Official Series Description


Lab Data Summary

Aggregate lab data for the BLENCOE soil series. This aggregation is based on all pedons with a current taxon name of BLENCOE, 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 BLENCOE were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
107BM89087351989MO087035mBlencoe4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.8830808,-95.0883146
115BM07071042007MO071004BLENCOE4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5489722,-90.8528611
115BM07071072007MO071007BLENCOE4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6646111,-91.29875
115BM08089602008MO089060BLENCOE4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9896944,-92.7728056
115BM08135512008MO135051BLENCOE4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.8913056,-92.5053056
115BM09183042009MO183004Blencoe3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.8319722,-90.1694167
115C40A2690S1974MO127003Blencoe6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.7722549,-91.3923645

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BLENCOE 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 BLENCOE 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 BLENCOE 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 BLENCOE 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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Competing Series

Soil series competing with BLENCOE 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 BLENCOE series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the BLENCOE 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.

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

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

Soil series sharing subgroup-level classification with BLENCOE, 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. IA-2010-09-02-24 | Monona County - 2003

    Typical pattern of soils and parent material in the Luton-Salix association (Soil Survey of Monona County, Iowa; 2003).

  2. IA-2010-09-03-09 | Woodbury - 2006

    Typical pattern of soils and underlying material in the Luton-Tieville association (Soil Survey of Woodbury County, Iowa; 2006).

  3. SD-2010-11-01-07 | Clay County - 2003

    Relationship of the major soils to parent material and position on the Missouri River flood plain (Soil Survey of Clay County, South Dakota; 2003).

Map Units

Map units containing BLENCOE 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
Blencoe silty clay441275406142fmmcia07119681:20000
Blencoe silty clay443466406769fn8lia08519711:15840
Blencoe silty clay, 0 to 2 percent slopes441069409570fr5yia12919791:15840
Blencoe silt clay, 0 to 2 percent slopes, rarely flooded446705447327h0gxia13319941:12000
Blencoe silty clay, 0 to 2 percent slopes44526410492fs4pia15519861:15840
Blencoe-Woodbury silty clays, 0 to 2 percent slopes, rarely flooded34403058741611swpyia19320031:12000
Blencoe silty clay loam, clayey substratum, 0 to 2 percent slopes, rarely flooded1350615336902664z996mo00519881:24000
Blencoe silty clay loam, 0 to 2 percent slopes, occasionally flooded66028227525336242qp8rmo01919981:24000
Blencoe silty clay loam, 0 to 2 percent slopes, frequently flooded6603210425336432qp8vmo01919981:24000
Blencoe silty clay loam, 0 to 2 percent slopes, occasionally flooded66028543225336252qp8rmo02719861:24000
Blencoe silty clay loam, 0 to 2 percent slopes, frequently flooded6603235025336442qp8vmo02719861:24000
Blencoe silty clay loam, 0 to 2 percent slopes, occasionally flooded6602871725336282qp8rmo05120021:24000
Blencoe silty clay loam, 0 to 2 percent slopes, frequently flooded660324225336472qp8vmo05120021:24000
Blencoe silty clay loam, 0 to 2 percent slopes, occasionally flooded6602872025336292qp8rmo05319931:24000
Blencoe silty clay loam, 0 to 2 percent slopes, frequently flooded6603254025336482qp8vmo05319931:24000
Blencoe silty clay, 0 to 2 percent slopes, rarely flooded1354010099887491yshrmo08719921:24000
Blencoe silty clay loam, 0 to 2 percent slopes, occasionally flooded660281207225336262qp8rmo08919751:24000
Blencoe silty clay loam, 0 to 2 percent slopes, frequently flooded6603245425336452qp8vmo08919751:24000
Blencoe silty clay loam, 0 to 2 percent slopes, occasionally flooded66028115725336302qp8rmo13519621:24000
Blencoe silty clay loam, 0 to 2 percent slopes, frequently flooded660329525336492qp8vmo13519621:24000
Blencoe silty clay loam, 0 to 2 percent slopes, occasionally flooded66028171025336232qp8rmo15119961:24000
Blencoe silty clay loam, 0 to 2 percent slopes, frequently flooded6603248025336422qp8vmo15119961:24000
Blencoe silt loam, 0 to 2 percent slopes, overwash, occasionally flooded66008194573590m7vxmo15119961:24000
Blencoe silty clay loam, 0 to 2 percent slopes, occasionally flooded6602817625336272qp8rmo18319791:24000
Blencoe silty clay loam, 0 to 2 percent slopes, frequently flooded66032525336462qp8vmo19519891:24000
Blencoe silty clay, rarely flooded77293012427806gc56ne02119781:20000
Blencoe silty clay loam, rarely flooded77282567427805gc55ne02119781:20000
Blencoe silty clay, rarely flooded77292684426716gb11ne04319721:20000
Blencoe silty clay, clayey substratum, rarely flooded7730162716916551ts9jne12719831:20000
Blencoe silty clay, 0 to 2 percent slopes, clayey substratumBf9843445531gylzsd02719951:24000
Blencoe silty clayBf2721453679h72tsd12719741:20000
Blencoe-Gayville complexBg422418055g10nsd13519771:20000
Blencoe silty clayBf376418054g10msd13519771:20000
Blencoe silty clay, 0 to 2 percent slopes, clayey substratumBs96418118g12psd13519771:20000

Map of Series Extent

Approximate geographic distribution of the BLENCOE 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 .