Official Series Description


Lab Data Summary

Aggregate lab data for the LOS GUINEOS soil series. This aggregation is based on all pedons with a current taxon name of LOS GUINEOS, 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 LOS GUINEOS 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
27086P0303S1986PR119010Los Guineos7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties18.313055,-65.8241653
27140A0572S1961PR057001Los Guineos6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties17.9866676,-66.038887
n/a86P025385PR119004Los Guineos6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a81P0323S1981PR003002LOS GUINEOS4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the LOS GUINEOS 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 LOS GUINEOS 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 LOS GUINEOS 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 LOS GUINEOS 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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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 LOS GUINEOS 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 LOS GUINEOS 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 LOS GUINEOS 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 LOS GUINEOS, 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-2012-05-10-02 | Caribbean National Forest and Luquillo Experimental Forest - 2002

    Typical pattern of the soils that are derived from volcanic sandstone and siltstone in the isothermic temperature regime. (The Dwarf soils are at the highest elevations and are in the isomesic temperature regime.) (Soil Survey of Caribbean National Forest and Luquillo Experimental Forest, Commonwealth of Puerto Rico; 2002).

Map Units

Map units containing LOS GUINEOS 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
Los Guineos clay, 40 to 60 percent slopesLgF76313264482tgwvpr68219791:20000
Los Guineos-Maricao-Rock outcrop association, steepLME4702326443bypfpr68219791:20000
Los Guineos clay, 20 to 40 percent slopesLgE23203264472tgwtpr68219791:20000
Los Guineos clay, 12 to 20 percent slopesLgD8463264462tgwxpr68219791:20000
Los Guineos clay, 20 to 60 percent slopes, erodedLuF21709326566bytdpr68419691:20000
Los Guineos clay, 12 to 20 percent slopesLuD1003265652tgwxpr68419691:20000
Los Guineos clay, 40 to 60 percent slopesLsF133873266812tgwvpr68619741:20000
Los Guineos clay, 20 to 40 percent slopesLsE31523266802tgwtpr68619741:20000
Los Guineos-Maricao association, steepLyFX6680326826bz2spr68819711:20000
Los Guineos clay, 40 to 60 percent slopesLuF51213268252tgwvpr68819711:20000
Los Guineos clay, 20 to 40 percent slopesLuE19603268242tgwtpr68819711:20000
Los Guineos clay, 40 to 60 percent slopesLsF113803269072tgwvpr68919691:20000
Los Guineos clay, 20 to 40 percent slopesLsE21973269062tgwtpr68919691:20000
Los Guineos-Yunque-Stony rock land association steepLyF432326908bz5fpr68919691:20000
Los Guineos clay, 12 to 20 percent slopesLsD2173269052tgwxpr68919691:20000
Yunque-Los Guineos-Moteado complex, 5 to 40 percent slopesYqE12027062382qz0ppr68919691:20000
Yunque-Los Guineos-Moteado complex, 5 to 40 percent slopesYqE192025538402qz0ppr70019921:20000

Map of Series Extent

Approximate geographic distribution of the LOS GUINEOS 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 .