Official Series Description


Lab Data Summary

Aggregate lab data for the LYNN HAVEN soil series. This aggregation is based on all pedons with a current taxon name of LYNN HAVEN, 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 LYNN HAVEN 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
152A89P051589FL067004Lynn Haven6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.0511112,-83.3080521

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the LYNN HAVEN 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 LYNN HAVEN 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 LYNN HAVEN 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 LYNN HAVEN 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 LYNN HAVEN 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 LYNN HAVEN series and competing. 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 LYNN HAVEN 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.

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Soil series sharing subgroup-level classification with LYNN HAVEN, 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. FL-2011-05-31-09 | City of Jacksonville, Duval County - 1978

    Typical pattern of soils and parent material in an area of the Leon-Hurricane/Ridgewood-Ortega general soil map unit. This map unit is dominantly used for urban development (Soil Survey of City of Jacksonville, Duval County, Florida; 1978).

  2. FL-2011-05-31-10 | City of Jacksonville, Duval County - 1978

    Typical pattern of soils and parent material in an area of the Leon-Boulogne-Evergreen/Wesconnett general soil map unit. Soils of this map unit are dominantly used for the production of pine trees. In the eastern part of the county, many areas are used for urban development (Soil Survey of City of Jacksonville, Duval County, Florida; 1978).

Map Units

Map units containing LYNN HAVEN 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
Lynn Haven fine sand5932901328444g79fl01919861:24000
Wesconnett and Lynn Haven soils, frequently ponded, 0 to 1 percent slopes63150814211382y51nfl02919981:24000
Lynn Haven fine sand, 0 to 2 percent slopes3516730738847sstsfl03119961:24000
Goldhead, Wet, and Lynn Haven soils, 2 to 5 percent slopes80820738892ssw7fl03119961:24000
Lynn Haven sand20741014770721ll0hfl03719901:20000
Lynn Haven and Allanton mucky fine sands, depressional813295321821bswbfl04119891:20000
Lynn Haven fine sand20347814727411lfhsfl04519971:24000
Wesconnett and Lynn Haven soils, frequently ponded, 0 to 1 percent slopes15325008865712y51nfl06719931:24000
Torhunta-Lynn Haven-Croatan complex, frequently flooded4723965322736bttvfl07720041:24000
Lynn Haven sand451380322734bttsfl07720041:24000
Lynn Haven-Wesconnett-Leon complex, depressional188851329044g97fl08919891:15840
Chipley-Lynn Haven, depressional-Boulogne complex, 0 to 3 percent slopes14647014252081jv1gfl12319981:24000
Lynn Haven, Allanton, and Kingsferry soils, ponded, 0 to 1 percent slopesLYA139024083632lv34ga29920081:24000
Lynn Haven fine sand, 0 to 2 percent slopesLvA3290526867712rz8rga61120121:24000
Lynn Haven, Allanton and Kingsferry soils, ponded, 0 to 1 percent slopesLYA3212526867932rz9gga61120121:24000
Lynn Haven sandLQ172512538346gmga61319691:20000
Lynn Haven and Torhunta soilsLy477801155003w5tnc01719831:24000
Lynn Haven sandLy2603811394w7b0nc04119821:24000
Torhunta and Lynn Haven soilsTR24518811149w723nc05119811:24000
Torhunta and Lynn Haven soilsTR1950811305w774nc09319811:24000
Lynn Haven fine sandLy54411160463wrfnc12919741:15840
Lynn Haven sandLy82811431w7c6nc14319821:24000
Lynn Haven sandLy209711150603vqmnc16319821:24000
Rosedhu fine sandRo132991324344ft2sc01319751:20000
Lynn Haven fine sand4213971322774fn0sc02919801:20000
Lynn Haven sandLy14001297604c0tsc03319761:20000
Lynn Haven fine sandLy10001298144c2ksc03519851:20000
Lynn Haven sandLz4461299684c7jsc04119691:20000
Lynn Haven sand507980639591pgjzsc04319801:20000
Lynn Haven sandLy225381301554cfksc05119831:20000
Lynn Haven fine sandLy9471325584fy2sc05319751:20000
Lynn Haven loamy sandLy23851305274ctksc06319721:20000
Lynn Haven sandLy38501305754cw3sc06719751:20000
Lynn Haven fine sandLy4751315314dvysc08919851:20000
St. Johns fine sandSa112261382994mx8sc69019671:24000

Map of Series Extent

Approximate geographic distribution of the LYNN HAVEN 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 .