Official Series Description


Lab Data Summary

Aggregate lab data for the WAPAL soil series. This aggregation is based on all pedons with a current taxon name of WAPAL, 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 WAPAL 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
43A85P08931985WA019001Wapal5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.6010583,-118.8396222

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the WAPAL 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 WAPAL 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 WAPAL 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 WAPAL 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 WAPAL 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 WAPAL 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 WAPAL 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 hills figure.

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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 WAPAL, 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 WAPAL 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
Rock outcrop, dioritic-Wapal family, moderately deep association, 45 to 75 percent slopes5036463470308hsd7ca70119841:24000
Wapal family, moderately deep-Deadman family, deep complex, 35 to 65 percent slopes5525736470319hsdlca70119841:24000
Wapal family, moderately deep-Hugo family, deep, dioritic association, 20 to 65 percent slopes5542721470320hsdmca70119841:24000
Wapal family, moderately deep, 35 to 65 percent slopes5502361470318hsdkca70119841:24000
Jayar, deep-Wapal families complex, 10 to 50 percent slopes.163st17190598421zbcca70219841:24000
Wapal-Patio deep-Anatone families association, 35 to 60 percent slopes.2827050470595hsphca70319831:24000
Wapal-Patio deep families association, 15 to 35 percent slopes.2812610470594hspgca70319831:24000
Wapal-Anatone-Patio deep families association, 60 to 90 percent slopes.280940470593hspfca70319831:24000
Jayar, deep-Wapal families complex, 10 to 50 percent slopes.1636017470761hsvvca70719831:24000
Typic Cryaquolls-Wapal family association, 0 to 30 percent slopes.3271315470925ht14ca70719831:24000
Rock outcrop, dioritic-Wapal family, moderately deep association, 45 to 75 percent slopes.503sr204186823220q1kca70719831:24000
Wapal family-Lithic Xerorthents, cool association, 50 to 75 percent slopesWpG17585471676httcca77719811:24000
Merkel-Wapal families complex, 30 to 50 percent slopesFbF6675471643hts9ca77719811:24000
Wapal-Corbett families association, 30 to 50 percent slopesWpF4575471675httbca77719811:24000
Corbett-Wapal families association, 2 to 30 percent slopesCoDE2640471621htrlca77719811:24000
Wapal gravelly ashy coarse sandy loam, 15 to 30 percent slopes3145202651287nvb9wa04319781:24000
Wapal gravelly ashy coarse sandy loam, 0 to 8 percent slopes31443437783727v9jjwa06320121:24000
Scoap-Wapal complex, 30 to 60 percent slopes31462904858772wc7wa06320121:24000
Wapal gravelly ashy coarse sandy loam, 15 to 30 percent slopes31452176621125nvb9wa06320121:24000
Bonner-Wapal complex, 8 to 15 percent slopes30311207783694v9hgwa06320121:24000
Bonner-Wapal complex, 8 to 15 percent slopes3031832651306v9hgwa06519781:24000
Wapal gravelly ashy sandy loam, 0 to 15 percent slopesWgC7081702082v73dwa61919681:24000
Wapal gravelly sandy loam, 35 to 65 percent slopesWgF2484702102c1vwa61919681:24000
Wapal gravelly sandy loam, 15 to 35 percent slopesWgE1461702092c1twa61919681:24000
Wapal sandy loam, 25 to 65 percent slopesWaF618702072c1rwa61919681:24000
Wapal ashy sandy loam, 0 to 20 percent slopes3911016026281qsnpwa61919681:24000
Wapal gravelly sandy loam, 30 to 65 percent slopes5084103706652cjjwa64819871:24000
Wapal gravelly ashy sandy loam, 0 to 15 percent slopes5052412706622v73dwa64819871:24000
Wapal gravelly sandy loam, 15 to 30 percent slopes507852706642cjhwa64819871:24000
Wapal cobbly sandy loam, 0 to 15 percent slopes506488706632cjgwa64819871:24000
Wapal ashy coarse sandy loam, 0 to 20 percent slopes5504805190286221w2nwa64920081:24000
Wapal-Rock outcrop complex, 35 to 65 percent slopes5561850210910928spswa64920081:24000
Wapal-Brevco complex, 15 to 35 percent slopes5541050210910828sprwa64920081:24000
Wapal stony ashy coarse sandy loam, 0 to 15 percent slopes5511020190000921s3mwa64920081:24000
Wapal-Sacheen complex, 35 to 65 percent slopes557690189982621rxqwa64920081:24000
Wapal stony ashy coarse sandy loam, 15 to 35 percent slopes552470190000721s3kwa64920081:24000
Wapal stony ashy coarse sandy loam, 35 to 65 percent slopes553310189999921s39wa64920081:24000
Wapal-Brevco complex, 35 to 65 percent slopes555195190000021s3bwa64920081:24000
Wapal-Brevco complex, 35 to 65 percent slopes39812170758712jygwa74920051:24000
Wapal-Rock outcrop complex, 35 to 65 percent slopes3998443758822jytwa74920051:24000
Wapal very stony ashy coarse sandy loam, dry, 35 to 65 percent slopes3964718758802jyrwa74920051:24000
Wapal very stony ashy coarse sandy loam, 15 to 35 percent slopes3944594758812jyswa74920051:24000
Wapal-Brevco complex, 15 to 35 percent slopes3973704758722jyhwa74920051:24000
Wapal stony ashy coarse sandy loam, 0 to 15 percent slopes3923294758872jyzwa74920051:24000
Wapal very stony ashy coarse sandy loam, 35 to 65 percent slopes3953167758702jyfwa74920051:24000
Wapal-Sacheen complex, 35 to 65 percent slopes4001543760342k3qwa74920051:24000
Lithic Haploxerepts-Wapal-Rock outcrop complex, 35 to 65 percent slopes2131507758792jyqwa74920051:24000
Wapal ashy sandy loam, 0 to 20 percent slopes3911339760572k4gwa74920051:24000
Wapal bouldery ashy sandy loam, 15 to 35 percent slopes393986760402k3xwa74920051:24000

Map of Series Extent

Approximate geographic distribution of the WAPAL 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 .