Official Series Description


Lab Data Summary

Aggregate lab data for the BLAKELAND soil series. This aggregation is based on all pedons with a current taxon name of BLAKELAND, 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 BLAKELAND 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 BLAKELAND 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 BLAKELAND 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 BLAKELAND 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 BLAKELAND 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 BLAKELAND 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 BLAKELAND 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 BLAKELAND 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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There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with BLAKELAND, 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 BLAKELAND 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
Blakeland-Truckton associationBt111629404834vtco00119681:20000
Blakeland loamy sand, 3 to 9 percent slopesBoD67459404734vsco00119681:20000
Blakeland loamy sand, 1 to 20 percent slopesBoE25879411534xzco00519711:20000
Blakeland loamy sand, 1 to 9 percent slopes, erodedBoD27899411434xyco00519711:20000
Blakeland loamy sand, 3 to 12 percent slopes1168261051973jggco07320011:24000
Eckley-Dix-Blakeland complex, 6 to 20 percent slopes2689999511735z9co61719801:24000
Ascalon-Blakeland complex, 3 to 15 percent slopes64525951542yqpcco61719801:24000
Blakeland loamy sand, 0 to 6 percent slopes1314269510335yvco61719801:24000
Blakeland loamy sand, 6 to 12 percent slopes1412819510435ywco61719801:24000
Blakeland-Orsa association, 1 to 4 percent slopesBo2084498702jqy5co62219681:20000
Blakeland sandy loam, 1 to 15 percent slopesBlE1843498701jqy4co62219681:20000
Bresser-Truckton-Blakeland complex, 3 to 9 percent slopesBtD44318952902xst2co62419631:20000
Blakeland loamy sandBe858295283364nco62419631:20000
Truckton, Bresser, and Blakeland soils, 5 to 20 percent slopes, erodedTrE2405595338366fco62419631:20000
Blakeland loamy sand, 1 to 9 percent slopes87287295444369vco62519751:24000
Blakeland-Fluvaquentic Haplaquolls941589545536b6co62519751:24000
Truckton-Blakeland complex, 9 to 20 percent slopes982249954642yvrnco62519751:24000
Blakeland loamy sand, 0 to 9 percent slopes121885497396jpl1co64119801:24000
Blakeland loamy sand, 9 to 15 percent slopes13510497407jpldco64119801:24000
Blakeland loamy sand, 6 to 12 percent slopes8661047863j16wy62119801:24000

Map of Series Extent

Approximate geographic distribution of the BLAKELAND 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 .