Official Series Description


Lab Data Summary

Aggregate lab data for the COHOCTAH soil series. This aggregation is based on all pedons with a current taxon name of COHOCTAH, 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 COHOCTAH 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
111CJR79361979IN073036Cohoctah3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.9106667,-87.084275
111DMY78131978IN107013Cohoctah3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.1471639,-86.7957833
111DTI84271984IN157027Cohoctah3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.4150278,-86.7550417
98WH76011976IN181001Cohoctah3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8961528,-86.7131361
98FU80071980IN049007Cohoctah3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.05585,-86.3194583
n/a86IL1250361986IL125036Cohoctah2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the COHOCTAH 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 COHOCTAH 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 COHOCTAH 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 COHOCTAH 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 COHOCTAH 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 COHOCTAH 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 COHOCTAH 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 COHOCTAH, 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. IN-2010-09-02-01 | Pulaski County - 2003

    Typical pattern of soils and underlying material in the Williamstown-Metea-Riddles association (Soil Survey of Pulaski County, Indiana; 2003).

  2. IN-2010-09-02-09 | Pulaski County - 2003

    Typical pattern of soils and underlying material in the Cohoctah-Abscota association (Soil Survery of Pulaski County, Indiana; 2003).

Map Units

Map units containing COHOCTAH 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
Cohoctah loam, 0 to 2 percent slopes, occasionally flooded8166A2417186279820jd8il01120071:12000
Cohoctah loam, 0 to 2 percent slopes, occasionally flooded8166A87224486286ssil07320011:12000
Cohoctah loam, 0 to 2 percent slopes, occasionally flooded8166A11201926839103g1il10320041:12000
Cohoctah loam, undrained, 0 to 2 percent slopes, frequently flooded, long duration1166L26851777505yywil12519891:15840
Cohoctah loam, 0 to 2 percent slopes, occasionally flooded8166A3015793142vmb7il19520031:12000
Cohoctah loam, 0 to 1 percent slopes, occasionally flooded, very brief durationCmbAW1362008806r10in00520021:12000
Cohoctah loam, occasionally floodedCn11621651535jvjin01519871:15840
Cohoctah variant very fine sandy loam, frequently floodedCr8401651555jvlin01519871:15840
Cohoctah loam, gravelly substratum, occasionally floodedCp7961651545jvkin01519871:15840
Cohoctah fine sandy loam, occasionally floodedCo45371625645g50in04919841:15840
Cohoctah loam, 0 to 1 percent slopes, occasionally flooded, very brief durationCmbAW716527561sgtqin08119751:15840
Cohoctah sandy loamCk508327265494q9in09119791:15840
Waterford-Cohoctah loams, 0 to 2 percent slopes, frequently flooded, brief durationWciAH399624957052qnffin09919781:15840
Cohoctah loam, 0 to 1 percent slopes, frequently flooded, brief durationCmbAI30124512232n8pqin09919781:15840
Cohoctah loam, frequently floodedCk28331630085gmbin10719841:15840
Cohoctah-Abscota complex, 0 to 1 percent slopes, frequently flooded, brief durationCnzAI179418493266fkin13120011:12000
Cohoctah loam, 0 to 1 percent slopes, frequently flooded, brief durationCmbAI115718493166fjin13120011:12000
Cohoctah loam, 0 to 1 percent slopes, frequently flooded, brief durationCmbAI1109612368nk6tin14120011:12000
Cohoctah sandy loamCo11581601945cpkin15119791:20000
Cohoctah loam, gravelly substratum, occasionally floodedCp26341639075hkbin15719901:15840
Cohoctah fine sandy loam, gravelly substratum, rarely floodedCo7741639065hk9in15719901:15840
Cohoctah fine sandy loam, occasionally floodedCk22681618435fdrin18119791:20000
Cohoctah silt loam2967202124517428mi00519841:15840
Cohoctah silt loam, protected6517982124837439mi00519841:15840
Cohoctah, Ceresco, and Kerston soils, 0 to 3 percent slopes, frequently floodedCohaaA1798340445531b25mi01119641:20000
Cohoctah loamy fine sandCo87225078236839mi01119641:20000
Cohoctah loamy fine sand5031811865366839mi01719781:20000
Cohoctah fine sandy loam611220186547683nmi01719781:20000
Chesaning-Cohoctah complex, frequently flooded1061472507993688lmi01719781:20000
Cohoctah sandy loam29827918616767qdmi02119791:15840
Cohoctah-Abscota sandy loams2191818615867q3mi02119791:15840
Cohoctah-Urban land complex80100118621167rtmi02119791:15840
Cohoctah sandy loam8640418699368l1mi02319841:15840
Cohoctah loam, gravelly substratum, frequently flooded6425021887216bcsmi02519931:15840
Cohoctah loam39445318693268j2mi02719881:15840
Cohoctah loamCh526735036cgkmi03519771:15840
Cohoctah loamCh219718636867xwmi03719741:15840
Cohoctah fine sandy loam, frequently floodedCh709718622567s8mi04519741:15840
Cohoctah silt loamCo223418683968f2mi04919671:20000
Cohoctah loamCj3823942312lcd8mi04919671:20000
Cohoctah loamCo29621897686cgkmi05119661:15840
Cohoctah-Ceresco fine sandy loams, gravelly substratumCo162418700868ljmi05719751:12000
Cohoctah fine sandy loam, gravelly substratumCh115118700768lhmi05719751:12000
Chesaning-Cohoctah complex, frequently floodedCp202673581688lmi05719751:12000
Cohoctah silt loamCh2810186724689cmi06519771:15840
Cohoctah-Sloan loamsCp540718792869k6mi06719651:15840
Cohoctah-Sloan sandy loamsCr55918792969k7mi06719651:15840
Cohoctah fine sandy loam, frequently flooded174190186606685kmi07319831:15840
Cohoctah fine sandy loam, occasionally flooded71783186588684zmi07319831:15840
Cohoctah fine sandy loam, gravelly substratum1133082673528686fmi07319831:15840
Cohoctah fine sandy loam2235511887596bf0mi07519791:15840
Cohoctah loam71243318719668slmi08119841:15840
Urban land-Cohoctah complex63264418718368s5mi08119841:15840
Cohoctah loamCm17661920106fswmi08719661:15840
Cohoctah sandy loamCr192508398693lmi08719661:15840
Cohoctah silt loamCn1724094402lw6wmi08719661:15840
Cohoctah fine sandy loamCt1726736666bj6mi08719661:15840
Cohoctah-Ceresco complex, 0 to 2 percent slopes, frequently floodedCohacA152618752731b2bmi09319681:20000
Cohoctah silt loamCo124392352mw70mi09319681:20000
Cohoctah fine sandy loamCm2140187630697lmi09919671:20000
Cohoctah loamCn2725085196fswmi09919671:20000
Cohoctah fine sandy loam, gravelly substratumCh6986186633686fmi11119761:15840
Cohoctah fine sandy loam, frequently floodedCk522673540685kmi11119761:15840
Cohoctah-Ceresco fine sandy loams, gravelly substratumCn41267354268ljmi11119761:15840
Cohoctah loamy fine sandCg3525079716839mi11119761:15840
Cohoctah loamCf1726735396cgkmi11119761:15840
Chesaning-Cohoctah complex, frequently floodedCe42673538688lmi11119761:15840
Cohoctah fine sandy loam, frequently flooded10816325091676fd4mi11519801:15840
Cohoctah-Ceresco-Palms complex, 0 to 2 percent slopes, frequently floodedCohabA1863342221731gsxmi11719561:20000
Ceresco-Cohoctah complex, 0 to 2 percent slopes, frequently floodedCeracA598342221631b2cmi11719561:20000
Cohoctah fine sandy loam83258186509682fmi12319901:15840
Cohoctah-Fox association6820731888776bjtmi12519801:15840
Cohoctah fine sandy loam4914331888586bj6mi12519801:15840
Cohoctah silt loam107524389122mvwlmi12519801:15840
Cohoctah fine sandy loam, occasionally flooded675851890766br7mi12719921:15840
Cohoctah loamCm30751926546ggnmi13919671:15840
Chesaning-Cohoctah complex, frequently flooded774228186700688lmi14519911:15840
Chesaning-Cohoctah complex, rarely flooded963594186710688xmi14519911:15840
Cohoctah loam15551218626867tnmi14919801:15840
Cohoctah sandy loamCt542508263693lmi15119551:15840
Cohoctah loamCn108018778869dpmi15519671:12000
Cohoctah silt loamCo424243662mcrcmi15519671:12000
Cohoctah sandy loam556286187506693lmi15719841:15840
Cohoctah fine sandy loam1511222508153683nmi15719841:15840
Cohoctah loamy fine sand1506925081526839mi15719841:15840
Algansee-Cohoctah complex661125818634567x4mi15919841:15840
Cohoctah fine sandy loam, frequently floodedCc31781916156fd4mi16119741:20000
Cohoctah fine sandy loam, frequently floodedCc87530150386bk3mi16319741:12000
Cohoctah loam, 0 to 2 percent slopes, frequently flooded11634185436192gmwqmn09319961:20000
Cohoctah fine sandy loam, 0 to 2 percent slopes, occasionally flooded1197605436212gmxcmn09319961:20000
Cohoctah loam, 0 to 2 percent slopes, frequently flooded1163142536689gmwqmn14519801:15840
Cohoctah mucky very fine sandy loamCo175225183079sw7ny04320181:24000
Cohoctah fine sandy loam, frequently floodedCh3921690745ny0oh05119811:15840
Cohoctah fine sandy loamCh1001689765ntvoh06919681:15840
Cohoctah loamCh2261681385mytoh17119751:15840

Map of Series Extent

Approximate geographic distribution of the COHOCTAH 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 .