Official Series Description


Lab Data Summary

Aggregate lab data for the PARRISH soil series. This aggregation is based on all pedons with a current taxon name of PARRISH, 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 PARRISH 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
15UCD561101756-CA-11-017Parrish3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4689407,-122.6065216
15UCD565200456-CA-52-004Parrish2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.1564293,-122.7555695
5UCD614511261-CA-45-112xPARRISH3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.4716034,-122.6852798

Water Balance

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

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 PARRISH 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 PARRISH 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 PARRISH 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 PARRISH, 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-2012-05-08-17 | Alameda Area - March 1966

    The relationship of geologic formations, landforms, and soil series in the Alameda Area (Soil Survey of Alameda Area, California; March, 1966).

Map Units

Map units containing PARRISH 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
Maymen-Parrish gravelly loams, 30 to 65 percent slopesMdpE2334458712hdb5ca02119611:20000
Parrish-Gullied land complex, 30 to 50 percent slopesPcE1296458795hddvca02119611:20000
Parrish gravelly loam, shallow, 30 to 50 percent slopesPbE1233458792hddrca02119611:20000
Parrish gravelly loam, 20 to 60 percent slopes, MLRA 15PaE11964587912w8cbca02119611:20000
Los Gatos-Parrish gravelly loams, 30 to 50 percent slopesLyE584458691hd9hca02119611:20000
Parrish-Gullied land complex, 10 to 30 percent slopesPcD496458794hddtca02119611:20000
Parrish gravelly loam, shallow, 50 to 65 percent slopesPbF428458793hddsca02119611:20000
Parrish-Yorkville-Gullied land complex, 30 to 50 percent slopesPdE144458797hddxca02119611:20000
Maymen-Parrish gravelly loams, 10 to 30 percent slopesMdpD102458711hdb4ca02119611:20000
Parrish-Yorkville-Gullied land complex, 10 to 30 percent slopesPdD76458796hddwca02119611:20000
Parrish loam, 30 to 50 percent slopesPcE5358460083hfrdca60719671:20000
Parrish loam, 8 to 30 percent slopesPcD2002460082hfrcca60719671:20000
Parrish loam, 50 to 70 percent slopesPcF539460084hfrfca60719671:20000
Parrish gravelly loam, 45 to 75 percent slopes, eroded, MLRA 15PaF239814566042tyy9ca60919631:20000
Parrish gravelly loam, 30 to 45 percent slopes, eroded, MLRA 15PaE2182528333852tyy8ca60919631:20000
Parrish gravelly loam, 20 to 60 percent slopes, MLRA 15PaE295204608982w8cbca64519611:20000
Parrish-Los Gatos gravelly loams, 30 to 50 percent slopesPgE3382460900hglrca64519611:20000
Parrish gravelly loam, 50 to 65 percent slopesPaF2323460899hglqca64519611:20000
Parrish gravelly loam, 10 to 30 percent slopesPaD848460897hglnca64519611:20000
Parrish gravelly clay loam, 50 to 75 percent slopesPfG6472457036hbl3ca64619671:24000
Parrish gravelly clay loam, 30 to 50 percent slopesPfF2517457035hbl2ca64619671:24000
Parrish gravelly clay loam, 9 to 30 percent slopesPfE619457034hbl1ca64619671:24000
Parrish gravelly loam, 30 to 45 percent slopes, eroded, MLRA 15PaE2aa50128333862tyy8ca64619671:24000
Parrish gravelly loam, 45 to 75 percent slopes, eroded, MLRA 15PaF2aa1156993932tyy9ca64619671:24000
Parrish-Goulding families complex, 20 to 60 percent slopes.2441611470842hsygca70719831:24000
Secca-Parrish families complex, 40 to 60 percent slopes.2871370470885hszvca70719831:24000
Parrish family, 20 to 50 percent slopes.243319470841hsyfca70719831:24000
Parrish loam, 8 to 30 percent slopesPcDsh39186844420q8dca70719831:24000
Parrish loam, 30 to 50 percent slopesPcEsh3186844620q8gca70719831:24000
Parrish loam, 50 to 70 percent slopesPcFsh3186844820q8jca70719831:24000
Parrish-Maymen complex, 10 to 40 percent slopes29330727478062q1yzca70920101:24000

Map of Series Extent

Approximate geographic distribution of the PARRISH 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 .