Official Series Description


Lab Data Summary

Aggregate lab data for the JOHNSTON soil series. This aggregation is based on all pedons with a current taxon name of JOHNSTON, 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 JOHNSTON 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
133A08N0249S08SC061002Johnston4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.9824982,-80.1816635
133A08N0250S08SC085001Johnston6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.9602776,-80.2277756
133A08N0251S08SC085002Johnston5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.9597206,-80.2202759
133A08N0252S08SC085003Johnston6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.980278,-80.223053
133A08N0253S08SC085004Johnston4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.9813881,-80.2197189
133AS89SC017-15S1993SC017014Johnston3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.5688868,-80.6679973
133AS92SC069-39S1995SC069023Johnston3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.3680549,-79.5952365
153A08N0256S08SC085007Johnston6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.9097214,-80.1761093
153A08N0259S08SC085010Johnston5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.8805542,-80.1463852

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the JOHNSTON 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 JOHNSTON 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 JOHNSTON 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 JOHNSTON 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 JOHNSTON 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 JOHNSTON 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 JOHNSTON 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 JOHNSTON, 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. NC-2012-02-07-40 | Sampson County - August 1985

    Pattern of soils in map units 1, 2, and 5 north of Clinton (Soil Survey of Sampson County, North Carolina; August 1985).

Map Units

Map units containing JOHNSTON 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
Wet loamy alluvial landWm41030328224c0jwal00319611:20000
Johnston, Bibb and Pamlico soils, 0 to 1 percent slopes, frequently floodedJBA3622229950612x5qyal09720181:24000
Johnston, Pamlico and Dorovan soils, 0 to 1 percent slopes, frequently floodedJPA1586029950212x5q8al09720181:24000
Johnston, Bibb and Smithton soils, 0 to 3 percent slopes, frequently floodedJOA1159129950622x5qzal09720181:24000
Dorovan and Johnston soils, 0 to 1 percent slopes, frequently floodedDJA784429950252x5s1al09720181:24000
Bibb, Johnston and Kinston soils, 0 to 1 percent slopes, frequently floodedBJK325029949662x5rkal09720181:24000
Bibb, Johnston and Kinston soils, 0 to 1 percent slopes, frequently floodedBJK7488726420572x5rkal12920131:24000
Kinston, Johnston, and Bibb soils, frequently flooded434470014447251khc1fl09119891:20000
Kinston-Johnston-Bibb complex, frequently flooded1538970323984bw43fl13119851:20000
Johnston loamJo30275324842bx0sga18519751:20000
Kinston and Johnston soils, 0 to 2 percent slopes, frequently floodedKJA2311524083572wwt9ga29920081:24000
Johnston and Rains (Kinston) soilsJd43780125137466pga60119691:20000
Kinston and Johnston soils, 0 to 2 percent slopes, frequently floodedKJ992901251742wwt9ga60219831:20000
Johnston-Osier-Bibb associationJob3188612535046fkga60919671:20000
Osier-Johnston-Bibb associationOjb883512535546fqga60919671:20000
Kinston and Johnston soils, 0 to 2 percent slopes, frequently floodedKJA6024526867672wwt9ga61120121:24000
Johnston loamJe170512537946ghga61319691:20000
Kinston and Johnston soils, 0 to 2 percent slopes, frequently floodedKJA4961526868052wwt9ga62620131:24000
Johnston soilsJo3760326001by75ga64319741:20000
Johnston and Bibb soilsJB2173512580846xbga64419801:20000
Johnston loamJo907332001c4gqms02319631:15840
Swamp (johnston loam)Sw4935332197c4p1ms03119621:15840
Dorovan-Johnston associationDh32916332260c4r2ms03919671:20000
Bibb, Johnston and Kinston soils, 0 to 1 percent slopes, frequently floodedBJK1395726421642x5rkms04120121:24000
Dorovan and Johnston soils, 0 to 1 percent slopes, frequently floodedDJA350126421782x5s1ms04120121:24000
Croatan and Johnston soils, 0 to 2 percent slopes, frequently flooded8839918332606c537ms05919971:24000
Johnston-Croatan complex, frequently floodedJt2421333125c5mzms09119831:20000
Johnston mucky loam, occasionally floodedJo913333264c5sgms09919791:20000
Johnston loam (0 to 2 percent slopes)Ja1404333321c5v9ms10119571:20000
Johnston and Croatan soils, frequently flooded135502334085c6myms13119971:24000
Johnston sandy loam, 0 to 2 percent slopes, frequently floodedJoA23741145263v5dnc00719991:24000
Bibb and Johnston loams, frequently floodedBB196301113913qx8nc01519841:24000
Johnston mucky loamJO174681154933w5lnc01719831:24000
Johnston loam, frequently floodedJs276331156493wbmnc04719861:24000
Johnston loamJT26855811107w70rnc05119811:24000
Bibb sandy loam, 0 to 1 percent slopes, frequently floodedBbA25445186594720mnvnc06119551:24000
Johnston and Pamlico soils, 0 to 1 percent slopes, frequently floodedJpA2624186596820mpjnc06119551:24000
Bibb soilsBB156611015483132pjnc06519761:20000
Johnston soilsJS24491015703132xmnc06519761:20000
Bibb loam, frequently floodedBB71961127963sclnc07919781:24000
Johnston loam, frequently floodedJS36341128033sctnc07919781:24000
Bibb soils, frequently floodedBb255461130843snwnc08519841:24000
Bibb soilsBB106681131503sr0nc09119811:24000
Johnston loamJT19280811283w76fnc09319811:24000
Bibb sandy loam, 0 to 2 percent slopes, frequently floodedBb287491135193t3xnc10119861:24000
Johnston soilsJS90051160003wpync10719731:20000
Bibb soils, frequently floodedBB85901159923wppnc10719731:20000
Bibb loam, frequently floodedBb227951111193qmhnc11719851:24000
Johnston muck, 0 to 2 percent slopes, frequently floodedJoA48022335882dz77nc12320071:24000
Bibb loam, 0 to 2 percent slopes, frequently floodedBb95821108923qd5nc12719841:24000
Johnston soilsJO49071160383wr5nc12919741:15840
Bibb complexBb247831143133tyjnc14719691:15840
Swamp (Johnston)Sw55511143453tzknc14719691:15840
Johnston mucky loam, 0 to 2 percent slopes, frequently floodedJmA1185314022361j24fnc15319961:24000
Johnston soilsJT757211147683vf6nc15519721:20000
Bibb soilsBB240801147583vdwnc15519721:20000
Bibb and Johnston soils, frequently floodedBH427941150413vq0nc16319821:24000
Johnston mucky loamJT220791150533vqdnc16319821:24000
Johnston soils, 0 to 2 percent slopes, frequently floodedJmA1294514086061j8rxnc16520061:12000
Pamlico and Johnston soils, 0 to 1 percent slopes, frequently floodedPcA801314146211jh0ync16520061:12000
Bibb soils, 0 to 2 percent slopes, frequently floodedBaA243614086051j8rwnc16520061:12000
Bibb sandy loamBb188091162293wybnc19119681:20000
Johnston loamJs126981162383wymnc19119681:20000
Bibb loam, 0 to 2 percent slopes, frequently floodedBb210141164243x4mnc19519801:24000
Johnston sandy loam, 0 to 2 percent slopes, frequently floodedJsA63851381164mqcsc00919971:24000
Johnston fine sandy loam, frequently floodedJo63341323284fpnsc01719931:24000
Johnston sandy loam, frequently floodedJo316141320204fcqsc02519891:20000
Portsmouth-Johnston associationPT111671322374flqsc02719721:20000
Johnston soilsJS91511322274fldsc02719721:20000
Johnston sandy loam, 0 to 2 percent slopes,frequently floodedJoA20763619093ns6rsc03119981:24000
Johnston-Rutlege association, frequently floodedJR185401297514c0jsc03319761:20000
Wehadkee and Johnston soils, frequently floodedWn316471299934c8bsc04119691:20000
Johnston loam3413850639587pgjvsc04319801:20000
Johnston loamJo511251301504cfdsc05119831:20000
Johnston loamJo5823943482lcj1sc05719671:20000
Johnston muck, 0 to 2 percent slopes, frequently floodedJoA1719416065711qxrwsc06120051:24000
Johnston-Mouzon complex, 0 to 2 percent slopes, frequently floodedJzA184216065731qxrysc06120051:24000
Johnston soilsJO178411305194ct9sc06319721:20000
Johnston association, frequently floodedJN148001305694cvxsc06719751:20000
Johnston mucky loam, frequently floodedJo18791306384cy4sc06919951:24000
Johnston sandy loamJs342491308904d68sc07519851:20000
Johnston loamJo180471311054df6sc07919761:20000
Johnston mucky sandy loam, 0 to 2 percent slopes, frequently floodedJnA2291024859192pfsysc08519691:20000
Johnston mucky sandy loam, 0 to 2 percent slopes, pondedJoA514424859212pft0sc08519691:20000
Johnston sandy loam, frequently floodedJs37041315274dvtsc08919851:20000
Johnston loamJo167321302054ch5sc61019851:20000
Johnston mucky loamJo249981317564f36sc61519811:20000
Johnston soils, frequently floodedJO18908115148817n6ssc66519731:24000
Johnston mucky loam, 0 to 2 percent slopes, frequently flooded16A589011966640j6va12719851:15840
Johnston complex17591712080741q0va69519811:15840
Johnston silt loam, 0 to 2 percent slopes, frequently flooded1272712241243csva71519951:12000
Johnston mucky loam, 0 to 3 percent slopes, frequently flooded21A2881400964ps7va76020041:24000

Map of Series Extent

Approximate geographic distribution of the JOHNSTON 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 .