Official Series Description


Lab Data Summary

Aggregate lab data for the MCDUFF soil series. This aggregation is based on all pedons with a current taxon name of MCDUFF, 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 MCDUFF 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
183P0030S1982OR019001McDuff6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.4877777,-123.8055573

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MCDUFF 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 MCDUFF 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 MCDUFF 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 MCDUFF 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 hills figure.

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

Competing Series

Soil series competing with MCDUFF 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 MCDUFF 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 MCDUFF 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.

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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 MCDUFF, 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 MCDUFF 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
Apt-McDuff complex, 5 to 30 percent slopes912998854152vwbor00320041:24000
Apt-McDuff complex, 30 to 50 percent slopes107399854162vwcor00320041:24000
McDuff-Absaquil-Blachly complex, 30 to 60 percent slopes75E14686125921r3or01119831:20000
Absaquil-Blachly-McDuff complex, 3 to 30 percent slopes66D2016124521qnor01119831:20000
Orford-McDuff complex, 15 to 30 percent slopes186E22126512725rwor01519951:24000
Orford-McDuff complex, 0 to 15 percent slopes186D9586512625rvor01519951:24000
McDuff silty clay loam, 3 to 25 percent slopes50D37976237722x5or05319771:20000
McDuff silty clay loam, 25 to 50 percent slopes50E27236237822x6or05319771:20000
Apt-McDuff complex, 5 to 30 percent slopes1E89014045591j4kcor05319771:20000
McDuff silty clay loam, 50 to 75 percent slopes50F8486237922x7or05319771:20000
Apt-McDuff complex, 30 to 50 percent slopes1F37214045601j4kdor05319771:20000
Apt-McDuff complex, 30 to 50 percent slopes501E7196713227vkor05720061:24000
Apt-McDuff complex, 5 to 30 percent slopes501D7066713127vjor05720061:24000
Apt-McDuff complex, 5 to 30 percent slopes501D1238271118127vjor07119671:24000
Apt-McDuff complex, 30 to 50 percent slopes501E486271118227vkor07119671:24000
McDuff clay loam, 3 to 25 percent slopes81D2576627482394or63719811:20000
McDuff clay loam, 25 to 50 percent slopes81F2477627492395or63719811:20000
McDuff clay loam, 50 to 70 percent slopes81G1009627502396or63719811:20000
Apt-McDuff silty clay loams, 5 to 30 percent slopes1E1665064624257nor63819901:20000
Apt-McDuff silty clay loams, 30 to 50 percent slopes1F455564625257por63819901:20000
McDuff silty clay loam, 25 to 50 percent slopes68F8756435624z0or63919831:20000
McDuff silty clay loam, 50 to 75 percent slopes68G4106435724z1or63919831:20000
McDuff-Absaquil-Honeygrove complex, 30 to 60 percent slopes148F14207663752724or64919941:24000
Absaquil-Honeygrove-McDuff complex, 3 to 30 percent slopes3E133526685127khor64919941:24000
McDuff-Absaquil-Blachly complex, 30 to 60 percent slopes147F7464663732722or64919941:24000
Absaquil-Blachly-McDuff complex, 3 to 30 percent slopes2E53196676927gvor64919941:24000
Orford-McDuff complex, 30 to 60 percent slopes182F5171665012766or64919941:24000

Map of Series Extent

Approximate geographic distribution of the MCDUFF 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 .