Official Series Description


Lab Data Summary

Aggregate lab data for the GOBLIN soil series. This aggregation is based on all pedons with a current taxon name of GOBLIN, 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 GOBLIN 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.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the GOBLIN 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 GOBLIN 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 GOBLIN 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 GOBLIN 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 GOBLIN 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 GOBLIN 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 GOBLIN 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 GOBLIN, 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

No block diagrams are available.

Map Units

Map units containing GOBLIN 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
Moenkopie-Goblin complex, 5 to 50 percent slopes5426364523731rhgaz62319941:24000
Berzatic family-Rock outcrop-Goblin complex, 35 to 70 percent slopes1023049522321rbxaz62319941:24000
Goblin gravelly fine sandy loam, 15 to 50 percent slopes2310702522991rf2az62319941:24000
Goblin-Gyppocket complex, 2 to 10 percent slopes242745523001rf3az62319941:24000
Mussentuchit-Goblin-Swell association, 3 to 20 percent slopes1063907616539381sj1vut62320111:24000
Goblin-Gypsum Land-Mussentuchit complex, 5 to 50 percent slopes055767116694581t16hut62320111:24000
Goblin-Clapper complex, 8 to 65 percent slopes0543841884046217hput62320111:24000
Goblin family-Badland, gypsum-Mussentuchit family complex, 5 to 50 percent slopes41172599931938652z932ut6251:24000
Mussentuchit-Goblin-Swell association, 3 to 20 percent slopes3135642319411030njtut6251:24000
Mussentuchit-Goblin-Swell association, 3 to 20 percent slopes311146431938882z93tut6251:24000
Goblin-Clapper, extremely stony complex, 8 to 65 percent slopes3130402319410530njnut6251:24000
Goblin-Chipeta complex3716958551641vdhut63119821:24000
Robroost-Goblin complex, eroded8513585552171vg6ut63119821:24000
Robroost-Goblin complex8410577552161vg5ut63119821:24000
Sheppard-Goblin complex1004264551111vbsut63119821:24000
Trachute-Goblin complex1123424551241vc6ut63119821:24000
Mivida-Goblin complex55574551841vf4ut63119821:24000
Lavodnas family-Goblin family-Badland complex, 4 to 35 percent slopes39210524855472pfdyut6421:63360
Goblin fine sandy loam, 15 to 70 percent slopes28602725044722q3scut68519901:24000
Goblin-Ivanpatch complex, 2 to 60 percent slopes30252625044672q3s6ut68519901:24000
Goblin-Clapper complex, 8 to 65 percent slopes29123425560382qdrkut68519901:24000
Mussentuchit-Goblin-Swell family association, 3 to 20 percent slopes5546825560372qdrjut68519901:24000
Goblin very gravelly sandy loam, 6 to 45 percent slopes9536323985992lhy5ut68820091:24000
Goblin very gravelly sandy loam, 6 to 45 percent slopes987324530272nbkxut6891:24000

Map of Series Extent

Approximate geographic distribution of the GOBLIN 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 .