Official Series Description


Lab Data Summary

Aggregate lab data for the EXETER soil series. This aggregation is based on all pedons with a current taxon name of EXETER, 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 EXETER 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
1793P024892CA107004Exeter7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.9008333,-119.0602778
1940A2840S1957CA065011EXETER5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.8291664,-117.203331

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the EXETER 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 EXETER 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 EXETER 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 EXETER 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 EXETER 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 EXETER 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 EXETER 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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There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with EXETER, 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. CA-2010-08-30-04 | Stanislaus County, Northern Part - 2007

    Typical pattern of soils and parent materials on the eastern side of the San Joaquin Valley and in the low hills of the metamorphic belt region of the Sierra Nevada Mountains. Consolidated parent materials are in the hills (Soil Survey of Stanislaus County, California, Northern Part; 2007).

Map Units

Map units containing EXETER 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
Exeter sandy loam, 0 to 2 percent slopes1574055462049hhstca07719901:24000
Exeter sandy loam, 0 to 2 percent slopes128296459338hdzcca10119841:24000
Exeter sandy clay loam, 0 to 2 percent slopes157201314034161j3chca63220061:24000
Exeter sandy loamEs12898464281hl3tca65419661:24000
Exeter loamEx5505464283hl3wca65419661:24000
Exeter sandy loam, shallowEt2764464282hl3vca65419661:24000
Exeter loam, 0 to 2 percent slopes11466250467186hp4jca65919991:24000
Exeter loam, 2 to 5 percent slopes1152030467187hp4kca65919991:24000
Exeter loam, 0 to 2 percent slopes12417474463589hkdhca66019771:24000
Exeter loam, 2 to 9 percent slopes1257496463590hkdjca66019771:24000
Exeter loam, 2 to 5 percent slopes115tw42322181172dg45ca66019771:24000
Exeter loam, 0 to 2 percent slopes114tw22181412dg4yca66619831:24000
Exeter sandy loam, 0 to 2 percent slopes15411431463699hkj1ca66619831:24000
Exeter sandy loam, 2 to 9 percent slopes155355463700hkj2ca66619831:24000
Exeter sandy loam, 2 to 9 percent slopes196801467318hp8sca66820071:24000
Exeter sandy loam, 0 to 2 percent slopes199184467321hp8wca66820071:24000
Exeter sandy loam, 0 to 2 percent slopesEnA3639458225hctgca67919671:15840
Exeter sandy loam, deep, 0 to 2 percent slopesEpA3210458228hctkca67919671:15840
Exeter sandy loam, 2 to 8 percent slopes, erodedEnC22126458226hcthca67919671:15840
Exeter sandy loam, deep, 2 to 8 percent slopes, erodedEpC21186458229hctlca67919671:15840
Exeter sandy loam, slightly saline-alkali, 0 to 5 perce nt slopesEoB661458227hctjca67919671:15840
Exeter very fine sandy loam, deep, 0 to 5 percent slopesEyB527458231hctnca67919671:15840
Exeter very fine sandy loam, 0 to 5 percent slopesEwB495458230hctmca67919671:15840

Map of Series Extent

Approximate geographic distribution of the EXETER 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 .