Official Series Description


Lab Data Summary

Aggregate lab data for the SANDVIEW soil series. This aggregation is based on all pedons with a current taxon name of SANDVIEW, 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 SANDVIEW 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
12185KY-155-00583KY155 Sandview-OSDSandview4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.6261292,-85.1747971
n/a93KY-239-00393KY-239-003Sandview3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a99KY-011-00799KY-011-007Sandview1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SANDVIEW 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 SANDVIEW 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 SANDVIEW 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 SANDVIEW 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 terrace figure.

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

Competing Series

Soil series competing with SANDVIEW 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 SANDVIEW 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 SANDVIEW 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.

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 SANDVIEW, 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. KY-2010-09-03-03 | Garrard and Lincoln Counties - 2006

    Typical pattern of soils and underlying material in the Sandview-Faywood-Lowell general soil map unit (Soil Survey of Garrard and Lincoln Counties, Kentucky; 2006).

  2. KY-2010-09-03-05 | Garrard and Lincoln Counties - 2006

    Typical pattern of soils and underlying material in the Lowell-Faywood-Cynthiana general soil map unit (Soil Survey of Garrard and Lincoln Counties, Kentucky; 2006).

  3. KY-2012-02-01-12 | Marion County - August 1991

    Typical pattern of soils and parent material in the Lowell-Sandview-Faywood general soil map unit (Soil Survey of Marion County, Kentucky; August 1991).

Map Units

Map units containing SANDVIEW 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
Lowell-Sandview silt loams, 2 to 6 percent slopesuLsoB737517274982zs5fky01120061:12000
Lowell-Sandview silt loams, 2 to 6 percent slopesuLsoB152505501562zs5fky04919621:15840
Lowell-Sandview silt loams, 2 to 6 percent slopesuLsoB100545527152zs5fky06919891:20000
Sandview silt loam, 2 to 6 percent slopesSaB374552735lk55ky06919891:20000
Lowell-Sandview silt loams, 2 to 6 percent slopesuLsoB89215518152zs5fky09719651:15840
Sandview silt loam, 2 to 6 percent slopesSaB96315330651ng8qky11120051:12000
Sandview silt loam, 6 to 12 percent slopesSaC18015330661ng8rky11120051:12000
Urban land-Alfic Udarents-Sandview complex, 0 to 12 percent slopesUuC17015364531nkt0ky11120051:12000
Lowell-Sandview silt loams, 2 to 6 percent slopesuLsoB194313978832zs5fky15119681:20000
Sandview silt loam, 2 to 6 percent slopesSaB6390552368ljsbky15519861:20000
Lowell-Sandview silt loams, 2 to 6 percent slopesuLsoB27655523462zs5fky15519861:20000
Sandview silt loam, 6 to 12 percent slopes, erodedSaC21305552369ljscky15519861:20000
Lowell-Sandview silt loams, 2 to 6 percent slopesuLsoB169705489322zs5fky16119831:20000
Lowell-Sandview silt loams, 2 to 6 percent slopesuLsoB36295505292zs5fky17319831:20000
Lowell-Sandview silt loams, 2 to 6 percent slopesuLsoB104555499732zs5fky17919671:15840
Lowell-Sandview silt loams, 2 to 6 percent slopesuLsoB24705515922zs5fky18519751:20000
Lowell-Sandview silt loams, 2 to 6 percent slopesuLsoB110745488662zs5fky20919741:15840
Lowell-Sandview silt loams, 2 to 6 percent slopesuLsoB136005516592zs5fky21119781:20000
Lowell-Sandview silt loams, 2 to 6 percent slopesuLsoB101705515022zs5fky22919831:20000
Lowell-Sandview silt loams, 2 to 6 percent slopesuLsoB93115516292zs5fky60119821:20000
Lowell-Sandview silt loams, 2 to 6 percent slopesuLsoB17826529812zs5fky60319681:15840
Lowell-Sandview silt loams, 2 to 6 percent slopesuLsoB307645520912zs5fky60419781:20000
Lowell-Sandview silt loams, 2 to 6 percent slopesuLsoB82515515442zs5fky60619791:20000
Lowell-Sandview silt loams, 2 to 6 percent slopesuLsoB37455509962zs5fky60819831:20000
Lowell-Sandview silt loams, 2 to 6 percent slopesuLsoB24525519962zs5fky61219721:15840
Lowell-Sandview silt loams, 2 to 6 percent slopesuLsoB59595529722zs5fky61819931:12000
Sandview silt loam, 2 to 6 percent slopesSaB3475552990lkfdky61819931:12000
Sandview silt loam, 6 to 12 percent slopesSaC1436552991lkffky61819931:12000
Lowell-Sandview silt loams, 2 to 6 percent slopesuLsoB2126529882zs5fky61919781:15840
Lowell-Sandview silt loams, 2 to 6 percent slopesuLsoB103355519242zs5fky62219891:20000
Lowell-Sandview silt loams, 2 to 6 percent slopesuLsoB13628859822zs5fky62419761:20000
Sandview silt loam, 2 to 6 percent slopesSaB302551856lj7tky63719891:12000
Lowell-Sandview silt loams, 2 to 6 percent slopesuLsoB1315518412zs5fky63719891:12000
Lowell-Sandview silt loams, 2 to 6 percent slopesuLsoB1003813988662zs5fky64319651:15840

Map of Series Extent

Approximate geographic distribution of the SANDVIEW 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 .