Official Series Description


Lab Data Summary

Aggregate lab data for the AYAR soil series. This aggregation is based on all pedons with a current taxon name of AYAR, 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 AYAR 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
15UCD581101458-CA-11-014Ayar2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4985657,-122.3289871

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the AYAR 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 AYAR 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 AYAR 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 AYAR 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 AYAR 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 AYAR 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 AYAR 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 AYAR, 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-2010-08-30-05 | Colusa County - 2006

    Typical pattern of soils on the western edge of the Sacramento Valley and on the Coast Range foothills (Soil Survey of Colusa County, California).

  2. CA-2012-05-08-20 | San Luis Obispo County, Carrizo Plain Area - 2003

    Idealized cross-section of the northwestern part of the survey area, showing soil-landscape-geology relationships (Soil Survey of San Luis Obispo County, California, Carrizo Plain Area; 2003).

Map Units

Map units containing AYAR 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
Ayar clay, 15 to 30 percent slopes2135122461597hhb7ca01119991:24000
Ayar clay, 5 to 15 percent slopes2123751461596hhb6ca01119991:24000
Balcom-Ayar complex, 30 to 50 percent slopes271907461617hhbwca01119991:24000
Balcom-Ayar complex, 15 to 30 percent slopes270817461616hhbvca01119991:24000
Ayar clay, 3 to 15 percent slopesAxC1158458588hd65ca02119611:20000
Ayar-Nacimiento clays, 10 to 30 percent slopesAyD558458589hd66ca02119611:20000
Ayar silty clay, 15 to 30 percent slopesAyE2040455560h91hca05319721:24000
Ayar silty clay, 5 to 15 percent slopesAyD1495455559h91gca05319721:24000
Ayar silty clay, 30 to 50 percent slopesAyF790455561h91jca05319721:24000
Diablo-Ayar clays, 9 to 30 percent slopes, erodedDaE220574456077h9l5ca09519691:24000
Diablo-Ayar clays, 2 to 9 percent slopesDaC7485456076h9l4ca09519691:24000
Ayar-Oneil complex, 30 to 50 percent slopes4201000466970hnxkca64219981:24000
Ayar clay, 30 to 50 percent slopes410815466969hnxjca64219981:24000
Ayar-Arburua complex, 15 to 30 percent slopes1282600462780hjkdca64719841:24000
Ayar clay, 30 to 50 percent slopes1261830462778hjkbca64719841:24000
Ayar clay, 5 to 8 percent slopes1231700462775hjk7ca64719841:24000
Ayar-Oneil complex, 30 to 50 percent slopes1301670462782hjkgca64719841:24000
Ayar clay 15 to 30 percent slopes125910462777hjk9ca64719841:24000
Ayar-Arburua complex, 8 to 15 percent slopes, MLRA 151278404627792tz0pca64719841:24000
Ayar clay, 8 to 15 percent slopes124600462776hjk8ca64719841:24000
Ayar-Arburua complex, 30 to 50 percent slopes129500462781hjkfca64719841:24000
Ayar-Arburua complex, 8 to 15 percent slopes, MLRA 158279184671502tz0pca65320001:24000
Ayar clay, 5 to 8 percent slopes823537467149hp3bca65320001:24000
Nacimiento-Ayar complex, 9 to 30 percent slopes17715695457280hbtzca66519771:24000
Ayar and Diablo soils, 15 to 30 percent slopes1108525457213hbrtca66519771:24000
Nacimiento-Ayar complex, 30 to 50 percent slopes1786260457281hbv0ca66519771:24000
Ayar and Diablo soils, 9 to 15 percent slopes1095610457212hbrsca66519771:24000
Millsholm-Ayar complex, 50 to 75 percent slopes1683415457271hbtpca66519771:24000
Ayar and Diablo soils, 30 to 50 percent slopes1112530457214hbrvca66519771:24000
Ayar-Hillbrick-Aido complex, 50 to 75 percent slopes1127718463657hkgpca66619831:24000
Ayar-Bluestone complex, 9 to 30 percent slopes1104819463655hkgmca66619831:24000
Ayar-Hillbrick-Aido complex, 30 to 50 percent slopes1114491463656hkgnca66619831:24000
Ayar silty clay, 5 to 9 percent slopes109298463654hkglca66619831:24000
Millsholm variant-Ayar association, 50 to 75 percent slopes199185463744hkkhca66619831:24000
Ayar-Hillbrick-Aido complex, 15 to 30 percent slopes2741630458476hd2kca66720031:24000
Ayar-Hillbrick-Aido complex, 30 to 50 percent slopes275885458477hd2lca66720031:24000
Ayar clay, 15 to 30 percent slopes271740458475hd2jca66720031:24000
Ayar silty clay, 5 to 9 percent slopes270250458553hd51ca66720031:24000
Ayar clay, 30 to 50 percent slopes, erodedAhF25336457560hc40ca67319741:24000
Ayar clay, 50 to 75 percent slopesAhG1322457561hc41ca67319741:24000
Ayar clay, 15 to 30 percent slopes, erodedAhE21178457559hc3zca67319741:24000
Ayar clay loam, 5 to 15 percent slopesAyD1051457804hccwca67519681:24000

Map of Series Extent

Approximate geographic distribution of the AYAR 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 .