Official Series Description


Lab Data Summary

Aggregate lab data for the PHELPS soil series. This aggregation is based on all pedons with a current taxon name of PHELPS, 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 PHELPS were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the PHELPS 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 PHELPS 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 PHELPS 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 PHELPS 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 PHELPS 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 PHELPS 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 PHELPS 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 PHELPS, 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. NY-2012-02-15-04 | Cayuga County - 1971

    Typical cross section of Honeoye-Lima association (Soil Survey of Cayuga County, New York; 1971).

  2. NY-2012-02-15-06 | Cayuga County - 1971

    Typical cross section of Langford-Erie association and Langford-Howard association in the southeastern part of the county (Soil Survey of Cayuga County, New York; 1971).

  3. NY-2012-02-15-22 | Genesee County - March 1969

    Cross section showing typical soil pattern in the Palmyra association (Soil Survey of Genesee County, New York; March 1969).

  4. NY-2012-02-15-27 | Madison County - March 1981

    Typical relationship of soils and underlying material in Palmyra-Phelps, undulating (Soil Survey of Madison County, New York; March 1981).

  5. NY-2012-02-15-47 | Tompkins County - July 1965

    Typical cross section of Lima-Honeoye association and Palmyra association in northwestern Tompkins County (Soil Survey of Tompkins County, New York; July 1965).

  6. NY-2012-02-15-48 | Tompkins County - July 1965

    Typical cross section of southern Tompkins County soils, consisting mainly of low-lime and very low-lime soils with a fragipan (Soil Survey of Tompkins County, New York; July 1965).

  7. NY-2012-02-16-05 | Wyoming County - April 1974

    Typical pattern of soils in association 11 (Soil Survey of Wyoming County, New York; April 1974).

Map Units

Map units containing PHELPS 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
Phelps gravelly silt loamPv11832894829q74ny01119681:15840
Phelps gravelly loam, 0 to 4 percent slopesPhA5082899439qq0ny01519691:20000
Phelps gravelly silt loam, 3 to 8 percent slopesPhB6152900289qsrny01719821:15840
Phelps gravelly silt loam, 0 to 3 percent slopesPhA1722900279qsqny01719821:15840
Phelps gravelly silt loam, 0 to 3 percent slopes210A137527230922rwcfny02320141:12000
Phelps gravelly loam, 0 to 3 percent slopesPhA29212908799rp6ny02919791:15840
Phelps gravelly loam, 3 to 8 percent slopesPhB7572908809rp7ny02919791:15840
Phelps gravelly loam, 3 to 8 percent slopesPsB2782301780b40vny03720041:24000
Phelps gravelly loam, 0 to 3 percent slopesPsA2145633062p7rcny03720041:24000
Phelps gravelly fine sandy loam, 0 to 4 percent slopesPpB221925183909syxny04320181:24000
Phelps gravelly loam, 0 to 3 percent slopesPhA18862918979sr1ny04519811:15840
Phelps gravelly loam, 3 to 8 percent slopesPhB6952918989sr2ny04519811:15840
Phelps gravelly silt loam, 0 to 3 percent slopes21A32531057882ywl7ny05120191:24000
Phelps gravelly silt loam, 3 to 8 percent slopes21B5231057892ywl8ny05120191:24000
Phelps gravelly silt loam, 0 to 3 percent slopesPpA34862926239thgny05319751:15840
Phelps gravelly silt loam, 3 to 8 percent slopesPpB7962926249thhny05319751:15840
Phelps gravelly fine sandy loam, 0 to 3 percent slopesPhA20142927589tmtny05519671:15840
Phelps gravelly fine sandy loam, 3 to 8 percent slopesPhB8412927599tmvny05519671:15840
Phelps gravelly loam, fanPr20832928789trpny05719731:24000
Phelps gravelly loam, 3 to 8 percent slopesPpB11212928779trnny05719731:24000
Phelps gravelly loam, 0 to 3 percent slopesPpA2152928769trmny05719731:24000
Phelps silt loam, 0 to 3 percent slopes28A35962933949v9bny06519931:24000
Phelps silt loam, 3 to 8 percent slopes28B6682933959v9cny06519931:24000
Phelps gravelly loam, 0 to 3 percent slopesPpA18742936499vkkny06719731:20000
Phelps gravelly loam, 3 to 8 percent slopesPpB12862936509vklny06719731:20000
Phelps gravelly silt loam, 0 to 3 percent slopes210A536617276261vzqwny06920121:12000
Phelps gravelly silt loam, 3 to 8 percent slopes210B79625124192q9m0ny06920121:12000
Phelps gravelly fine sandy loamPp18212940729w06ny07319731:15840
Phelps gravelly loam, 0 to 3 percent slopesPpA280309641bd6fny09319731:15840
Phelps gravelly loam, 3 to 8 percent slopesPpB223309642bd6gny09319731:15840
Phelps gravelly loam, fanPr95309643bd6hny09319731:15840
Phelps gravelly silt loam, clay substratum, 2 to 8 percent slopesPlB8162945419whbny09519651:15840
Phelps gravelly silt loam, 0 to 5 percent slopesPhA3842945409wh9ny09519651:15840
Phelps gravelly silt loam, 3 to 8 percent slopesPhB19352956769xnyny10919631:20000
Phelps gravelly silt loam, 0 to 3 percent slopesPhA11032956759xnxny10919631:20000
Phelps gravelly loam, 0 to 3 percent slopesPoA72312957779xs6ny11719721:15840
Phelps gravelly loam, 3 to 8 percent slopesPoB46512957789xs7ny11719721:15840
Phelps cobbly loam, 0 to 3 percent slopesPpA2922957799xs8ny11719721:15840
Phelps gravelly loam, 0 to 3 percent slopesPpA12092954189xdmny12119691:20000
Phelps gravelly loam, 3 to 8 percent slopesPpB4102954199xdnny12119691:20000
Phelps gravelly silt loam, 3 to 8 percent slopes210B65632503562q9m0ny12319481:12000
Phelps gravelly silt loam, 0 to 3 percent slopes210A29832502761vzqwny12319481:12000
Phelps gravelly loamPhA962893099q1kny60519811:24000
Phelps gravelly loam, 0 to 5 percent slopesPsA43292930419txyny66419681:15840
Phelps gravelly silt loam, 3 to 8 percent slopesPhB638194884623dy0pa09520071:12000

Map of Series Extent

Approximate geographic distribution of the PHELPS 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 .