Official Series Description


Lab Data Summary

Aggregate lab data for the ELDRIDGE soil series. This aggregation is based on all pedons with a current taxon name of ELDRIDGE, 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 ELDRIDGE 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
144A40A047655NH017003Eldridge4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.1699982,-70.9263916

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ELDRIDGE 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 ELDRIDGE 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 ELDRIDGE 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 ELDRIDGE 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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Click the image to view it full size.

Competing Series

Soil series competing with ELDRIDGE 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 ELDRIDGE 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 ELDRIDGE 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 ELDRIDGE, 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. NH-2012-02-14-20 | Rockingham County - October 1994

    Typical pattern of soils and parent material in the Hoosic-Paxton-Eldridge general soil map unit (Soil Survey of Rockingham County, New Hampshire; October 1994).

Map Units

Map units containing ELDRIDGE 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
Eldridge fine sandy loam, 0 to 3 percent slopes221A3346309347bcwyma02320101:12000
Eldridge fine sandy loam, 3 to 8 percent slopes221B3201309348bcwzma02320101:12000
Eldridge loamy sand, 0 to 6 percent slopes221B38827741499nvma60719751:15840
Eldridge fine sandy loam, 3 to 8 percent slopesElB8442845399k2pme02719791:20000
Eldridge fine sandy loam, 8 to 15 percent slopesElC5562845409k2qme02719791:20000
Eldridge fine sandy loam, 3 to 8 percent slopesEgB18492846969k7rme60119831:20000
Eldridge fine sandy loam, 3 to 8 percent slopes38B50622793209cnbnh01519861:24000
Eldridge fine sandy loam, 0 to 3 percent slopes38A31932793199cn9nh01519861:24000
Belgrade and Eldridge soils, 0 to 3 percent slopesBlA20322816679g31vt00719691:15840
Belgrade and Eldridge soils, 3 to 8 percent slopesBlB14452816689g32vt00719691:15840
Belgrade and Eldridge soils, 8 to 15 percent slopesBlC2342816699g33vt00719691:15840
Belgrade and Eldridge soils, 15 to 25 percent slopesBlD1582816709g34vt00719691:15840
Eldridge loamy fine sand, 0 to 3 percent slopesEdA15812817899g6zvt01119761:20000
Eldridge loamy fine sand, 3 to 8 percent slopesEdB12382817909g70vt01119761:20000
Eldridge loamy fine sand, 8 to 15 percent slopesEdC8342817919g71vt01119761:20000
Eldridge fine sandy loam, 3 to 8 percent slopes61B6632823969gvkvt02119851:20000
Eldridge fine sandy loam, 0 to 3 percent slopes61A4112823959gvjvt02119851:20000
Eldridge fine sandy loam, 3 to 8 percent slopes45B2792832119hpvvt02720001:20000
Eldridge fine sandy loam, 25 to 50 percent slopes45E1542832149hpyvt02720001:20000
Eldridge fine sandy loam, 8 to 15 percent slopes45C892832129hpwvt02720001:20000
Eldridge fine sandy loam, 15 to 25 percent slopes45D772832139hpxvt02720001:20000

Map of Series Extent

Approximate geographic distribution of the ELDRIDGE 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 .