Official Series Description


Lab Data Summary

Aggregate lab data for the WACA soil series. This aggregation is based on all pedons with a current taxon name of WACA, 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 WACA 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
22AUCD673200167-CA-32-001xWACA3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.7004662,-120.9721909
22AUCD720404972-CA-04-049xWACA2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9893112,-121.4459915
22A00P035899CA061005Waca6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2177811,-120.1660156
22BUCD614512961-CA-45-129WACA2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6053085,-121.7091522
22BUCD794519579-CA-45-195xWACA1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6592522,-121.7381287
n/a84P046383CA091325Waca7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the WACA 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 WACA 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 WACA 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 WACA 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 flats position figure.

Competing Series

Soil series competing with WACA 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 WACA series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the WACA 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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Click the image to view it full size.

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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 WACA, 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-2010-08-30-02 | Tahoe Basin Area, California and Nevada - 2007

    Representative diagram of the Blackwood Canyon area (not to scale). The Waca-Ellispeak general soil map unit is in this area (Soil Survey of the Tahoe Basin Area, California and Nevada; 2007).

Map Units

Map units containing WACA 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
Waca-Windy complex, 2 to 30 percent slopes ***WAE3732331272zms1ca61419671:24000
Waca-Humicryepts, wet-Windy complex, 30 to 50 percent slopesWBF1132331292zms2ca61419671:24000
Waca very gravelly medial coarse sandy loam, 9 to 30 percent slopes7231236516522121sg85ca69320061:24000
Waca very gravelly medial coarse sandy loam, 30 to 50 percent slopes7232180716522131sg86ca69320061:24000
Ellispeak-Waca complex, 9 to 30 percent slopes713196616520991sg4jca69320061:24000
Ellispeak-Waca complex, 30 to 50 percent slopes713244116521001sg4kca69320061:24000
Waca very gravelly medial coarse sandy loam, 50 to 70 percent slopes723328616522141sg87ca69320061:24000
Ellispeak-Waca complex, 50 to 70 percent slopes713326416521011sg4lca69320061:24000
Waca-Woodseye families complex, 30 to 50 percent slopes.29442631471303htfbca71319841:24000
Waca-Woodseye families complex, 0 to 30 percent slopes.29323573471302htf9ca71319841:24000
Gibsonville-Waca families complex, 2 to 30 percent slopes.17910391471188ht9mca71319841:24000
Woodseye-Waca families-Rock outcrop complex, 10 to 50 percent slopes.3059472471314htfpca71319841:24000
Gibsonville-Waca families complex, 30 to 50 percent slopes.1807076471189ht9nca71319841:24000
Fopiano-Waca families complex, 30 to 50 percent slopes.1676087471176ht97ca71319841:24000
Waca-Woodseye families complex, 20 to 70 percent slopes, slumped.2965641471305htfdca71319841:24000
Waca-Woodseye families complex, 50 to 85 percent slopes.2955314471304htfcca71319841:24000
Gibsonville-Waca families complex, 50 to 75 percent slopes.1815310471190ht9pca71319841:24000
Fopiano-Waca families complex, 0 to 30 percent slopes.1664447471175ht96ca71319841:24000
Fopiano-Waca families complex, 50 to 70 percent slopes.1684039471177ht98ca71319841:24000
Woodseye-Waca families-Rock outcrop complex, 50 to 70 percent slopes.3063634471315htfqca71319841:24000
Waca-Portola families complex, 30 to 50 percent slopes.2913359471300htf7ca71319841:24000
Waca-Haypress families complex, 0 to 30 percent slopes.289809471298htf5ca71319841:24000
Waca-Portola families complex, 50 yo 70 percent slopes.292578471301htf8ca71319841:24000
Waca-Portola families complex, 0 to 30 percent slopes.290385471299htf6ca71319841:24000
Waca-Meiss complex, 30 to 50 percent slopesWDF25790464834hlpnca71919821:24000
Waca-Windy complex, 2 to 30 percent slopes ***WAE2116532331262zms1ca71919821:24000
Waca-Windy complex, 30 to 50 percent slopesWAF18609464829hlphca71919821:24000
Waca-Meiss complex, 2 to 30 percent slopesWDE16695464833hlpmca71919821:24000
Meiss-Waca complex, 30 to 50 percent slopesMKF14820464749hllxca71919821:24000
Waca-Meiss-Cryumbrepts, wet complex, 30 to 50 percent slopesWEF13499464836hlpqca71919821:24000
Meiss-Waca-Cryumbrepts, wet complex, 30 to 75 percent slopesMLG11598464752hlm0ca71919821:24000
Waca-Meiss-Cryumbrepts, wet complex, 2 to 30 percent slopesWEE9484464835hlppca71919821:24000
Waca-Humicryepts, wet-Windy complex, 30 to 50 percent slopesWBF633532331282zms2ca71919821:24000
Meiss-Waca-Rock outcrop complex, 30 to 50 percent slopes, severe ly erodedMKF36299464750hllyca71919821:24000
Waca-Cryumbrepts, wet-Windy complex, 2 to 30 percent slopesWBE6146464830hlpjca71919821:24000
Meiss-Waca complex, 2 to 30 percent slopesMKE6016464748hllwca71919821:24000
Meiss-Waca-Cryumbrepts, wet complex, 2 to 30 percent slopesMLE4544464751hllzca71919821:24000
Ahart-Waca, rhyolitic substratum-Cryumbrepts, wet complex, 2 to 30 percent slopesADE3925464602hlg5ca71919821:24000
Waca-Gullied land-Cryumbrepts, wet complex, 30 to 50 percent slo pesWCF3703464832hlplca71919821:24000
Ahart-Waca, rhyolitic substratum-Cryumbrepts, wet complex, 30 to 50 percent slopesADF3621464603hlg6ca71919821:24000
Ahart-Waca, rhyolitic substratum, 2 to 30 percent slopesACE3151464600hlg3ca71919821:24000
Ahart-Waca, rhyolitic substratum complex, 30 to 50 percent slopesACF2922464601hlg4ca71919821:24000
Jorge-Waca-Tahoma complex, 30 to 50 percent slopesJWF1638464708hlklca71919821:24000
Jorge-Waca-Cryumbrepts, wet complex, 2 to 30 percent slopesJXE1319464709hlkmca71919821:24000
Jorge-Waca-Tahoma complex, 2 to 30 percent slopesJWE764464707hlkkca71919821:24000
Jorge-Waca-Cryumbrepts, wet complex, 30 to 50 percent slopesJXF485464710hlknca71919821:24000
Rock outcrop-Waca, rhyolitic substratum-Ledmount variant complex ,2 to 30 percent slopesRVE439464792hln9ca71919821:24000
Waca-Windy complex, 5 to 30 percent slopes21610797464965hltwca72419851:24000
Waca cobbly sandy loam, 5 to 30 percent slopes2117694464960hltqca72419851:24000
Lithic Cryumbrepts-Waca association, 5 to 30 percent slopes1623265464912hls5ca72419851:24000
Ahart-Waca, rhyolitic substratum, 2 to 30 percent slopes complexACEtf318115913401qdxkca72419851:24000
Waca cobbly sandy loam, 30 to 50 percent slopes2122827464961hltrca72419851:24000
Waca-Lithic Cryumbrepts-Cryumbrepts, wet association 5 to 30 percent slopes2141752464963hlttca72419851:24000
Waca-Windy complex, 30 to 50 percent slopes2171663464966hltxca72419851:24000
Waca-Lithic Cryumbrepts association, 30 to 50 percent slopes2131400464962hltsca72419851:24000
Lithic Cryumbrepts-Waca association, 30 to 50 percent slopes163906464913hls6ca72419851:24000
Waca-Lithic Cryumbrepts-Cryumbrepts, wet association, 30 to 50 percent slopes215336464964hltvca72419851:24000

Map of Series Extent

Approximate geographic distribution of the WACA 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 .