Official Series Description


Lab Data Summary

Aggregate lab data for the SWEETWATER soil series. This aggregation is based on all pedons with a current taxon name of SWEETWATER, 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 SWEETWATER 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
7207N0502S2007KS199001Sweetwater8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.8320833,-101.6669998

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SWEETWATER 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 SWEETWATER 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 SWEETWATER 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 SWEETWATER 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 .

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.

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

Competing Series

Soil series competing with SWEETWATER 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 SWEETWATER 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 SWEETWATER 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 SWEETWATER, 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. KS-2012-01-23-02 | Finney County - November 1965

    Typical cross section of the valley of the Arkansas River (Soil Survey of Finney County, Kansas; 1965).

  2. KS-2012-01-23-20 | Gray County - January 1968

    Approximate geologic cross section through the central part of Gray County and the general location of soils on the landscape (Soil Survey of Gray County, Kansas; 1968).

  3. KS-2012-01-23-25 | Hamilton County - November 1961

    Geologic profile extending in a north-south direction through the central part of Hamilton County (Soil Survey of Hamilton County, Kansas; 1961).

  4. OK-2012-02-16-03 | Beaver County - August 1962

    Parent material and parent rock of most of the soils in Beaver County, and their position on the landscape (Soil Survey of Beaver County, Oklahoma; August 1962).

  5. OK-2012-02-16-09 | Cimarron County - June 1960

    Typical landscape in the central and eastern part of Cimarron County: Associations 1, 2, 3, and 5 (Soil Survey of Cimarron County, Oklahoma; June 1960).

  6. OK-2012-02-16-30 | Ellis County - April 1966

    Major soils of associations 7, 8, and 10 (Soil Survey of Ellis County, Oklahoma; April 1966).

  7. OK-2012-02-17-12 | Major County - October 1968

    Soil associations in the central part of the county (Soil Survey of Major County, Oklahoma; October 1968).

  8. OK-2012-02-17-13 | Major County - October 1968

    Cross section along a line extending across the middle of the county from the western to the eastern boundary (Soil Survey of Major County, Oklahoma; October 1968).

  9. OK-2012-02-17-53 | Texas County - July 1961

    Typical pattern of the soils in association 3, Texas County, Okla (Soil Survey of Texas County, Oklahoma; July 1961).

  10. OK-2012-02-17-60 | Woodward County - November 1963

    Typical pattern of soils of the Port association (Soil Survey of Woodward County, Oklahoma; November 1963).

Map Units

Map units containing SWEETWATER 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
Sweetwater clay loam, occasionally flooded12581678115234917p3kks05519621:24000
Lesho-Sweetwater complex, occasionally flooded2157220313805741hblnks06919651:24000
Sweetwater clay loam, occasionally flooded125882713806041hbmmks06919651:24000
Sweetwater clay loam, occasionally flooded12582567115223717nzyks07519591:24000
Sweetwater clay loam, occasionally flooded12583867115228517p1hks09319611:24000
Sweetwater clay loam, occasionally flooded1258469115054717m7fks10919621:24000
Sweetwater clay loam, occasionally flooded1258191114962917l8tks18119671:24000
Sweetwater clay loam, occasionally flooded12582062115020817lwhks19919841:24000
Sweetwater silty clay loam, saline, 0 to 2 percent slopes, occasionally floodedSwtB4512194795323d06ok00720211:24000
Sweetwater silty clay loam, saline, 0 to 2 percent slopes, occasionally floodedSw1077538247123d06ok04519631:24000
Sweetwater silty clay loam, saline, 0 to 2 percent slopes, occasionally floodedSw105538477923d06ok12919611:24000
Sweetwater silty clay loam, saline, 0 to 2 percent slopes, occasionally floodedSw881938492323d06ok13919591:24000
Sweetwater silty clay loam, saline, 0 to 2 percent slopes, occasionally floodedSw453638530323d06ok15319611:24000
Sweetwater silty clay loam, saline, 0 to 2 percent slopes, occasionally floodedSw126536520823d06tx12919751:24000
Sweetwater silty clay loam, saline, 0 to 2 percent slopes, occasionally floodedSw242439195523d06tx17919651:20000
Sweetwater silty clay loam, saline, 0 to 2 percent slopes, occasionally floodedSw938236759123d06tx21119671:20000
Sweetwater silty clay loam, saline, 0 to 2 percent slopes, occasionally floodedSw481536794023d06tx23319721:24000
Sweetwater silty clay loam, saline, 0 to 2 percent slopes, occasionally floodedSw170436947823d06tx29519711:24000
Sweetwater silty clay loam, saline, 0 to 2 percent slopes, occasionally floodedSw443837153723d06tx39319791:24000
Sweetwater silty clay loam, saline, 0 to 2 percent slopes, occasionally floodedSw697837332623d06tx48319701:24000

Map of Series Extent

Approximate geographic distribution of the SWEETWATER 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 .