to 75 slopes18025430459472hf3pca04119791:24000
Tocaloma-McMullin complex, 30 to 50 percent slopes1797545459471hf3nca04119791:24000
Tocaloma-McMullin-Urban land complex, 30 to 50 percent slopes1824700459474hf3rca04119791:24000
Bressa variant-McMullin variant complex, 30 to 50 percent slopes1091410459401hf1dca04119791:24000
Tocaloma-McMullin-Urban land complex, 15 to 30 percent slopes1811075459473hf3qca04119791:24000
Tocaloma-McMullin complex, 15 to 30 percent slopes178350459470hf3mca04119791:24000
McMullin-Plaskett complexMd18175455660h94qca05319721:24000
Bressa variant-McMullin variant complex, 30 to 50 percent slopes109m16074381qynvca09719681:20000
Tocaloma-McMullin complex, 30 to 50 percent slopes179m16074421qynzca09719681:20000
Tocaloma-McMullin complex, 15 to 30 percent slopes178m16074411qynyca09719681:20000
McMullin-Rock outcrop complex, 35 to 60 percent slopes113G1280712057rwylca60219781:24000
Heppsie-McMullin complex, 35 to 70 percent south slopes82G200712054rwyhca60219781:24000
Skookum-Rock outcrop-McMullin complex, 20 to 50 percent slopes173F94712064rwytca60219781:24000
McMullin-Rock outcrop complex, 3 to 35 percent slopes113E28712056rwykca60219781:24000
Skookum-Rock outcrop-McMullin complex, 1 to 20 percent slopes173D9712063rwysca60219781:24000
Lompico-McMullin loams, 30 to 75 percent slopes15420385457126hbp0ca66419771:24000
Lompico-McMullin loams, 15 to 30 percent slopes153380457125hbnzca66419771:24000
Lompico-McMullin complex, 50 to 75 percent slopes16214165457265hbthca66519771:24000
McMullin-Rock outcrop complex, 50 to 75 percent slopes1658325457268hbtlca66519771:24000
McMullin gravelly loam, 30 to 60 percent slopes56F381469495hrk0or03319791:20000
Medco-McMullin complex, 12 to 50 percent slopes125F36436469591hrn3or63219891:20000
McMullin-Rock outcrop complex, 35 to 60 percent slopes113G31150469573hrmjor63219891:20000
McMullin-Rock outcrop complex, 3 to 35 percent slopes113E21985469572hrmhor63219891:20000
Heppsie-McMullin complex, 35 to 70 percent south slopes82G10970469793hrvmor63219891:20000
McNull-McMullin gravelly loams, 35 to 60 percent south slopes116G10790469579hrmqor63219891:20000
McNull-McMullin gravelly loams, 12 to 35 percent south slopes116E9548469578hrmpor63219891:20000
McMullin-Medco complex, 12 to 50 percent slopes112F9355469571hrmgor63219891:20000
Medco-McMullin complex, 1 to 12 percent slopes125C6470469590hrn2or63219891:20000
McNull-McMullin complex, 35 to 60 percent north slopes117G6237469580hrmror63219891:20000
Skookum-Rock outcrop-McMullin complex, 20 to 50 percent slopes173F5982469654hrq4or63219891:20000
Skookum-Rock outcrop-McMullin complex, 1 to 20 percent slopes173D5698469653hrq3or63219891:20000
McMullin-McNull gravelly loams, 35 to 60 percent south slopes111G5341469570hrmfor63219891:20000
McMullin gravelly loam, 3 to 35 percent slopes110E3169469569hrmdor63219891:20000
McMullin-Reston complex, 30 to 75 percent slopes149F5819663772726or64919941:24000
McMullin-Reston complex, 3 to 30 percent slopes149E1902663762725or64919941:24000
McMullin-Reston-Rock outcrop complex, 30 to 75 percent slopes150F153966389272lor64919941:24000

Map of Series Extent

Approximate geographic distribution of the MCMULLIN 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 .