Official Series Description


Lab Data Summary

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

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
130B88P087288NC199005Thunder7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.9677773,-82.2688904

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the THUNDER 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 THUNDER 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 THUNDER series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

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

Click the image to view it full size.

Geomorphic description summaries for the THUNDER 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 .

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.

Soil series sharing subgroup-level classification with THUNDER, 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 THUNDER 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
Saunook-Thunder complex, 15 to 30 percent slopes, very stonyShD5183548104ldbsnc01119971:12000
Saunook-Thunder complex, 8 to 15 percent slopes, very stonyShC949548103ldbrnc01119971:12000
Thunder-Saunook complex, 15 to 30 percent slopes, very boulderyTsD25548116ldc5nc01119971:12000
Thunder-Saunook complex, 30 to 50 percent slopes, very boulderyTsE10548117ldc6nc01119971:12000
Thunder-Saunook complex, 8 to 15 percent slopes, very boulderyTsC3548115ldc4nc01119971:12000
Thunder-Saunook complex, 15 to 30 percent slopes, very boulderyTsD8678547597lctfnc12119971:12000
Saunook-Thunder complex, 15 to 30 percent slopes, stonySdD7761547587lct3nc12119971:12000
Thunder-Saunook complex, 30 to 50 percent slopes, very boulderyTsE4739547598lctgnc12119971:12000
Thunder-Saunook complex, 8 to 15 percent slopes, very boulderyTsC2242547596lctdnc12119971:12000
Saunook-Thunder complex, 30 to 50 percent slopes, stonySdE718547588lct4nc12119971:12000
Thunder-Saunook complex, 2 to 8 percent slopes, very boulderyTsB272547595lctcnc12119971:12000
Thunder-Saunook complex, 15 to 30 percent slopes, very boulderyTsD6277547868ld35nc19919971:12000
Thunder-Saunook complex, 30 to 50 percent slopes, very boulderyTsE4630547869ld36nc19919971:12000
Saunook-Thunder complex, 15 to 30 percent slopes, stonySdD3726547865ld32nc19919971:12000
Thunder-Saunook complex, 8 to 15 percent slopes, very boulderyTsC1158547867ld34nc19919971:12000
Thunder-Saunook complex, 2 to 8 percent slopes, very boulderyTsB278547866ld33nc19919971:12000
Thunder cobbly loam, 35 to 55 percent slopes, very bouldery57E59816705711t2cdva07720061:24000
Thunder cobbly loam, 15 to 35 percent slopes, very bouldery57D413516792kbrqva07720061:24000
Thunder cobbly loam, 35 to 55 percent slopes56E11316125361r3z9va07720061:24000
Thunder cobbly loam, 15 to 35 percent slopes56D10216125371r3zbva07720061:24000
Thunder cobbly loam, 2 to 15 percent slopes, very bouldery57C43516791kbrpva07720061:24000
Thunder cobbly loam, 2 to 15 percent slopes56C3516125381r3zcva07720061:24000
Saunook-Thunder complex, 15 to 25 percent slopes, very stony42D59814742751lh38va14120081:24000
Saunook-Thunder complex, 8 to 15 percent slopes, very stony42C46314742741lh37va14120081:24000
Saunook-Thunder complex, 2 to 8 percent slopes, very stony42B1714742731lh36va14120081:24000
Thunder-Saunook complex, 15 to 35 percent slopes, very bouldery66E170225148622qdddva16320101:24000
Thunder-Saunook complex, 35 to 55 percent slopes, very bouldery66F162225148632qddfva16320101:24000
Thunder-Saunook complex, 3 to 15 percent slopes, very bouldery66C120425148612qddcva16320101:24000
Thunder extremely stony loam, 15 to 35 percent slopes, rubbly38DS282124210382m890va6061:24000
Thunder very cobbly loam, 15 to 35 percent slopes, very stony38D189424210362m88yva6061:24000
Thunder very cobbly loam, 35 to 60 percent slopes, very stony38E142024200792m792va6061:24000
Thunder extremely stony loam, 35 to 60 percent slopes, rubbly38ES102124210392m891va6061:24000
Thunder extremely stony loam, 3 to 15 percent slopes, rubbly38CS53624210372m88zva6061:24000
Thunder very cobbly loam, 3 to 15 percent slopes, very stony38C44724200812m794va6061:24000
Thunder-Sylva complex, 0 to 15 percent slopes, very bouldery3928124200782m791va6061:24000
Thunder extremely stony loam, 60 to 80 percent slopes, rubbly38FS25924210402m892va6061:24000
Thunder very cobbly loam, 15 to 35 percent slopes, bouldery38DU17224210412m893va6061:24000
Thunder very cobbly loam, 15 to 35 percent slopes, very stony32E7431740802z3fmva8501:24000

Map of Series Extent

Approximate geographic distribution of the THUNDER 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 .