Official Series Description


Lab Data Summary

Aggregate lab data for the QUERENCIA soil series. This aggregation is based on all pedons with a current taxon name of QUERENCIA, 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 QUERENCIA 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
3687P068387NM043001Querencia6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.7127762,-106.9988861
3687P0684S87NM043001Querencia7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.7127778,-106.9988889

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the QUERENCIA 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 QUERENCIA 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 QUERENCIA 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 QUERENCIA 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 QUERENCIA 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 QUERENCIA 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 QUERENCIA 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 mountains figure.

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Soil series sharing subgroup-level classification with QUERENCIA, 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 QUERENCIA 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
Wineg-Querencia association, 0 to 3 percent slopes332418833812502zmybaz63119801:24000
Querencia-Manikan association, 3 to 10 percent slopes365185332960272ttgjaz63119801:24000
Wineg-Querencia association, 0 to 5 percent slopes253290344147931kglaz6951:24000
Querencia family, 1 to 6 percent slopes15335251566622644az7121:24000
Begay-Querencia-Rizno complex, 1 to 10 percent slopes114235924279032sdxjaz71320111:24000
Querencia clay loam, 0 to 3 percent slopes266420547142sfmgaz71419851:24000
Querencia and Gish soils, 0 to 2 percent slopes9014813580962sfl4az71520071:24000
Querencia clay loam, 0 to 3 percent slopes8973216506622sfmgaz71520071:24000
Querencia loam, 1 to 8 percent slopes23122450563661wn8nm65619871:24000
Querencia-Zia complex, 2 to 8 percent slopes23422125563671wn9nm65619871:24000
Sandoval-Querencia association, 2 to 7 percent slopes1311436563301wm3nm65619871:24000
Penistaja-Querencia complex, 2 to 7 percent slopes6810942564591wr8nm65619871:24000
Querencia-Lavodnas association, 2 to 15 percent slopes2226047572311xk5nm69220011:24000
Begay, saline-Querencia, saline-sodic complex, 1 to 9 percent slopes10320925044762q3shut68519901:24000
Querencia-Lybrook complex, 2 to 35 percent slopes, saline-sodic65190425074412q70but68519901:24000

Map of Series Extent

Approximate geographic distribution of the QUERENCIA 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 .