Official Series Description


Lab Data Summary

Aggregate lab data for the LUDDEN soil series. This aggregation is based on all pedons with a current taxon name of LUDDEN, 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 LUDDEN 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
55A84ND049023S1984ND049023Ludden4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.5452778,-100.4941667
55B83P001181SD013062Ludden3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.4527779,-98.2638855
55B83P001281SD013063Ludden3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.4366684,-98.246109
55B83P001381SD013064Ludden3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.4550018,-98.2463913

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the LUDDEN 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 LUDDEN 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 LUDDEN 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 LUDDEN 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 LUDDEN 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 LUDDEN 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 LUDDEN 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 hills figure.

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 LUDDEN, 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. SD-2010-11-01-13 | Spink County - 2009

    Pattern of soils and underlying materials in the Great Bend-Beotia, Harmony-Aberdeen-Nahon, and Ludden-Lamoure associations (Soil Survey of Spink County, South Dakota; 2009).

  2. SD-2012-03-14-08 | Brown County - April 1993

    Typical pattern of soils and parent material in the Great Bend-Beotia, Harmony-Aberdeen-Nahon, and Ludden-Lamoure associations (Soil Survey of Brown County, SD; 1993).

Map Units

Map units containing LUDDEN 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
Wahpeton-Ludden silty clays, 0 to 6 percent slopes, floodedI135B2581279888021wszmn06920071:12000
Sinai-Ludden, flooded, clays, very-fine family, 0 to 6 percent slopesI137B2455279888221x2vmn06920071:12000
Wahpeton-Ludden silty clays, 0 to 6 percent slopes, floodedI135B8279900121wszmn08919941:20000
Ludden silty clay loam, 0 to 1 percent slopes, frequently floodedI782A314427999712ql27mn15519861:20000
Ludden silty clay loam19506357351czvgmn15519861:20000
Ludden silty clay, 0 to 1 percent slopes, frequently floodedG55A2925735852q3vcnd00319881:20000
Ryan-Ludden, saline silty clays, 0 to 1 percent slopes, frequently floodedG551A251825738002q5pknd0051:12000
Ryan-Ludden, saline silty clays, 0 to 1 percent slopes, frequently floodedF551A56925877542q56pnd0051:12000
Ludden silty clay, wet, 0 to 1 percent slopes, frequently floodedF527A846225860672q56lnd00919811:20000
Ludden silty clay, 0 to 1 percent slopes, frequently floodedG55A287725752722q3vcnd02119891:20000
Ryan-Ludden, saline silty clays, 0 to 1 percent slopes, frequently floodedG551A283625753562q5pknd02119891:20000
Ryan-Ludden, saline silty clays, 0 to 1 percent slopes, frequently floodedG551A152325763262q5pknd0271:12000
Ludden silty clay, 0 to 1 percent slopes, frequently floodedG55A56725754152q3vcnd0271:12000
Ludden silty clay, 0 to 1 percent slopes, frequently floodedG55A61725765742q3vcnd03919911:24000
Ryan-Ludden, saline silty clays, 0 to 1 percent slopes, frequently floodedG551A38825766402q5pknd03919911:24000
Ryan-Ludden, saline silty clays, 0 to 1 percent slopes, frequently floodedG551A188225771022q5pknd04519661:20000
Ludden silty clay, 0 to 1 percent slopes, frequently floodedG55A68625770352q3vcnd04519661:20000
Ludden silty clay, 0 to 1 percent slopes, frequently floodedF55A1748925857342q4g1nd04919871:20000
Ludden silty clay, wet, 0 to 1 percent slopes, frequently floodedF527A1326725857902q56lnd04919871:20000
Ludden-Fluvaquents, channeled complex, 0 to 2 percent slopes, frequently floodedF531A594225856012q56mnd04919871:20000
Ryan-Ludden, saline silty clays, 0 to 1 percent slopes, frequently floodedF551A163025857722q56pnd04919871:20000
Ludden silty clay, 0 to 1 percent slopes, frequently floodedG55A8825713362q3vcnd04919871:20000
Ludden silty clay, 0 to 1 percent slopes, frequently floodedG55A44125772602q3vcnd0631:12000
Ryan-Ludden, saline silty clays, 0 to 1 percent slopes, frequently floodedG551A27125773462q5pknd0631:12000
Ludden silty clay, wet, 0 to 1 percent slopes, frequently floodedF527A145225854672q56lnd07519721:20000
Ludden silty clay, 0 to 1 percent slopes, frequently floodedF55A98325854312q4g1nd07519721:20000
Ludden silty clay, 0 to 1 percent slopes, occasionally floodedI177A80026424752qkvdnd09719741:20000
Ryan-Ludden, strongly saline silty clays, 0 to 1 percent slopes, frequently floodedI380A159526429012ptx1nd09919671:20000
Ludden silty clay, 0 to 1 percent slopes, occasionally floodedI177A119926428842qkvdnd09919671:20000
Ludden silty clay, wet, 0 to 1 percent slopes, frequently floodedF527A269525852902q56lnd10119671:20000
Ludden silty clay, 0 to 1 percent slopes, frequently floodedF55A210225852422q4g1nd10119671:20000
Ludden-Fluvaquents, channeled complex, 0 to 2 percent slopes, frequently floodedF531A22625851282q56mnd10119671:20000
Ludden silty clay loam, 0 to 1 percent slopes, occasionally floodedC59A21725669422q77bnd10119671:20000
Ryan-Ludden, saline silty clays, 0 to 1 percent slopes, frequently floodedG551A13325796722q5pknd10319661:12000
Lowe, occasionally flooded-Ludden, frequently flooded, complex, 0 to 1 percent slopesZ155A598927652822rkyksd01119951:24000
Ludden, moderately saline-Ludden silty clays, 0 to 1 percent slopes, frequently floodedZ256A278927652872rkyrsd01119951:24000
Ludden silty clay, 0 to 1 percent slopes, frequently floodedZ156A207127652832rkylsd01119951:24000
Lowe-Ludden complex, 0 to 1 percent slopesLr91418777g1rysd01119951:24000
Ludden, saline-Ludden silty clays, 0 to 1 percent slopesLu71418779g1s0sd01119951:24000
Ludden-Ludden, saline silty clays, 0 to 1 percent slopes, frequently floodedG541A1114327977882sd42sd01319871:20000
Ludden silty clay, ponded, 0 to 1 percent slopes, frequently flooded-Water complexG991A1089927978422sd75sd01319871:20000
Ludden silty clay, 0 to 1 percent slopes, frequently floodedG055A761127976422q3vcsd01319871:20000
Ryan-Ludden, saline silty clays, 0 to 1 percent slopes, frequently floodedG551A720527976892q5pksd01319871:20000
Ludden silty clay, ponded, 0 to 1 percent slopes, frequently floodedG529A335727978522sl42sd01319871:20000
Ludden silty clay, saline, 0 to 1 percent slopes, occasionally floodedG542A237827977892sd43sd01319871:20000
Ludden silty clay loam, strongly saline, 0 to 1 percent slopes, occasionally floodedC058A64727656162t7tksd01319871:20000
Ludden silty clay loam, strongly saline, 0 to 1 percent slopes, occasionally floodedC058A114927979532t7tksd02119781:20000
Ludden silty clay, salineLw6417755g0pzsd02519921:20000
Ludden silty clay, ponded, 0 to 1 percent slopes, frequently floodedG529A57427985472sl42sd03719921:20000
Ludden silty clay, 0 to 1 percent slopes, frequently floodedG055A55227984442q3vcsd03719921:20000
Ryan-Ludden, saline silty clays, 0 to 1 percent slopes, frequently floodedG551A34227984632q5pksd03719921:20000
Ludden-Ludden, saline silty clays, 0 to 1 percent slopes, frequently floodedG541A20927985062sd42sd03719921:20000
Ludden silty clay, saline, 0 to 1 percent slopes, occasionally floodedG542A15427985072sd43sd03719921:20000
Ludden silty clayLu63417099g00tsd03719921:20000
Ludden silty clay loam, strongly saline, 0 to 1 percent slopes, occasionally floodedC058A527986832t7tksd04919811:20000
Ludden silty clayLc1925418165g146sd05119771:20000
Ludden silty clay, 0 to 1 percent slopes, frequently floodedG055A254827992742q3vcsd09119701:20000
Ludden silty clayLu1791416584fzh6sd09119701:20000
Ludden silty clay, ponded, 0 to 1 percent slopes, frequently floodedG529A55227994042sl42sd09119701:20000
Ludden silty clay, saline, 0 to 1 percent slopes, occasionally floodedG542A33727993522sd43sd09119701:20000
Ludden-Ludden, saline silty clays, 0 to 1 percent slopes, frequently floodedG541A5527993512sd42sd09119701:20000
Ryan-Ludden, saline silty clays, 0 to 1 percent slopes, frequently floodedG551A3127993092q5pksd09119701:20000
Ludden clayLu2986417847g0sysd10919771:20000
Ludden silty clay, 0 to 1 percent slopes, frequently floodedG055A354627995392q3vcsd11519971:24000
Ludden-Ludden, saline silty clays, 0 to 1 percent slopes, frequently floodedG541A236327996092sd42sd11519971:24000
Ryan-Ludden, saline silty clays, 0 to 1 percent slopes, frequently floodedG551A197327995542q5pksd11519971:24000
Ludden silty clay, saline, 0 to 1 percent slopes, occasionally floodedG542A86927996102sd43sd11519971:24000
Ludden silty clay, ponded, 0 to 1 percent slopes, frequently floodedG529A84928000682sl42sd11519971:24000
Ludden silty clay loam, strongly saline, 0 to 1 percent slopes, occasionally floodedC058A42627995262t7tksd11519971:24000
Ludden silty clay, wet, 0 to 1 percent slopesLw13356683cz4xsd11519971:24000
Ludden silty clay loam, strongly saline, 0 to 1 percent slopes, occasionally floodedC058A112728001552t7tksd12919751:20000

Map of Series Extent

Approximate geographic distribution of the LUDDEN 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 .