Official Series Description


Lab Data Summary

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

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 SLAUGHTERVILLE, 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-2010-09-29-10 | Noble County - 2005

    Typical pattern of soils and underlying material in the Teller-Konawa general soil map unit (Soil Survey of Noble County, Oklahoma; 2005).

  2. OK-2010-09-29-14 | Noble County - 2005

    Typical pattern of soils and underlying material in the Vanoss-Slaughterville general soil map unit (Soil Survey of Noble County, Oklahoma; 2005).

  3. OK-2012-02-16-13 | Cleveland County - April 1987

    Typical pattern of soils and underlying material in the Norge-Teller-Vanoss map unit and Asher-Keokuk-Canadian map unit (Soil Survey of Cleveland County, Oklahoma; April 1987).

  4. 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).

  5. OK-2012-02-17-31 | Payne County - April 1987

    Typical pattern of soils and underlying material in the Konawa-Dougherty-Derby map unit (Soil Survey of Payne Oklahoma; April 1987).

Map Units

Map units containing SLAUGHTERVILLE 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
Slaughterville fine sandy loam, 3 to 5 percent slopes711909382135dtmyok02719841:24000
Slaughterville fine sandy loam, 1 to 3 percent slopes701807382134dtmxok02719841:24000
Slaughterville fine sandy loam, 5 to 8 percent slopes, loamy substratum72853382136dtmzok02719841:24000
Slaughterville fine sandy loam, 8 to 25 percent slopes73607382137dtn0ok02719841:24000
Slaughterville-Urban land complex, 1 to 5 percent slopes54553382117dtmcok02719841:24000
Slaughterville-Urban land complex, 8 to 25 percent slopes5523382118dtmdok02719841:24000
Slaughterville fine sandy loam, 8 to 20 percent slopes67472516370dx5dok03719521:24000
Slaughterville fine sandy loam, 0 to 3 percent slopesHaB1689383226dvs4ok06719671:24000
Slaughterville fine sandy loam, 8 to 20 percent slopesHaE878383227dvs5ok06719671:24000
Slaughterville fine sandy loam, 3 to 8 percent slopesSlaD749383677dw7pok08319941:12000
Slaughterville fine sandy loam, 1 to 3 percent slopesSlaB703383676dw7nok08319941:12000
Slaughterville fine sandy loam, 8 to 20 percent slopesSlaF128383678dw7qok08319941:12000
Slaughterville fine sandy loam, 0 to 1 percent slopesMsA4131383725dw97ok08519631:24000
Slaughterville fine sandy loam, 1 to 3 percent slopesMsB2995383726dw98ok08519631:24000
Slaughterville fine sandy loam, 3 to 5 percent slopesMsC2312383727dw99ok08519631:24000
Slaughterville fine sandy loam, 0 to 3 percent slopesSlaB770384112dwpqok10319941:24000
Slaughterville fine sandy loam, 8 to 45 percent slopesSlaG439384114dwpsok10319941:24000
Slaughterville fine sandy loam, 3 to 5 percent slopesSlaC220384113dwprok10319941:24000
Slaughterville fine sandy loam, 8 to 45 percent slopesSlaG24316773681t9fnok11720071:24000
Slaughterville fine sandy loam, 1 to 3 percent slopes932011384592dx66ok11919831:24000
Derby-Slaughterville complex, 1 to 5 percent slopes821780384584dx5yok11919831:24000
Slaughterville fine sandy loam, 8 to 20 percent slopes671405384567dx5dok11919831:24000
Slaughterville fine sandy loam, 3 to 5 percent slopes201108384516dx3rok11919831:24000

Map of Series Extent

Approximate geographic distribution of the SLAUGHTERVILLE 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 .