Official Series Description


Lab Data Summary

Aggregate lab data for the SAC soil series. This aggregation is based on all pedons with a current taxon name of SAC, 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 SAC 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
107A40A14541959IA041005Sac6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0447222,-95.3288889
107A84P077084IA035001Sac7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.7091675,-95.430275
107A84P077284IA035003Sac7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.8888893,-95.4833298
107A85P050584IA1410011Sac5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.1444435,-95.5916672
107A85P050684IA1410012Sac5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.1444435,-95.5916672
107A85P050784IA1410021Sac5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0250015,-95.5138855
107A85P050884IA1410022Sac5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0250015,-95.5138855
107A85P050984IA1410023Sac5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0250015,-95.5138855
107A85P029385IA0350021Sac4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.8916664,-95.7249985
107A85P029485IA0350022Sac4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.8916664,-95.7249985
107A85P029585IA0350023Sac5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.8916664,-95.7249985
107A86P033985IA0350031Sac5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.9000015,-95.5500031
107A86P034085IA0350032Sac5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.9000015,-95.5500031
107A86P034185IA0350033Sac5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.9000015,-95.5500031
107A86P042085IA1410031Sac5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0499992,-95.4833298
107A86P042285IA1410033Sac5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0499992,-95.4833298
107A86P042385IA1410041Sac5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.1472206,-95.6166687
107A86P042485IA1410042Sac5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.1472206,-95.6166687
107A87P033286IA0350041Sac5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.8844452,-95.6022186
107A86P042186IA1410032Sac5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0499992,-95.4833298
107A87P035987IA1410051Sac5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.9141655,-95.4455566
107A87P036087IA1410052Sac5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.914444,-95.4461136
107A87P036187IA1410053Sac5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.9150009,-95.4455566
107A40A1455S1959IA041006Sac6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0149994,-95.2291641
107A96P0060S1995IA041005Sac7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0441666,-95.3291702

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SAC 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 SAC 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 SAC 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 SAC 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 SAC 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 SAC 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 SAC 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 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 SAC, 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-2010-09-02-06 | Clay County - 2005

    Typical pattern of soils and underlying material in the McCreath-Gillett Grove-Sac association (Soil Survey of Clay County, Iowa; 2005).

  2. IA-2011-06-01-27 | Osceola County - 1988

    Typical pattern of soils and parent material in the Sac-Primghar association (Soil Survey of Osceola County, Iowa; 1988).

Map Units

Map units containing SAC 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
Sac silty clay loam, loam substratum, 2 to 5 percent slopes77B251994033272wxrdia02119731:15840
Sac silty clay loam, 2 to 5 percent slopes78B39374033292wxrcia02119731:15840
Sac silty clay loam, loam substratum, 5 to 9 percent slopes, eroded77C236274033282wxrlia02119731:15840
Sac silty clay loam, 5 to 9 percent slopes, eroded78C218064033302wxrkia02119731:15840
Sac silty clay loam, loam substratum, 2 to 5 percent slopes, eroded77B229184039562wxrgia03519871:15840
Sac silty clay loam, loam substratum, 2 to 5 percent slopes77B24764039552wxrdia03519871:15840
Sac silty clay loam, 2 to 5 percent slopes, eroded78B222104039602wxrfia03519871:15840
Sac silty clay loam, 5 to 9 percent slopes, eroded78C221704039622wxrkia03519871:15840
Sac silty clay loam, loam substratum, 5 to 9 percent slopes, eroded77C216834039582wxrlia03519871:15840
Sac silty clay loam, 2 to 5 percent slopes78B14184039592wxrcia03519871:15840
Sac silty clay loam, 5 to 9 percent slopes78C3794039612wxrhia03519871:15840
Sac silty clay loam, loam substratum, 5 to 9 percent slopes77C3764039572wxrjia03519871:15840
Sac silty clay loam, loam substratum, 2 to 5 percent slopes77B141803994212wxrdia04120021:12000
Sac silty clay loam, loam substratum, 5 to 9 percent slopes, eroded77C29843994232wxrlia04120021:12000
Sac silty clay loam, loam substratum, 5 to 9 percent slopes77C4973994222wxrjia04120021:12000
Sac silty clay loam, loam substratum, 2 to 5 percent slopes77B288618690332wxrdia05920111:12000
Sac silty clay loam, 5 to 9 percent slopes, eroded78C220444072032wxrkia09319891:15840
Sac silty clay loam, 2 to 5 percent slopes, eroded78B27464072012wxrfia09319891:15840
Sac silty clay loam, 9 to 14 percent slopes, eroded78D25894072062wxrmia09319891:15840
Sac silty clay loam, 5 to 9 percent slopes78C3944072022wxrhia09319891:15840
Sac silty clay loam, 2 to 5 percent slopes78B1574072002wxrcia09319891:15840
Sac silty clay loam, loam substratum, 2 to 5 percent slopes77B102214091392wxrdia11919731:15840
Sac silty clay loam, loam substratum, 2 to 5 percent slopes, eroded77B225024091402wxrgia11919731:15840
Sac silty clay loam, loam substratum, 5 to 9 percent slopes, eroded77C216814091412wxrlia11919731:15840
Sac silty clay loam, loam substratum, 9 to 14 percent slopes, eroded77D21404091422wxrnia11919731:15840
Sac silty clay loam, loam substratum, 2 to 5 percent slopes77B408404100962wxrdia14119771:15840
Sac silty clay loam, loam substratum, 5 to 9 percent slopes, eroded77C236204100972wxrlia14119771:15840
Sac variant silty clay loam, 2 to 5 percent slopes89B744410100frr1ia14119771:15840
Sac variant silty clay loam, 5 to 9 percent slopes, moderately eroded89C2227410101frr2ia14119771:15840
Sac silty clay loam, loam substratum, 2 to 5 percent slopes77B159394101742wxrdia14319851:15840
Sac silty clay loam, loam substratum, 0 to 2 percent slopes7741664101732wxrbia14319851:15840
Sac silty clay loam, loam substratum, 2 to 5 percent slopes, eroded77B223144101752wxrgia14319851:15840
Sac silty clay loam, loam substratum, 5 to 9 percent slopes, eroded77C22104101762wxrlia14319851:15840
Sac silty clay loam, 5 to 9 percent slopes, eroded78C244164108372wxrkia16119751:15840
Sac silty clay loam, loam substratum, 2 to 5 percent slopes77B43504108302wxrdia16119751:15840
Sac silty clay loam, 2 to 5 percent slopes78B36294108342wxrcia16119751:15840
Sac silty clay loam, loam substratum, 5 to 9 percent slopes, eroded77C233054108332wxrlia16119751:15840
Sac silty clay loam, 2 to 5 percent slopes, eroded78B28674108352wxrfia16119751:15840
Sac silty clay loam, 5 to 9 percent slopes78C6344108362wxrhia16119751:15840
Sac silty clay loam, loam substratum, 5 to 9 percent slopes77C4544108322wxrjia16119751:15840
Sac silty clay loam, loam substratum, 2 to 5 percent slopes, eroded77B22564108312wxrgia16119751:15840
Sac silty clay loam, 5 to 9 percent slopes, eroded78C216104112542wxrkia16719871:15840
Sac silty clay loam, 2 to 5 percent slopes, eroded78B28394112532wxrfia16719871:15840
Sac silty clay loam, 9 to 14 percent slopes, eroded78D24194112552wxrmia16719871:15840
Sac silty clay loam, loam substratum, 2 to 5 percent slopesP30B2015321962wxrdmn10120081:12000
Sac silty clay loam, loam substratum, 2 to 5 percent slopesP30B207166300572wxrdmn10520041:12000
Sac silty clay loam, loam substratum, 2 to 5 percent slopesP30B11427255172wxrdmn11720051:12000
Sac silty clay loam, loam substratum, 2 to 5 percent slopesP30B135314326962wxrdmn13320021:12000
Sac silty clay loam, 5 to 10 percent slopes, erodedP30C2157432697gj7zmn13320021:12000

Map of Series Extent

Approximate geographic distribution of the SAC 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 .