Official Series Description


Lab Data Summary

Aggregate lab data for the YOLO soil series. This aggregation is based on all pedons with a current taxon name of YOLO, 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 YOLO 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
1784P023665CA113002Yolo7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.533226,-121.7843781
1784P030683CA113001Yolo8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5373917,-121.7718811

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the YOLO 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 YOLO 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 YOLO 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 YOLO 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 YOLO 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 YOLO 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 YOLO 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 YOLO, 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 YOLO 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
Yolo clay loam, shallow over clayYh1849458913hdjnca02119611:20000
Yolo clay loam, moderately deep over clayYd1768458910hdjkca02119611:20000
Yolo clay loam, 0 to 3 percent slopes, MLRA 17Yc9094589092w89wca02119611:20000
Yolo silt loam, silty clay loam substratumYo318458915hdjqca02119611:20000
Yolo clay loam, slightly saline-alkaliYma257458914hdjpca02119611:20000
Yolo clay loam, deep over claypanYf178458911hdjlca02119611:20000
Yolo clay loam, moderately deep over hardpanYg27458912hdjmca02119611:20000
Yolo loam, 0 to 20 percent slopes, occasionally flooded, MLRA 15YoA13706935422w89mca05319721:24000
Yolo loam, 0 to 10 percent slopes, moist, MLRA 1418139554590052w89nca05519741:24000
Yolo loam, 0 to 15 percent slopes, moist, MLRA 151827304590062w89kca05519741:24000
Yolo silty clay loam, 0 to 2 percent slopes, MLRA 17Ysso268165332w8b1ca05519741:24000
Yolo loam, 0 to 15 percent slopes, dry, MLRA 15YoC31324563162w89lca06919651:20000
Yolo gravelly loam, 1 to 8 percent slopes, MLRA 15YvB18544563172vbtxca06919651:20000
Yolo loam, 0 to 20 percent slopes, occasionally flooded, MLRA 15YoA5984563152w89mca06919651:20000
Yolo silty clay loam, 0 to 2 percent slopes, MLRA 17Ys272584561392w8b1ca09519691:24000
Yolo loam, 0 to 4 percent slopes, MLRA 17Yo105064561372w89pca09519691:24000
Yolo loam, clay substratumYr4224456138h9n4ca09519691:24000
Yolo loam, 0 to 10 percent slopes, moist, MLRA 14181n788168822w89nca09519691:24000
Yolo silt loam, 0 to 5 percent slopes, MLRA 14YsA41264599122w8b0ca09719681:20000
Yolo sandy loam, overwash, 0 to 5 percent slopesYmB4025459908hfkrca09719681:20000
Yolo loam, 0 to 10 percent slopes, moist, MLRA 14YnA39584599092w89nca09719681:20000
Yolo sandy loam, 0 to 2 percent slopesYlA1553459907hfkqca09719681:20000
Yolo loam, overwash, 0 to 5 percent slopesYoB1524459910hfktca09719681:20000
Yolo clay loam, 0 to 5 percent slopes, MLRA 14YtA14684599132w89xca09719681:20000
Yolo gravelly loam, 0 to 8 percent slopes, MLRA 14YrB13934599112w89gca09719681:20000
Yolo silt loam, 0 to 2 percent slopes, MLRA 17Ya406364593082w89yca11319681:20000
Yolo silty clay loam, 0 to 2 percent slopes, MLRA 17Yb50394593092w8b1ca11319681:20000
Yolo loam, calcareous substratum, 0 to 6 percent slopes, MLRA 14YmA45294566312w89tca60919631:20000
Yolo loam over gravel, 0 to 3 percent slopesYo852456633hb53ca60919631:20000
Yolo loam, 0 to 8 percent slopes, MLRA 15YmB8244566322w89hca60919631:20000
Yolo gravelly loam, 0 to 3 percent slopesYr421456634hb54ca60919631:20000
Yolo sandy loam, 0 to 3 percent slopesYs306456635hb55ca60919631:20000
Yolo silt loam, 0 to 3 percent slopes, dry, MLRA 1416163754567142w89zca61019751:24000
Yolo silt loam, very gravelly substratum, 0 to 10 percent slopes, MLRA 17Yo23384609792w89qca64519611:20000
Yolo loam, clay loam substratumYs541460980hgpbca64519611:20000
Yolo clay loam, 0 to 3 percent slopes, MLRA 17Yt3244609812w89wca64519611:20000
Yolo loam, 0 to 7 percent slopes, MLRA 14YaA32124570642w89rca64619671:24000
Yolo silty clay loam, 0 to 2 percent slopes, rarely flooded, MLRA 14YeA18994570662w8b2ca64619671:24000
Yolo loam, 0 to 8 percent slopes, MLRA 15YaB4844570652w89hca64619671:24000
Yolo silty clay loam, 1 to 9 percent slopes, MLRA 14YeC2544570672w8b3ca64619671:24000
Yolo loam, 0 to 5 percent slopes, dry, MLRA 17YdA23984632252w89vca64819591:20000
Yolo loam, deep over hardpan, 0 to 1 percent slopesYeA497463226hk0sca64819591:20000
Yolo loam, 2 to 9 percent slopesYoC3512457941hcj9ca67519681:24000
Yolo loam, fan piedmont, 0 to 9 percent slopes, MLRA 20YoA30674579402w89sca67519681:24000
Yolo loam, 0 to 18 percent slopes, MLRA 20YoC377798882w89jca77619811:24000

Map of Series Extent

Approximate geographic distribution of the YOLO 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 .