Official Series Description


Lab Data Summary

Aggregate lab data for the ARVADA soil series. This aggregation is based on all pedons with a current taxon name of ARVADA, 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 ARVADA 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
58B40A3431S1954WY025001Arvada6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.8052788,-106.5916672
58B40A3809S1977WY005001ARVADA8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.2880554,-105.0961075
60A79P017078SD047311Arvada6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0592833,-103.2890222
60A86P059586NE165018Arvada7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.9213905,-103.9113922
60A81P0461S1981NE165002Arvada6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.9294434,-103.5141678
67B91P086891CO123004Arvada8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8288879,-104.7450027
6990P00361999CO073002TUDArvada8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5967778,-103.3553889
6987P026187CO073001Arvada7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5327797,-103.621666
6984P069499CO073141ARVADA6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5708917,-103.8431333
n/a82P075382KS199003Arvada3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ARVADA 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 ARVADA 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 ARVADA 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 ARVADA 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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Click the image to view it full size.

There are insufficient data to create the 3D mountains figure.

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Click the image to view it full size.

Competing Series

Soil series competing with ARVADA 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 ARVADA 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 ARVADA 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 ARVADA, 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. CO-2011-05-27-18 | Prowers County - 1966

    Main soils and underlying materials in soil association 8 (Soil Survey of Prowers County, Colorado; 1966).

  2. CO-2011-05-27-19 | Prowers County - 1966

    Cross sections showing relationships of the soils to the landscape and to the underlying geologic formations in Prowers County. The upper cross section shows relationships in the western part of the county, and the lower shows those in the eastern part of the county (Soil Survey of Prowers County, Colorado; 1966).

Map Units

Map units containing ARVADA 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
Arvada loam, 0 to 3 percent slopesAdB200529403934vjco00119681:20000
Arvada-Deertrail complex, 0 to 1 percent slopes26708943073545co01719851:24000
Arvada clay loam, 0 to 5 percent slopes102589761050023j85co07320011:24000
Arvada silt loam931569457635dvco07519741:24000
Arvada clay loamAc17299479235mtco09919631:15840
Arvada loam, 0 to 3 percent slopesAaA1639952713648co62419631:20000
Arvada complex, 0 to 3 percent slopes, erodedAcB2496952723649co62419631:20000
Arvada-Keyner complex, 0 to 4 percent slopesAR10534954812xyr8co62619741:24000
Arvada clay loam, 0 to 2 percent slopes6638497505jppkco64119801:24000
Arvada loam, 1 to 6 percent slopes310000496770jnxvco68319771:24000
Arvada loam, 6 to 20 percent slopes45300496781jny6co68319771:24000
Bridgeport-Arvada complex, rarely flooded1351348114960817l84ks18119671:24000
Bridgeport-Arvada complex, rarely flooded13512873115018717lvtks19919841:24000
Arvada-Laurel complexAx6368345381cldbmt10319611:20000
Gilt Edge-Arvada complexGb6245345428clfvmt10319611:20000
Arvada complexAv1923345380cld9mt10319611:20000
Arvada loam, 0 to 3 percent slopesAr146345379cld8mt10319611:20000
Arvada-Bone silty clay loams, 0 to 1 percent slopesAx8889345684clq3mt11119661:20000
Arvada-Bone clays, 0 to 1 percent slopesAy8106345685clq4mt11119661:20000
Hydro-Arvada clay loams, 0 to 2 percent slopesHw7292345741clrymt11119661:20000
Vananda-Bone clays, 4 to 7 percent slopesVe5451345815clvbmt11119661:20000
Arvada clay loam, 0 to 1 percent slopesAu4394345681clq0mt11119661:20000
Arvada clay loam, 1 to 4 percent slopesAv4145345682clq1mt11119661:20000
Fort Collins-Arvada clay loams, 0 to 1 percent slopesFl2542345714clr2mt11119661:20000
Arvada clay loam, 4 to 7 percent slopesAw738345683clq2mt11119661:20000
Fort Collins-Arvada clay loams, 1 to 4 percent slopesFo315345715clr3mt11119661:20000
Arvada-Laurel complexAv56381472964y8hmt60219631:20000
Beckton-Arvada clay loamsBc50291473024y8pmt60219631:20000
Rhoades-Arvada complexRo40441474094yd4mt60219631:20000
Arvada-Beckton complex, salineAu7921472954y8gmt60219631:20000
Arvada-Beckton cobbly clay loamsAt6601472944y8fmt60219631:20000
Arvada-Terrad claysAw3781472974y8jmt60219631:20000
Arvada-Bone claysAye12624345870clx3mt60719701:24000
Arvada silty clay loamAyd3725345869clx2mt60719701:24000
Arvada-Bone complex, 0 to 4 percent slopesAb45859347833cnyfmt64319671:20000
Hydro-Arvada complex, 2 to 8 percent slopesHw13141347878cnzwmt64319671:20000
Arvada clay loam, 0 to 1 percent slopes505141116536921shsxne15719651:20000
Arvada loam, 0 to 3 percent slopes5050926027592342qp1qne16519931:20000
Arvada-Slickspots complex, 0 to 3 percent slopesAsA3452127680352s040sd01919701:24000
Arvada silt loam, 0 to 3 percent slopesArA1294827680342s03zsd01919701:24000
Arvada loam, 0 to 3 percent slopesAr1935927680442qp1qsd04719801:24000
Lohmiller-Arvada complexLv4697354113cwh0sd05519921:24000
Arvada silt loamAr1979354070cwfmsd05519921:24000
Arvada-Slickspots complexAs240354071cwfnsd05519921:24000
Arvada-Slickspots complex, 0 to 3 percent slopes600B1527680492s040sd08120071:24000
Arvada silt loam, 0 to 3 percent slopesAnB1599227680552s03zsd60019741:24000
Arvada-Slickspots complex, 0 to 3 percent slopesArB146327680562s040sd60019741:24000
Arvada loam, 0 to 3 percent slopesArA1546927680662qp1qsd60620111:24000
Beckton-Arvada complex, 0 to 4 percent slopesBhA511325808712y6dysd60620111:24000
Arvada-Slickspots complex, 0 to 3 percent slopesAsA171127680712s040sd60720111:24000
Satanta-Arvada complex, 2 to 6 percent slopesSfB6662586440cyf2sd60720111:24000
Arvada variant loam, 0 to 2 percent slopesApA3592586402cyc1sd60720111:24000
Arvada loamAr86692581000cy1xsd61120111:24000
Beckton-Arvada loams, 0 to 2 percent slopesBdA25212581004cy21sd61120111:24000
Arvada-Slickspots complexAs18312581001cy1ysd61120111:24000
Arvada, thick surface-Arvada-Slickspots complex, 0 to 6 percent slopes2572117802512v09wwy01119781:24000
Absted-Arvada complex, 0 to 3 percent slopes1005799349513cqpmwy02719931:24000
Forkwood-Haverdad association2129732152065537bwy04319761:24000
Arvada-Olney association578171520955389wy04319761:24000
Arvada, thick surface-Arvada-Slickspots complex, 0 to 6 percent slopes13111623616862v09wwy04519841:24000
Absted-Arvada complex, 0 to 3 percent slopes15233416148371r6cjwy04519841:24000
Arvada, thick surface-Arvada-Slickspots complex, 0 to 6 percent slopes102360283497872v09wwy60519951:24000
Emigha, sodic-Arvada, thick surface complex, 0 to 4 percent slopes1424190349827cr0rwy60519951:24000
Arvada, thick surface very fine sandy loam, 0 to 6 percent slopes1013890349786cqzfwy60519951:24000
Absted-Arvada-Slickspots complex, 0 to 6 percent slopes101132929206402v093wy60920061:24000
Absted-Arvada-Bone complex, 0 to 6 percent slopes1006416697781t1jtwy60920061:24000
Petrie-Arvada complex, 0 to 6 percent slopes236188168482wlrpwy61919711:24000
Arvada-Absted-Slickspots complex, 0 to 6 percent slopes112702815021902v099wy62519851:24000
Petrie-Arvada complex, 0 to 6 percent slopes236294765023622wlrpwy62519851:24000
Arvada-Slickspots complex, 0 to 3 percent slopes113138995021912yrz1wy62519851:24000
Arvada fine sandy loam, 0 to 6 percent slopes -- Draft40AB15255253r1wy6291:24000
Winnett-like-Arvada-Ulm complex, 0 to 10 percent slopes -- Draft34015252353q3wy6291:24000
Bidman-Arvada fine sandy loams, 0 to 6 percent slopes1122744361103d3rhwy63319871:24000
Bidman-Arvada complex, moist, 0 to 3 percent slopes1131471361104d3rjwy63319871:24000
Absted-Arvada-Slickspots complex, 0 to 6 percent slopes253263329206412v093wy70520031:24000
Absted-Arvada-Bone complex, 0 to 6 percent slopes10157399351479csr1wy70919831:24000
Absted-Arvada complex, 0 to 3 percent slopes22393414278411jxsdwy70919831:24000
Arvada, thick surface-Arvada-Slickspots complex, 0 to 6 percent slopes2001133612682v09wwy70919831:24000
Arvada-Absted-Slickspots complex, 0 to 6 percent slopes2504114279072v099wy70919831:24000

Map of Series Extent

Approximate geographic distribution of the ARVADA 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 .