Official Series Description


Lab Data Summary

Aggregate lab data for the DEFORD soil series. This aggregation is based on all pedons with a current taxon name of DEFORD, 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 DEFORD 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 DEFORD 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 DEFORD 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 DEFORD 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 DEFORD 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 DEFORD 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 DEFORD 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 DEFORD 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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Click the image to view it full size.

Soil series sharing subgroup-level classification with DEFORD, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. MI-2010-09-07-23 | Montmorency County - 2003

    Typical pattern of soils and underlying material in the Rubicon-Grayling-Tawas and Millersburg-Klacking-Horsehead associations (Soil Survey of Montmorency County, Michigan; 2003).

  2. MI-2010-09-07-24 | Montmorency County - 2003

    Typical pattern of soils and underlying material in the Deford-Au Gres-Croswell association (Soil Survey of Montmorency County, Michigan; 2003).

  3. MI-2010-09-10-05 | Keweenaw County Area - 2006

    Typical pattern of soils and parent material in the Dawson-Au Gres-Croswell association (Soil Survey of Keweenaw County Area, Michigan; 2006).

  4. MI-2010-09-10-06 | Keweenaw County Area - 2006

    Typical pattern of soils and parent material in the Deer Park-Rubicon-Croswell association (Soil Survey of Keweenaw County Area, Michigan; 2006).

  5. MI-2010-09-10-07 | Keweenaw County Area - 2006

    Typical pattern of soils and parent material in the Garlic-Waiska-Alcona association (Soil Survey of Keweenaw County Area, Michigan; 2006).

  6. MI-2010-09-10-08 | Keweenaw County Area - 2006

    Typical pattern of soils and parent material in the Lupton-Tawas-Deford association (Soil Survey of Keweenaw County Area, Michigan; 2006).

  7. MI-2012-02-06-38 | Menominee County - September 1989

    Typical pattern of soils and parent material in the Deford-Wainola-Rousseau map unit (Soil Survey of Menominee County, Michigan; September 1989).

  8. WI-2012-03-23-18 | Marinette County - February 1991

    Pattern of soils and parent material in the Wainola-Deford association (Soil Survey of Marinette County, WI; 1991).

Map Units

Map units containing DEFORD 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
Tawas-Deford mucks931182914553051kvcbmi00320071:24000
Deford and Leafriver soils, 0 to 2 percent slopes1975214552542xxj3mi00320071:24000
Wurtsmith-Deford complex, 0 to 6 percent slopes298B22614554331kvhgmi00320071:24000
Deford muck369182091912746f14mi00719981:12000
Au Gres-Deford complex, 0 to 3 percent slopes368A65331913426f3bmi00719981:12000
Proper-Deford-Rousseau complex, 0 to 40 percent slopes396F44441912816f1cmi00719981:12000
Deford muck, 0 to 2 percent slopesDefaaA185231558992ytj8mi00919761:15840
Au Gres-Deford complex, 0 to 3 percent slopesAugdeA152131558912ytj7mi00919761:15840
Deford loamy fine sandDn36461891476btjmi01119641:20000
Deford loamDm2191891466bthmi01119641:20000
Deford and Leafriver soils, 0 to 2 percent slopes811418124418942xxj3mi01319841:20000
Deford muck, 0 to 2 percent slopesDefaaA731560152ytj8mi02919701:15840
Deford and Leafriver soils, 0 to 2 percent slopes50105344151592xxj3mi03319891:15840
Deford and Leafriver soils, 0 to 2 percent slopesDm67015880422xxj3mi04119691:24000
Deford and Leafriver soils, 0 to 2 percent slopes2643484152122xxj3mi04319851:20000
Deford loamy fine sandDf3061893236c06mi04719681:20000
Roscommon-Deford associationRD42581898476ck3mi05119661:15840
Wainola-Deford associationWD14191898656ckpmi05119661:15840
Deford and Leafriver soils, 0 to 2 percent slopes65027614562262xxj3mi05320071:24000
Deford-Tawas complex, 0 to 1 percent slopes7710564416160fz1jmi06119891:20000
Deford and Leafriver soils, 0 to 2 percent slopes6721684161512xxj3mi06119891:20000
Ingalls-Deford complex, 0 to 4 percent slopes8156A84624847952pdmpmi06119891:20000
Deford muck369140081918326fm4mi06919951:15840
Au Gres-Deford complex, 0 to 3 percent slopes368A77261918316fm3mi06919951:15840
Finch-Deford-Au Gres complex, 0 to 3 percent slopes409A18301918556fmwmi06919951:15840
Proper-Finch-Deford complex, 0 to 6 percent slopes410B9231918576fmymi06919951:15840
Au Gres-Deford complex, 0 to 3 percent slopesAugdeA431870382ytj7mi07919981:12000
Croswell, rarely flooded-Deford, frequently flooded complex, 0 to 6 percent slopes201B1728631370p5zsmi09520041:24000
Deford and Leafriver soils, 0 to 2 percent slopes2310846274672xxj3mi09520041:24000
Deford and Leafriver soils, 0 to 2 percent slopes23125404163792xxj3mi09719941:20000
Wainola-Deford fine sands, 0 to 2 percent slopesWdA2425086686924mi09919671:20000
Tawas-Deford mucks9313492395304f8brmi10319991:24000
Croswell-Deford complex, 0 to 3 percent slopes118A9344394998f80wmi10319991:24000
Deford and Leafriver soils, 0 to 2 percent slopes1924663951462xxj3mi10319991:24000
Au Gres-Deford complex, 0 to 3 percent slopes203A1955395160f863mi10319991:24000
Deford-Wainola-Rousseau complex, 0 to 12 percent slopes45C35413415481fybmmi10919851:20000
Tawas-Deford complex4421162415480fyblmi10919851:20000
Deford and Leafriver soils, 0 to 2 percent slopes2190674154592xxj3mi10919851:20000
Urban land-Deford complex341023415472fybbmi10919851:20000
Wainola-Deford associationWD3426735666ckpmi11119761:15840
Deford-Au Gres-Croswell complex, 0 to 6 percent slopes352B55191922486g1kmi11919971:12000
Deford muck36951611922616g1zmi11919971:12000
Morganlake-Iosco-Deford complex, 0 to 6 percent slopes422B16401922956g32mi11919971:12000
Tonkey and Deford soilsTd536918738468znmi12119661:15840
Deford fine sandDs202718734368ybmi12119661:15840
Deford-Tawas complex, 0 to 1 percent slopes90A161114565011kwlxmi13120071:24000
Au Gres-Deford complex, 0 to 3 percent slopes19A106214564001kwhnmi13120071:24000
Deford and Leafriver soils, 0 to 2 percent slopes30A70914564092xxj3mi13120071:24000
Ingalls-Deford complex, 0 to 4 percent slopes8156A13116748451t6t8mi13120071:24000
Deford-Au Gres-Croswell complex, 0 to 6 percent slopes352B7632241413836jmi13520031:12000
Au Gres-Deford complex, 0 to 3 percent slopes368A212520904170j8mi13520031:12000
Deford muck369778241423836vmi13520031:12000
Deford muck3697681914866f7zmi13719981:12000
Au Gres-Deford complex, 0 to 3 percent slopes368A6501914856f7ymi13719981:12000
Deford-Au Gres-Croswell complex, 0 to 6 percent slopes352B5911914836f7wmi13719981:12000
Deford muck36957211909866dqvmi14319991:12000
Augres-Deford complex, 0 to 3 percent slopes368A51321909856dqtmi14319991:12000
Deford-Kinross mucks4736611909746dqgmi14319991:12000
Proper-Finch-Deford complex, 0 to 6 percent slopes410B2831910446dsqmi14319991:12000
Wainola-Deford fine sands, 0 to 2 percent slopesWdA254181874616924mi14719691:20000
Deford fine sandDe703187412690kmi14719691:20000
Wainola-Deford fine sands, 0 to 2 percent slopesWfA2525083166924mi15119551:15840
Deford fine sandDe32508265690kmi15119551:15840
Deford and Leafriver soils, 0 to 2 percent slopes632401614569482xxj3mi15320071:24000
Ausable, Deford, and Tawas mucks, frequently flooded651720014570231kx4rmi15320071:24000
Deford-Rubicon-Au Gres complex, 0 to 15 percent slopes540D1477916123041r3qtmi15320071:24000
Deford-Meehan-Seney complex, 0 to 3 percent slopes493A952616118841r398mi15320071:24000
Rousseau-Neconish-Deford complex, 0 to 25 percent slopes22E773515380361nmg2mi15320071:24000
Pelkie, occasionally flooded-Deford,frequently flooded, complex, 0 to 4 percent slopes67B656414569131kx16mi15320071:24000
Au Gres-Deford complex, 0 to 3 percent slopes19A650614569381kx20mi15320071:24000
Deer Park-Deford-Tawas complex, 0 to 60 percent slopes70F620614569521kx2gmi15320071:24000
Wurtsmith-Tawas-Deford complex, 0 to 6 percent slopes86B584714570291kx4ymi15320071:24000
Deford-Meehan complex, 0 to 3 percent slopes, drained516A462514569821kx3fmi15320071:24000
Neconish-Deford, rarely flooded-Wainola complex, 0 to 6 percent slopes491B249016118201r376mi15320071:24000
Deford-Seney complex, frequently flooded, 0 to 3 percent slopes518A130616503451sd9ymi15320071:24000
Tawas-Deford complex, 0 to 4 percent slopes137172800734vw74mi60520041:24000
Au Gres-Deford-Croswell complex, 0 to 6 percent slopes126B3486800765vw84mi60520041:24000
Betsy Bay-Burt-Deford complex, 0 to 3 percent slopes39A1667800738vw78mi60520041:24000
Meehan-Deford complex, 0 to 3 percent slopesB77A31982653435sfxwmn00719911:24000
Deford-Leafriver complex, 0 to 2 percent slopesB76A4592653434sfxvmn00719911:24000
Redby-Deford-Hiwood complex, 0 to 3 percent slopesB252A1144131151422z32mmn02119931:20000
Redby-Deford-Hiwood complex, 0 to 3 percent slopesB252A1007831151452z32mmn06119821:24000
Meehan-Deford complex, 0 to 3 percent slopesB77A237162943772sfxwmn62520151:24000
Leafriver-Deford, depressional-Markey complex, 0 to 1 percent slopesB71A233662943770sfxsmn62520151:24000
Deford-Leafriver complex, 0 to 2 percent slopesB76A201812943771sfxvmn62520151:24000
Deford loamy fine sandDd126202949299wwvny08919901:24000
Deford mucky loamy fine sandDf125032949309wwwny08919901:24000
Deford loamy fine sandDe2469422226g5c6wi02919751:15840
Rousseau-Deford fine sands, 2 to 6 percent slopesRrB2320422271g5dnwi02919751:15840
Deford and Cormant soils, 0 to 2 percent slopesDeCo1908531190472xxj0wi07519871:20000
Deford and Leafriver soils, 0 to 2 percent slopesDeLe1869331190482xxj3wi07519871:20000
Deford muck, 0 to 2 percent slopesDe18574223852tnyswi07519871:20000
Deford and Leafriver soils, 0 to 2 percent slopesDeLeA15383958552xxj3wi07819981:12000
Deford and Cormant soils, 0 to 2 percent slopesDeCo1709231190522xxj0wi08319851:15840
Deford and Leafriver soils, 0 to 2 percent slopesDeLe409931190532xxj3wi08319851:15840
Deford loamy fine sandDe6872422542g5pdwi08719751:15840
Deford and Cormant soils, 0 to 2 percent slopesDeCo233731190562xxj0wi11519811:15840
Deford and Leafriver soils, 0 to 2 percent slopesDeLe133631190582xxj3wi11519811:15840

Map of Series Extent

Approximate geographic distribution of the DEFORD 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 .