Official Series Description


Lab Data Summary

Aggregate lab data for the DONIPHAN soil series. This aggregation is based on all pedons with a current taxon name of DONIPHAN, 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 DONIPHAN 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
115BM87161021987MO161002Doniphan2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM91105101991MO105010Doniphan2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM93043011993MO043001Doniphan4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
116A81P00281980MO105004Doniphan6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.5947227,-92.3905563
116A81P00291980MO105005Doniphan6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.5941658,-92.3899994
116AM91105191990MO105180Doniphan3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.7352778,-92.5755556
116AM92105821992MO105348Doniphan4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.5513889,-92.3980556
116AM92613121992MO203012MDoniphan4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.2131,-91.3829083
116AM94C_W041994MO203914MDoniphan4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.1750333,-91.1387417
116AM95601121995MO035012MDoniphan4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.0090944,-91.1981472
116AM95091311995MO091141Doniphan4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.0365722,-91.8177111
116AM96223051996MO223081Doniphan4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.1554794,-90.6746597
116AM97067331997MO067125Doniphan4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.9479861,-92.2718778
116AM97067361997MO067128Doniphan4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.9370306,-92.249525
116AM97091031997MO091018Doniphan4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.8435972,-92.0172861
116AM97223141997MO223056Doniphan4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.0966492,-90.4129639
116AM97223151997MO223070Doniphan4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.0657425,-90.4730225
116AM97223631997MO223208Doniphan4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.0267525,-90.3694992
116AM98153151998MO153236Doniphan4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36,-92
116AM98613781998MO203078Doniphan4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.0969833,-91.0873889
116AM99017041999MO017004Doniphan4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4208031,-90.1282272
116AM01149102001MO149010Doniphan4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.6728889,-91.5064722
116A82P0142S1981MO185004Doniphan7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0753326,-93.5640945
116BM96119321996MO119070Doniphan4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.7337083,-94.1273083
116BM04179112004MO179011Doniphan4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.2037917,-93.4213056
116CM93223101993MO223010Doniphan3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.3079262,-90.2559204
116CM94223351994MO223035Doniphan4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.2787933,-90.3858795

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the DONIPHAN 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 DONIPHAN 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 DONIPHAN 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 DONIPHAN 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 flats position figure.

Competing Series

Soil series competing with DONIPHAN 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 DONIPHAN 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 DONIPHAN 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 DONIPHAN, 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. MO-2012-02-06-17 | Butler County and Part of Ripley County - November 1983

    Typical pattern of soils and parent material in the Doniphan-Captina association (Soil Survey of Butler County and Part of Ripley County, Missouri; November 1983).

  2. MO-2012-02-06-18 | Butler County and Part of Ripley County - November 1983

    Typical pattern of soils and parent material in the Doniphan-Clarksville association (Soil Survey of Butler County and Part of Ripley County, Missouri; November 1983).

Map Units

Map units containing DONIPHAN 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
Doniphan very gravelly silt loam, 8 to 20 percent slopes154900728044642ygp7ar00519781:20000
Doniphan very gravelly silt loam, 3 to 8 percent slopes142723128044632ygp6ar00519781:20000
Gassville-Doniphan complex, 3 to 8 percent slopes1639340280460030c9var04919791:20000
Gassville-Doniphan complex, 3 to 8 percent slopes166469285627830c9var06519791:20000
Doniphan very gravelly silt loam, 8 to 20 percent slopes151954728045212ygp7ar08919781:20000
Doniphan very gravelly silt loam, 3 to 8 percent slopes141469128045202ygp6ar08919781:20000
Gepp-Doniphan association, rolling1931290564490lydcar12119761:20000
Doniphan-Gepp association, undulating1513140564486lyd7ar12119761:20000
Doniphan gravelly silt loam, 8 to 12 percent slopes14121305644852ygp4ar12119761:20000
Doniphan gravelly silt loam, 3 to 8 percent slopes1339905644842ygp5ar12119761:20000
Doniphan gravelly silt loam, 3 to 8 percent slopes9191225645842ygp5ar13519811:20000
Doniphan gravelly silt loam, 8 to 12 percent slopes10121995645572ygp4ar13519811:20000
Doniphan very gravelly silt loam, 15 to 35 percent slopes7342265025025512vxt4mo02319821:24000
Doniphan very gravelly silt loam, 8 to 15 percent slopes7342126025025462vxt3mo02319821:24000
Doniphan very gravelly silt loam, 3 to 8 percent slopes7342011325025442vxt2mo02319821:24000
Doniphan gravelly silt loam, 3 to 8 percent slopes73416201625025402q24hmo03519881:24000
Doniphan very gravelly silt loam, 15 to 35 percent slopes7342245125025522vxt4mo03519881:24000
Doniphan very gravelly silt loam, 8 to 15 percent slopes7342118825025472vxt3mo03519881:24000
Clarksville-Doniphan complex, high elevation, 35 to 50 percent slopes, very stony73398903910083262t7g1mo06519711:24000
Clarksville-Doniphan complex, high elevation, 15 to 35 percent slopes, very stony73397215310083252t7g0mo06519711:24000
Doniphan gravelly silt loam, 3 to 8 percent slopes73416391625025412q24hmo14920041:24000
Doniphan very gravelly silt loam, 8 to 15 percent slopes73421110825025482vxt3mo14920041:24000
Doniphan very gravelly silt loam, 15 to 35 percent slopes734224825025532vxt4mo14920041:24000
Doniphan very gravelly silt loam, 3 to 8 percent slopes734203603925025452vxt2mo18119821:24000
Doniphan very gravelly silt loam, 8 to 15 percent slopes734211910025025492vxt3mo18119821:24000
Doniphan very gravelly silt loam, 15 to 35 percent slopes73422806525025542vxt4mo18119821:24000
Doniphan gravelly silt loam, 3 to 8 percent slopes73416770525025422q24hmo18119821:24000
Doniphan very gravelly silt loam, 8 to 15 percent slopes, stony7341916539945622t7ftmo18119821:24000
Doniphan gravelly silt loam, 3 to 8 percent slopes73416104625025432q24hmo20320041:24000
Doniphan very gravelly silt loam, 8 to 15 percent slopes7342131825025502vxt3mo20320041:24000
Doniphan very gravelly silt loam, 15 to 35 percent slopes734228025025552vxt4mo20320041:24000
Doniphan gravelly silt loam, 1 to 3 percent slopesBhB25648571843m61kok04119671:24000
Doniphan-Tonti complex, 3 to 5 percent slopesBlC16617571844m61lok04119671:24000

Map of Series Extent

Approximate geographic distribution of the DONIPHAN 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 .