Official Series Description


Lab Data Summary

Aggregate lab data for the STARKS soil series. This aggregation is based on all pedons with a current taxon name of STARKS, 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 STARKS 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
108A85IL0291301985IL029130Starks2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4537861,-88.0460722
108A88IL0450051988IL045005Starks2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.594775,-87.5537667
108A81P0676S1981IL115046Starks6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9339218,-88.7533875
111ADC78181978IN031018Starks3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4020111,-85.5971
111DCS74011974IN017001Starks3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.650325,-86.3732444
111DCT75061975IN023006Starks2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.3673361,-86.4403833
111DMY78141978IN107014Starks2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.1119111,-86.8544389
111DCA84071984IN015007Starks2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5097167,-86.5750806
111DTI84211984IN157021Starks2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.434625,-86.7324917
111D05N0046S04IN157002Starks7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.2189167,-86.7729333
11384IL0291061984IL029106Starks2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3803833,-88.4590583
11383P0061S1982IL029022STARKS6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3919449,-88.4508362
115A68IL0590031968IL059003Starks5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.7894993,-88.2090868
95B67IL1110031967IL111003Starks5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.4529206,-88.6454901

Water Balance

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

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 STARKS 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 STARKS 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 STARKS 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 .

Click the image to view it full size.

Click the image to view it full size.

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 STARKS, 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. IL-2010-08-31-15 | Cumberland County - 2002

    Typical pattern of soils and parent material in the Starks-Drummer-Camden association (Soil Survey of Cumberland County, Illinois; 2002).

  2. IL-2010-09-01-05 | Edgar County - 2002

    Typical pattern of soils and parent material in the Camden-Starks association (Soil Survey of Edgar County, Illinois; 2002).

  3. IL-2011-08-03-20 | Coles County - 1993

    Typical pattern of soils and parent material in the Drummer-Starks-Brooklyn association (Soil Survey of Coles County, Illinois; 1993).

  4. IL-2011-08-05-01 | Wabash County - 1964

    General relationship of some Wabash County soils to physiographic position, relief, parent material, and native vegetation (Soil Survey of Wabash County, Illinois; 1964).

  5. IN-2010-09-09-04 | Boone County - 2004

    General pattern of soils, topography, and parent material in the Starks-Crosby-Cyclone association (Soil Survey of Boone County, Indiana; 2004).

Map Units

Map units containing STARKS 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
Starks silt loam, 0 to 2 percent slopes132A177016699671t1qxil02320061:12000
Starks silt loam, 0 to 2 percent slopes132A162716031801qt7hil02920051:12000
Starks silt loam, 0 to 2 percent slopes, rarely flooded7132A38714283861jybzil02920051:12000
Starks silt loam 0 to 2 percent slopes132A23321747865vw8il03519921:15840
Starks silt loam, 2 to 5 percent slopes132B4651747875vw9il03519921:15840
Starks silt loam, 0 to 2 percent slopes132A23852001766q99il04120041:12000
Starks silt loam, 0 to 2 percent slopes132A3995843540x9rzil04519971:12000
Starks silt loam, 0 to 2 percent slopes132A1474211590735hil05919661:20000
Starks silt loam, 2 to 6 percent slopes132B580211591735jil05919661:20000
Starks silt loam, 0 to 2 percent slopes132A133914158911jjbxil06320051:12000
Starks silt loam, 0 to 2 percent slopes132A13152633588v1fil09920061:12000
Starks silt loam, 0 to 2 percent slopes132A33641766435xt5il10119521:42240
Starks silt loam, 2 to 4 percent slopes132B5731766445xt6il10119521:42240
Starks silt loam, 0 to 2 percent slopes132A22301769165y2zil10519911:15840
Starks silt loam, 0 to 2 percent slopes132A1561913931227lqil11520071:12000
Starks silt loam, 0 to 2 percent slopes, frequently flooded3132A41724653588jril13919991:12000
Starks silt loam, 0 to 2 percent slopes132A42620895470fgil14319861:15840
Starks silt loam1322360178987607sil17319901:15840
Starks silt loam, 0 to 2 percent slopes132A223916011201qr31il18320061:12000
Starks silt loam, 0 to 2 percent slopes132A47917960860wtil18519621:20000
Starks silt loam, 2 to 4 percent slopes, eroded132B233217960960wvil18519621:20000
Starks silt loam, 0 to 2 percent slopes132A69718515666nsil19720021:12000
Starks-Crosby silt loams, 0 to 2 percent slopesStjA26916792202w0vxin01120031:12000
Starks silt loam, 0 to 2 percent slopesSteA12546792192w0vlin01120031:12000
Fincastle-Starks silt loams, 0 to 2 percent slopesFaA394551651622t4m8in01519871:15840
Fincastle-Starks silt loams, 1 to 3 percent slopesFbB80131651635jvvin01519871:15840
Starks silt loam, 0 to 2 percent slopesStA64751652402w0vlin01519871:15840
Starks silt loam, 0 to 2 percent slopesSrA8321624582w0vlin01719791:15840
Starks silt loam, 0 to 2 percent slopesSx72891623612w0vlin02319781:20000
Starks silt loam, 0 to 2 percent slopesSr8481624112w0vlin03119801:15840
Starks silt loam, 0 to 2 percent slopesSteA18642425062w0vlin04519991:12000
Fincastle-Starks silt loams, 0 to 2 percent slopesFdnA18212424022t4m8in04519991:12000
Starks silt loam, 0 to 2 percent slopesSx1932913322w0vlin06719671:20000
Starks-Crosby silt loams, 0 to 2 percent slopesSrA226311630682w0vxin10719841:15840
Starks silt loam, 0 to 2 percent slopesSlA219131630672w0vlin10719841:15840
Starks-Fincastle complex, 0 to 2 percent slopesSwA336531643155hzhin15719901:15840
Urban land-Starks-Fincastle complex, 0 to 2 percent slopesUsA60941643555j0sin15719901:15840
Starks silt loam, 0 to 2 percent slopesSx332913712w0vlin15919851:15840
Starks silt loamSo5861604735czkin16519771:20000
Starks silt loam, till substratum, 0 to 2 percent slopesSlA74951631695gsjin17119871:15840

Map of Series Extent

Approximate geographic distribution of the STARKS 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 .