Official Series Description


Lab Data Summary

Aggregate lab data for the SACVILLE soil series. This aggregation is based on all pedons with a current taxon name of SACVILLE, 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 SACVILLE 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
115BM99051131999MO051169Sacville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672644,-92.3451678
115BM99131011999MO131002Sacville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672644,-92.3451678
116AM99131021999MO131003Sacville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1324238,-92.4324481
116AM99131181999MO131018Sacville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1087998,-92.4490793
116AM07135022007MO135002SACVILLE4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6628333,-92.59

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SACVILLE 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 SACVILLE 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 SACVILLE 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 SACVILLE 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 SACVILLE 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 SACVILLE 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 SACVILLE 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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Click the image to view it full size.

Soil series sharing subgroup-level classification with SACVILLE, 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 SACVILLE 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
Sacville silty clay loam, 1 to 3 percent slopes70039948525340392qpc2mo01519861:24000
Sacville silt loam, 2 to 5 percent slopes7004613125340702qpc7mo01519861:24000
Sacville silt loam, 2 to 5 percent slopes70046101125340712qpc7mo05120021:24000
Sacville silty clay loam, 1 to 3 percent slopes70039788425340382qpc2mo05919881:24000
Sacville silty clay loam, 1 to 3 percent slopes, occasionally flooded7613943026730632rt1kmo05919881:24000
Sacville silty clay loam, 1 to 3 percent slopes70039217525340452qpc2mo07719791:24000
Parsons-Sacville complex, 1 to 3 percent slopes70139103525342232qpdmmo07719791:24000
Sacville silty clay loam, 1 to 3 percent slopes70039585025340402qpc2mo08519881:24000
Sacville silty clay loam, 1 to 3 percent slopes, rarely flooded76140178726730832rt1lmo08519881:24000
Sacville silty clay loam, 1 to 3 percent slopes7003940825340462qpc2mo10919791:24000
Parsons-Sacville complex, 1 to 3 percent slopes70139825342222qpdmmo10919791:24000
Sacville silt loam, 2 to 5 percent slopes70046253125340722qpc7mo13120011:24000
Sacville silt loam, 2 to 5 percent slopes70046849025340732qpc7mo13519621:24000
Sacville silt loam, 2 to 5 percent slopes70046650025340692qpc7mo14119961:24000
Sacville silty clay loam, 1 to 3 percent slopes7003931425340412qpc2mo15919901:24000
Sacville silty clay loam, 1 to 3 percent slopes70039803325340422qpc2mo16719931:24000
Sacville silty clay loam, 1 to 3 percent slopes700396325340432qpc2mo18519841:24000
Sacville silty clay loam, 1 to 3 percent slopes70039108125340442qpc2mo22919791:24000

Map of Series Extent

Approximate geographic distribution of the SACVILLE 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 .