Official Series Description


Lab Data Summary

Aggregate lab data for the ARGONAUT soil series. This aggregation is based on all pedons with a current taxon name of ARGONAUT, 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 ARGONAUT 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
17UCD660400166-CA-04-001xARGONAUT3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3354874,-121.4852448
18UCD660501866-CA-05-018xArgonaut3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.9205437,-120.722509
18UCD660501966-CA-05-019xArgonaut3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.9751405,-120.7370031
18UCD675811867-CA-58-118xARGONAUT4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3730125,-121.2338867
18UCD730507573-CA-05-075xArgonaut3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0296086,-120.586181
1884P088084CA115004Argonaut8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.1313896,-121.2811127
1891P041390CA115003Argonaut7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2694435,-121.3022232
1891P041690CA115006Argonaut6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2355537,-121.3044434
1891P041790CA115007Argonaut7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2355537,-121.3044434
1891P041890CA115008Argonaut7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2355537,-121.3044434
1840A2913S1959CA005005Argonaut4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3544426,-120.7958298
1840A2880S1959CA005006Argonaut5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3608322,-120.8083344

Water Balance

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

Soil series sharing subgroup-level classification with ARGONAUT, 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 ARGONAUT 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
Argonaut-Auburn complex, 3 to 8 percent slopes1078300461851hhlfca06719891:24000
Auburn-Argonaut-Rock outcrop complex, 8 to 30 percent slopes1103710461854hhljca06719891:24000
Argonaut-Auburn-Urban land complex, 3 to 8 percent slopes108760461852hhlgca06719891:24000
Vistarobles-Redding-Argonaut taxadjunct-Haploxererts , 0 to 9 percent slopes5906247824117wnkfca61220051:24000
Dunstone-Lomarica-Argonaut taxadjunct , 15 to 30 percent slopes5514766461424hh4nca61220051:24000
Dunstone-Loafercreek-Argonaut taxadjunct , 2 to 15 percent slopes5674575461541hh8fca61220051:24000
Dunstone-Argonaut taxadjunct-Sunnyslope , 2 to 15 percent slopes5654148461434hh4zca61220051:24000
Argonaut-Auburn complex, 3 to 8 percent slopes1025065460368hg1lca61819911:24000
Argonaut-Auburn complex, 8 to 15 percent slopes1032120460370hg1nca61819911:24000
Argonaut-Auburn complex, 15 to 30 percent slopes1041885460372hg1qca61819911:24000
Auburn-Timbuctoo-Argonaut complex, 8 to 15 percent slopes1221145460408hg2wca61819911:24000
Auburn-Timbuctoo-Argonaut complex, 3 to 8 percent slopes121545460406hg2tca61819911:24000
Auburn-Argonaut complex, 2 to 15 percent slopesAwC1399460186hfvqca61919701:24000
Argonaut-Rock outcrop complex, 2 to 30 percent slopesAsD1066460181hfvkca61919701:24000
Argonaut gravelly loam, 2 to 15 percent slopesArC825460180hfvjca61919701:24000
Argonaut-Auburn complex, 3 to 8 percent slopes102405640461phg1ca61919701:24000
Auburn-Argonaut complex, 2 to 15 percent slopes1153500460279hfyqca62019751:24000
Auburn-Argonaut-Rock outcrop complex, 2 to 15 percent slopes1162200460280hfyrca62019751:24000
Rescue very stony sandy loam, 3 to 15 percent slopesRfC6535462272hj10ca62419681:20000
Rescue very stony sandy loam, 15 to 30 percent slopesRfD2471462273hj11ca62419681:20000
Argonaut very rocky loam, 3 to 30 percent slopesAmD2304462191hhydca62419681:20000
Argonaut gravelly loam, 2 to 15 percent slopesAkC2304462189hhybca62419681:20000
Argonaut loam, seeped variantAoB1203462193hhygca62419681:20000
Rescue sandy loam, 9 to 15 percent slopesReC740462270hj0yca62419681:20000
Argonaut clay loam, 3 to 9 percent slopesAnB653462192hhyfca62419681:20000
Argonaut extremely stony loam, 15 to 30 percent slopesAlD542462190hhycca62419681:20000
Rescue sandy loam, 15 to 30 percent slopesReD249462271hj0zca62419681:20000
Auburn-Argonaut very rocky silt loams, 3 to 31 percent slopesAxD3554462336hj32ca62819631:20000
Argonaut very rocky loam, 3 to 31 percent slopesAoD3098462323hj2nca62819631:20000
Auburn-Argonaut silt loams, 0 to 16 percent slopesAwC1445462335hj31ca62819631:20000
Argonaut gravelly loam, 3 to 31 percent slopesAnD697462322hj2mca62819631:20000
Agua Dulce-Botella-Argonaut families association 20 to 60 percent slopes111799465274hm4vca77219811:24000

Map of Series Extent

Approximate geographic distribution of the ARGONAUT 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 .