Official Series Description


Lab Data Summary

Aggregate lab data for the BROADBROOK soil series. This aggregation is based on all pedons with a current taxon name of BROADBROOK, 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 BROADBROOK 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
144A40A4188S1977MA005006Broadbrook7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.5408134,-71.0283585
14599P055499CT003010Broadbrook7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.9647064,-72.7220154
1451980MA015003S1980MA015003Broadbrook4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.3939611,-72.521975
n/a40A5212S1977MA005001Broadbrook7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a40A5213S1977MA005006ABroadbrook6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a40A5214S1977MA005006BBroadbrook6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a40A5215S1977MA005006CBroadbrook6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

There are insufficient data to create the 3D terrace figure.

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Competing Series

Soil series competing with BROADBROOK 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 BROADBROOK 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 BROADBROOK 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 .

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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.

Soil series sharing subgroup-level classification with BROADBROOK, 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. MA-2010-09-10-05 | Middlesex County - 2009

    A typical pattern of soils and underlying material in the Narragansett-Haven association (Soil Survey of Middlesex County, Massachusetts; 2009).

Map Units

Map units containing BROADBROOK 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
Broadbrook silt loam, 3 to 8 percent slopes82B495133958289lr3ct60120031:12000
Broadbrook silt loam, 8 to 15 percent slopes82C135533958299lr4ct60120031:12000
Broadbrook silt loam, 3 to 8 percent slopes, very stony83B110433958319lr6ct60120031:12000
Broadbrook-Urban land complex, 3 to 8 percent slopes282B78133957019llsct60120031:12000
Broadbrook silt loam, 15 to 25 percent slopes82D64733958309lr5ct60120031:12000
Broadbrook silt loam, 8 to 15 percent slopes, very stony83C62933958329lr7ct60120031:12000
Broadbrook silt loam, 3 to 8 percent slopes82B60534002019lr3ct60220031:12000
Broadbrook silt loam, 3 to 8 percent slopes, very stony83B17934002049lr6ct60220031:12000
Broadbrook silt loam, 15 to 25 percent slopes82D534002039lr5ct60220031:12000
Broadbrook very fine sandy loam, 3 to 8 percent slopes340B8462768659934ma01719911:24000
Broadbrook very fine sandy loam, 3 to 8 percent slopes, very stony341B6932768679936ma01719911:24000
Broadbrook very fine sandy loam, 8 to 15 percent slopes, very stony341C6302768689937ma01719911:24000
Broadbrook very fine sandy loam, 8 to 25 percent slopes340D446796725vr1tma01719911:24000
Broadbrook very fine sandy loam, 15 to 25 percent slopes, very stony341D3602768699938ma01719911:24000
Broadbrook very fine sandy loam, 3 to 8 percent slopes, very stony341B10202961249y4dma02320101:12000
Broadbrook very fine sandy loam, 3 to 8 percent slopes340B2232961259y4fma02320101:12000
Broadbrook very fine sandy loam, 8 to 15 percent slopes340C1992961229y4bma02320101:12000
Broadbrook very fine sandy loam, 8 to 15 percent slopes, very stony341C1162961269y4gma02320101:12000
Broadbrook very fine sandy loam, 0 to 3 percent slopes340A742961239y4cma02320101:12000
Broadbrook silt loam, 8 to 15 percent slopes, very stony341C69727738699myma60719751:15840
Broadbrook gravelly silt loam, 3 to 8 percent slopes340B58127738399mvma60719751:15840
Broadbrook silt loam, 3 to 8 percent slopes, very stony341B54527738599mxma60719751:15840
Broadbrook silt loam, 15 to 25 percent slopes, very stony341D48327738799mzma60719751:15840
Broadbrook silt loam, 8 to 15 percent slopes, extremely stony726C39527738999n1ma60719751:15840
Broadbrook gravelly silt loam, 8 to 15 percent slopes340C33027738499mwma60719751:15840
Broadbrook silt loam, 3 to 8 percent slopes, extremely stony726B25527738899n0ma60719751:15840
Broadbrook silt loam, 3 to 8 percent slopesBrB16852862169ltsri60019771:12000
Broadbrook very stony silt loam, 0 to 8 percent slopesBsB10222862179lttri60019771:12000
Broadbrook silt loam, 0 to 3 percent slopesBrA8912862159ltrri60019771:12000

Map of Series Extent

Approximate geographic distribution of the BROADBROOK 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 .