Official Series Description


Lab Data Summary

Aggregate lab data for the GALWAY soil series. This aggregation is based on all pedons with a current taxon name of GALWAY, 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 GALWAY 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
14390P011388NY035003Galway4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0475006,-74.651947
144A81P075281VT021008Galway6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.4880562,-73.0313873

Water Balance

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

Soil series competing with GALWAY 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 GALWAY 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 GALWAY 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.

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Click the image to view it full size.

Soil series sharing subgroup-level classification with GALWAY, 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. VT-2012-03-22-08 | Rutland County - 1998

    Typical pattern of soils and underlying material in the Farmington-Galway unit (Soil Survey of Rutland County, VT; 1998).

Map Units

Map units containing GALWAY 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
Rock outcrop-Farmington-Galway complex, 15 to 35 percent slopesRnfD17122624845nz69nj03720021:24000
Rock outcrop-Farmington-Galway complex, 8 to 15 percent slopesRnfC8405624844nz68nj03720021:24000
Galway loam, 35 to 60 percent slopes, very rockyGawEh542624811nz56nj03720021:24000
Rock outcrop-Farmington-Galway complex, 15 to 35 percent slopesRnfD9769740977sw1hnj04120071:12000
Rock outcrop-Farmington-Galway complex, 8 to 15 percent slopesRnfC4966740976sw1gnj04120071:12000
Farmington-Galway complex, hilly, very rockyFcD57552906529rfwny02719921:24000
Galway-Farmington complex, rolling, rockyGfC55422906579rg1ny02719921:24000
Farmington-Galway complex, rolling, very rockyFcC43102906519rfvny02719921:24000
Galway-Farmington complex, undulating, rockyGfB21312906569rg0ny02719921:24000
Galway-Farmington complex, hillyGfD14002906589rg2ny02719921:24000
Farmington-Galway complex, undulating, very rockyFcB5522906509rftny02719921:24000
Galway-Farmington-Urban land complex, rolling, rockyGlC4292906609rg4ny02719921:24000
Galway-Farmington-Urban land complex, undulating, rockyGlB3852906599rg3ny02719921:24000
Farmington-Galway complex, 3 to 15 percent slopes, very rocky, very stonyFgB13632913119s44ny03120071:24000
Galway loam, 3 to 8 percent slopes21B18332915069sbfny03520071:24000
Galway loam, 8 to 15 percent slopes21C4682915079sbgny03520071:24000
Galway-Farmington gravelly silt loams, 2 to 8 percent slopes, rockyGfB11472916329sghny03919851:24000
Galway-Farmington gravelly silt loams, rolling, rockyGfC10402916339sgjny03919851:24000
Galway-Farmington gravelly silt loam, hilly, rockyGfD3022916349sgkny03919851:24000
Galway silt loam, 3 to 8 percent slopesGlB172882918249snpny04519811:15840
Galway very stony silt loam, 0 to 15 percent slopesGmC109892918269snrny04519811:15840
Galway silt loam, 0 to 3 percent slopesGlA100712918239snnny04519811:15840
Galway silt loam, 8 to 15 percent slopesGlC7082918259snqny04519811:15840
Galway loam, 2 to 8 percent slopesNcB50072677749bmmjny04920181:24000
Galway loam, 3 to 8 percent slopesAfB21222677622bmhfny04920181:24000
Galway loam, 0 to 3 percent slopesAfA9292677621bmhdny04920181:24000
Galway loam, 15 to 25 percent slopesNdD9192677751bmmlny04920181:24000
Galway loam, 8 to 15 percent slopesNcC8462677750bmmkny04920181:24000
Galway loam, 0 to 3 percent slopes211A84231057712ywkwny05120191:24000
Galway silt loam, 3 to 8 percent slopes515B9422934449vbyny06519931:24000
Galway silt loam, 8 to 15 percent slopes515C6412934459vbzny06519931:24000
Galway silt loam, 3 to 8 percent slopes, cool845B37814602081l0ghny06519931:24000
Galway silt loam, 0 to 3 percent slopes, cool845A20714602061l0gfny06519931:24000
Galway silt loam, 0 to 3 percent slopes515A1542934439vbxny06519931:24000
Galway silt loam, 8 to 15 percent slopes, cool845C6314602101l0gkny06519931:24000
Galway loam, 3 to 8 percent slopesGaB40142943779wb1ny09119931:24000
Galway loam, 8 to 15 percent slopesGaC16252943789wb2ny09119931:24000
Galway loam, 3 to 8 percent slopesGaB3382958829xwlny11319821:15840
Galway-Farmington complex, 25 to 50 percent slopes, very rocky41E58972814889fx8vt00319921:20000
Galway-Nellis-Farmington complex, 15 to 25 percent slopes, rocky40D34702814822wrfnvt00319921:20000
Galway-Farmington complex, 15 to 25 percent slopes, very rocky41D30992814879fx7vt00319921:20000
Galway-Nellis-Farmington complex, 8 to 15 percent slopes, rocky40C19182814812wrfmvt00319921:20000
Galway-Farmington complex, 8 to 15 percent slopes, very rocky41C8022814869fx6vt00319921:20000
Galway-Nellis-Farmington complex, 3 to 8 percent slopes, rocky40B3162814802wrflvt00319921:20000
Farmington-Galway-Galoo complex, 5 to 25 percent slopes, very rocky41C122532823279gsbvt02119851:20000
Farmington-Galway-Galoo complex, 25 to 50 percent slopes, very rocky41E90572823299gsdvt02119851:20000
Galway-Nellis-Farmington complex, 8 to 15 percent slopes, rocky40C36752823242wrfmvt02119851:20000
Galway-Nellis-Farmington complex, 15 to 25 percent slopes, rocky, very stony40D24962823252xj4kvt02119851:20000
Galway-Nellis-Farmington complex, 3 to 8 percent slopes, rocky39B15982823042wrflvt02119851:20000

Map of Series Extent

Approximate geographic distribution of the GALWAY 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 .