Official Series Description


Lab Data Summary

Aggregate lab data for the KEWAUNEE soil series. This aggregation is based on all pedons with a current taxon name of KEWAUNEE, 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 KEWAUNEE 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
95A40A1538S1959WI015001Kewauneen/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.9463882,-88.2805557
95A40A1539S1959WI039002Kewauneen/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.8911095,-88.5852814
95A40A1540S1960WI071001Kewauneen/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.2580566,-87.6044464
95A40A1541S1960WI071002Kewauneen/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.310276,-87.5958328
95A18N0323S2016WI071001Kewauneen/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.9784355163574,-87.7972717285156
95A20N0556S2018WI087001Kewauneen/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.2610015869141,-88.2271118164062
95A21N0167S2020WI039008Kewauneen/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.8181114196777,-88.5645599365234
95A20N0823S2020WI039012Kewauneen/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.8581886291504,-88.5944671630859
95A21N0169S2020WI071050Kewauneen/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0587196350098,-88.023063659668
95B13N5527S2010WI001001Kewauneen/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.6623278,-89.6937722

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the KEWAUNEE 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 KEWAUNEE 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 KEWAUNEE 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 KEWAUNEE 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 KEWAUNEE 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 KEWAUNEE 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 KEWAUNEE 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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Soil series sharing subgroup-level classification with KEWAUNEE, 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 KEWAUNEE 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
Kewaunee silt loam, 2 to 6 percent slopes, eroded7314B256494229433074jwi00119781:20000
Kewaunee silt loam, 6 to 12 percent slopes7314C18564229442xzpwwi00119781:20000
Kewaunee silt loam, 12 to 20 percent slopes, eroded7314D24384229452tjxtwi00119781:20000
Kewaunee silt loam, 2 to 6 percent slopes, eroded7314B2623914261943074jwi00919701:20000
Kewaunee silt loam, 6 to 12 percent slopes, eroded7314C297564261952tjxswi00919701:20000
Kewaunee-Manawa complex, 2 to 6 percent slopes7718B78144262012tjxqwi00919701:20000
Kewaunee silt loam, 12 to 20 percent slopes, eroded7314D225134261962tjxtwi00919701:20000
Kewaunee loam, gravelly substratum, 2 to 6 percent slopes7712B15714261922xzptwi00919701:20000
Kewaunee silt loam, 20 to 30 percent slopes, eroded7314E214584261972xzpvwi00919701:20000
Kewaunee sandy loam, 2 to 6 percent slopes7714B8344261902xzq0wi00919701:20000
Kewaunee soils, 12 to 20 percent slopes, severely eroded7414D3724426199g9hcwi00919701:20000
Kewaunee soils, 6 to 12 percent slopes, severely eroded7414C3660426198g9hbwi00919701:20000
Kewaunee-Sisson complex, 15 to 30 percent slopes, eroded7923E26324262032xzq7wi00919701:20000
Kewaunee-Manawa complex, 2 to 6 percent slopes, eroded7718B23964262022xzqhwi00919701:20000
Kewaunee soils, 20 to 30 percent slopes, severely eroded7414E3321426200g9hdwi00919701:20000
Kewaunee sandy loam, 6 to 12 percent slopes, eroded7714C21554261912xzq2wi00919701:20000
Kewaunee loam, 2 to 6 percent slopes, eroded7714B24775232684832xzq9wi01520231:15840
Kewaunee loam, 6 to 12 percent slopes, eroded7714C2431632684842xzppwi01520231:15840
Manawa-Kewaunee-Poygan complex, 0 to 4 percent slopes7718B400232684972tjxpwi01520231:15840
Kewaunee loam, 12 to 20 percent slopes, eroded7714D2121632684852xzpqwi01520231:15840
Kewaunee loam, 20 to 30 percent slopes, eroded7714E219832684862xzprwi01520231:15840
Kewaunee-Boyer-Nichols complex, 12 to 20 percent slopes7426D1932684892xzq5wi01520231:15840
Kewaunee-Boyer-Nichols complex, 2 to 6 percent slopes7426B1732684872xzq3wi01520231:15840
Kewaunee-Boyer-Nichols complex, 6 to 12 percent slopes, eroded7426C2232684882xzq4wi01520231:15840
Kewaunee silt loam, 2 to 6 percent slopes, eroded7314B2133874222383074jwi02919751:15840
Kewaunee silt loam, 6 to 12 percent slopes, eroded7314C211354222392tjxswi02919751:15840
Kewaunee silt loam, 0 to 2 percent slopes7314A11344222372tjxrwi02919751:15840
Kewaunee soils, 12 to 20 percent slopes, severely eroded7414D3223422240g5cnwi02919751:15840
Kewaunee silt loam, 2 to 6 percent slopes, eroded7314B2116544254663074jwi03919671:15840
Kewaunee silty clay loam, 2 to 6 percent slopes, eroded7414B260604254702tjxvwi03919671:15840
Kewaunee silt loam, 0 to 2 percent slopes7314A16294254642tjxrwi03919671:15840
Kewaunee silty clay loam, 2 to 6 percent slopes7414B1171425469g8qtwi03919671:15840
Kewaunee silty clay loam, 0 to 2 percent slopes7414A10694254682xzpxwi03919671:15840
Kewaunee silty clay loam, 6 to 12 percent slopes, eroded7414C26254254712tjxwwi03919671:15840
Kewaunee soils, 2 to 6 percent slopes, severely eroded7414B3487425474g8qzwi03919671:15840
Kewaunee silt loam, 6 to 12 percent slopes, eroded7314C24674254672tjxswi03919671:15840
Kewaunee soils, 6 to 12 percent slopes, severely eroded7414C3335425475g8r0wi03919671:15840
Kewaunee silty clay loam, 12 to 20 percent slopes, eroded7414D22724254722tjxxwi03919671:15840
Kewaunee silty clay loam, 20 to 30 percent slopes, eroded7414E22484254732xzpywi03919671:15840
Kewaunee soils, 12 to 20 percent slopes, severely eroded7414D3169425476g8r1wi03919671:15840
Kewaunee silt loam, moderately shallow variant, 2 to 6 percent slopes7915B88425477g8r2wi03919671:15840
Kewaunee silt loam, 2 to 6 percent slopes, eroded7314B2106514223153074jwi06119781:15840
Kewaunee silty clay loam, 2 to 6 percent slopes, eroded7414B275094223162tjxvwi06119781:15840
Kewaunee silty clay loam, 6 to 12 percent slopes, eroded7414C243494223172tjxwwi06119781:15840
Kewaunee-Manawa silt loams, 1 to 6 percent slopes7718B2948422322g5g9wi06119781:15840
Kewaunee silty clay, 12 to 20 percent slopes, severely eroded7414D36414223202szgbwi06119781:15840
Kewaunee silty clay, 20 to 35 percent slopes, severely eroded7414E34954223212xzpzwi06119781:15840
Kewaunee silty clay loam, 12 to 20 percent slopes, eroded7414D24604223182tjxxwi06119781:15840
Kewaunee silty clay, 6 to 12 percent slopes, severely eroded7414C34424223192szg9wi06119781:15840
Kewaunee loam, 2 to 6 percent slopes, eroded7714B25849832685382xzq9wi07120231:15840
Manawa-Kewaunee-Poygan complex, 0 to 4 percent slopes7718B1720832685492tjxpwi07120231:15840
Kewaunee loam, 6 to 12 percent slopes, eroded7714C21391032685392xzppwi07120231:15840
Kewaunee loam, 12 to 20 percent slopes, eroded7714D2422832685402xzpqwi07120231:15840
Kewaunee-Boyer-Nichols complex, 12 to 20 percent slopes7426D216832685702xzq5wi07120231:15840
Kewaunee loam, 20 to 30 percent slopes, eroded7714E2175932685412xzprwi07120231:15840
Kewaunee-Boyer-Nichols complex, 2 to 6 percent slopes7426B110932685422xzq3wi07120231:15840
Kewaunee-Boyer-Nichols complex, 6 to 12 percent slopes, eroded7426C292732685432xzq4wi07120231:15840
Kewaunee silt loam, 2 to 6 percent slopes, eroded7314B2359034033623074jwi07920231:15840
Kewaunee silt loam, 6 to 12 percent slopes, eroded7314C228634033202tjxswi07920231:15840
Kewaunee silt loam, 2 to 6 percent slopes, eroded7314B2152814225613074jwi08719751:15840
Kewaunee-Manawa complex, 2 to 6 percent slopes7718B22984225652tjxqwi08719751:15840
Kewaunee soils, 20 to 45 percent slopes, severely eroded7414F31983422564g5q3wi08719751:15840
Kewaunee silt loam, 6 to 12 percent slopes, eroded7314C210124225622tjxswi08719751:15840
Kewaunee silt loam, 12 to 20 percent slopes, eroded7314D22114225632tjxtwi08719751:15840
Kewaunee silt loam, 2 to 6 percent slopes, eroded7314B2231034259803074jwi08919671:15840
Kewaunee silty clay loam, 2 to 6 percent slopes, eroded7414B2114364259812tjxvwi08919671:15840
Kewaunee silty clay loam, 6 to 12 percent slopes, eroded7414C246944259822tjxwwi08919671:15840
Kewaunee silty clay, 6 to 12 percent slopes, severely eroded7414C332574259832szg9wi08919671:15840
Kewaunee silt loam, 0 to 2 percent slopes7314A29324259792tjxrwi08919671:15840
Kewaunee silty clay, 12 to 20 percent slopes, severely eroded7414D313944259842szgbwi08919671:15840
Kewaunee silt loam, 2 to 6 percent slopes, eroded7314B2436134238983074jwi11719741:15840
Kewaunee silty clay loam, 2 to 6 percent slopes, eroded7414B2130724238992tjxvwi11719741:15840
Kewaunee silty clay loam, 6 to 12 percent slopes, eroded7414C2110614239002tjxwwi11719741:15840
Kewaunee silt loam, 0 to 2 percent slopes7314A19724238972tjxrwi11719741:15840
Kewaunee silty clay loam, 12 to 20 percent slopes, eroded7414D213054239012tjxxwi11719741:15840
Kewaunee silty clay, 12 to 20 percent slopes, severely eroded7414D37814239032szgbwi11719741:15840
Kewaunee silty clay, 6 to 12 percent slopes, severely eroded7414C36724239022szg9wi11719741:15840
Kewaunee loam, 2 to 6 percent slopes, eroded7714B232574239622xzq9wi13719861:20000
Kewaunee silt loam, 2 to 6 percent slopes, eroded7314B2403694227883074jwi13919771:20000
Kewaunee loamy fine sand, 2 to 6 percent slopes7713B22074227872xzq8wi13919771:20000
Kewaunee silty clay loam, 6 to 12 percent slopes, eroded7414C220344227892tjxwwi13919771:20000

Map of Series Extent

Approximate geographic distribution of the KEWAUNEE 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 .