Official Series Description


Lab Data Summary

Aggregate lab data for the COUNCELOR soil series. This aggregation is based on all pedons with a current taxon name of COUNCELOR, 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 COUNCELOR 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
3588P074688NM031001Councelor8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.9827766,-107.371666
3688P013388NM039001Councelor8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.3047218,-107.2772217
3688P013888NM039006Councelor8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.2883339,-107.4058304

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the COUNCELOR 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 COUNCELOR 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 COUNCELOR 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 COUNCELOR 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 COUNCELOR 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 COUNCELOR 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 COUNCELOR 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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Soil series sharing subgroup-level classification with COUNCELOR, 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. NM-2010-09-13-05 | McKinley County -

    Generalized cross section illustrating soil-geomorphic-geologic relationships of soils on the Chaco slope of the San Juan Basin (Soil Survey of McKinley County, New Mexico).

  2. NM-2012-02-14-06 | Jicarilla Apache Nation, Parts of Rio Arriba and Sandoval Counties - 2004

    Conceptual diagram of the major soil and landscape positions of the Largo Plains-Tapicito Plateau transition (Soil Survey of Jicarilla Apache Nation, New Mexico, Parts of Rio Arriba and Sandoval Counties; 2004).

Map Units

Map units containing COUNCELOR 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
Mespun-Councelor-Mespun, limy substratum complex, 0 to 10 percent slopes302576514723512v4k1az70720111:24000
Mespun-Councelor-Mespun, limy substratum complex, 0 to 10 percent slopes2412612310181052v4k1az71120081:24000
Councelor-Moclom-Hawaikuh complex, 1 to 60 percent slopes85059320248962v1bzaz71120081:24000
Tsosie-Councelor-Campanile complex, 1 to 6 percent slopes546296924233492sdxdaz71320111:24000
Tsosie-Councelor-Riverwash complex, 0 to 4 percent slopes554177124233502sdxfaz71320111:24000
Councelor-Moclom-Hawaikuh complex, 1 to 60 percent slopes143965623982382v1bzaz71320111:24000
Pinavetes-Gish-Councelor complex, 1 to 15 percent slopes392429824325932sdxkaz71320111:24000
Blancot-Councelor-Tsosie association, 0 to 5 percent slopes27059888563781wnnnm65619871:24000
Councelor-Eslendo-Mespun complex, 5 to 30 percent slopes1807491563401wmfnm65619871:24000
Tsosie-Councelor-Blancot fine sandy loams, 1 to 3 percent slopes1018890572112r73wnm69220011:24000
Councelor-Calladito complex, 1 to 8 percent slopes137954572232s28dnm69220011:24000
Councelor-Eslendo-Calladito complex, 2 to 25 percent slopes147064572241xjynm69220011:24000
Blancot-Councelor-Tsosie complex, 0 to 5 percent slopes7017350574871xtfnm69820001:24000

Map of Series Extent

Approximate geographic distribution of the COUNCELOR 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 .