Official Series Description


Lab Data Summary

Aggregate lab data for the SIMEON soil series. This aggregation is based on all pedons with a current taxon name of SIMEON, 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 SIMEON 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
6509N1178S09NE171015Simeon6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.9500351,-100.4375305
6684P019783NE031050Simeon6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.7672234,-100.9563904

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SIMEON 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 SIMEON 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 SIMEON 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 SIMEON 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 SIMEON 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 SIMEON 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 SIMEON 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 mountains figure.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with SIMEON, 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. NE-2012-02-13-38 | Kearney County - September 1984

    Typical pattern of soils in the Alda-Wann-Boel association (Soil Survey of Kearney County, Nebraska; September 1984).

  2. NE-2012-02-13-50 | Knox County - June 1997

    Typical pattern of soils and parent material in the Brunswick-Paka-Simeon association (Soil Survey of Knox County, Nebraska; June 1997).

  3. NE-2012-02-13-54 | Loup County - October 1990

    Typical pattern of soils and parent material in the Ipage-Valentine-Elsmere and Almeria-Calamus-Bolent associations (Soil Survey of Loup County, Nebraska; October 1990).

  4. NE-2012-02-13-71 | Platte County - September 1988

    Typical landscape pattern of the soils and the underlying material in the Valentine-Thurman association (Soil Survey of Platte County, Nebraska; September 1988).

Map Units

Map units containing SIMEON 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
Simeon loamy sand, 5 to 15 percent slopes27989462115054617m7dks10919621:24000
Simeon loamy sand, 5 to 15 percent slopes2798449115001017lp3ks17919821:24000
Simeon sandy loam, 0 to 3 percent slopes893238722161072dd1bne00119701:20000
Valentine-Simeon complex, moist, 0 to 9 percent slopes4877198328766972v9w8ne00319751:20000
Valentine-Simeon complex, 6 to 11 percent slopes48791846427011gbbkne00319751:20000
Valentine-Simeon sands, 3 to 9 percent slopes488140322159532dcwcne00319751:20000
Simeon sand, 6 to 30 percent slopes, eroded893121722159862dcxfne00319751:20000
Simeon sandy loam, 0 to 6 percent slopes89332122159882dcxhne00319751:20000
Simeon sand, 0 to 3 percent slopes8929404716994982v9wfne00919881:20000
Valentine-Simeon complex, moist, 0 to 9 percent slopes4877110016995102v9w8ne00919881:20000
Simeon sand, 3 to 30 percent slopes893060916994991v1gkne00919881:20000
Simeon-Valentine complex, 0 to 9 percent slopes89396422191572v9w9ne00919881:20000
Simeon-Valentine complex, 3 to 30 percent slopes, eroded89408497357669d05qne01519761:20000
Simeon loamy sand, 0 to 3 percent slopes892529883576672v9wgne01519761:20000
Simeon-Valentine loamy sands, 0 to 6 percent slopes89462751357668d05pne01519761:20000
Simeon-Valentine complex, 0 to 9 percent slopes89391840528767012v9w9ne01719871:20000
Valentine-Simeon complex, 9 to 40 percent slopes, eroded488071841000413c34ne01719871:20000
Simeon loamy sand, 0 to 3 percent slopes892558011000252v9wgne01719871:20000
Simeon loamy sand, 3 to 11 percent slopes892826741000263c2nne01719871:20000
Simeon sandy loam, 0 to 3 percent slopes893255217000781v227ne01919671:20000
Simeon loamy sand, 0 to 3 percent slopes8925129516913251trywne02319791:20000
Simeon-Talmo-Ortello complex, 11 to 30 percent slopes89376069427134gbgjne02719821:20000
Simeon sand, 6 to 30 percent slopes, eroded89311422168232ddsfne02719821:20000
Simeon-Valentine complex, 0 to 9 percent slopes8939185741004312v9w9ne03119951:24000
Simeon sand, 0 to 3 percent slopes892985461004302v9wfne03119951:24000
Simeon-Valentine complex, 9 to 24 percent slopes894129491004322v9wcne03119951:24000
Simeon loamy sand, 3 to 30 percent slopes892719616998031v1scne07119841:20000
Simeon loamy sand, 0 to 3 percent slopes892536116999642v9wgne07719871:20000
Simeon sandy loam, 0 to 3 percent slopes8932166217001761v25dne07920031:12000
Valentine-Simeon sands, 9 to 30 percent slopes, eroded4882153821001693c78ne08919811:20000
Simeon loamy sand, 0 to 3 percent slopes8925123491001562v9wgne08919811:20000
Valentine-Simeon sands, 3 to 9 percent slopes488158061001683c77ne08919811:20000
Simeon sand, 0 to 3 percent slopes892928161001552v9wfne08919811:20000
Simeon sand, 6 to 30 percent slopes, eroded8931127922196102dhpbne08919811:20000
Simeon-Valentine sands, 11 to 60 percent slopes, eroded89474922196262dhpvne08919811:20000
Simeon loamy sand, 0 to 3 percent slopes89253562997433bsjne09319681:12000
Simeon sandy loam, 0 to 3 percent slopes8932923716918711tsjhne09919821:20000
Simeon-Holt variant-Ronson complex, 6 to 17 percent slopes893530295357735d07vne10319771:20000
Simeon-Valentine loamy sands, 0 to 3 percent slopes89454917357737d07xne10319771:20000
Simeon-Valentine fine sands, 6 to 17 percent slopes, eroded89432008357736d07wne10319771:20000
Simeon-Valentine loamy sands, 0 to 6 percent slopes8946822175952dflbne10319771:20000
Simeon sand, 6 to 30 percent slopes, eroded893110074114428917dqkne10719891:20000
Simeon-Thurman complex, 6 to 30 percent slopes89386816114429217dqnne10719891:20000
Simeon loamy sand, 0 to 6 percent slopes89262537114429017dqlne10719891:20000
Simeon sandy loam, 0 to 6 percent slopes89332269114429117dqmne10719891:20000
Simeon sand, 0 to 3 percent slopes8929186216995492v9wfne11519861:20000
Boelus sandy substratum-Simeon loamy sands, 0 to 3 percent slopes6644150516995191v1h6ne11519861:20000
Valentine-Simeon complex, moist, 0 to 9 percent slopes4877113016995632v9w8ne11519861:20000
Simeon sand, 3 to 30 percent slopes893038216995501v1j6ne11519861:20000
Simeon loamy sand, 0 to 3 percent slopes8925113417096811vd20ne12119781:20000
Simeon loamy sand, 0 to 3 percent slopes89253822289742dtfdne12519581:20000
Simeon sandy loam, 0 to 3 percent slopes893229922194712dhjvne13719671:20000
Simeon sandy loam, 3 to 11 percent slopes8934742427605gbyqne13919701:20000
Simeon loamy sand, 0 to 3 percent slopes8925828427677gc11ne14119841:20000
Simeon loamy sand, 0 to 3 percent slopes8925248022189932dh1fne14319671:20000
Simeon-Valentine sands, 11 to 60 percent slopes, eroded894781211002563cb2ne14919821:20000
Simeon loamy sand, 0 to 3 percent slopes892549521002542v9wgne14919821:20000
Valentine-Simeon complex, 9 to 40 percent slopes, eroded4880454122198422dhxtne14919821:20000
Simeon-Meadin complex, 0 to 9 percent slopes893632861002553cb1ne14919821:20000
Simeon loamy sand, 3 to 11 percent slopes89286322198402dhxrne14919821:20000
Simeon-Valentine complex, 9 to 24 percent slopes894134626056842v9wcne17119631:24000
Simeon-Valentine complex, 0 to 9 percent slopes893930226056832v9w9ne17119631:24000
Simeon sand, 0 to 3 percent slopes89299126056822v9wfne17119631:24000
Simeon loamy sand, 3 to 30 percent slopes892789216999111v1wvne17519831:20000
Simeon loamy sand, 0 to 3 percent slopes892520116999102v9wgne17519831:20000

Map of Series Extent

Approximate geographic distribution of the SIMEON 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 .