Official Series Description


Lab Data Summary

Aggregate lab data for the ZAMORA soil series. This aggregation is based on all pedons with a current taxon name of ZAMORA, 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 ZAMORA 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
1590P022889CA021004Zamora7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.7822227,-122.4722214
1790P022789CA021003Zamora7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.7819443,-122.461113

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ZAMORA 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 ZAMORA 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 ZAMORA 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 ZAMORA 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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Competing Series

Soil series competing with ZAMORA 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 ZAMORA 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 ZAMORA 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 ZAMORA, 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 ZAMORA 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
Zamora silty clay loam, 0 to 3 percent slopes, MLRA 14ZaA54154558702xcbtca01319731:24000
Zamora silty clay loam, 2 to 15 percent slopes, MLRA 14ZaB9704558712xcc0ca01319731:24000
Zamora silty clay loam, 0 to 3 percent slopes, MLRA 17ZbA215314589182xcbvca02119611:20000
Zamora silty clay loam, 2 to 8 percent slopesZbB3555458919hdjvca02119611:20000
Zamora silty clay loam, slightly saline-alkali, 0 to 2 percent slopesZma1305458922hdjyca02119611:20000
Zamora silty clay loam, deep over silty clay, 0 to 2 percent slopesZd1093458921hdjxca02119611:20000
Zamora silty clay, 0 to 2 percent slopesZa749458917hdjsca02119611:20000
Zamora silty clay loam, moderately saline-alkali, 0 to 2 percen slopesZmb496458923hdjzca02119611:20000
Zamora silty clay loam, deep over hardpan, 0 to 2 percent slopeZc156458920hdjwca02119611:20000
Zamora silty clay loam, moist, 0 to 2 percent slopes, MLRA 14ZaA94094599192xcbwca09719681:20000
Zamora silty clay loam, moist, 0 to 8 percent slopes, MLRA 14ZaB31374599202xcc1ca09719681:20000
Zamora loamZa3420459310hdygca11319681:20000
Zamora silt loam, 0 to 4 percent slopesZa2280456636hb56ca60919631:20000
Zamora silty clay loam, dry, 0 to 1 percent slopes, MLRA 14Zc6804566372xcbyca60919631:20000
Zamora loam, 2 to 9 percent slopes4091324354762mr9rca64120091:24000
Zamora clay loam, 0 to 3 percent slopesZc4018460983hgpfca64519611:20000
Zamora loam, 0 to 3 percent slopesZa1608460982hgpdca64519611:20000
Zamora silt loam, 0 to 3 percent slopesZm1064460984hgpgca64519611:20000
Zamora silty clay loam, 0 to 1 percent slopes, MLRA 17Zo6654609852xcbzca64519611:20000
Zamora clay loam, 0 to 2 percent slopesZbA2871457070hbm6ca64619671:24000
Zamora clay loam, 2 to 9 percent slopesZbC855457071hbm7ca64619671:24000
Zamora loam, 0 to 2 percent slopesZaA540457068hbm4ca64619671:24000
Zamora loam, 2 to 9 percent slopesZaC411457069hbm5ca64619671:24000
Zamora and Cropley soils, 2 to 9 percent slopes, severely erodedZeC3339457072hbm8ca64619671:24000
Zamora loam, 2 to 9 percent slopesZmC2117457793hccjca67419681:24000
Zamora loam, 9 to 15 percent slopes, erodedZmD21153457794hcckca67419681:24000
Ojai-Zamora loams, 15 to 30 percent slopesOzE1225457881hcgcca67519681:24000
Zamora loam, 2 to 9 percent slopesZaC720457942hcjbca67519681:24000
Zamora loam, 9 to 15 percent slopesZaD94457943hcjcca67519681:24000
Zamora clay loam, 2 to 9 percent slopesZcC8457944hcjdca67519681:24000

Map of Series Extent

Approximate geographic distribution of the ZAMORA 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 .