Official Series Description


Lab Data Summary

Aggregate lab data for the ECKMAN soil series. This aggregation is based on all pedons with a current taxon name of ECKMAN, 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 ECKMAN 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
102AUMN1987S1975MN023(1987)Eckman3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.094321,-95.932074
102AUMN1936S1975MN1731936Eckman2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.7475662,-96.2733078
102AUMN3338S1980MN167020 (3338)Eckman2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.6121483,-96.3255463
102AUMN4433S1989MN073069 (4433)Eckman3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.1845627,-96.1866531
55B40A003153ND103001Eckman6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.7030556,-100.04
55B40A003253ND103002Eckman6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.6880556,-100.0483333
55B83P000482SD013006Eckman5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.7677765,-98.0208359
55B40A2390S1950SD115006Eckman8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.1863899,-98.4736099

Water Balance

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

Competing Series

Soil series competing with ECKMAN 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 ECKMAN series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the ECKMAN 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.

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

Soil series sharing subgroup-level classification with ECKMAN, 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. ND-2012-02-08-67 | Wells County - June 1970

    Parent material and position of soils in association 10 (Soil Survey of Wells County, North Dakota; June 1970

Map Units

Map units containing ECKMAN 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
Eckman silt loam, 1 to 6 percent slopesJ15B1168924230352xpp8mn02319801:15840
Zell-Eckman complex, 2 to 6 percent slopesJ38B32924230502mbcxmn02319801:15840
Zell-Eckman complex, 6 to 12 percent slopes, moderately erodedJ38C23524230512mbcymn02319801:15840
Eckman silt loam, 1 to 6 percent slopesRoB12283973172xpp8mn04119701:12000
Eckman silt loam, 1 to 6 percent slopes290B9703980322xpp8mn05119741:20000
Eckman silt loam, 1 to 6 percent slopes290B53794302822xpp8mn07319941:20000
Eckman silt loam, 1 to 6 percent slopes290B11503992222xpp8mn08719921:20000
Eckman silt loam, 1 to 6 percent slopes29013334356862xpp8mn11119961:20000
Zell-Eckman silt loams, 15 to 25 percent slopesI202E380027996881nyrxmn11919961:20000
Eckman very fine sandy loam, 1 to 4 percent slopesI856A26527999232ql13mn14919661:15840
Eckman silt loam, 1 to 6 percent slopesEcB2264283322xpp8mn14919661:15840
Zell-Eckman complex, 2 to 6 percent slopesJ38B1217434821glghmn15120001:12000
Eckman silt loam, 1 to 6 percent slopesJ15B8794347872xpp8mn15120001:12000
Zell-Eckman complex, 6 to 12 percent slopes, erodedJ38C2326434822glgjmn15120001:12000
Eckman silt loam, 1 to 6 percent slopes290B10113574122xpp8mn16719851:20000
Zell-Eckman complex, 6 to 12 percent slopes, moderately erodedJ38C252716540001sj3vmn17319791:20000
Eckman silt loam, 1 to 6 percent slopesJ15B31430266142xpp8mn17319791:20000
Zell-Eckman complex, 2 to 6 percent slopesJ38B13516539991sj3tmn17319791:20000
Zell-Eckman loams, 15 to 25 percent slopesG486E109025736192q5nwnd00319881:20000
Eckman-Zell loams, 6 to 9 percent slopesG486C106225736182q5ntnd00319881:20000
Gardena-Eckman loams, 2 to 6 percent slopesF486B102025877682q565nd0051:12000
Eckman-Zell loams, 6 to 9 percent slopesF486C74325876112q566nd0051:12000
Gardena-Eckman loams, 2 to 6 percent slopesG486B28025736802q5nsnd0051:12000
Eckman-Zell loams, 6 to 9 percent slopesG486C825737302q5ntnd0051:12000
Gardena-Eckman loams, 2 to 6 percent slopesF486B794225860762q565nd00919811:20000
Zell-Eckman silt loams, 15 to 25 percent slopesI202E361326409021nyrxnd01719831:20000
Eckman-Zell complex, 6 to 9 percent slopesI201C51525215962qkv4nd01719831:20000
Eckman-Zell loams, 2 to 6 percent slopesI521B17126408341tbnrnd01719831:20000
Eckman-Gardena loams, 2 to 6 percent slopesI493B8226408981tbn7nd01719831:20000
Zell-Eckman silt loams, 9 to 15 percent slopesI202D4626408911nyrwnd01719831:20000
Gardena-Eckman loams, 2 to 6 percent slopesG486B177525753472q5nsnd02119891:20000
Gardena-Eckman loams, 0 to 2 percent slopesG486A25325763182q5nrnd0271:12000
Gardena-Eckman loams, 2 to 6 percent slopesG486B7425763192q5nsnd0271:12000
Gardena-Eckman silt loams, 2 to 6 percent slopesI202B2226425331nyrtnd03519801:20000
Zell-Eckman silt loams, 9 to 15 percent slopesI202D126425341nyrwnd03519801:20000
Gardena-Eckman loams, 2 to 6 percent slopesG486B258625766322q5nsnd03919911:24000
Eckman-Zell loams, 6 to 9 percent slopesG486C145625766332q5ntnd03919911:24000
Zell-Eckman loams, 9 to 15 percent slopesG486D45825766342q5nvnd03919911:24000
Zell-Eckman loams, 15 to 25 percent slopesG486E10625766352q5nwnd03919911:24000
Gardena-Eckman loams, 0 to 2 percent slopesG486A313225770892q5nrnd04519661:20000
Gardena-Eckman loams, 2 to 6 percent slopesG486B75025770902q5nsnd04519661:20000
Eckman-Zell loams, 6 to 9 percent slopesG486C4125770912q5ntnd04519661:20000
Gardena-Eckman loams, 2 to 6 percent slopesG486B78225773392q5nsnd0631:12000
Zell-Eckman silt loams, 9 to 15 percent slopesI202D25826429501nyrwnd06719721:20000
Gardena-Eckman loams, 2 to 6 percent slopesF486B727725872932q565nd06919751:20000
Eckman-Zell loams, 6 to 9 percent slopesF486C78725871822q566nd06919751:20000
Gardena-Eckman loams, 0 to 2 percent slopesG486A139525811792q5nrnd07319921:20000
Eckman-Zell loams, 2 to 6 percent slopesG478B117025811772q5nknd07319921:20000
Zell-Eckman silt loams, 15 to 25 percent slopesI202E50926412681nyrxnd07319921:20000
Eckman-Zell complex, 6 to 9 percent slopesI201C42126413602qkv4nd07319921:20000
Gardena-Eckman loams, 2 to 6 percent slopesG486B37925811802q5nsnd07319921:20000
Eckman-Gardena loams, 2 to 6 percent slopesI493B34726413351tbn7nd07319921:20000
Eckman-Zell loams, 6 to 9 percent slopesG486C12325811812q5ntnd07319921:20000
Gardena-Eckman loams, 0 to 2 percent slopesI493A6626413361tbn8nd07319921:20000
Gardena-Eckman silt loams, 2 to 6 percent slopesI202B519626411531nyrtnd07720051:12000
Eckman-Zell complex, 6 to 9 percent slopesI201C212026409752qkv4nd07720051:12000
Zell-Eckman silt loams, 9 to 15 percent slopesI202D157326411161nyrwnd07720051:12000
Zell-Eckman silt loams, 15 to 25 percent slopesI202E78126411341nyrxnd07720051:12000
Eckman-Gardena loams, 2 to 6 percent slopesI493B1026411291tbn7nd07720051:12000
Eckman-Zell loams, 6 to 9 percent slopesG486C525774052q5ntnd07720051:12000
Gardena-Eckman loams, 0 to 2 percent slopesF486A196225881132q564nd07919901:24000
Gardena-Eckman loams, 2 to 6 percent slopesF486B42025882182q565nd07919901:24000
Gardena-Eckman loams, 2 to 6 percent slopesG486B322925794342q5nsnd08119591:12000
Gardena-Eckman silt loams, 2 to 6 percent slopesI202B36826411931nyrtnd08119591:12000
Gardena-Eckman loams, 0 to 2 percent slopesG486A31425795742q5nrnd08119591:12000
Eckman-Zell complex, 6 to 9 percent slopesI201C24726412662qkv4nd08119591:12000
Eckman-Zell loams, 6 to 9 percent slopesG486C21725794732q5ntnd08119591:12000
Eckman and Maddock loams, undulatingEmB97341575cgfknd08119591:12000
Zell-Eckman silt loams, 9 to 15 percent slopesI202D8426411941nyrwnd08119591:12000
Eckman silt loam, 1 to 6 percent slopesEcB473415742xpp8nd08119591:12000
Eckman and Maddock loams, rollingEmC2341576cgflnd08119591:12000
Zell-Eckman silt loams, 15 to 25 percent slopesI202E11926413651nyrxnd09119911:20000
Gardena-Eckman silt loams, 2 to 6 percent slopesI202B1926413641nyrtnd09119911:20000
Zell-Eckman silt loams, 15 to 25 percent slopesI202E108926415751nyrxnd09719741:20000
Gardena-Eckman silt loams, 2 to 6 percent slopesI202B91826415731nyrtnd09719741:20000
Eckman-Zell complex, 6 to 9 percent slopesI201C51426425082qkv4nd09719741:20000
Zell-Eckman silt loams, 9 to 15 percent slopesI202D7726415741nyrwnd09719741:20000
Gardena-Eckman silt loams, 2 to 6 percent slopesI202B35125094971nyrtnd09919671:20000
Zell-Eckman silt loams, 9 to 15 percent slopesI202D17425094981nyrwnd09919671:20000
Gardena-Eckman loams, 0 to 2 percent slopesG486A334525796652q5nrnd10319661:12000
Eckman-Gardena very fine sandy loams, 0 to 2 percent slopesG493A1315227977792sd3qsd01319871:20000
Eckman-Gardena very fine sandy loams, 2 to 6 percent slopesG493B1309927977802sd3rsd01319871:20000
Eckman-Zell very fine sandy loams, 2 to 6 percent slopesG495B131627977812sd3ssd01319871:20000
Eckman-Gardena very fine sandy loams, 0 to 2 percent slopesG493A4527984982sd3qsd03719921:20000
Eckman-Gardena very fine sandy loams, 2 to 6 percent slopesG493B827984992sd3rsd03719921:20000
Eckman-Zell very fine sandy loams, 2 to 6 percent slopesG495B727985002sd3ssd03719921:20000
Zell-Eckman complex, 6 to 12 percent slopesZrC333416914fztvsd03919921:20000
Eckman loam, 2 to 6 percent slopesEcB330416849fzrrsd03919921:20000
Eckman-Gardena very fine sandy loams, 0 to 2 percent slopesG493A29327993442sd3qsd09119701:20000
Eckman-Gardena very fine sandy loams, 2 to 6 percent slopesG493B22527993452sd3rsd09119701:20000
Gardena-Eckman loams, 2 to 6 percent slopesG486B1727993042q5nssd09119701:20000
Eckman silt loam, 1 to 6 percent slopesEcB83904178152xpp8sd10919771:20000
Gardena-Eckman loams, 0 to 2 percent slopesI493A147028002051tbn8sd10919771:20000
Eckman-Zell complex, 6 to 9 percent slopesEeC1030417816g0rysd10919771:20000
Eckman-Gardena loams, 2 to 6 percent slopesI493B62428002041tbn7sd10919771:20000
Zell-Eckman silt loams, 9 to 15 percent slopesI202D41528001631nyrwsd10919771:20000
Zell-Eckman complex, 9 to 25 percent slopesZeD149417886g0v6sd10919771:20000
Eckman-Zell complex, 6 to 9 percent slopesI201C3528002322qkv4sd10919771:20000
Gardena-Eckman silt loams, 2 to 6 percent slopesI202B728001621nyrtsd10919771:20000
Zell-Eckman silt loams, 15 to 25 percent slopesI202E628001641nyrxsd10919771:20000
Eckman-Gardena very fine sandy loams, 0 to 2 percent slopesG493A357127996032sd3qsd11519971:24000
Eckman-Zell very fine sandy loams, 2 to 6 percent slopesG495B139127996052sd3ssd11519971:24000
Eckman-Gardena very fine sandy loams, 2 to 6 percent slopesG493B73827996042sd3rsd11519971:24000

Map of Series Extent

Approximate geographic distribution of the ECKMAN 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 .