Official Series Description


Lab Data Summary

Aggregate lab data for the ROSHOLT soil series. This aggregation is based on all pedons with a current taxon name of ROSHOLT, 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 ROSHOLT 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
90A40A166175WI095006Rosholt7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.396389,-92.2536087
90A78P051078WI115006Rosholt7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.7077789,-89.151947
90A88P017487WI013010Rosholt5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.7174988,-92.0341644
90AUMN1004S1967MN0651004Rosholt3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.8534966,-93.3370132
90A78P0431S1978WI073004Rosholt4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.879,-89.34136
90A78P0432S1978WI073005Rosholt4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.92322,-89.24589
90A81P0828S1981WI073005ROSHOLT7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.7608337,-89.3988876
90B40A2022S1947WI005007Rosholt4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.5105553,-91.7041702
90B83P0166S1982WI017001Rosholt5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.19816,-91.42779
90B83P0167S1982WI017002Rosholt5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.21338,-91.457
90B83P0845S1983WI017004Rosholt5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.03151,-91.39445
90B89P0249S1988WI005001Rosholt6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.3466682,-91.7069473
90B92P0438S1991WI107003Rosholt6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.3202782,-91.5208359

Water Balance

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

There are insufficient data to create the 3D mountains figure.

There are insufficient data to create the 3D terrace figure.

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Soil series sharing subgroup-level classification with ROSHOLT, 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. WI-2010-11-08-02 | Barron County - 2001

    Typical pattern of soils and parent material in the Anigon-Rosholt-Chetek association (Soil Survey of Barron County, Wisconsin; 2001).

  2. WI-2012-03-23-15 | Marathon County - September 1989

    Pattern of soils and parent material in the Chetek-Rosholt-Oesterle association (Soil Survey of Marathon County, WI; 1989).

  3. WI-2012-03-23-32 | Shawano County - October 1982

    Relationship of sols and substratum in the Kennan-Rosholt general map unit (Soil Survey of Shawano County, WI; 1982).

  4. WI-2012-03-23-39 | Waupaca County - September 1984

    Topography, underlying material, and pattern of soils in the Kennan-Rosholt map unit (Soil Survey of Waupaca County, WI; 1984).

Map Units

Map units containing ROSHOLT 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
Rosholt fine sandy loam, 2 to 6 percent slopes302B7109432902gjglmn00119961:20000
Rosholt fine sandy loam, 6 to 12 percent slopes302C780432903gjgmmn00119961:20000
Rosholt-Chetek complex, 2 to 8 percent slopesC17B1877527326662slmmmn03520091:24000
Rosholt-Chetek complex, 0 to 2 percent slopesC17A1393927326632qlnrmn03520091:24000
Rosholt-Chetek complex, 8 to 15 percent slopesC17C415927326672slmnmn03520091:24000
Rosholt fine sandy loam3023724622182nn4dmn05919561:20000
Rosholt-Chetek complex, 2 to 8 percent slopesC17B834516734611t5cmmn06520061:12000
Rosholt-Chetek complex, 8 to 15 percent slopesC17C450316734621t5cnmn06520061:12000
Rosholt-Chetek complex, 0 to 2 percent slopesC17A130916734601t5clmn06520061:12000
Rosholt-Chetek complex, 15 to 40 percent slopesC17E88516734631t5cpmn06520061:12000
Rosholt-Chetek complex, 2 to 8 percent slopesC17B409616763621t8d6mn09520061:12000
Rosholt-Chetek complex, 8 to 15 percent slopesC17C164416763631t8d7mn09520061:12000
Rosholt-Chetek complex, 0 to 2 percent slopesC17A28116763611t8d5mn09520061:12000
Rosholt-Chetek complex, 15 to 40 percent slopesC17E7716763641t8d8mn09520061:12000
Rosholt silt loam, 1 to 4 percent slopes302B1327400383ffmlmn09719871:20000
Rosholt sandy loam, 6 to 15 percent slopes302C24216772292tnzfmn12319781:15840
Rosholt sandy loam, 2 to 6 percent slopes302B22416772282tnzdmn12319781:15840
Rosholt sandy loam, 6 to 15 percent slopes302C273816770942tnzfmn16319781:15840
Rosholt sandy loam, 2 to 6 percent slopes302B253416770932tnzdmn16319781:15840
Rosholt sandy loam, 2 to 6 percent slopesRoB166474313342tnzdwi00519931:20000
Rosholt sandy loam, 0 to 2 percent slopesRoA103924313332tnzcwi00519931:20000
Chetek-Rosholt complex, 12 to 25 percent slopesClD9903431287ggshwi00519931:20000
Rosholt sandy loam, 6 to 15 percent slopesRoC222874313352tnzfwi00519931:20000
Amery-Rosholt complex, 12 to 20 percent slopes, very stony127D37594481892zcwdwi01320041:12000
Haugen-Rosholt complex, 6 to 12 percent slopes, very stony28C33464352642zcwcwi01320041:12000
Haugen-Rosholt complex, 2 to 6 percent slopes, very stony28B22754352632zcw9wi01320041:12000
Amery-Rosholt complex, 20 to 45 percent slopes, very stony127E20334481902zcwfwi01320041:12000
Cress-Rosholt complex, 12 to 25 percent slopes380D1321448299h1h8wi01320041:12000
Rosholt sandy loam, 2 to 6 percent slopes38B10804352682tnzdwi01320041:12000
Cress-Rosholt complex, 6 to 12 percent slopes380C935448298h1h7wi01320041:12000
Rosholt sandy loam, 6 to 15 percent slopes38C8394352712tnzfwi01320041:12000
Cress-Rosholt complex, 2 to 6 percent slopes380B609448293h1h2wi01320041:12000
Rosholt sandy loam, 0 to 2 percent slopes38A1984352672tnzcwi01320041:12000
Rosholt sandy loam, 15 to 35 percent slopes38D1864352722tnzgwi01320041:12000
Rosholt sandy loam, 2 to 6 percent slopesRoB90404215762tnzdwi01719851:15840
Rosholt sandy loam, 0 to 2 percent slopesRoA73704215752tnzcwi01719851:15840
Rosholt sandy loam, 6 to 15 percent slopesRoC241234215772tnzfwi01719851:15840
Rosholt sandy loam, 2 to 6 percent slopesRoB10084319222tnzdwi01919941:20000
Rosholt sandy loam, 6 to 15 percent slopesRoC6004319232tnzfwi01919941:20000
Rosholt sandy loam, 0 to 2 percent slopesRoA4824319212tnzcwi01919941:20000
Rosholt sandy loam, 2 to 6 percent slopesRoB66744314162tnzdwi07319981:20000
Rosholt sandy loam, 6 to 15 percent slopesCkC47324313572tnzfwi07319981:20000
Rosholt sandy loam, 15 to 35 percent slopesCkE29564313582tnzgwi07319981:20000
Rosholt sandy loam, 0 to 2 percent slopesRoA24294314152tnzcwi07319981:20000
Rosholt sandy loam, 2 to 6 percent slopesRoB35413958562tnzdwi07819981:12000
Rosholt sandy loam, 6 to 15 percent slopesRoC26543958582tnzfwi07819981:12000
Rosholt sandy loam, 15 to 35 percent slopesRoD11193958572tnzgwi07819981:12000
Amery-Rosholt complex, 12 to 20 percent slopes, very stonyAoD365734211382zcwdwi09519781:15840
Haugen-Rosholt complex, 6 to 12 percent slopes, very stony28C2266724870332zcwcwi09519781:15840
Rosholt sandy loam, 2 to 6 percent slopesRoB205144212082tnzdwi09519781:15840
Rosholt sandy loam, 6 to 15 percent slopesRoC2188794212092tnzfwi09519781:15840
Rosholt-Cromwell complex, 12 to 20 percent slopesRpD16668421213g49jwi09519781:15840
Rosholt-Cromwell complex, 6 to 12 percent slopesRpC9917421212g49hwi09519781:15840
Rosholt sandy loam, 15 to 35 percent slopesRoD53794212102tnzgwi09519781:15840
Amery-Rosholt complex, 20 to 45 percent slopes, very stonyAoE37384211392zcwfwi09519781:15840
Haugen-Rosholt complex, 2 to 6 percent slopes, very stony28B293324870322zcw9wi09519781:15840
Rosholt-Cromwell complex, 20 to 30 percent slopesRpE2255421214g49kwi09519781:15840
Rosholt sandy loam, 0 to 2 percent slopesRoA16234212072tnzcwi09519781:15840
Rosholt-Cromwell complex, 2 to 6 percent slopesRpB1183421211g49gwi09519781:15840
Rosholt variant silt loam, 2 to 6 percent slopesRvB300421215g49lwi09519781:15840
Cress-Rosholt complex, 2 to 6 percent slopes380B4524870392pgz2wi09519781:15840
Cress-Rosholt complex, 12 to 25 percent slopes380D3924870412pgz4wi09519781:15840
Cress-Rosholt complex, 6 to 12 percent slopes380C1624870402pgz3wi09519781:15840
Rosholt sandy loam, 2 to 6 percent slopesRrB260584265612tnzdwi09719721:20000
Rosholt sandy loam, 6 to 15 percent slopesRrC2129244265622tnzfwi09719721:20000
Rosholt complex, 20 to 40 percent slopesRuE4817426567g9w7wi09719721:20000
Rosholt complex, 12 to 20 percent slopesRuD3229426566g9w6wi09719721:20000
Rosholt sandy loam, 0 to 2 percent slopesRrA23444265602tnzcwi09719721:20000
Rosholt loam, loamy substratum, 0 to 2 percent slopesRt1208426565g9w5wi09719721:20000
Rosholt sandy loam, 2 to 6 percent slopes38B25366250132tnzdwi10720061:12000
Rosholt sandy loam, 6 to 15 percent slopes38C4426250142tnzfwi10720061:12000
Rosholt sandy loam, 15 to 35 percent slopes38D876250152tnzgwi10720061:12000
Haugen-Rosholt complex, 6 to 12 percent slopes, very stonyAnC242674221032zcwcwi10919751:15840
Amery-Rosholt complex, 12 to 20 percent slopes, very stonyAnD240764221042zcwdwi10919751:15840
Rosholt sandy loam, 2 to 6 percent slopesOmB35754221642tnzdwi10919751:15840
Rosholt sandy loam, 6 to 15 percent slopesOmC218404221652tnzfwi10919751:15840
Rosholt sandy loam, 2 to 6 percent slopes38B20456253442tnzdwi11320061:12000
Rosholt sandy loam, 15 to 35 percent slopes38D19156253462tnzgwi11320061:12000
Rosholt sandy loam, 6 to 15 percent slopes38C16906253452tnzfwi11320061:12000
Rosholt sandy loam, 0 to 2 percent slopes38A12356253432tnzcwi11320061:12000
Amery-Rosholt complex, 12 to 20 percent slopes, very stony127D5776253672zcwdwi11320061:12000
Haugen-Rosholt complex, 6 to 12 percent slopes, very stony28C5036253392zcwcwi11320061:12000
Haugen-Rosholt complex, 2 to 6 percent slopes, very stony28B4586253382zcw9wi11320061:12000
Amery-Rosholt complex, 20 to 45 percent slopes, very stony127E4546253682zcwfwi11320061:12000
Cress-Rosholt complex, 12 to 25 percent slopes380D20517038321v5zbwi11320061:12000
Rosholt sandy loam, 2 to 6 percent slopesRoB424124226142tnzdwi11519811:15840
Rosholt sandy loam, 6 to 15 percent slopesRoC116234226152tnzfwi11519811:15840
Rosholt sandy loam, 15 to 35 percent slopesRoD27804226162tnzgwi11519811:15840
Elderon-Rosholt complex, 12 to 20 percent slopesEcD2462422666g5tdwi11519811:15840
Elderon-Rosholt complex, 20 to 35 percent slopesEcE2424422667g5tfwi11519811:15840
Rosholt-Rock outcrop complex, 2 to 35 percent slopesRrD2108422619g5rwwi11519811:15840
Rosholt sandy loam, 0 to 2 percent slopesRoA14764226132tnzcwi11519811:15840
Rosholt-Elderon complex, 6 to 12 percent slopesRpC848422618g5rvwi11519811:15840
Rock outcrop-Rosholt variant complex, 2 to 35 percent slopesRmD748422612g5rnwi11519811:15840
Rosholt-Elderon complex, 2 to 6 percent slopesRpB619422617g5rtwi11519811:15840
Haugen-Rosholt complex, 6 to 12 percent slopes, very stony28C151114354542zcwcwi12920021:12000
Amery-Rosholt complex, 12 to 20 percent slopes, very stony127D81914354802zcwdwi12920021:12000
Rosholt sandy loam, 6 to 15 percent slopes38C67184354592tnzfwi12920021:12000
Amery-Rosholt complex, 20 to 45 percent slopes, very stony127E40234354812zcwfwi12920021:12000
Rosholt sandy loam, 2 to 6 percent slopes38B38134354582tnzdwi12920021:12000
Rosholt sandy loam, 15 to 35 percent slopes38D35054354602tnzgwi12920021:12000
Haugen-Rosholt complex, 2 to 6 percent slopes, very stony28B25354354532zcw9wi12920021:12000
Cress-Rosholt complex, 12 to 25 percent slopes380D1755435503gm5hwi12920021:12000
Cress-Rosholt complex, 6 to 12 percent slopes380C1416435502gm5gwi12920021:12000
Rosholt sandy loam, 0 to 2 percent slopes38A11824354572tnzcwi12920021:12000
Cress-Rosholt complex, 2 to 6 percent slopes380B684435501gm5fwi12920021:12000
Rosholt sandy loam, 2 to 6 percent slopesRoB300554227432tnzdwi13519821:15840
Rosholt sandy loam, 6 to 15 percent slopesRoC104304227442tnzfwi13519821:15840
Elderon-Rosholt complex, 12 to 30 percent slopesEcD8283422709g5vswi13519821:15840
Rosholt sandy loam, 0 to 2 percent slopesRoA49114227422tnzcwi13519821:15840
Elderon-Rosholt complex, 6 to 12 percent slopesEcC3940422708g5vrwi13519821:15840
Rosholt sandy loam, 15 to 35 percent slopesRoD37964227452tnzgwi13519821:15840
Rosholt-Rock outcrop complex, 2 to 10 percent slopesRrB1494422746g5wzwi13519821:15840
Rosholt sandy loam, 0 to 2 percent slopesOnA7174264782tnzcwi14119711:12000

Map of Series Extent

Approximate geographic distribution of the ROSHOLT 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 .