Official Series Description


Lab Data Summary

Aggregate lab data for the RARDEN soil series. This aggregation is based on all pedons with a current taxon name of RARDEN, 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 RARDEN 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
114B90P029489IN143005Rarden7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6183319,-85.7527771
114B90P029589IN143006Rarden6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6225014,-85.7519455
114B90P029689IN143007Rarden6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6213875,-85.7530594
116A59ID191959AR06319Rarden3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.8267,-91.7746
116A61ID031961AR06303Rarden3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.8267,-91.7746
11764WS211964AR14300Rarden3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.0383333,-94.4184054
11740A4401S1960AR047001Rarden5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.630928,-93.7915955
11740A4402S1960AR047002Rarden5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.6503754,-93.7315903
120CJN80181980IN071018Rarden1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9945667,-86.1232833
12407N0554S07KY043004Rardenn/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3953889,-83.1546111
n/a56WS051956AR14305Rarden3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aHO-0031956-OH073-003Rarden3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aRO-0171956-OH141-017Rarden3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aPK-s111960-OH131-S11Rarden2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aJK-0031961-OH079-003Rarden2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aDL-0451962-OH041-045Rarden3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aDL-0491962-OH041-049Rarden3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aGL-w031962-OH053-W03Rarden3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aGL-w051962-OH053-W05Rarden3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aPK-w011962-OH131-W01Rarden3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aJK-0111978-OH079-011Rarden4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aJK-0191980-OH079-019Rarden5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the RARDEN 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 RARDEN 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 RARDEN 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 RARDEN 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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Competing Series

Soil series competing with RARDEN 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 RARDEN 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 RARDEN 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 terrace figure.

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

Soil series sharing subgroup-level classification with RARDEN, 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. AL-2012-04-24-13 | Calhoun County - September 1961

    Some of the general soil areas, or soil associations, in relation to topographic position and parent material (Soil Survey of Calhoun County, Alabama; September 1961).

  2. KY-2010-09-03-19 | Lawrence and Martin Counties - 2005

    Typical pattern of soils, parent material, and topograhy in the Upshur-Vandalia-Rarden general soil map unit. This map unit is on the mountains (Soil Survey of Lawrence and Martin Counties, Kentucky; 2005).

  3. KY-2012-01-26-17 | Bath County - September 1963

    Typical landscape in the knobby areas of the county showing the topography, the relationship of some of the principal soils, and the parent rocks (Soil Survey of Bath County, Kentucky; September 1963).

  4. KY-2012-01-26-25 | Bath County - September 1963

    Cross section of Bath County showing the major soils and their relationship to the rock formations and to relief (Soil Survey of Bath County, Kentucky; September 1963).

  5. OH-2012-02-16-40 | Scioto County - January 1989

    Typical pattern of soils and parent material in the Latham-Wharton-Shelocta association (Soil Survey of Scioto County, Ohio; January 1989).

Map Units

Map units containing RARDEN 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
Rarden silt loam, shallow, 2 to 6 percent slopes, erodedRdB26049523377kkm4al01519591:20000
Rarden silt loam, shallow, 6 to 10 percent slopes, erodedRdC25169523378kkm5al01519591:20000
Rarden-Montevallo complex, 2 to 10 percent slopes, erodedRmC25114523381kkm8al01519591:20000
Rarden silty clay loam, shallow, 6 to 10 percent slopes , severely erodedReC34718523380kkm7al01519591:20000
Rarden gravelly loam, shallow, 6 to 10 percent slopes, erodedRaC23014523376kkm3al01519591:20000
Rarden silty clay loam, shallow, 2 to 6 percent slopes, severely erodedReB31466523379kkm6al01519591:20000
Rarden gravelly loam, shallow, 2 to 6 percent slopes, erodedRaB21053523375kkm2al01519591:20000
Coolville-Rarden-Stonehead silt loams, 12 to 18 percent slopes, erodedColD25452022906shhin00520021:12000
Rarden-Coolville complex, 12 to 22 percent slopes, severely erodedRctD33902022916shjin00520021:12000
Coolville-Rarden complex, 6 to 12 percent slopes, severely erodedConC356246119883bin00520021:12000
Coolville-Rarden complex, 12 to 18 percent slopesConD48312009436r31in01920011:12000
Coolville-Rarden complex, 6 to 12 percent slopes, severely erodedConC36172009426r30in01920011:12000
Rarden silty clay loam, 12 to 18 percent slopes, severely erodedRblD33782107167289in01920011:12000
Rarden silty clay, 6 to 18 percent slopes, gulliedRbmD53318517566pdin01920011:12000
Rarden-Coolville complex, 12 to 22 percent slopes, severely erodedRctD348018518166plin04320001:12000
Coolville-Rarden complex, 6 to 12 percent slopes, severely erodedConC320827143793g1in04320001:12000
Rarden silty clay loam, 12 to 18 percent slopes, severely erodedRblD39331907348220rcin07119851:15840
Rarden silt loam, 6 to 12 percent slopes, severely erodedRcsC36251907347220rbin07119851:15840
Coolville-Rarden complex, 6 to 12 percent slopes, severely erodedConC322027077261blin07119851:15840
Coolville-Rarden complex, 12 to 18 percent slopesConD8571656335kc0in14319951:12000
Rarden silty clay loam, 12 to 18 percent slopes, severely erodedRblD32911657595kh2in14319951:12000
Rarden silty clay loam, 6 to 12 percent slopes, severely erodedRblC31511657585kh1in14319951:12000
Rarden silty clay, 6 to 18 percent slopes, gulliedRbmD51031657605kh3in14319951:12000
Upshur-Rarden complex, 12 to 25 percent slopesUpD132188467921853ky06320071:12000
Upshur-Rarden complex, 6 to 12 percent slopesUpC25188467821852ky06320071:12000
Rarden silt loam, 12 to 20 percent slopesRdD1975549679lfzlky08519671:20000
Rarden silty clay loam, 12 to 20 percent slopes, severely erodedReD31330549681lfznky08519671:20000
Rarden silt loam, 6 to 12 percent slopesRdC955549678lfzkky08519671:20000
Rarden silty clay loam, 6 to 12 percent slopes, severely erodedReC3645549680lfzmky08519671:20000
Rarden silt loam, 12 to 20 percent slopes, erodedRaD246913979051hxmqky15119681:20000
Rarden silt loam, 6 to 12 percent slopesRaC36413979041hxmpky15119681:20000
Upshur-Rarden complex, 12 to 25 percent slopesUpD19924550919lh8lky64019961:24000
Upshur-Rarden complex, 25 to 60 percent slopes, rockyUpF13239550920lh8mky64019961:24000
Upshur-Rarden complex, 6 to 12 percent slopesUpC1307550918lh8kky64019961:24000
Rarden silt loam, 20 to 50 percent slopes, erodedRdF22101720815s20oh04119971:12000
Rarden silt loam, 2 to 6 percent slopes, erodedRdB2151720795s1yoh04119971:12000
Rarden silt loam, 6 to 15 percent slopes, erodedRdC2131720805s1zoh04119971:12000
Rarden silt loam, 20 to 50 percent slopes, erodedRdF241664125l54oh04919771:15840
Rarden-Steinsburg association, steepRrSZE11830024504532n7wwoh05319881:15840
Gilpin-Rarden association, steepGlRZE11010024504262n7w0oh05319881:15840
Lily-Rarden complex, 15 to 25 percent slopesLiRXD1633524504362n7wboh05319881:15840
Rarden-Gilpin silt loams, 8 to 15 percent slopes, erodedRrG1C2540824504492n7wroh05319881:15840
Rarden-Gilpin silt loams, 15 to 25 percent slopes, erodedRrG1D2479724504512n7wtoh05319881:15840
Rarden-Gilpin silt loams, 8 to 15 percent slopesRrG1C1259624504482n7wqoh05319881:15840
Rarden-Gilpin silt loams, 15 to 25 percent slopesRrG1D1209724504502n7wsoh05319881:15840
Gilpin-Rarden silt loams, 25 to 40 percent slopesGlR1E1107024504252n7vzoh05319881:15840
Rarden-Wharton silt loams, 8 to 15 percent slopes, erodedRrW1C211024504462n7wnoh05319881:15840
Rarden-Wharton silt loams, 15 to 25 percent slopes, erodedRrW1D23624504472n7wpoh05319881:15840
Rarden silt loam, 8 to 15 percent slopes, erodedRar1C21324504452n7wmoh05319881:15840
Gilpin-Rarden silt loams, 15 to 25 percent slopes, erodedGlR1D2524504242n7vyoh05319881:15840
Rarden-Wharton silt loams, 8 to 15 percent slopes, erodedRrW1C22064424510372n8hqoh07919811:15840
Shelocta-Rarden association, steepShRZE1287524510552n8j9oh07919811:15840
Rarden-Wharton silt loams, 15 to 25 percent slopes, erodedRrW1D2259424510402n8htoh07919811:15840
Rarden silt loam, 8 to 15 percent slopes, erodedRar1C2186324510322n8hkoh07919811:15840
Rarden silt loam, 3 to 8 percent slopesRar1B196324510302n8hhoh07919811:15840
Rigley-Rarden complex, 15 to 25 percent slopesRgRXD188624510502n8j4oh07919811:15840
Rarden-Steinsburg association, steepRrSZE172724510482n8j2oh07919811:15840
Rarden-Gilpin silt loams, 8 to 15 percent slopesRrG1C156024510412n8hvoh07919811:15840
Rigley-Rarden association, steepRgRZE141324510522n8j6oh07919811:15840
Gilpin-Rarden association, steepGlRZE130624510142n8gzoh07919811:15840
Rarden silt loam, 8 to 15 percent slopesRar1C115224510332n8hloh07919811:15840
Rarden-Gilpin silt loams, 8 to 15 percent slopes, erodedRrG1C210724510422n8hwoh07919811:15840
Lily-Rarden complex, 15 to 25 percent slopesLiRXD18424510152n8h0oh07919811:15840
Rarden-Gilpin silt loams, 15 to 25 percent slopes, erodedRrG1D25224510462n8j0oh07919811:15840
Rarden-Gilpin silt loams, 15 to 25 percent slopesRrG1D15224510452n8hzoh07919811:15840
Blairton-Rarden-Gilpin association, rollingBmC714605161l0sfoh07919811:15840
Rarden-Gilpin silt loams, 15 to 25 percent slopesRrG1D1249024511122n8l4oh08719891:15840
Rarden-Gilpin silt loams, 8 to 15 percent slopesRrG1C1200624511112n8l3oh08719891:15840
Rarden-Lily complex, 15 to 25 percent slopesRrLXD19224511132n8l5oh08719891:15840
Gilpin-Rarden silt loams, 25 to 40 percent slopesGlR1E1880424551072ndr0oh10519911:15840
Gilpin-Rarden silt loams, 15 to 25 percent slopes, erodedGlR1D2271224551062ndqzoh10519911:15840
Rarden silt loam, 8 to 15 percent slopes, erodedRar1C2179024512862n8rroh10519911:15840
Gilpin-Rarden silt loams, 15 to 25 percent slopesGlR1D111224551052ndqyoh10519911:15840
Rarden-Coolville silt loams, 12 to 18 percent slopes, moderately erodedRcD2330537814l1mvoh11119681:15840
Coolville-Rarden silt loams, 6 to 12 percent slopes, moderately erodedCrC2241537761l1l4oh11119681:15840
Coolville-Rarden silt loams, 12 to 18 percent slopes, moderately erodedCrD2158537762l1l5oh11119681:15840
Rarden silt loam, 15 to 25 percent slopesRdD8146537712l1jkoh13119841:15840
Blairton-Rarden-Gilpin association, rollingBdC7864537611l1f9oh13119841:15840
Rarden silt loam, 8 to 15 percent slopesRdC6534537711l1jjoh13119841:15840
Coolville-Rarden silt loams, 8 to 15 percent slopesCtC48316890441tpl9oh13119841:15840
Rarden silt loam, 8 to 15 percent slopes, erodedRdC23516890381tpl3oh13119841:15840
Rarden-Wharton silt loams, 8 to 15 percent slopes, erodedRrW1C22424799902p7mpoh13119841:15840
Coolville-Rarden silt loams, 8 to 15 percent slopesCpC7911537230l110oh14519841:15840
Rarden silt loam, 8 to 15 percent slopesRbC123537293l131oh14519841:15840
Rarden-Gilpin silt loams, 8 to 15 percent slopesRrG1C110524526702nb6doh14519841:15840
Gilpin-Rarden silt loams, 25 to 40 percent slopesGlR1E1830224535942nc56oh16319981:15840
Gilpin-Rarden silt loams, 6 to 15 percent slopesGlR1C1707724535922nc54oh16319981:15840
Gilpin-Rarden silt loams, 15 to 25 percent slopesGlR1D1483224535932nc55oh16319981:15840
Rarden-Wharton silt loams, 8 to 15 percent slopes, erodedRrW1C2250624539332ncj4oh16319981:15840
Shelocta-Rarden association, steepShRZE182624535912nc53oh16319981:15840
Rarden silt loam, 8 to 15 percent slopes, erodedRar1C218824533752nby4oh16319981:15840
Rarden-Wharton silt loams, 15 to 25 percent slopes, erodedRrW1D29724539342ncj5oh16319981:15840

Map of Series Extent

Approximate geographic distribution of the RARDEN 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 .