Official Series Description


Lab Data Summary

Aggregate lab data for the BOONTON soil series. This aggregation is based on all pedons with a current taxon name of BOONTON, 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 BOONTON 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
144A01N03272000NJ013001Boonton7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7547874,-74.2882462
149B00P0503S1999NY085029Boonton7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.529583,-74.2216644
149B09N0887S2009NY085001Boonton7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5333366,-74.1764908

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BOONTON 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 BOONTON 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 BOONTON 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 BOONTON 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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Competing Series

Soil series competing with BOONTON 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 BOONTON 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 BOONTON 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 BOONTON, 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

No block diagrams are available.

Map Units

Map units containing BOONTON 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
Boonton-Urban land complex, 8 to 15 percent slopesBouC750214443471kgyvnj00319861:24000
Boonton-Urban land complex, 0 to 8 percent slopesBouB464314443451kgysnj00319861:24000
Boonton-Urban land complex, 15 to 25 percent slopesBouD440714443481kgywnj00319861:24000
Boonton moderately well drained gravelly loam, 8 to 15 percent slopesBohC135714443371kgyjnj00319861:24000
Boonton moderately well drained-Rock outcrop complex, 25 to 45 percent slopesBorE116314443441kgyrnj00319861:24000
Boonton moderately well drained-Rock outcrop complex, 8 to 15 percent slopesBorC95514443421kgypnj00319861:24000
Boonton moderately well drained gravelly loam, 3 to 8 percent slopesBohB89814443351kgygnj00319861:24000
Boonton moderately well drained-Rock outcrop complex, 15 to 25 percent slopesBorD58914443431kgyqnj00319861:24000
Boonton-Urban land complex, 25 to 45 percent slopesBouE57914443491kgyxnj00319861:24000
Boonton moderately well drained-Rock outcrop complex, 3 to 8 percent slopesBorB55714443411kgynnj00319861:24000
Boonton moderately well drained gravelly loam, 8 to 15 percent slopes, very stonyBohCb50414443381kgyknj00319861:24000
Boonton moderately well drained gravelly loam, 15 to 25 percent slopesBohD50214443391kgylnj00319861:24000
Boonton moderately well drained gravelly loam, 25 to 45 percent slopesBohE49614443401kgymnj00319861:24000
Boonton moderately well drained gravelly loam, 15 to 25 percent slopes, very stonyBohDb31914443461kgytnj00319861:24000
Boonton moderately well drained gravelly loam, 0 to 8 percent slopes, very stonyBohBb277298629b0r6nj00319861:24000
Urban land, Boonton substratum - Boonton complex, red sandstone lowland, 0 to 8 percent slopesUSBOOB11372813350w9c3nj01320031:12000
Boonton - Urban land, Boonton substratum complex, 0 to 8 percent slopesBouB7631298946b12fnj01320031:12000
Boonton - Urban land, Boonton substratum complex, red sandstone lowland, 0 to 8 percent slopesBowrB6715812704w8p8nj01320031:12000
Boonton loam, 0 to 8 percent slopes, extremely stonyBogBc2484298941b128nj01320031:12000
Boonton - Urban land, Boonton substratum complex, terminal moraine, 0 to 8 percent slopesBowtB1930812695w8nznj01320031:12000
Urban land, Boonton substratum - Boonton complex, red sandstone lowland, 8 to 15 percent slopesUSBOOC1906813351w9c4nj01320031:12000
Boonton - Urban land, Boonton substratum complex, 8 to 15 percent slopesBouC1904298945b12dnj01320031:12000
Boonton loam, 8 to 15 percent slopes, extremely stonyBogCc1683298933b120nj01320031:12000
Boonton - Urban land, Boonton substratum complex, red sandstone lowland, 8 to 15 percent slopesBowrC1084812705w8p9nj01320031:12000
Boonton loam, 15 to 35 percent slopes, extremely stonyBogDc1002298942b129nj01320031:12000
Boonton silt loam, red sandstone lowland, 3 to 8 percent slopesBooB392682809qxj3nj01320031:12000
Boonton - Udorthents, Boonton substratum complex, red sandstone lowland, 0 to 8 percent slopesBotB387812702w8p6nj01320031:12000
Urban land, Boonton substratum - Boonton complex, 0 to 8 percent slopesUSBONB350813348w9c1nj01320031:12000
Boonton - Urban land, Boonton substratum complex, terminal moraine, 8 to 15 percent slopesBowtC337812696w8p0nj01320031:12000
Boonton sandy loam, terminal moraine, 8 to 15 percent slopes, extremely stonyBoeCc179682381qx29nj01320031:12000
Boonton silt loam, red sandstone lowland, 8 to 15 percent slopes, extremely stonyBooCc173682812qxj6nj01320031:12000
Boonton sandy loam, terminal moraine, 0 to 8 percent slopes, extremely stonyBoeBc165682380qx28nj01320031:12000
Boonton silt loam, red sandstone lowland, 0 to 8 percent slopes, extremely stonyBooBc147682810qxj4nj01320031:12000
Boonton sandy loam, terminal moraine, 15 to 25 percent slopes, extremely stonyBoeDc137682379qx27nj01320031:12000
Boonton loam, 3 to 8 percent slopesBogB115298102b066nj01320031:12000
Boonton loam, 8 to 15 percent slopesBogC115298103b067nj01320031:12000
Boonton silt loam, red sandstone lowland, 8 to 15 percent slopesBooC107682811qxj5nj01320031:12000
Boonton - Urban land, Boonton substratum complex, 15 to 25 percent slopesBouD93298106b06bnj01320031:12000
Yalesville - Boonton - Holyoke complex, 0 to 8 percent slopes, extremely stonyYaobBc66813406w9dxnj01320031:12000
Urban land, Boonton substratum - Boonton complex, 8 to 15 percent slopesUSBONC35813349w9c2nj01320031:12000
Boonton - Udorthents, Boonton substratum complex, 0 to 8 percent slopesBosB24812694w8nynj01320031:12000
Boonton - Udorthents, Boonton substratum complex, red sandstone lowland, 8 to 15 percent slopesBotC20812703w8p7nj01320031:12000
Boonton - Urban land, Boonton substratum complex, terminal moraine, 15 to 25 percent slopesBowtD19812697w8p1nj01320031:12000
Urban land-Boonton complex, 0 to 8 percent slopesUSBONB57225153651jsq2nj01720121:12000
Boonton loam, 3 to 8 percent slopesBocB11325153532qf95nj01720121:12000
Urban land-Boonton complex, 8 to 15 percent slopesUSBONC4625153661jsq3nj01720121:12000
Boonton loam, 8 to 15 percent slopesBocC3225153542pbqxnj01720121:12000
Boonton-Urban land complex, 0 to 8 percent slopesBouB855114268101jwq4nj02319851:24000
Boonton loam, 3 to 8 percent slopesBogB367814268071jwq1nj02319851:24000
Boonton-Urban land-Haledon complex, 0 to 8 percent slopesBovB81014268121jwq6nj02319851:24000
Boonton loam, 8 to 15 percent slopesBogC44014268081jwq2nj02319851:24000
Boonton-Urban land complex, 15 to 25 percent slopesBouD1214268111jwq5nj02319851:24000
Boonton moderately well drained gravelly loam, 8 to 15 percent slopesBohC514268091jwq3nj02319851:24000
Boonton moderately well drained gravelly loam, 8 to 15 percent slopesBohC111114440391kgmxnj02719741:24000
Boonton moderately well drained gravelly loam, 3 to 8 percent slopesBohB100514440381kgmwnj02719741:24000
Boonton and Haledon soils, 8 to 15 percent slopes, extremely stonyBOXCC858298483b0lhnj02719741:24000
Urban land-Boonton complex, red sandstone lowland, 0 to 8 percent slopesUSBOOB831814525951krjxnj03119721:24000
Urban land-Boonton complex, 0 to 8 percent slopesUSBONB238514239251jsq2nj03119721:24000
Urban land-Boonton complex, 8 to 15 percent slopesUSBONC220614239261jsq3nj03119721:24000
Urban land-Boonton complex, red sandstone lowland, 8 to 15 percent slopesUSBOOC151614525961krjynj03119721:24000
Boonton silt loam, 3 to 8 percent slopes, stonyBonBa74714443271kgy6nj03119721:24000
Boonton silt loam, 8 to 15 percent slopes, stonyBonCa73814443281kgy7nj03119721:24000
Boonton-Urban land complex, 0 to 8 percent slopesBouB52814443321kgycnj03119721:24000
Boonton moderately well drained-Rock outcrop complex, 25 to 45 percent slopesBorE49014443311kgybnj03119721:24000
Boonton silt loam, 15 to 35 percent slopes, very stonyBonDb48514443291kgy8nj03119721:24000
Boonton-Urban land complex, 8 to 15 percent slopesBouC23614443331kgydnj03119721:24000
Boonton moderately well drained-Rock outcrop complex, 8 to 15 percent slopesBorC9314443301kgy9nj03119721:24000
Boonton silt loam, red sandstone lowland, 8 to 15 percent slopes, extremely stonyBooCc7014525871krjnnj03119721:24000
Boonton loam, 0 to 8 percent slopes, extremely stonyBogBc5314525851krjlnj03119721:24000
Boonton moderately well drained gravelly loam, 0 to 8 percent slopes, very stonyBohBb34600623n4zynj03119721:24000
Boonton moderately well drained gravelly loam, 15 to 25 percent slopes, very stonyBohDb2914443261kgy5nj03119721:24000
Boonton moderately well drained gravelly loam, 8 to 15 percent slopes, very stonyBohCb2314443251kgy4nj03119721:24000
Boonton loam, 8 to 15 percent slopesBogC314443221kgy1nj03119721:24000
Boonton moderately well drained gravelly loam, 8 to 15 percent slopesBohC214443241kgy3nj03119721:24000
Boonton-Urban land-Haledon complex, 0 to 8 percent slopesBovB1370214440521kgnbnj03919891:24000
Boonton loam, 3 to 8 percent slopesBogB131514440481kgn6nj03919891:24000
Boonton-Urban land complex, 15 to 25 percent slopesBouD127514440511kgn9nj03919891:24000
Boonton-Urban land complex, terminal moraine, 0 to 8 percent slopesBowtB56014449221khkdnj03919891:24000
Boonton-Urban land complex, red sandstone lowland, 0 to 8 percent slopesBowrB44214526561krlwnj03919891:24000
Boonton moderately well drained gravelly loam, 8 to 15 percent slopesBohC40914440491kgn7nj03919891:24000
Boonton moderately well drained gravelly loam, 15 to 25 percent slopesBohD37014440501kgn8nj03919891:24000
Boonton-Urban land complex, terminal moraine, 15 to 25 percent slopesBowtD22314449241khkgnj03919891:24000
Boonton-Urban land complex, terminal moraine, 8 to 15 percent slopesBowtC7214449231khkfnj03919891:24000
Boonton sandy loam, terminal moraine, 15 to 25 percent slopes, extremely stonyBoeDc1614449211khkcnj03919891:24000
Boonton-Urban land complex, 0 to 8 percent slopesBouB714537631ksrlnj03919891:24000
Urban land-Boonton complex, 0 to 8 percent slopesUSBONB514537691ksrsnj03919891:24000
Boonton-Haledon complex, 0 to 8 percent slopesBHBu68624217272m907ny08520141:12000
Boonton loam, 8 to 15 percent slopesBtC64524829732pbqxny08520141:12000
Boonton loam, 3 to 8 percent slopesBtB47425153522qf95ny08520141:12000
Boonton loam, terminal moraine, 15 to 35 percent slopesBtEt31326028332qx47ny08520141:12000
Boonton loam, moderately well drained, 3 to 8 percent slopesBmB21025188632qf9fny08520141:12000
Boonton loam, moderately well drained, 0 to 3 percent slopesBmA20425188622qf9dny08520141:12000
Boonton loam, 15 to 25 percent slopesBtD14425890642r2zkny08520141:12000
Boonton loam, 0 to 3 percent slopesBtA8625153512qf96ny08520141:12000
Boonton loam, 25 to 35 percent slopesBtE6625890652r2zlny08520141:12000

Map of Series Extent

Approximate geographic distribution of the BOONTON 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 .