Official Series Description


Lab Data Summary

Aggregate lab data for the GADDY soil series. This aggregation is based on all pedons with a current taxon name of GADDY, 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 GADDY 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 GADDY 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 GADDY 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 GADDY 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 GADDY 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.

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.

Competing Series

Soil series competing with GADDY 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 GADDY 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 GADDY 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 .

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

There are insufficient data to create the 3D mountains figure.

Click the image to view it full size.

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

Soil series sharing subgroup-level classification with GADDY, 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. OK-2010-09-29-08 | Noble County - 2005

    Typical pattern of soils and underlying material in the Keokuk-Goodnight-Ashport and the McLain-Braman-Lela general soil map units (Soil Survey of Noble County, Oklahoma; 2005).

  2. OK-2012-02-17-25 | Payne County - April 1987

    Typical pattern of soils and underlying material in the Yahola-Gaddy-Hawley map unit (Soil Survey of Payne County, Oklahoma; April 1987).

  3. TX-2010-11-04-05 | McLennan County - 2001

    Pattern of soils in the Weswood-Yahola-Ships general soil map unit (Soil Survey of McLennan County, Texas; 2001).

  4. TX-2010-11-04-14 | Robertson County - 2007

    Pattern of soils and underlying material on the flood plain along the Brazos and Little Brazos Rivers and on adjacent terraces. Included are the Chazos-Dutek-Silawa, Ships-HIghbank, and Weswood-Yahola-Coarsewood general soil map units (Soil Survey of Robertson County, Texas; 2007).

  5. TX-2012-03-21-56 | Palo Pinto County - August 1981

    Typical pattern of soils in the Bastrop-Apalo map unit (Soil Survey of Palo Pinto County, TX; 1981).

Map Units

Map units containing GADDY 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
Gaddy loamy fine sand, 0 to 1 percent slopes, frequently floodedLs39783814312tp6qok00319711:24000
Gaddy loamy fine sand, 0 to 1 percent slopes, occasionally floodedLn86863817402tp6rok01119651:24000
Gracemore-Gaddy complex, 0 to 1 percent slopes, occasionally flooded42129382107dtm1ok02719841:24000
Yahola-Gaddy complex, 0 to 1 percent slopes, frequently flooded856474382621dv4mok04919821:24000
Gaddy loamy fine sand, 0 to 1 percent slopes, occasionally flooded1025753826972tp6rok05319831:24000
Gaddy fine sand, 0 to 1 percent slopes, frequently flooded919203827502tp6tok05319831:24000
Gaddy fine sand, 0 to 1 percent slopes, frequently floodedCr193103832232tp6tok06719671:24000
Gaddy loamy fine sand, 0 to 1 percent slopes, occasionally floodedYf12453833832tp6rok07119651:24000
Gaddy fine sand, 0 to 1 percent slopes, frequently floodedLm6913833392tp6tok07119651:24000
Gaddy loamy fine sand, 0 to 1 percent slopes, occasionally floodedLc62843833992tp6rok07319601:24000
Gaddy and Gracemore soils, 0 to 1 percent slopes, frequently floodedLn5776383400dvyrok07319601:24000
Gaddy loamy fine sand, 0 to 1 percent slopes, occasionally floodedCr2023835062tp6rok08119661:24000
Gaddy-Gracemore complex, 0 to 1 percent slopes, frequently floodedGaGA182238361530x61ok08319941:12000
Gaddy loamy fine sand, 0 to 1 percent slopes, occasionally floodedGadA12203836162tp6rok08319941:12000
Gaddy loam, 0 to 1 percent slopes, frequently floodedLs10928383722dw94ok08519631:24000
Gaddy-Gracemore complex, 0 to 1 percent slopes, occasionally flooded9314638381030x62ok08719761:24000
Gaddy fine sand, 0 to 1 percent slopes, frequently floodedLs175563838362tp6tok09319651:24000
Gaddy loam, 0 to 1 percent slopes, occasionally floodedLn2830383835dwdsok09319651:24000
Gaddy loamy fine sand, 0 to 1 percent slopes, occasionally floodedGadA5963840532tp6rok10319941:24000
Gaddy loamy fine sand, 0 to 1 percent slopes, rarely floodedGayA104384054dwmvok10319941:24000
Gaddy loamy fine sand, 0 to 1 percent slopes, frequently floodedGdyA16263841622tp6qok10719961:24000
Gaddy loamy fine sand, 0 to 1 percent slopes, occasionally floodedGadA11033841582tp6rok10719961:24000
Gaddy-Gracemore complex, 0 to 1 percent slopes, frequently floodedGaGA301738429230x61ok10919961:12000
Yahola-Gaddy complex, 0 to 1 percent slopes, occasionally floodedYaGA677384375dwz6ok10919961:12000
Gaddy loamy fine sand, 0 to 1 percent slopes, frequently flooded2756986234222tp6qok11319751:24000
Gaddy fine sandy loam, 0 to 1 percent slopes, occasionally flooded522546623447nxr6ok11319751:24000
Gaddy loamy fine sand, 0 to 1 percent slopes, occasionally flooded2624726234212tp6rok11319751:24000
Gaddy loamy fine sand, 0 to 1 percent slopes, occasionally floodedGadA153914231562tp6rok11720071:24000
Gaddy loamy fine sand, 0 to 1 percent slopes, frequently floodedGdyA70918872832tp6qok11720071:24000
Gaddy-Gracemore complex, 0 to 1 percent slopes, frequently flooded19303238451430x61ok11919831:24000
Gaddy loamy fine sand, 0 to 1 percent slopes, occasionally flooded1816293845132tp6rok11919831:24000
Gaddy-Gracemore complex, 0 to 1 percent slopes, frequently floodedLn374638463630x61ok12319671:24000
Gaddy loamy fine sand, 0 to 1 percent slopes, occasionally floodedGadA79233846742tp6rok12519751:24000
Gaddy loamy fine sand, 0 to 1 percent slopes, occasionally flooded1210623847972tp6rok13319761:24000
Gaddy loamy fine sand, 0 to 1 percent slopes, frequently floodedGdyA3053851882tp6qok15119951:24000
Yahola-Gaddy complex, frequently floodedYg991363033d5rrtx03519771:24000
Gaddy loamy fine sand, frequently floodedGa692363443d65ztx05119941:24000
Gaddy soils, frequently flooded255106364473d786tx09719731:24000
Gaddy fine sandy loam, 0 to 1 percent slopes, occasionally flooded242220364472d785tx09719731:24000
Gaddy soils, frequently flooded262808365444d88jtx14519751:20000
Gaddy silt loam, occasionally flooded25979365443d88htx14519751:20000
Yahola-Gaddy complex, occasionally floodedYa725368221dc53tx25119811:20000
Yahola-Gaddy complex, occasionally floodedYg4422370139df4ztx30919921:24000
Gaddy loamy fine sand, frequently floodedGa413370097df3mtx30919921:24000
Gaddy fine sandy loam, frequently floodedGaA1479370674dfq7tx33119881:24000
Yahola-Gaddy complex, occasionally flooded465048370793dfv2tx33719751:24000
Gaddy soils, frequently flooded192307370763dft3tx33719751:24000
Yahola and Gaddy soils, 0 to 2 percent slopes, occasionally floodedYg4583390980f3v8tx36319791:24000
Gaddy soils, 0 to 2 percent slopes, frequently floodedLf1922390890f3rctx36719731:20000
Gaddy loamy fine sand, 0 to 2 percent slopes, frequently floodedGa724371714dgsstx39519961:24000
Gaddy loamy fine sand, 0 to 1 percent slopes, frequently floodedLn1291393221f65ktx45319691:20000
Gaddy soils and Urban land, 0 to 1 percent slopes, occasionally floodedLu387393222f65ltx45319691:20000
Yahola-Gaddy complex, occasionally floodedYg5273374375dkkmtx60919751:20000

Map of Series Extent

Approximate geographic distribution of the GADDY 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 .