Official Series Description


Lab Data Summary

Aggregate lab data for the MONTELL soil series. This aggregation is based on all pedons with a current taxon name of MONTELL, 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 MONTELL 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
83A10N1328S10TX3111007Montell8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties28.5158889,-98.7379722
83B86P0206S85TX271001Montell8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.1466675,-100.4338913

Water Balance

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

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Competing Series

Soil series competing with MONTELL 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 MONTELL 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 MONTELL 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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Click the image to view it full size.

Soil series sharing subgroup-level classification with MONTELL, 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. TX-2010-11-05-06 | Zapata County -

    Typical pattern of soils in the Maverick-Veleno-Catarina general soil map unit (Soil Survey of Zapata County, Texas).

Map Units

Map units containing MONTELL 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
Montell clay, 0 to 1 percent slopesMoA101043660032sxv1tx16319851:24000
Montell clay association, 0 to 1 percent slopesMc579893687002tlfftx27119651:20000
Montell clay, low, occasionally floodedMo7755368701dcnltx27119651:20000
Montell clay, saline, nearly levelMNA939368998dcz5tx28319881:24000
Montell clay, 0 to 3 percent slopesMtB334113702002tlfgtx31120101:24000
Montell clay association, 0 to 1 percent slopesMTA1050823926762tlfftx32319721:24000
Montell clay, 0 to 1 percent slopesMoA7243392679f5m2tx32319721:24000
Mercedes-Montell association, depressional, pondedMNA3362392675f5lytx32319721:24000
Montell clay, 0 to 1 percent slopesMcA339303705592sxv1tx32519721:24000
Montell clay, 1 to 3 percent slopesMcB8658370560dflktx32519721:24000
Montell clay, 0 to 3 percent slopesMt201363721332tlfgtx42719661:24000
Montell clay, 0 to 1 percent slopesMoA418553729042sxv1tx46319701:24000
Montell clayMe4706372903dj14tx46319701:24000
Montell clay, 1 to 3 percent slopesMoB4231372905dj16tx46319701:24000
Montell clay, 0 to 3 percent slopesMnB1729803732292tlfgtx47919821:31680
Montell clay, 0 to 3 percent slopesMtB78524416252tlfgtx50520091:24000
Montell clay association, 0 to 1 percent slopesMOA366123741142tlfftx60519821:24000
Montell clay, 0 to 1 percent slopesMnA268093741152sxv1tx60519821:24000

Map of Series Extent

Approximate geographic distribution of the MONTELL 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 .