Official Series Description


Lab Data Summary

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

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

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Soil series sharing subgroup-level classification with TAHAWUS, 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 TAHAWUS 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
Monadnock-Tahawus complex, 3 to 15 percent slopes, very bouldery657C15444318503bpf9ny03120071:24000
Monadnock-Tunbridge-Tahawus complex, 0 to 15 percent slopes, rocky, very bouldery649C150493185052xj23ny03120071:24000
Adirondack-Tahawus complex, 0 to 8 percent slopes, very bouldery705B13523318502bpf8ny03120071:24000
Tahawus peat, 0 to 5 percent slopes, very boulderyTaA418617144291vk05ny03120071:24000
Monadnock-Tahawus complex, 15 to 35 percent slopes, very bouldery657D2735318504bpfbny03120071:24000
Adirondack-Tahawus complex, 0 to 8 percent slopes, very bouldery705B114091913249226wqny03320181:24000
Monadnock-Tahawus complex, 3 to 15 percent slopes, very bouldery657C87871913244226wkny03320181:24000
Monadnock-Tunbridge-Tahawus complex, 0 to 15 percent slopes, rocky, very bouldery649C254619132342xj23ny03320181:24000
Monadnock-Tahawus complex, 15 to 35 percent slopes, very bouldery657D11621913243226wjny03320181:24000
Wilmington-Tahawus complex, 0 to 8 percent slopes, very bouldery938B3925216502ql2yny03320181:24000
Tahawus peat, 0 to 5 percent slopes, very boulderyTaA3926794921vk05ny03320181:24000
Adirondack-Tahawus complex, 0 to 8 percent slopes, very bouldery705B243118069226wqny03520071:24000
Monadnock-Tahawus complex, 3 to 15 percent slopes, very bouldery657C13118068226wkny03520071:24000
Adirondack-Tahawus complex, 0 to 8 percent slopes, very bouldery705B2413118073226wqny04119941:62500
Monadnock-Tahawus complex, 15 to 35 percent slopes, very bouldery657D153118072226wjny04119941:62500
Monadnock-Tahawus complex, 3 to 15 percent slopes, very bouldery657C139382518247226wkny04320181:24000
Monadnock-Tunbridge-Tahawus complex, 0 to 15 percent slopes, rocky, very bouldery649C1203525149782xj23ny04320181:24000
Adirondack-Tahawus complex, 0 to 8 percent slopes, very bouldery705B71892518232226wqny04320181:24000
Wilmington-Tahawus complex, 0 to 8 percent slopes, very bouldery938B193825216492ql2yny04320181:24000
Monadnock-Tahawus complex, 15 to 35 percent slopes, very bouldery657D4612514985226wjny04320181:24000
Adirondack-Tahawus complex, 0 to 8 percent slopes, very bouldery705B52072516311226wqny04920181:24000
Monadnock-Tahawus complex, 3 to 15 percent slopes, very bouldery657C30662516805226wkny04920181:24000
Monadnock-Tunbridge-Tahawus complex, 0 to 15 percent slopes, rocky, very bouldery649C147425168012xj23ny04920181:24000
Adirondack-Tahawus complex, 0 to 8 percent slopes, very bouldery705B103118094226wqny06519931:24000
Monadnock-Tahawus complex, 3 to 15 percent slopes, very bouldery657C1743118043226wkny08919901:24000
Adirondack-Tahawus complex, 0 to 8 percent slopes, very bouldery705B533118044226wqny08919901:24000

Map of Series Extent

Approximate geographic distribution of the TAHAWUS 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 .