Official Series Description


Lab Data Summary

Aggregate lab data for the GRANGEVILLE soil series. This aggregation is based on all pedons with a current taxon name of GRANGEVILLE, 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 GRANGEVILLE 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
1785P019484CA031004Grangeville7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.2083321,-119.7833328
1787P073087CA107020Grangeville5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.3827362,-119.1162262

Water Balance

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

Soil series competing with GRANGEVILLE 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 GRANGEVILLE 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 GRANGEVILLE 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 GRANGEVILLE, 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

No block diagrams are available.

Map Units

Map units containing GRANGEVILLE 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
Grangeville sandy loam, saline-alkali1199944461780hhj4ca03119801:24000
Grangeville fine sandy loam, saline-alkali, partially d rained1216665461782hhj6ca03119801:24000
Grangeville fine sandy loam, partially drained1205439461781hhj5ca03119801:24000
Grangeville fine sandy loam, partially drained, 0 to 2 percent slopes1667900462058hht3ca07719901:24000
Grangeville clay loam, partially drained, 0 to 2 percent slopes1673075462059hht4ca07719901:24000
Grangeville fine sandy loam, 0 to 2 percent slopesGoA3970456824hbc8ca63819671:24000
Grangeville very fine sandy loam, 0 to 1 percent slopesGmA2859462594hjcdca64419591:24000
Grangeville fine sandy loam, 0 to 1 percent slopes, MLRA 17GfA14654625902vncxca64419591:24000
Grangeville very fine sandy loam, slightly saline-alkali, 0 to 1 percent slopesGnA680462595hjcfca64419591:24000
Grangeville sandy loam, slightly saline-alkali, 0 to 1 percent slopesGkA314462593hjccca64419591:24000
Grangeville very fine sandy loam, moderately saline-alkali, 0 to 1 percent slopesGoA226462596hjcgca64419591:24000
Grangeville sandy loam, 0 to 1 percent slopesGhA225462592hjcbca64419591:24000
Grangeville fine sandy loam, slightly saline-alkali, 0 to 1 percent slopesGgA158462591hjc9ca64419591:24000
Grangeville fine sandy loam, 0 to 1 percent slopes, MLRA 17GaA54984630322vncxca64819591:20000
Grangeville loam, 0 to 1 percent slopesGbA3465463033hjtkca64819591:20000
Grangeville loam, slightly saline-alkali, 0 to 1 percent slopesGcA2116463034hjtlca64819591:20000
Grangeville loam, moderately saline-alkali, 0 to 1 percent slopesGdA92463035hjtmca64819591:20000
Grangeville fine sandy loam, 0 to 1 percent slopes, MLRA 17GaA12345329585930r8qca65119591:20000
Grangeville fine sandy loam, over traver soils, 0 to 1 percent slopesGcA11699329586030r8sca65119591:20000
Grangeville fine sandy loam, slightly saline-alkali, 0 to 1 percent slopesGbA4541463421hk72ca65119591:20000
Grangeville fine sandy loam, over traver soils, slightly saline alkali, 0 to 1 percent slopesGdA1813463423hk74ca65119591:20000
Grangeville fine sandy loam, deep over alkali hardpan, 0 to 1 percent slopesGhA1269463426hk77ca65119591:20000
Grangeville sandy loam, 0 to 1 percent slopesGmA1048463428hk79ca65119591:20000
Grangeville fine sandy loam, deep over hardpan, 0 to 1 percent slopesGfA914463425hk76ca65119591:20000
Grangeville sandy loam, slightly saline-alkali, 0 to 1 percent slopesGnA778463429hk7bca65119591:20000
Grangeville fine sandy loam, deep over alkali hardpan, slightly saline-alkali, 0 to 1 percent slopesGkA556463427hk78ca65119591:20000
Grangeville fine sandy loam, moderately deep and deep over temple soils, 0 to 1 percent slopesGeA501463424hk75ca65119591:20000
Grangeville fine sandy loam, 0 to 1 percent slopes, MLRA 17Gf165744643152vncxca65419661:24000
Grangeville sandy loamGa3459464312hl4tca65419661:24000
Grangeville fine sandy loam, saline alkaliGg3091464316hl4yca65419661:24000
Grangeville soils, channeledGp2578464323hl55ca65419661:24000
Grangeville fine sandy loam, sandy substratumGm1952464320hl52ca65419661:24000
Grangeville fine sandy loam, gravelly substratumGl1831464319hl51ca65419661:24000
Grangeville fine sandy loam, hard substratum, saline-alkaliGo1256464322hl54ca65419661:24000
Grangeville fine sandy loam, hard substratumGn1242464321hl53ca65419661:24000
Grangeville sandy loam, sandy substratumGe1039464314hl4wca65419661:24000
Grangeville fine sandy loam, water table, saline alkaliGk739464318hl50ca65419661:24000
Grangeville fine sandy loam, water tableGh552464317hl4zca65419661:24000
Grangeville sandy loam, saline alkaliGd494464313hl4vca65419661:24000
Grangeville fine sandy loam, partially drained120ki478464557hldqca65419661:24000
Grangeville fine sandy loam, saline-alkali, partially drained121ki252464556hldpca65419661:24000
Grangeville sandy loam, drained, 0 to 2 percent slopes12223050467194hp4sca65919991:24000
Grangeville fine sandy loam, saline-sodic, 0 to 1 percent slopes1231750467195hp4tca65919991:24000
Grangeville silt loam, drained1314692463596hkdqca66019771:24000
Grangeville sandy loam, drained, 0 to 2 percent slopes122tw51022181182dg46ca66019771:24000
Grangeville fine sandy loam, warm MAAT, MLRA 19Gr75104579612vncyca67719721:24000
Grangeville fine sandy loam, saline-alkaliGs1350457962hcjzca67719721:24000
Grangeville fine sandy loam, drained, 0 to 2 percent sl opesGtA3836458262hcvnca67919671:15840
Grangeville loamy fine sand, drained, 0 to 5 percent slopesGoB3272458258hcvjca67919671:15840
Grangeville fine sandy loam, saline-alkali, 0 to 5 percent slopesGvB3069458265hcvrca67919671:15840
Grangeville fine sandy loam, poorly drained, saline-alk ali, 0 to 5 percent slopesGuB2373458264hcvqca67919671:15840
Grangeville fine sandy loam, loamy substratum, drained, saline-a lkali, 0 to 2 percent slopesGxA877458267hcvtca67919671:15840
Grangeville sandy loam, sandy substratum, drained, saline-alkali , 0 to 5 percent slopesGsB859458261hcvmca67919671:15840
Grangeville sandy loam, sandy substratum, drained, 0 to 5 percent slopesGrB733458260hcvlca67919671:15840
Grangeville fine sandy loam, loamy substratum, drained, 0 to 2 percent slopesGwA726458266hcvsca67919671:15840
Grangeville sandy loam, drained, saline-alkali, 0 to 5 percent slopesGpB621458259hcvkca67919671:15840
Grangeville fine sandy loam, drained, 5 to 15 percent s lopesGtD120458263hcvpca67919671:15840
Grangeville fine sandy loam, warm MAAT, MLRA 19Gr537291202vncyca67919671:15840
Grangeville fine sandy loam, saline-alkaliGs34729121sgq1ca67919671:15840

Map of Series Extent

Approximate geographic distribution of the GRANGEVILLE 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 .