Official Series Description


Lab Data Summary

Aggregate lab data for the TORTUGAS soil series. This aggregation is based on all pedons with a current taxon name of TORTUGAS, 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 TORTUGAS were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
3578P003577AZ005004Tortugas7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.3730545,-112.898056

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the TORTUGAS 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.

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the TORTUGAS series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

There are insufficient data to create the sibling sketch figure.

Select annual climate data summaries for the TORTUGAS series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the TORTUGAS 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 .

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

There are insufficient data to create the 3D mountains figure.

There are insufficient data to create the 3D terrace figure.

There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with TORTUGAS share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

There are insufficient data to create the competing sketch figure.

Select annual climate data summaries for the TORTUGAS series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the TORTUGAS 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 .

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

There are insufficient data to create the 3D mountains figure.

There are insufficient data to create the 3D terrace figure.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with TORTUGAS, 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-2011-05-27-23 | Long Valley Area - 1974

    Typical patterns of soil in area south of East Clear Creek (Soil Survey of Long Valley Area, Arizona; 1974).

  2. AZ-2011-05-27-24 | Long Valley Area - 1974

    Typical pattern of soils in area north of East Clear Creek (Soil Survey of Long Valley Area, Arizona; 1974).

  3. UT-2012-05-10-03 | Washington County Area - October 1977

    West to east cross section of the Washington County Area, showing the relationship of the soils on the landscape (Soil Survey of Washington County Area, Utah; October 1977).

Map Units

Map units containing TORTUGAS 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
Tortugas extremely rocky loam, 15 to 60 percent slopesTnF69234529361s2maz63719681:31680
Tortugas very rocky loam, 8 to 30 percent slopesTmD57390529351s2laz63719681:31680
Tortugas gravelly loam, 2 to 8 percent slopesTlB9631529341s2kaz63719681:31680
Tortugas very stony loam, 0 to 30 percent sloepsToD1963715275221n8hxaz64319671:31680
Jacks-Tortugas extremely rocky complex, 20 to 45 percent slopesJtE812115274971n8h3az64319671:31680
Jacks-Tortugas extremely rocky complex, 0 to 20 percent slopesJtD703715274961n8h2az64319671:31680
Faraway-Tortugas-Rock outcrop association, steepFtF1803014252881jv41az66719711:20000
Tortugas-Rock outcrop complex, 25 to 60 percent slopesTrF1332814278081jxrbaz66719711:20000
Tortugas-Rock outcrop complex, 5 to 25 percent slopesTrE883414278071jxr9az66719711:20000
Tortugas-Roundtop-Rock outcrop complex, 30 to 50 percent slopes109E27046539201t3caz68319741:24000
Tortugas-Rock outcrop complex, 30 to 50 percent slopes107E21645539181t39az68319741:24000
Tortugas cobbly loam, 15 to 30 percent slopes106D19950539171t38az68319741:24000
Tortugas-Chevelon-Rock outcrop complex, 30 to 50 percent slopes108E16382539191t3baz68319741:24000
Roundtop-Tortugas-Rock outcrop complex, 30 to 50 percent slopes76E5822539981t5waz68319741:24000
Tortugas-Showlow-Rock outcrop complex, 30 to 50 percent slopes110E2033539221t3faz68319741:24000
Tortugas-Daze complex, 0 to 15 percent slopes15A629617130391vhkbaz6931:24000
Tortugas cobbly loam, 2 to 15 percent slopes15248117130381vhk9az6931:24000
Tortugas cobbly and gravelly loam, 15 to 30 percent slopes15B96417130401vhkcaz6931:24000
Tortugas-Rock outcrop association, extremely steep9177272375656dlwynm63219811:63360
Tortugas-Asparas-Rock outcrop association, moderately sloping8945503375653dlwvnm63219811:63360
Tortugas-Rock outcrop association, moderately sloping9044124375655dlwxnm63219811:63360
Tanbark-Tortugas association, very steep8820100375652dlwtnm63219811:63360
Ruidoso-Tortugas association, moderately sloping7710610375640dlwfnm63219811:63360
Tortugas-Ruidoso-Rock outcrop association, very steep925178375657dlwznm63219811:63360
Penapon-Tortugas very cobbly loams, extremely steep602555375622dlvvnm63219811:63360
Tortugas cobbly loam, 5 to 30 percent slopesTOE91421635717pbj0nm64619761:24000
Rock outcrop-Tortugas-Ustifluvents complex, 0 to 80 percent slopesRTE13705635706pbhnnm64619761:24000
Tortugas-Deama association, moderately steepTPE9886635718pbj1nm64619761:24000
Tortugas-Deama association, very steepTPG9070635719pbj2nm64619761:24000
Welring-Tortugas very gravelly loams, 20 to 70 percent slopesWAG31050484817j8h8ut64119711:24000
Tortugas-Rock land associationTG2485484810j8h1ut64119711:24000

Map of Series Extent

Approximate geographic distribution of the TORTUGAS 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 .