Official Series Description


Lab Data Summary

Aggregate lab data for the FORESTDALE soil series. This aggregation is based on all pedons with a current taxon name of FORESTDALE, 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 FORESTDALE were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
131AM91143021991MO143002Forestdale4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.5373878,-89.5743332
131AM98223361998MO223101Forestdale4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.9990616,-90.1991882
131AM99017341999MO017050Forestdale4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.0462456,-90.0830307
131AM99017631999MO017071Forestdale4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.1327286,-89.9902878
131AM99017521999MO017073Forestdale4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.1676636,-89.9048004
131AM99017731999MO017100Forestdale4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.1462517,-89.925087
131AM03023122003MO023012Forestdale4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.5936699,-90.344223
131AM03023162003MO023016Forestdale4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.5956993,-90.3407669
131AM03155072003MO155009Forestdale4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.3862915,-89.6457748
131AM04143022004MO143003Forestdale4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.7046776,-89.5063248
131AM05207042005MO207004FORESTDALE4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.7833333,-90.1
131A10N0428S09MS133022Forestdale7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.3431389,-90.6213056
131A40A4971S1961TN045014Forestdale6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.1308327,-89.4761124
131A40A4972S1961TN045015Forestdale5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.1238899,-89.4616699
131A10N0426S2009MS135021Forestdale7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.0489722,-90.2761667
13440A1331S1972LA123005Forestdale2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.7605553,-91.5811081
13440A1332S1972LA123006Forestdale2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.7065544,-91.4034576

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the FORESTDALE 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.

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the FORESTDALE series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the FORESTDALE series and siblings. 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 FORESTDALE 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 .

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.

Competing Series

Soil series competing with FORESTDALE share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the FORESTDALE 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 FORESTDALE 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 FORESTDALE, 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. LA-2012-02-01-03 | Richland Parish - September 1993

    Relationship of soils, landscape, and parent material in Richland Parish (Soil Survey of Richland Parish, Louisiana; September 1993).

  2. LA-2012-04-27-03 | Franklin Parish - August 1981

    Soils, parent material, and landscape position from east to west in the parish (Soil Survey of Franklin Parish, Louisiana; August 1981).

  3. MS-2012-02-06-01 | Carroll County - May 1990

    Pattern of soils and underlying material in the Dundee-Dubbs-Sharkey general soil map unit (Soil Survey of Carroll County, Mississippi; May 1990).

  4. MS-2012-04-26-10 | Humphreys County - September 1959

    Northwest-southeast cross section showing relation of soils and topography in Humphreys County, Miss (Soil Survey of Humphreys County, Mississippi; September 1959).

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

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

  6. MS-2012-04-27-03 | Sunflower County - February 1959

    East-west cross section, 2 miles south of Doddsville, showing relation of soils to topography (Soil Survey of Sunflower County, Mississippi; February 1959).

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

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

  8. MS-2012-04-27-10 | Bolivar County - December 1958

    Soil associations in Bolivar County: 1. Alluvial soils; 2. Commerce-Robinsonville-Crevasse; 3. Forestdale-Dundee-Bosket; 4. Brittain-Pearson-Dexter; 5. Dowling-Alligator-Sharkey (Soil Survey of Bolivar County, Mississippi; December 1958).

Map Units

Map units containing FORESTDALE 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
Forestdale fine sandy loamFo3819329661c217al06320131:
Forestdale silty clay loam, 0 to 1 percent slopes, frequently flooded7A3363579302mft5ar00119951:24000
Forestdale silty clay loamFo23030564172ly23ar03519701:20000
Forestdale silty clay loam, 0 to 1 percent slopes, frequently flooded16A23730577958mddtar05519951:24000
Forestdale silty clay loam, 0 to 1 percent slopes15A3807577957mddsar05519951:24000
Forestdale silt loam, frequently flooded247590565744lzptar06319801:20000
Amagon and Forestdale silt loamsAf36290565793lzrdar06719711:20000
Forestdale silty clay loamFo11425565808lzrwar06719711:20000
Forestdale silty clay loamFo2790564346ly7qar09319671:20000
Forestdale-Routon complexFr1520564347ly7rar09319671:20000
Forestdale silt loamFe1340564345ly7par09319671:20000
Forestdale silty clay loam, 0 to 1 percent slopes, frequently floodedFdA6580749405t4tcar14719951:24000
Forestdale silty clay loam, occasionally floodedFe55917256441vxnyla02119851:24000
Forestdale silty clay loam, 0 to 1 percent slopes, occasionally floodedFo401717223912v185la02519831:24000
Forestdale silty clay loamFd57617223901vt8zla02519831:24000
Forestdale silty clay loam, 0 to 1 percent slope, occasionally flooded, upland phaseFs1325317111002wf6hla04119791:24000
Forestdale silty clay loam, 0 to 1 percent slopes, occasionally floodedFh971316001682v185la05919861:24000
Forestdale silty clay loamFf521216001671qq39la05919861:24000
Idee-Forestdale complexId7832569804m3xsla06719811:24000
Forestdale silty clay loam, 0 to 1 percent slopes, rarely flooded, upland phaseFo29635697872v187la06719811:24000
Forestdale silty clay loam, 0 to 1 percent slopes, rarely flooded, upland phaseFr1836917147752v187la08319881:24000
Forestdale silty clay loam, 0 to 1 percent slope, occasionally flooded, upland phaseFt1085717147762wf6hla08319881:24000
Forestdale silty clay loam, 0 to 1 percent slopes, rarely flooded, upland phase15105955703722v187la12319751:24000
Forestdale silty clay loam, 0 to 1 percent slopes, occasionally flooded86004271825007952pzygmo01720041:24000
Forestdale silty clay loam, 0 to 1 percent slopes, rarely flooded820469862689834z1hnmo01720041:24000
Forestdale silty clay loam, 0 to 1 percent slopes, frequently ponded820023924977722pqq0mo01720041:24000
Forestdale silty clay loam, 0 to 1 percent slopes, rarely flooded82046852571694z1hnmo03119781:24000
Forestdale silty clay loam, 0 to 1 percent slopes, occasionally flooded860047725716982pzygmo03119781:24000
Forestdale silty clay loam, 0 to 1 percent slopes, rarely flooded82046832689863z1hnmo13319781:24000
Forestdale silt loam, 0 to 1 percent slopes, rarely flooded820456478895164z1h8mo14319741:24000
Forestdale silty clay loam, 0 to 1 percent slopes, rarely flooded820462288895176z1hnmo14319741:24000
Forestdale silty clay loam, 0 to 1 percent slopes, occasionally flooded860048526898862pzygmo14319741:24000
Forestdale silty clay loam, 0 to 1 percent slopes, occasionally flooded86004339925007942pzygmo20719831:24000
Forestdale silty clay loam, 0 to 1 percent slopes, frequently ponded82002258924977742pqq0mo20719831:24000
Forestdale silty clay loam, 0 to 1 percent slopes, rarely flooded820462912689925z1hnmo20719831:24000
Forestdale silty clay loam, 0 to 1 percent slopes, frequently ponded82002325724977732pqq0mo22320041:24000
Forestdale silty clay loam, 0 to 3 percent slopesFe26068567502m1jjms01119561:20000
Forestdale silt loam, 0 to 3 percent slopesFa21911567498m1jdms01119561:20000
Forestdale silty clay, 0 to 3 percent slopesFc11713567500m1jgms01119561:20000
Forestdale soils, 0 to 3 percent slopesFh1314567504m1jlms01119561:20000
Forestdale silty clay, 3 to 7 percent slopesFd450567501m1jhms01119561:20000
Forestdale silty clay loam, 3 to 7 percent slopesFg424567503m1jkms01119561:20000
Forestdale silt loam, 3 to 7 percent slopesFb73567499m1jfms01119561:20000
Forestdale silt loam241459567534m1kkms01519851:20000
Forestdale silty clay loam, 0.5 to 3 percent slopesFh16677567652m1pcms02719561:24000
Forestdale silty clay, 0.5 to 3 percent slopesFd13299567649m1p8ms02719561:24000
Forestdale silt loam, 0.5 to 3 percent slopesFb3985567647m1p6ms02719561:24000
Forestdale silty clay, 0 to 0.5 percent slopesFc1591567648m1p7ms02719561:24000
Forestdale silty clay loam, 0 to 0.5 percent slopesFg703567651m1pbms02719561:24000
Forestdale silty clay, 3 to 7 percent slopesFe483567650m1p9ms02719561:24000
Forestdale silt loam, 0 to 0.5 percent slopesFa317567646m1p5ms02719561:24000
Forestdale silty clay loam, 3 to 7 percent slopesFk148567653m1pdms02719561:24000
Forestdale silty clay loam, nearly level phaseFd1525567747m1sfms03319551:24000
Forestdale silty clay loamFo357567850m1wrms04319651:15840
Forestdale silt loam, 0 to 2 percent slopesFm29757568026m22fms05319561:20000
Forestdale silty clay loam, 0.5 to 2 percent slopesFd22555568021m228ms05319561:20000
Alligator, Dowling, and Forestdale soils, frequently flooded (alligator, alligator, forestdale)An1880426934322rv64ms05319561:20000
Forestdale-Brittain silt loams (forestdale, amagon)Fu5765568033m22nms05319561:20000
Forestdale very fine sandy loam, 0 to 2 percent slopesFs5272568031m22lms05319561:20000
Forestdale silty clay, 0 to 2 percent slopesFa5099568018m225ms05319561:20000
Forestdale silty clay loam, 0.5 to 2 percent slopes, frequently floodedFe256126934402rv69ms05319561:20000
Forestdale silt loam, 2 to 5 percent slopesFp1937568029m22jms05319561:20000
Forestdale silty clay loam, 2 to 5 percent slopesFh1720568024m22cms05319561:20000
Forestdale silt loam, 0 to 2 percent slopes, moderately shallow phaseFo1303568028m22hms05319561:20000
Forestdale silty clay loam, 2 to 5 percent slopes, frequently floodedFk116226934432rv67ms05319561:20000
Forestdale silty clay loam, 0.5 to 2 percent slopes, shallow phaseFg1039568023m22bms05319561:20000
Forestdale silty clay loam, 0 to 0.5 percent slopesFc976568020m227ms05319561:20000
Forestdale silt loam, 0 to 2 percent slopes, frequently floodedFn80026934412rv68ms05319561:20000
Forestdale very fine sandy loam, 2 to 5 percent slopesFt504568032m22mms05319561:20000
Forestdale silty clay, 2 to 5 percent slopesFb492568019m226ms05319561:20000
Forestdale silt loam, moderately eroded, 5 to 8 percent slopesFr179568030m22kms05319561:20000
Forestdale silty clay loam, 0 to 2 percent slopesFd341568052m238ms05519601:20000
Forestdale silty clay loam, nearly level phaseFe17117568390m2g5ms11919561:24000
Forestdale silt loam, nearly level phaseFc9686568388m2g3ms11919561:24000
Forestdale silty clay loam, gently sloping phaseFg1342568391m2g6ms11919561:24000
Forestdale silt loam, gently sloping phaseFd199568389m2g4ms11919561:24000
Forestdale silty clay loam, 0 to 2 percent slopesFd9030568430m2hgms12519601:20000
Forestdale silt loam, 0 to 2 percent slopesFa3980568428m2hdms12519601:20000
Forestdale silty clay loam, 2 to 5 percent slopesFe754568431m2hhms12519601:20000
Forestdale silt loam, 2 to 5 percent slopesFc317568429m2hfms12519601:20000
Forestdale silt loam, 0.5 to 3 percent slopesFb57568568475m2jxms13319561:20000
Forestdale silty clay loam, 0.5 to 3 percent slopesFm41368568482m2k4ms13319561:20000
Forestdale silty clay, 0.5 to 3 percent slopesFg8180568479m2k1ms13319561:20000
Forestdale silty clay loam, 3 to 7 percent slopesFn2244568483m2k5ms13319561:20000
Forestdale very fine sandy loam, 0.5 to 3 percent slopesFr2076568486m2k8ms13319561:20000
Forestdale silt loam, 3 to 7 percent slopesFc1821568476m2jyms13319561:20000
Forestdale silt loam, 0 to 0.5 percent slopesFa1286568474m2jwms13319561:20000
Forestdale silty clay, 3 to 7 percent slopesFh1144568480m2k2ms13319561:20000
Forestdale silty clay loam, 0 to 0.5 percent slopesFk676568481m2k3ms13319561:20000
Forestdale silty clay loam, 7 to 10 percent slopesFo248568484m2k6ms13319561:20000
Forestdale very fine sandy loam, 3 to 7 percent slopesFs180568487m2k9ms13319561:20000
Forestdale silt loam, 7 to 10 percent slopesFd153568477m2jzms13319561:20000
Forestdale silty clay, 0 to 0.5 percent slopesFe97568478m2k0ms13319561:20000
Forestdale very fine sandy loam, 0 to 0.5 percent slopesFp6568485m2k7ms13319561:20000
Forestdale silty clay loam, 0 to 3 percent slopesFr18301568524m2lhms13519661:24000
Forestdale silt loam, depressionalFo1474568523m2lgms13519661:24000
Forestdale silty clay loam, 0 to 2 percent slopesFd18398568761m2v4ms15119591:20000
Forestdale silty clay, 0 to 2 percent slopesFb15387568759m2v2ms15119591:20000
Forestdale silt loam, 0 to 2 percent slopesFa6031568758m2v1ms15119591:20000
Forestdale silty clay, 2 to 5 percent slopesFc923568760m2v3ms15119591:20000
Forestdale silty clay loam, 2 to 5 percent slopesFe650568762m2v5ms15119591:20000
Sharkey and Forestdale soils, frequently floodedSf3822126934732rv5kms16319691:20000
Forestdale silty clay loamFr17949568792m2w4ms16319691:20000
Forestdale silt loamFo976568791m2w3ms16319691:20000
Forestdale silt loamFd7795566785m0sdtn04519631:15840
Forestdale-Crevasse complexFo4454566786m0sftn04519631:15840
Forestdale silt loamFo1226527983kqdqtn12519721:15840
Forestdale silty clay loamFe245567245m187tn13119661:15840
Forestdale silt loamFd216567244m186tn13119661:15840
Forestdale silt loam3717291188963zqcva04119741:15840
Forestdale fine sandy loam1211691189873zt9va07519761:15840
Forestdale loam, frequently flooded3016901191033zy1va08519761:15840
Forestdale loam293901191023zy0va08519761:15840
Forestdale silt loamFo2411192344028va08719731:15840
Forestdale silt loamFo225119367406kva10919721:15840
Forestdale loam725911947540b1va11119791:20000
Forestdale silty clay loam124000120179411rva14519841:15840
Forestdale silt loamFo16712070541lqva63119731:15840

Map of Series Extent

Approximate geographic distribution of the FORESTDALE 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 .