Official Series Description


Lab Data Summary

Aggregate lab data for the CAGUABO soil series. This aggregation is based on all pedons with a current taxon name of CAGUABO, 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 CAGUABO 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
27001N1040S2001PR125001RCaguabo6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties18.0925007,-67.0361099

Water Balance

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

There are insufficient data to create the water balance bar figure.



There are insufficient data to create the water balance line figure.

Sibling Summary

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

Click the image to view it full size.

Select annual climate data summaries for the CAGUABO 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 CAGUABO 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

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

Click the image to view it full size.

Select annual climate data summaries for the CAGUABO 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 CAGUABO 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 CAGUABO, 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. PR-2012-05-10-01 | Caribbean National Forest and Luquillo Experimental Forest - 2002

    Typical pattern of soils in the isohyperthermic temperature regime (Soil Survey of Caribbean National Forest and Luquillo Experimental Forest, Commonwealth of Puerto Rico; 2002).

Map Units

Map units containing CAGUABO 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
Caguabo-Rock outcrop complex, 20 to 60 percent slopesCbF21193264022wx4rpr68219791:20000
Caguabo clay loam, 20 to 60 percent slopesCaF10883264012thqspr68219791:20000
Caguabo clay loam, 20 to 60 percent slopesCbF126903265172thqspr68419691:20000
Caguabo clay loam, 40 to 60 percent slopesCaF543563266452wx4ppr68619741:20000
Caguabo clay loam, 20 to 40 percent slopesCaE29513266442wx4npr68619741:20000
Caguabo-Rock outcrop complex, 20 to 60 percent slopesCbF23243266462wx4rpr68619741:20000
Caguabo gravelly clay loam, 20 to 60 percent slopesCbF2222383267952wx4qpr68819711:20000
Caguabo-Rock outcrop complex, 20 to 60 percent slopesCdF80153267962wx4rpr68819711:20000
Caguabo clay loam, 20 to 60 percent slopesCbF314903268632thqspr68919691:20000
Sonadora-Caguabo complex, 40 to 90 percent slopesSoG100027062332qz0hpr68919691:20000
Urban land-Caguabo complex, 20 to 60 percent slopesUcF50033188242yg2vpr68919691:20000
Sonadora-Caguabo complex, 20 to 40 percent slopesSoE19027062322qz0gpr68919691:20000
Caguabo clay loam, 12 to 20 percent slopesCbD1333268622thqqpr68919691:20000
Caguabo gravelly clay loam, 12 to 20 percent slopesCaD8027062312qz0jpr68919691:20000
Sonadora-Caguabo complex, 40 to 90 percent slopesSoG72625538352qz0hpr70019921:20000
Sonadora-Caguabo complex, 20 to 40 percent slopesSoE31025538342qz0gpr70019921:20000
Caguabo gravelly clay loam, 12 to 20 percent slopesCaD14825538322qz0jpr70019921:20000
Caguabo clay loam, 20 to 60 percent slopesCbF1257613560802thqspr78720071:20000
Caguabo clay loam, 12 to 20 percent slopesCbD15313560782thqqpr78720071:20000

Map of Series Extent

Approximate geographic distribution of the CAGUABO 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 .