Official Series Description


Lab Data Summary

Aggregate lab data for the GROVE soil series. This aggregation is based on all pedons with a current taxon name of GROVE, 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 GROVE 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
171C0047S1971WA031001GROVE4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.7495232,-122.8781891

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the GROVE 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 GROVE 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 GROVE 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 GROVE 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 hills figure.

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There are insufficient data to create the 3D terrace figure.

There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with GROVE 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 GROVE 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 GROVE 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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There are insufficient data to create the 3D hills figure.

Click the image to view it full size.

Click the image to view it full size.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with GROVE, 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 GROVE 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
Wind River-Grove-Waterman families complex, 25 to 70 percent slopes.30415915471313htfnca71319841:24000
Hoodsport-Grove very gravelly sandy loams, 0 to 30 percent slopesHrD1954737672grlwa63119681:20000
Grove very gravelly loamy sand, 0 to 15 percent slopesGoC945737502gr1wa63119681:20000
Grove very gravelly sandy loam, 0 to 15 percent slopesGrC541737532gr4wa63119681:20000
Grove very gravelly sandy loam, 15 to 30 percent slopesGrD522737542gr5wa63119681:20000
Grove very gravelly loamy sand, 30 to 50 percent slopesGoE420737522gr3wa63119681:20000
Grove very gravelly loamy sand, 15 to 30 percent slopesGoD321737512gr2wa63119681:20000
Grove very gravelly sandy loam, 0 to 3 percent slopes111510741802h5xwa63519771:24000
Grove very gravelly sandy loam, 3 to 15 percent slopes12980741812h5ywa63519771:24000
Grove very gravelly sandy loam, 15 to 30 percent slopes13570741822h5zwa63519771:24000
Grove gravelly sandy loam, 0 to 5 percent slopesGh43770745432hkmwa64519531:31680
Grove gravelly sandy loam, 5 to 15 percent slopesGk10494745442hknwa64519531:31680
Grove gravelly sandy loam, 15 to 30 percent slopesGm3529745452hkpwa64519531:31680
Grove cobbly sandy loam, 0 to 5 percent slopesGb2133745372hkfwa64519531:31680
Grove gravelly sandy loam, 30 to 45 percent slopesGn1056745462hkqwa64519531:31680
Grove cobbly sandy loam, 5 to 15 percent slopesGc622745382hkgwa64519531:31680
Grove gravelly loam, basin phase, 0 to 5 percent slopesGg594745422hklwa64519531:31680
Grove gravelly sandy loam, basin phase, 0 to 5 percent slopesGo396745472hkrwa64519531:31680
Grove gravelly loam, 0 to 5 percent slopesGe383745402hkjwa64519531:31680
Grove stony sandy loam, 0 to 5 percent slopesGp367745482hkswa64519531:31680
Grove cobbly sandy loam, 15 to 30 percent slopesGd201745392hkhwa64519531:31680
Grove gravelly loam, 5 to 15 percent slopesGf144745412hkkwa64519531:31680
Grove very gravelly sandy loam, 3 to 15 percent slopes42167724546702nd8xwa66719831:24000

Map of Series Extent

Approximate geographic distribution of the GROVE 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 .