Official Series Description


Lab Data Summary

Aggregate lab data for the MALLORY soil series. This aggregation is based on all pedons with a current taxon name of MALLORY, 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 MALLORY 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
991P010990ID069001Mallory6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.2038879,-116.8633347
991P011090ID069002Mallory6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.2083321,-116.8616638

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MALLORY 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 MALLORY 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 MALLORY 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 MALLORY 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 MALLORY 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 MALLORY 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 MALLORY 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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Click the image to view it full size.

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 MALLORY, 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 MALLORY 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
Mallory-Jacket complex, 10 to 40 percent slopes832968796992nxyid61119941:24000
Gwinly-Mallory complex, 30 to 60 percent slopes5027CO31531202821qpxsor60720181:24000
Mallory-Sopher complex, 30 to 60 percent slopes5028CO27331202861qq1jor60720181:24000
Gwinly-Sopher-Mallory complex, 15 to 30 percent slopes5026BO16831202901qqk4or60720181:24000
Gwinly-Mallory-Kettenbach complex, 60 to 90 percent south slopes85F1966404524mzor62519791:20000
Gwinly-Mallory-Kettenbach complex, 30 to 60 percent south slopes85E1556404624n0or62519791:20000
Gwinly-Mallory-Kettenbach complex, 15 to 30 percent south slopes85D186404324mxor62519791:20000
Gwinly-Kettenbach-Mallory complex, 60 to 90 percent south slopes5867DO97312437384nj3nor63120181:24000
Gwinly-Kettenbach-Mallory complex, 30 to 60 percent south slopes5867CO44432437383nj3lor63120181:24000
Gwinly-Mallory-Rock outcrop complex, 40 to 90 percent south slopes6113DR33272437466nj3qor63120181:24000
Gwinly-Kettenbach-Mallory complex, 15 to 30 percent south slopes5867BO2262437382nj3jor63120181:24000
Gwinly-Mallory-Kettenbach complex, 30 to 60 percent south slopes10117118844722twxor67019991:24000
Gwinly-Mallory-Kettenbach complex, 60 to 90 percent south slopes1026394844732twyor67019991:24000
Mallory-Lawyer-Rock outcrop complex, 60 to 90 percent north slopes2023855845802v0dor67019991:24000
Gwinly-Mallory-Kettenbach complex, 15 to 30 percent south slopes1002502844712twwor67019991:24000
Gwinly-Mallory-Rock outcrop complex, 40 to 90 percent south slopes1032205844602twjor67019991:24000
Gwinly-Mallory complex, 30 to 70 percent south slopes991125844592twhor67019991:24000
Mallory-Gwinly-Lawyer complex, 30 to 60 percent north slopes201713845792v0cor67019991:24000
Gwinly-Mallory complex, 3 to 30 percent slopes98518844582twgor67019991:24000
Mallory-Gwinly-Lawyer complex, 15 to 30 percent north slopes200198845762v08or67019991:24000
Gwinly-Mallory very stony silt loams, 30 to 70 percent slopes3720201694372b7xwa60319841:24000
Gwinly-Mallory-Rock outcrop complex, 40 to 90 percent slopes3813274694382b7ywa60319841:24000
Mallory-Rock outcrop complex, 40 to 90 percent slopes644499694672b8wwa60319841:24000
Gwinly-Mallory complex, 3 to 30 percent slopes363886694362b7wwa60319841:24000
Lawyer-Mallory complex, 30 to 90 percent slopes542756694562b8jwa60319841:24000
Mallory-Lawyer-Rock outcrop complex, 60 to 90 percent north slopes117461817781wfz1wa60319841:24000
Ferdinand variant-Mallory variant association, 8 to 70 percent slopes29445694282b7mwa60319841:24000
Gwinly-Mallory very stony silt loams, 30 to 70 percent slopes3754697472bkxwa62319701:20000
Gwinly-Mallory complex, 3 to 30 percent slopes3620697462bkwwa62319701:20000

Map of Series Extent

Approximate geographic distribution of the MALLORY 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 .