Official Series Description


Lab Data Summary

Aggregate lab data for the COLLINS soil series. This aggregation is based on all pedons with a current taxon name of COLLINS, 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 COLLINS 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
115BM05201032005MO201003Collins4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.1438637,-89.5806961
115BM05201042005MO201004Collins4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.145359,-89.5807724
115BM05201052005MO201005Collins4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.147049,-89.578476
120A68KY-107-00568KY-107-005Collins4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.2993,-87.5907833
13407KY-039-0012007KY039001Collins2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.9156528,-88.9804333
13407KY-039-0052007KY039005Collins2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.9436111,-88.8133333
13407KY-039-0072007KY039007Collins2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.9483333,-88.8477778
13408KY-039-0022008KY039002Collins3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.7758333,-88.8297222
13409KY-039-0012009KY039001Collins2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.8011111,-89.02
13409KY-105-0032009KY105003Collins2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.7555556,-89.0536111
13481P084281MS107008Collins6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.2861099,-89.8444443
13440A4938S1959TN047003Collins5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.1869431,-89.336113
13440A4939S1959TN047008Collins5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.2227783,-89.3358307
13440A4940S1959TN047009Collins5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.2411118,-89.3147202
13440A4941S1959TN047010Collins4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.3375015,-89.4008331
13440A4942S1959TN047011Collins5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.0099983,-89.3466644

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the COLLINS 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 COLLINS 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 COLLINS 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 COLLINS 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 COLLINS 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 COLLINS 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 COLLINS 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 COLLINS, 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. KY-2012-01-27-52 | Crittenden County - September 1988

    Relationship of soils to topography and underlying material in the Zanesville-Loring-Frondorf map unit (Soil Survey of Crittenden County, Kentucky; September 1988).

  2. KY-2012-01-27-53 | Crittenden County - September 1988

    Relationship of soils to topography and underlying material in the McGary-Belknap-Otwell map unit (Soil Survey of Crittenden County, Kentucky; September 1988).

  3. KY-2012-01-27-54 | Crittenden County - September 1988

    Relationship of soils to topography and underlying material in the Belknap-Collins-Waverly map unit (Soil Survey of Crittenden County, Kentucky; September 1988).

  4. KY-2012-01-31-02 | Henderson County - February 1967

    Parent material, position, and pattern of soils in the Uniontown-Dekoven-Henshaw association (Soil Survey of Henderson County, Kentucky; February 1967).

  5. MS-2010-09-08-02 | Holmes County -

    Typical pattern of soils and underlying material in the Collins-Morganfield-Bruno general soil map unit.

  6. MS-2012-02-06-12 | Tate County - March 1967

    Pattern of soils in the Calloway-Henry association (soils over thick loess) and the Collins-Falaya association (soils over alluvium) (Soil Survey of Tate County, Mississippi; March 1967).

  7. MS-2012-04-26-09 | De Soto County - September 1959

    Soil associations in De Soto County (Soil Survey of De Soto County, Mississippi; September 1959).

  8. MS-2012-04-27-01 | Quitman County - December 1958

    Soil associations, Quitman County, Miss. (Soil Survey of Quitman County, Mississippi; December 1958).

  9. MS-2012-04-27-07 | Tippah County - February 1966

    Distribution and pattern of major soils in Falaya-Urbo-Waverly association (Soil Survey of Tippah County, Mississippi; February 1966).

  10. MS-2012-04-27-09 | Tunica County - May 1956

    Soil association map of Tunica County, Miss (Soil Survey of Tunica County, Mississippi; May 1956).

  11. TN-2012-03-16-07 | Gibson County - September 1994

    Pattern of soils in the Routon-Grenada-Center and Falaya-Collins general soil map units (Soil Survey of Gibson County, TN; 1994).

  12. TN-2012-03-16-08 | Gibson County - September 1994

    Pattern of soils in the Loring-Memphis-Grenada general soil map unit (Soil Survey of Gibson County, TN; 1994).

  13. TN-2012-03-16-09 | Gibson County - September 1994

    Pattern of soils in the Providence-Lexington-Smithdale general soil map unit (Soil Survey of Gibson County, TN; 1994).

  14. TN-2012-03-16-10 | Gibson County - September 1994

    Pattern of soils in the Rosebloom-Arkabutla general soil map unit (Soil Survey of Gibson County, TN; 1994).

Map Units

Map units containing COLLINS 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
Collins silt loam, 0 to 1 percent slopes, occasionally flooded, brief duration20203365640522t23jar02119751:20000
Collins silt loamCo10295565298lz7far02519651:15840
Collins silt loam, 0 to 1 percent slopes, occasionally flooded, brief duration11222005641172t23jar03119761:20000
Collins silt loamCo6390564380ly8tar03719661:20000
Collins silt loam, 0 to 1 percent slopes, occasionally flooded, brief durationCo89065642672t23jar11119731:20000
Collins silt loamCo1110564438lybpar12319641:20000
Collins silt loam, 0 to 2 percent slopes, occasionally flooded, very brief durationCg5746541562t23mky07520021:12000
Collins silt loam, 0 to 2 percent slopes, occasionally flooded, very brief durationCn393855706232t23mky08319951:12000
Collins silt loam, frequently floodedCo10978570624m4s7ky08319951:12000
Collins-Iuka complex, occasionally floodedCu7111570625m4s8ky08319951:12000
Falaya-Collins complex, 0 to 2 percent slopes, occasionally floodedFa2389815973281qm4qky60219721:12000
Falaya-Collins complex, 0 to 2 percent slopes, frequently floodedFc300015973361qm4zky60219721:12000
Collins-Iuka complex, 0 to 4 percent slopes, rarely floodedCo87015973321qm4vky60219721:12000
Collins-Iuka complex, 0 to 2 percent slopes, occasionally floodedCu1489022322322dxthky61019681:12000
Collins-Iuka complex, 0 to 2 percent slopes, frequently floodedCi807422323332dxxrky61019681:12000
Collins silt loam, 0 to 2 percent slopes, frequently floodedCo45122323342dxxsky61019681:12000
Collins silt loam, 0 to 1 percent slopes, frequently flooded86117926076492r02fmo02319821:24000
Collins silt loam, 0 to 3 percent slopes, rarely flooded9060292026898572r03tmo06919771:24000
Collins silt loam, 0 to 1 percent slopes, rarely flooded9600143124977272pqqjmo06919771:24000
Collins silt loam, 0 to 1 percent slopes, frequently flooded8611732425715672r02fmo06919771:24000
Collins silt loam, 0 to 3 percent slopes9031615126898562q2fsmo06919771:24000
Collins silt loam, 0 to 1 percent slopes, occasionally flooded, brief duration9600018488940732t23jmo20719831:24000
Collins silt loam, 0 to 3 percent slopes9031652925035282q2fsmo20719831:24000
Collins silt loam, 0 to 1 percent slopes, frequently flooded8611726925715522r02fmo20719831:24000
Collins silt loamCo6785567403m1fbms00119661:15840
Collins silt loamCo3206567439m1ghms00519711:20000
Collins silt loam (oaklimeter)Co13064331828c494ms01319631:15840
Collins silt loam, local alluvium (oaklimeter)Cm2558331827c493ms01319631:15840
Collins silt loamCn17403567576m1lxms02119611:20000
Collins silt loam (adler)Cg33471567725m1rqms03319551:24000
Collins and Falaya silt loams, local alluvium phasesCl28816567728m1rtms03319551:24000
Vicksburg and Collins silt loams, local alluvium phasesVb4503567795m1tzms03319551:24000
Collins silty clay loam (adler)Ch1276567726m1rrms03319551:24000
Collins loamy sand, overwash phase (nugent)Cf1046567724m1rpms03319551:24000
Collins silty clay loam, shallow phase (adler)Ck542567727m1rsms03319551:24000
Collins silt loam, occasionally flooded111802567798m1v2ms03719921:20000
Collins silt loamCm12015567839m1wdms04319651:15840
Falaya-Collins associationFc9282567847m1wnms04319651:15840
Collins silt loam, local alluviumCn1334567840m1wfms04319651:15840
Collins silt loam, occasionally floodedCn3944417130611vhl1ms05119971:20000
Collins and Silverdale soils, frequently floodedCS440717130631vhl3ms05119971:20000
Collins silt loam, 0 to 2 percent slopesCo331884365217tzms05119971:20000
Collins silt loamCa9464568072m23xms06319761:20000
Collins silt loam, 0 to 2 percent slopes12984568127m25pms08319971:24000
Collins silt loam, 0 to 2 percent slopes, occasionally flooded2307568128m25qms08319971:24000
Collins silt loam (vicksburg)Co4587568146m269ms08519611:20000
Collins and Iuka soilsCs4139568147m26bms08519611:20000
Collins-Arkabutla-Falaya associationCR10839568264m2b3ms09319681:20000
Collins silt loam, 0 to 2 percent slopes, frequently flooded, brief durationCo46435682702t23kms09319681:20000
Collins-Arkabutla-Bruno associationCN4019568263m2b2ms09319681:20000
Collins silt loamCm19317333240c5rpms09719711:20000
Collins silt loam (occasionally flooded)Cm49109568309m2ckms10719611:24000
Collins silt loam, local alluvium (occasionally flooded)Co21982568310m2clms10719611:24000
Mixed alluvial land (bruno and Collins soils, frequently flooded)Mx14721568344m2dpms10719611:24000
Collins silt loamCo4744333639c65kms11319651:15840
Collins silt loam, local alluviumCl4710333638c65jms11319651:15840
Collins silt loam, 0 to 2 percent slopes, occasionally flooded, brief durationCh31285683692t23lms11919561:24000
Collins silty clay loam (arkabutla)Ck1800568370m2fjms11919561:24000
Collins soils and Waverly soils, local alluvium phasesCo1623568373m2fmms11919561:24000
Collins-Falaya silt loams, nearly level phases (collins, waverly)Cm272568371m2fkms11919561:24000
Collins-Falaya silt loams, gently sloping phases (collins, waverly)Cn222568372m2flms11919561:24000
Collins silt loamCn22200568510m2l1ms13519661:24000
Collins silt loam, clayey subsoil variantCo493568511m2l2ms13519661:24000
Collins silt loamCm30912568564m2msms13719641:15840
Collins silt loam, local alluvium, 0 to 2 percent slopes, occasionally flooded, brief durationCo181985685652t23nms13719641:15840
Collins silt loam (oaklimeter)Cn2453334178c6qyms13919631:15840
Collins silt loam, local alluvium (oaklimeter)Co517334179c6qzms13919631:15840
Collins silt loam (oaklimeter)Co614334305c6w1ms14719651:20000
Collins silt loam, local alluviumCm678568679m2rhms14919621:15840
Collins silt loamCi644568678m2rgms14919621:15840
Collins silt loam, rarely flooded67160571061m57bms15720061:24000
Collins silt loam, occasionally floodedCn20344334644c76zms16119751:20000
Collins silt loam, frequently floodedCo1487334645c770ms16119751:20000
Collins silt loam, 0 to 2 percent slopes, occasionally flooded, brief durationCo278883271692t23ltn01719801:15840
Collins silt loam, 0 to 2 percent slopes, occasionally flooded, brief durationCo2517531163672t23ltn03319851:24000
Collins silt loam, 0 to 2 percent slopes, frequently flooded, brief durationCl36485667732t23ktn04519631:15840
Collins silt loam, 0 to 2 percent slopes, occasionally flooded, brief durationCo168585669662t23ltn04719611:15840
Collins silt loam, local alluvium, 0 to 2 percent slopes, occasionally flooded, brief durationCu139765669672t23ntn04719611:15840
Collins fine sandy loamCf6809566964m0z5tn04719611:15840
Collins fine sandy loam, local alluviumCm5393566965m0z6tn04719611:15840
Collins silt loam, 0 to 2 percent slopes, occasionally flooded, brief durationCo379145670412t23ltn05319901:24000
Collins silt loam, 0 to 2 percent slopes, occasionally flooded, brief durationCo717431164262t23ltn07519901:24000
Hymon silt loam, local alluvium phase (Collins)He6577327750c01ltn07719551:20000
Hymon silt loam (Collins)Hd504327749c01ktn07719551:20000
Collins silt loam, 0 to 2 percent slopes, frequently flooded, brief durationCs258785671932t23ktn11319741:20000
Collins silt loam, 0 to 2 percent slopes, occasionally flooded, brief durationCl601931164242t23ltn13119661:15840
Collins silt loam, 0 to 2 percent slopes, occasionally flooded, brief durationCo36815672842t23ltn15719661:15840
Collins silt loam, 0 to 2 percent slopes, occasionally flooded, brief durationCo284415673682t23ltn18319861:24000
Collins silt loam, rarely floodedCn4674567367m1d5tn18319861:24000

Map of Series Extent

Approximate geographic distribution of the COLLINS 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 .