Official Series Description


Lab Data Summary

Aggregate lab data for the GRITNEY soil series. This aggregation is based on all pedons with a current taxon name of GRITNEY, 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 GRITNEY 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
133AS92AL-113-492AL113004-pgmGritney3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.3252778,-85.3341667

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the GRITNEY 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 GRITNEY 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 GRITNEY 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 GRITNEY 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 GRITNEY 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 GRITNEY 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 GRITNEY 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 mountains figure.

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Click the image to view it full size.

Soil series sharing subgroup-level classification with GRITNEY, 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. NC-2012-02-07-31 | Northampton County - August 1994

    Typical relationship of soils and landscape in the Gritney-Caroline and Norfolk-Bonneau-Goldsboro general soil map units (Soil Survey of Northampton County, North Carolina; August 1994).

Map Units

Map units containing GRITNEY 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
Troup-Gritney-Saffell complex, 8 to 15 percent slopesTgD33239328743c12mal03519851:20000
Gritney-Malbis-Fuquay complex, 1 to 8 percent slopesGyC31929328729c125al03519851:20000
Gritney fine sandy loam, 2 to 5 percent slopesGrB14203304622x5s5al08719971:24000
Gritney loamy fine sand, 0 to 2 percent slopesGrA914330461c2w1al08719971:24000
Gritney fine sandy loam, 2 to 5 percent slopesGrB121729950132x5s5al09720181:24000
Gritney fine sandy loam, 2 to 5 percent slopesGrB50103313722x5s5al11319971:24000
Gritney fine sandy loam, 2 to 5 percent slopesGrB366226420842x5s5al12920131:24000
Gritney loamy sand, 2 to 5 percent slopes1522601017248134jgfl05919711:12000
Gritney loamy sand, 5 to 8 percent slopes1621401017249134jhfl05919711:12000
Gritney loamy sand, 2 to 5 percent slopes462023984602lhspfl13320091:12000
Cowarts-Gritney complex, 5 to 8 percent slopesCgC4705754249t9vmga08720011:24000
Cowarts-Gritney complex, 8 to 12 percent slopesCgD2195754250t9vnga08720011:24000
Cowarts-Gritney complex, 5 to 8 percent slopesCgC4606336564c96xga13120001:12000
Cowarts-Gritney complex, 8 to 12 percent slopesCgD1300336565c96yga13120001:12000
Gritney loamy sand, 2 to 5 percent slopesGrB756525803712qdy1ga25120111:24000
Cowarts-Gritney-Urban land complex, 2 to 5 percent slopesCtB123525802692qbf6ga25120111:24000
Gritney fine sandy loam, 2 to 7 percent slopesGrB57771154903w5hnc01719831:24000
Gritney fine sandy loam, 7 to 15 percent slopesGrD7581154913w5jnc01719831:24000
Gritney loamy fine sand, 2 to 7 percent slopesGyB9591156473wbknc04719861:24000
Gritney fine sandy loam, 6 to 10 percent slopesGyC9341015562132s2nc06519761:20000
Gritney fine sandy loam, 10 to 15 percent slopesGyD4071015561132s1nc06519761:20000
Gritney fine sandy loam, 5 to 12 percent slopes, erodedGyC224811128023scsnc07919781:24000
Gritney fine sandy loam, 2 to 6 percent slopesGtB155931130413smhnc08319951:24000
Gritney sandy clay loam, 2 to 6 percent slopes, moderately erodedGyB229451130433smknc08319951:24000
Gritney fine sandy loam, 6 to 10 percent slopesGtC27881130423smjnc08319951:24000
Gritney sandy loam, 2 to 6 percent slopesGrB29131109063qdmnc12719841:24000
Gritney sandy loam, 6 to 10 percent slopesGrC21951109073qdnnc12719841:24000
Gritney sandy loam, 2 to 6 percent slopesGxB180941140423tnsnc13119881:24000
Gritney sandy loam, 6 to 10 percent slopesGxC41911140433tntnc13119881:24000
Gritney sandy clay loam, 2 to 6 percent slopes, moderately erodedGyB225341140443tnvnc13119881:24000
Gritney sandy clay loam, 6 to 10 percent slopes, moderately erodedGyC22871140453tnwnc13119881:24000
Gritney fine sandy loam, 4 to 8 percent slopesGtC26661150523vqcnc16319821:24000
Gritney sandy loam, 2 to 6 percent slopesGrB11614086141j8s5nc16520061:12000
Gritney sandy loam, 6 to 10 percent slopesGrC5514086151j8s6nc16520061:12000
Gritney sandy loam, 6 to 10 percent slopesGrC718530502542xh9xnc18319661:24000
Craven sandy loam, 6 to 10 percent slopes, eroded (Gritney)CrC245971162333wygnc19119681:20000
Craven sandy loam, 2 to 6 percent slopes, eroded (Gritney)CrB216141162323wyfnc19119681:20000
Gritney sandy loam, 2 to 5 percent slopes, moderately erodedGtB293161164323x4wnc19519801:24000
Gritney sandy loam, 5 to 12 percent slopes, moderately erodedGtC214941164333x4xnc19519801:24000
Gritney-Urban land complex, 2 to 12 percent slopesGu8731164343x4ync19519801:24000
Faceville-Gritney fine sandy loams, 2 to 6 percent slopes157B68021188363znfva04119741:15840
Gritney fine sandy loam, 2 to 6 percent slopes17B16001188533znzva04119741:15840
Faceville-Gritney gravelly fine sandy loams, 6 to 12 percent slopes110C13441188203zmxva04119741:15840
Gritney fine sandy loam, 6 to 12 percent slopes17C9171188543zp0va04119741:15840
Faceville-Gritney gravelly fine sandy loams, 2 to 6 percent slopes110B3481188193zmwva04119741:15840
Faceville-Gritney-Urban land complex, 2 to 6 percent slopes18B17281400924ps3va76020041:24000
Faceville-Gritney-Urban land complex, 6 to 12 percent slopes18C4111400594pr1va76020041:24000

Map of Series Extent

Approximate geographic distribution of the GRITNEY 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 .