Official Series Description


Lab Data Summary

Aggregate lab data for the DELNORTE soil series. This aggregation is based on all pedons with a current taxon name of DELNORTE, 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 DELNORTE 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
4285P064685TX141001Delnorte6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.9127769,-106.543335
4285P064785TX141002Delnorte6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.9127769,-106.5175018
n/a97P009096NM013003Delnorte7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the DELNORTE 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 DELNORTE 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 DELNORTE 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 DELNORTE 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 DELNORTE 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 DELNORTE 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 DELNORTE 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 flats position figure.

Soil series sharing subgroup-level classification with DELNORTE, 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. AZ-2010-08-30-04 | Pima County, Eastern Part - 2003

    Typical soil and landscape relationship in the San Pedro River Valley (Soil Survey of Pima County, Arizona, Eastern Part; 2003).

  2. AZ-2011-05-27-27 | Pima County, Eastern Part - 2003

    Typical soil and landscape relationship in the San Pedro River Valley (Soil Survey of Pima County, Arizona, Eastern Part; 2003).

Map Units

Map units containing DELNORTE 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
Stagecoach-Haplogypsids-Delnorte complex, 5 to 80 percent slopes9348735114630717gtnaz66120091:24000
Nahda-Delnorte complex, 1 to 10 percent slopes6936100114630817gtpaz66120091:24000
Stagecoach-Delnorte complex, 5 to 45 percent slopes923529322316802dx7paz66120091:24000
Delnorte-Nahda complex, 3 to 20 percent slopes271580024056012lr71az66120091:24000
Stagecoach-Whitlock-Delnorte complex, chihuahuan, 5 to 20 percent slopes771550016774061t9gwaz66620071:24000
Stagecoach-Whitlock-Delnorte complex, sonoran, 5 to 20 percent slopes78540016931671ttw9az66620071:24000
Delnorte-Stagecoach complex, 1 to 20 percent slopes229604537812tdt9az66919931:24000
Delnorte-Nahda complex, 5 to 45 percent slopes161047225136032qcf4az6731:24000
Stagecoach-Delnorte complex, 5 to 45 percent slopes458624985702pzp5az6731:24000
Nahda-Delnorte complex, 1 to 10 percent slopes286724985672pzp2az6731:24000
Stagecoach-Haplogypsids-Delnorte complex, 5 to 80 percent slopes465424985712pzp6az6731:24000
Stagecoach-Whitlock-Delnorte complex, sonoran, 5 to 20 percent slopes48524985632pznyaz6731:24000
Nahda-Delnorte complex, 1 to 10 percent slopes50272023847942l1kvaz67520091:24000
Stagecoach-Haplogypsids-Delnorte complex, 5 to 80 percent slopes7936923847922l1ksaz67520091:24000
Delnorte-Stagecoach complex, 1 to 20 percent slopes16114280545532tdt9az70319931:24000
Delnorte-Vado family complex, 5 to 25 percent slopes200132940302x17mnm02319671:31680
Delnorte-Cave-Tencee complex, moderately rolling30156150565071wstnm66019811:48000
Nickel-Tencee-Delnorte complex, moderately sloping6448904565481wv4nm66019811:48000
Delnorte-Stagecoach-Turney complex, 0 to 15 percent slopes245414424043042lpw6nm68820141:24000
Stagecoach-Delnorte-Riverwash association, 0 to 35 percent slopes complex7641708190653221zx1nm68820141:24000
Delnorte-Canutio complex, 8 to 15 percent slopes95639582101ykrnm71920001:24000
Delnorte-Canutio complex, 3 to 8 percent slopes94602582091ykqnm71920001:24000
Delnorte association, gently undulating681928585221ywttx37119771:31680
Delnorte-Chilicotal association, rolling12403636585311yx3tx38919761:24000
Upton-Delnorte association, nearly level4257658585641yy5tx38919761:24000
Canutio-Delnorte complex, 1 to 3 percent slopes109026585291yx1tx38919761:24000
Delnorte gravelly soils, undulatingDE99485590111zdltx47519691:24000
Chamberino-Delnorte association, rollingCDD11394586591z17tx61519941:31680
Delnorte-Canutio association hillyDCD29900696619rcwltx62419671:31680
Delnorte-Canutio association, undulatingDCB16598696618rcwktx62419671:31680

Map of Series Extent

Approximate geographic distribution of the DELNORTE 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 .