Official Series Description


Lab Data Summary

Aggregate lab data for the MCCROSKET soil series. This aggregation is based on all pedons with a current taxon name of MCCROSKET, 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 MCCROSKET 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
905N0148S2004ID009008McCrosket6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.1688881,-117.0063858

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MCCROSKET 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 MCCROSKET 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 MCCROSKET 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 MCCROSKET 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 terrace figure.

There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with MCCROSKET 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 MCCROSKET 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 MCCROSKET 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 terrace figure.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with MCCROSKET, 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 MCCROSKET 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
McCrosket-Ardenvoir complex, 20 to 50 percent slopesTk5232214877081ly2lid05720131:24000
McCrosket-Ardenvoir association, 35 to 65 percent slopes14722448794372v729id60619761:24000
McCrosket-Tekoa association, 12 to 60 percent slopes14812799794382v72bid60619761:24000
McCrosket-Ardenvoir association, 20 to 35 percent slopes1466700794362nngid60619761:24000
Ardenvoir-McCrosket association, 15 to 35 percent slopes6012326629861hnbzid60619761:24000
Kruse-McCrosket complex, 35 to 65 percent slopes1561038777322v2vxid61220031:24000
Taney-McCrosket complex, 15 to 35 percent slopes223946777406v2ymid61220031:24000
McCrosket-Ardenvoir association, 35 to 65 percent slopes71180113900472v729id62020131:24000
Ardenvoir-McCrosket association, 35 to 65 percent slopes70176613900331hnfsid62020131:24000
McCrosket-Tekoa association, 12 to 60 percent slopes71249213900502v72bid62020131:24000
McCrosket-Ardenvoir association, 15 to 35 percent slopes71049213900441hng4id62020131:24000
Ardenvoir-McCrosket association, 15 to 35 percent slopes60140513899461hnbzid62020131:24000
McCrosket-Ardenvoir association, 35 to 65 percent slopes2v729219729366332v729id6701:24000
McCrosket-Ardenvoir association, 20 to 35 percent slopes2nng158828510142nngid6701:24000
McCrosket-Tekoa association, 12 to 60 percent slopes2v72b158029366382v72bid6701:24000
McCrosket-Ardenvoir association, 15 to 35 percent slopes971068822302381hng4wa06320121:24000
McCrosket-Tekoa association, 12 to 60 percent slopes971240022302402v72bwa06320121:24000
Ardenvoir-McCrosket association, 35 to 65 percent slopes970117722302341hnfswa06320121:24000
McCrosket-Ardenvoir association, 35 to 65 percent slopes97114622302392v729wa06320121:24000
McCrosket-Tekoa association, 12 to 60 percent slopes971210226513872v72bwa07519751:20000
McCrosket-Ardenvoir association, 15 to 35 percent slopes710227430951hng4wa07519751:20000

Map of Series Extent

Approximate geographic distribution of the MCCROSKET 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 .