Official Series Description


Lab Data Summary

Aggregate lab data for the PETERS soil series. This aggregation is based on all pedons with a current taxon name of PETERS, 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 PETERS 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
17UCD585203358-CA-52-033PETERS2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.2787132,-122.2251205
17UCD770405777-CA-04-057xPETERS3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.6379623,-121.6812668
18UCD800508980-CA-05-089xPeters3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0176468,-120.8709869
1805N0397S04CA077-001Peters7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0374444,-120.9277778

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the PETERS 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 PETERS 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 PETERS 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 PETERS 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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Click the image to view it full size.

Competing Series

Soil series competing with PETERS 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 PETERS 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 PETERS 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 PETERS, 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 PETERS 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
Peters clay, 2 to 8 percent slopes1899504619332x8l6ca06719891:24000
Peters clay, 2 to 8 percent slopes21232104621042x8l6ca07719901:24000
Peters clay, 3 to 9 percent slopesPtB177462432hj65ca62819631:20000
Pentz-Peters association, 2 to 15 percent slopes451131229248852x8l9ca63020181:24000
Pentz-Peters association, 2 to 50 percent slopes47558929248862x8lbca63020181:24000
Peters clay, 2 to 8 percent slopes2126529248832x8l6ca63020181:24000
Peters-Pentz association, 2 to 8 percent slopes4016329248842x8l8ca63020181:24000
Pentz-Peters association, 2 to 15 percent slopes4512773316055112x8l9ca63220061:24000
Pentz-Peters association, 2 to 50 percent slopes4751188216055092x8lbca63220061:24000
Peters-Pentz association, 2 to 8 percent slopes401705714034392x8l8ca63220061:24000
Peters clay, 2 to 8 percent slopes21275614034302x8l6ca63220061:24000
Pentz-Peters-Cometa association, 2 to 15 percent slopes45275016055101qwnnca63220061:24000
Peters clay, 0 to 2 percent slopes28531314034381j3d6ca63220061:24000
Peters-Pentz complex, 0 to 8 percent slopesPxB7586462679hjg4ca64419591:24000
Peters clay, 2 to 8 percent slopesPtB40764626752x8l6ca64419591:24000
Peters cobbly clay, 0 to 8 percent slopesPvB3386462677hjg2ca64419591:24000
Peters-Pentz complex, 8 to 15 percent slopesPxC2672462680hjg5ca64419591:24000
Peters cobbly clay, 8 to 15 percent slopesPvC765462678hjg3ca64419591:24000
Peters clay, 8 to 15 percent slopesPtC533462676hjg1ca64419591:24000
Pentz-Peters association, 2 to 15 percent slopes4514329249672x8l9ca64419591:24000
Peters clay, 8 to 30 percent slopes, erodedPrD22979460906hglyca64519611:20000
Peters-Newville complex, 30 to 50 percent slopesPsE2880460908hgm0ca64519611:20000
Peters clay, 8 to 30 percent slopesPrD614460905hglxca64519611:20000
Peters clay, 1 to 8 percent slopesPrB107460904hglwca64519611:20000
Peters clay, 30 to 50 percent slopesPrE53460907hglzca64519611:20000
Peters cobbly clay, 0 to 8 percent slopesPoB1728463115hjx6ca64819591:20000
Peters clay, 2 to 8 percent slopesPnB11254631132x8l6ca64819591:20000
Peters cobbly clay, 8 to 30 percent slopesPoD907463116hjx7ca64819591:20000
Peters clay, 8 to 15 percent slopesPnC200463114hjx5ca64819591:20000

Map of Series Extent

Approximate geographic distribution of the PETERS 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 .