Official Series Description


Lab Data Summary

Aggregate lab data for the SCRIBA soil series. This aggregation is based on all pedons with a current taxon name of SCRIBA, 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 SCRIBA 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 SCRIBA 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 SCRIBA 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 SCRIBA 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 SCRIBA 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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Click the image to view it full size.

Competing Series

Soil series competing with SCRIBA 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 SCRIBA 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 SCRIBA 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 .

Click the image to view it full size.

Click the image to view it full size.

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 SCRIBA, 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. NY-2012-02-15-39 | Rensselaer County - January 1988

    Typical relationship of soils and underlying material in the Bernardston-Pittstown-Nassau general soil map unit (Soil Survey of Rensselaer County, New York; January 1988).

Map Units

Map units containing SCRIBA 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
Scriba gravelly loamSk16192894909q7dny01119681:15840
Scriba very stony loamSm6422894919q7fny01119681:15840
Scriba gravelly silt loam, 3 to 8 percent slopesSdB2282919159srmny04519811:15840
Scriba gravelly silt loam, 0 to 3 percent slopesSdA1832919149srlny04519811:15840
Burdett-Scriba channery silt loams, 3 to 8 percent slopesBvB1992927989tp3ny05719731:24000
Burdett-Scriba channery silt loams, 8 to 15 percent slopesBvC152927999tp4ny05719731:24000
Burdett-Scriba channery silt loams, 0 to 3 percent slopesBvA62927979tp2ny05719731:24000
Burdett-Scriba association, extremely stony, gently slopingBXB22928009tp5ny05719731:24000
Scriba gravelly fine sandy loam, 0 to 8 percent slopesScB350642941479w2mny07519731:15840
Scriba very stony soils, gently slopingSDB127432941509w2qny07519731:15840
Scriba gravelly fine sandy loam, 8 to 15 percent slopesScC2102941489w2nny07519731:15840
Scriba silt loam, 3 to 8 percent slopesSrB88392932049v36ny08319801:15840
Scriba very stony silt loam, 3 to 8 percent slopesStB12192932059v37ny08319801:15840
Scriba silt loam, 0 to 3 percent slopesSrA5772932039v35ny08319801:15840
Scriba-Pittstown association, gently slopingSvB2382932069v38ny08319801:15840
Burdett-Scriba channery silt loams, 3 to 8 percent slopesBvB20305309551bd3jny09319731:15840
Burdett-Scriba channery silt loams, 8 to 15 percent slopesBvC4051309552bd3kny09319731:15840
Burdett-Scriba channery silt loams, 0 to 3 percent slopesBvA3890309550bd3hny09319731:15840
Burdett-Scriba association, extremely stony, gently slopingBXB2133309553bd3lny09319731:15840
Scriba and Morris loams, gently sloping, rubblySeB97192951252vxdtny10519841:15840
Scriba loam, 0 to 3 percent slopes, stonyScA27192951239x33ny10519841:15840
Scriba loam, 3 to 8 percent slopes, stonyScB26592951249x34ny10519841:15840
Scriba and Morris soils, gently sloping, very boulderySEB94072955402vxd3ny11119741:15840
Scriba and Morris soils, gently sloping, extremely boulderySGB28652955412vxd4ny11119741:15840
Scriba and Morris soils, 0 to 8 percent slopesSdB4942955392vcm8ny11119741:15840
Scriba gravelly silt loam, 3 to 8 percent slopesScB37182960139y0tny11519721:20000
Scriba gravelly silt loam, 0 to 3 percent slopesScA15042960129y0sny11519721:20000
Scriba very stony soils, nearly level through slopingSDC13222960099y0pny11519721:20000

Map of Series Extent

Approximate geographic distribution of the SCRIBA 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 .