Aggregate lab data for the PORTALES soil series. This aggregation is based on all pedons with a current taxon name of PORTALES, 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 PORTALES were used in the calculation. Source: KSSL snapshot Methods used to assemble the KSSL snapshot used by SoilWeb / SDE
.Pedons used in the lab summary:
Monthly water balance estimated using a leaky-bucket style model for the PORTALES 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.
Siblings are those soil series that occur together in map units, in this case with the PORTALES series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot
, parsed OSD records and snapshot of SC database .Select annual climate data summaries for the PORTALES series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data
.Geomorphic description summaries for the PORTALES 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 .
Soil series competing with PORTALES share the same family level classification in Soil Taxonomy. Source: parsed OSD records
and snapshot of the SC database .Select annual climate data summaries for the PORTALES series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data
.Geomorphic description summaries for the PORTALES 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 .
Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.
Relative position and underlying material of main soils of Portales Valley: A, B, Mansker (shallow) and Potter (very shallow), underlain by rocky caliche and High Plains marl. C, Church, underlain by strongly calcareous lake sediments. D, Drake, underlain by strongly calcareous sediments from lakebeds. E, F, Arch and Portales, underlain by strongly calcareous valley fill of mixed wind- and water-deposited materials. G, Blackwater, underlain by valley fill and, in turn, by hard caliche at moderate depths. H, Clovis, underlain by mixed water- and wind-deposited sediments from the High Plains upland. I, J, K, Kimbrough, Amarillo, and Arvana, underlain by mixed water- and wind-deposited materials from the High Plains upland; Kimbrough soils underlain by hard caliche at shallow depth, and Arvana soils by hard caliche at moderate depth. L, M, Springer (deep) and Tivoli (very deep), underlain by wind-deposited sands (Soil Survey of Portales Area, New Mexico; May 1959).
Typical landscape in the central and eastern part of Cimarron County: Associations 1, 2, 3, and 5 (Soil Survey of Cimarron County, Oklahoma; June 1960).
Typical pattern of soils in the Pullman general soil map unit (Soil Survey of Deaf Smith County, Texas; 2007).
Acuff-Olton-Amarillo (Soil Survey of Hockely County, Texas).
Amarillo-Acuff (Soil Survey of Hockely County, Texas).
Berda-Potter-Creta (Soil Survey of Hockely County, Texas).
Midessa-Portales-Drake (Soil Survey of Hockely County, Texas).
Patricia-Amarillo (Soil Survey of Hockely County, Texas).
Pattern of soils and underlying materials in the Arch general soil map unit (Soil Survey of Lynn County, Texas; 2008).
Pattern of soils and underlying materials in the Estacado-Pep general soil map unit (Soil Survey of Lynn County, Texas; 2008).
Pattern of soils and underlying materials in the Midessa-Lenorah-Hindman general soil map unit (Soil Survey of Lynn County, Texas; 2008).
Pattern of soils and underlying materials in the Midessa-Potter-Drake general soil map unit (Soil Survey of Lynn County, Texas; 2008).
Amarillo fine sandy loam association (Soil Survey of Bailey County, TX; 1963).
Arch-Drake association (Soil Survey of Bailey County, TX; 1963).
Soils and underlying formations associated with a saline lake in Bailey County (Soil Survey of Bailey County, TX; 1963).
Soils in a playa on high plains and associated soils (Soil Survey of Dawson County, TX; 1960).
Diagram showing typical locations of soil series and the underlying parent material (Soil Survey of Hansford County, TX; 1960).
Some soils of general soil area 1 (Soil Survey of Lamb County, TX; 1962).
Soils and underlying formations surrounding a saline lake (now Bull and Illusion Lakes) (Soil Survey of Lamb County, TX; 1962).
Soils formed in plains outwash (Soil Survey of Runnels County, TX; 1970).
Soils in a playa (Soil Survey of Terry County, TX; 1962).
Relationship of soils in the Abilene-Mobeetie-Berda association to parent material and relief (Soil Survey of Wheeler County, TX; 1975).
Map units containing PORTALES as a major component. Limited to 250 records.
Approximate geographic distribution of the PORTALES 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 .