Official Series Description


Lab Data Summary

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

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

Soil series sharing subgroup-level classification with LOVEDALE, 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-2010-09-29-19 | Woods County - 2003

    Typical pattern of soils and underlying material in the Eda-Devol-Lovedale general soil map unit (Soil Survey of Woods County, Oklahoma; 2003).

Map Units

Map units containing LOVEDALE 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
Lovedale fine sandy loam, 1 to 3 percent slopesShB120213814452tq6zok00319711:24000
Lovedale fine sandy loam, 3 to 5 percent slopesLvdC386225412tq70ok00319711:24000
Lovedale fine sandy loam, 1 to 3 percent slopesShA255753817692tq6zok01119651:24000
Lovedale fine sandy loam, 3 to 5 percent slopesShC145163817702tq70ok01119651:24000
Lovedale fine sandy loam, 5 to 12 percent slopes, severely erodedEr5581381723dt6nok01119651:24000
Lovedale-Teller complex, 5 to 8 percent slopesStD3232381773dt88ok01119651:24000
Carwile-Lovedale complex, 0 to 1 percent slopesCsA20373817162t6pvok01119651:24000
Lovedale-Teller complex, 5 to 8 percent slopes, erodedStD21551381774dt89ok01119651:24000
Lovedale fine sandy loam, 1 to 3 percent slopesShB37443819212tq6zok01519671:24000
Lovedale fine sandy loam, 3 to 5 percent slopesShC27723819222tq70ok01519671:24000
Lovedale fine sandy loam, 1 to 3 percent slopesShB152983819792tq6zok01719721:24000
Lovedale fine sandy loam, 3 to 5 percent slopesShC108373819802tq70ok01719721:24000
Lovedale fine sandy loam, 5 to 8 percent slopesShD40873819812tq7zok01719721:24000
Lovedale-Wisby complex, 5 to 12 percent slopesSnE2367381983dth1ok01719721:24000
Lovedale fine sandy loam, 5 to 8 percent slopes, erodedShD212923819822tq80ok01719721:24000
Lovedale fine sandy loam, 1 to 3 percent slopesShB83023823402tq6zok03919731:24000
Lovedale fine sandy loam, 3 to 5 percent slopesShC39233823412tq70ok03919731:24000
Lovedale-Carwile, ponded complex, 0 to 3 percent slopesSrB10899382530dv1pok04719651:24000
Lovedale fine sandy loam, 1 to 3 percent slopesShB49203825292tq6zok04719651:24000
Lovedale fine sandy loam, 0 to 1 percent slopesShA49103825282tq7yok04719651:24000
Lovedale fine sandy loam, 1 to 3 percent slopes5180523827422tq6zok05319831:24000
Lovedale fine sandy loam, 3 to 5 percent slopesShC26353833662tq70ok07119651:24000
Lovedale fine sandy loam, 1 to 3 percent slopesShB18573833652tq6zok07119651:24000
Lovedale fine sandy loam, 3 to 5 percent slopes, severely erodedEt591383329dvwgok07119651:24000
Lovedale fine sandy loam, 5 to 8 percent slopesShD5803833672tq7zok07119651:24000
Lovedale fine sandy loam, 3 to 5 percent slopesShC215013834182tq70ok07319601:24000
Lovedale fine sandy loam, 1 to 3 percent slopesShB188693834172tq6zok07319601:24000
Lovedale-Carwile, ponded complex, 0 to 3 percent slopesCa16020383429dvzpok07319601:24000
Lovedale fine sandy loam, 0 to 1 percent slopesShA61063834162tq7yok07319601:24000
Lovedale fine sandy loam, 5 to 8 percent slopes, erodedShD342693834192tq80ok07319601:24000
Lovedale fine sandy loam, 1 to 3 percent slopesStB213663838632tq6zok09319651:24000
Carwile-Lovedale complex, 0 to 1 percent slopesCsA75653838192t6pvok09319651:24000
Lovedale fine sandy loam, 0 to 1 percent slopesLvdA2813835702tq7yok09319651:24000
Wisby-Lovedale complex, 1 to 5 percent slopesWiLC373384126dwq5ok10319941:24000
Lovedale sandy loam, 1 to 3 percent slopesLveB67384079dwnnok10319941:24000
Lovedale fine sandy loam, 1 to 3 percent slopes4492903850302tq6zok14919761:24000
Lovedale fine sandy loam, 3 to 5 percent slopes4577603850312tq70ok14919761:24000
Lovedale fine sandy loam, 1 to 3 percent slopesLvdB92323852102tq6zok15119951:24000
Lovedale fine sandy loam, 3 to 5 percent slopesLvdC12033852112tq70ok15119951:24000

Map of Series Extent

Approximate geographic distribution of the LOVEDALE 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 .