Official Series Description


Lab Data Summary

Aggregate lab data for the SUMMERVILLE soil series. This aggregation is based on all pedons with a current taxon name of SUMMERVILLE, 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 SUMMERVILLE 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 SUMMERVILLE 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.

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the SUMMERVILLE series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the SUMMERVILLE series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the SUMMERVILLE 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 .

Click the image to view it full size.

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.

Competing Series

Soil series competing with SUMMERVILLE share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the SUMMERVILLE series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the SUMMERVILLE 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 .

Click the image to view it full size.

Click the image to view it full size.

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 SUMMERVILLE, 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. MI-2012-02-06-41 | Menominee County - September 1989

    Typical pattern of soils and parent material in the Onaway-Summerville-Lupton map unit (Soil Survey of Menominee County, Michigan; September 1989).

Map Units

Map units containing SUMMERVILLE 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
Summerville fine sandy loam, 1 to 6 percent slopes52B26214552781kvbgmi00320071:24000
Summerville fine sandy loam, 0 to 6 percent slopes482B52491913896f4vmi00719981:12000
Summerville fine sandy loam, 6 to 12 percent slopes482C4451913906f4wmi00719981:12000
Summerville sandy loam, 2 to 6 percent slopesSvB631892816byvmi01119641:20000
Summerville sandy loam, 0 to 2 percent slopesSvA221892806bytmi01119641:20000
Summerville stony sandy loam, 0 to 6 percent slopesSuB7721905116d7jmi02919701:15840
Summerville-Rock outcrop complex, 1 to 15 percent slopes41D7433415148fxzwmi03319891:15840
Summerville-Longrie complex, 1 to 6 percent slopes, rocky57B3648415163fy0cmi03319891:15840
Summerville-Rock outcrop complex, 15 to 45 percent slopes41F640415149fxzxmi03319891:15840
Summerville fine sandy loam, 0 to 4 percent slopesSuA1763915881161q9kkmi04119691:24000
Longrie and Summerville sandy loams, 6 to 18 percent slopesLsD133715880771q9j9mi04119691:24000
Summerville fine sandy loam, 1 to 6 percent slopes52B512395225f886mi10319991:24000
Nahma-Sundell-Summerville complex, 0 to 6 percent slopes59B9420415493fyc0mi10919851:20000
Summerville-Cunard fine sandy loams, 0 to 6 percent slopes62B7701415496fyc3mi10919851:20000
Nadeau-Summerville fine sandy loams, 3 to 12 percent slopes55B872415490fybxmi10919851:20000
Summerville flaggy fine sandy loam, 0 to 6 percent slopes, rocky9B70031909676dq7mi14119891:15840
Summerville flaggy fine sandy loam, 6 to 18 percent slopes, rocky9C10071909686dq8mi14119891:15840
Neckrock-Summerville complex, strongly sloping, very rockyNeC48002902049qzfny01919951:24000
Adjidaumo-Summerville-Rock outcrop complex, 0 to 15 percent slopesArC1925682472w5k0ny04920181:24000
Summerville-Rock outcrop-Nehasne complex, rollingSmC203412950209wzsny08919901:24000
Summerville-Rock outcrop complex,hillySlD173882950199wzrny08919901:24000
Summerville-Gouverneur complex, 0 to 8 percent slopes, rockySkB103902950189wzqny08919901:24000
Adjidaumo-Summerville-Rock outcrop complex, 0 to 15 percent slopesArC61982949082w5k0ny08919901:24000
Summerville fine sandy loam, 0 to 8 percent slopesShB33852950179wzpny08919901:24000
Neckrock-Summerville complex, gently sloping, rocky94B1022960819y30ny68919991:24000
Neckrock-Summerville complex, strongly sloping, rocky94C62960829y31ny68919991:24000
Summerville silt loam, clayey subsoil variant, 1 to 6 percent slopesSvB951426258g9k8wi00919701:20000
Summerville loam, 1 to 6 percent slopesSuB739426256g9k6wi00919701:20000
Summerville loam, 6 to 20 percent slopes, erodedSuD2176426257g9k7wi00919701:20000
Summerville loam, 2 to 6 percent slopesSvB31567422278g5dwwi02919751:15840
Summerville loam, 0 to 2 percent slopesSvA11175422277g5dvwi02919751:15840
Summerville loam, 6 to 12 percent slopesSvC2844422279g5dxwi02919751:15840
Summerville loam, 12 to 20 percent slopesSvD591422280g5dywi02919751:15840
Summerville fine sandy loam, 1 to 6 percent slopesSuB633422451g5lgwi07519871:20000
Summerville fine sandy loam, 6 to 12 percent slopesSuC255422452g5lhwi07519871:20000
Summerville fine sandy loam, 2 to 8 percent slopesSuB503422517g5nlwi08319851:15840
Summerville fine sandy loam, 20 to 45 percent slopesSuE158422518g5nmwi08319851:15840

Map of Series Extent

Approximate geographic distribution of the SUMMERVILLE 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 .