Official Series Description


Lab Data Summary

Aggregate lab data for the NEWBELL soil series. This aggregation is based on all pedons with a current taxon name of NEWBELL, 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 NEWBELL 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 NEWBELL 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 NEWBELL 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 NEWBELL 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 NEWBELL 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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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with NEWBELL 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 NEWBELL 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 NEWBELL 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 terrace figure.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with NEWBELL, 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 NEWBELL 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
Highfalls-Pearsoncreek-Newbell families, complex, glaciated mountain slopes, belt geology, south aspects2lg1h60628507882lg1hid60120021:24000
Pearsoncreek-Highfalls-Newbell families, complex, moderately to deeply incised glaciated mountain slopes, belt geology, south aspects2lg1m23728507922lg1mid60120021:24000
Pearsoncreek-Marblecreek-Newbell families, complex, glaciated stream breaklands, metasedimentary belt geology2lfxz16228507792lfxzid60120021:24000
Pepoon-Newbell families-Rock outcrop complex, glaciated steep scoured mountain slopes, belt geology, south aspects2lg1z16128508002lg1zid60120021:24000
Pepoon-Newbell families-Rock outcrop complex, glaciated scoured ridges and upper mountain slopes, belt geology, south aspects2lg1x12028507982lg1xid60120021:24000
Highfalls-Pearsoncreek-Newbell families, complex, steep glaciated mountain slopes, belt geology, south aspects2lg1k9328507902lg1kid60120021:24000
Highfalls-Pearsoncreek-Newbell families, complex, moderately steep glaciated mountain slopes, belt geology, south aspects2lg1j7328507892lg1jid60120021:24000
Pearsoncreek-Highfalls-Newbell families, complex, shallow incised glaciated mountain slopes, belt geology, south aspects2lg1l4428507912lg1lid60120021:24000
Newbell-Pepoon families-Rock outcrop complex, glaciated scoured mountain slopes, belt geology, south aspects2lg1y1828507992lg1yid60120021:24000
Pearsoncreek-Highfalls-Newbell families, complex, glaciated mountain slopes, belt geology, all aspects2lg2n828508012lg2nid60120021:24000
Highfalls-Pearsoncreek-Newbell families, complex, moderately steep glaciated mountain slopes, belt geology, south aspects2lg1j22028508632lg1jid60419811:24000
Highfalls-Pearsoncreek-Newbell families, complex, glaciated mountain slopes, belt geology, south aspects2lg1h16228508352lg1hid60419811:24000
Highfalls-Pearsoncreek-Newbell families, complex, steep glaciated mountain slopes, belt geology, south aspects2lg1k15228508362lg1kid60419811:24000
Newbell-Pepoon families-Rock outcrop complex, glaciated scoured mountain slopes, belt geology, south aspects2lg1y6528508442lg1yid60419811:24000
Pepoon-Newbell families-Rock outcrop complex, glaciated steep scoured mountain slopes, belt geology, south aspects2lg1z6328508452lg1zid60419811:24000
Pearsoncreek-Highfalls-Newbell families, complex, moderately to deeply incised glaciated mountain slopes, belt geology, south aspects2lg1m5228508382lg1mid60419811:24000
Pepoon-Newbell families-Rock outcrop complex, glaciated scoured ridges and upper mountain slopes, belt geology, south aspects2lg1x3928508432lg1xid60419811:24000
Pearsoncreek-Marblecreek-Newbell families, complex, glaciated stream breaklands, metasedimentary belt geology2lfxz3728508232lfxzid60419811:24000
Pearsoncreek-Highfalls-Newbell families, complex, shallow incised glaciated mountain slopes, belt geology, south aspects2lg1l1628508372lg1lid60419811:24000
Pearsoncreek-Marblecreek-Newbell families, complex, glaciated stream breaklands, metasedimentary belt geology, rain-on-snow2lfy01029367712lfy0id60419811:24000
Highfalls-Pearsoncreek-Newbell families, complex, glaciated mountain slopes, belt geology, south aspects2505029823967802lg1hid6701:24000
Highfalls-Pearsoncreek-Newbell families, complex, moderately steep glaciated mountain slopes, belt geology, south aspects2512261423967812lg1jid6701:24000
Pearsoncreek-Marblecreek-Newbell families, complex, glaciated stream breaklands, metasedimentary belt geology1062236123966712lfxzid6701:24000
Pearsoncreek-Highfalls-Newbell families, complex, shallow incised glaciated mountain slopes, belt geology, south aspects2531159323967832lg1lid6701:24000
Pepoon-Newbell families-Rock outcrop complex, glaciated steep scoured mountain slopes, belt geology, south aspects2721083723967952lg1zid6701:24000
Pearsoncreek-Highfalls-Newbell families, complex, moderately to deeply incised glaciated mountain slopes, belt geology, south aspects255955923967842lg1mid6701:24000
Pepoon-Newbell families-Rock outcrop complex, glaciated scoured ridges and upper mountain slopes, belt geology, south aspects270833823967932lg1xid6701:24000
Newbell-Pepoon families-Rock outcrop complex, glaciated scoured mountain slopes, belt geology, south aspects271795623967942lg1yid6701:24000
Highfalls-Pearsoncreek-Newbell families, complex, steep glaciated mountain slopes, belt geology, south aspects252730223967822lg1kid6701:24000
Pearsoncreek-Highfalls-Newbell families, complex, glaciated mountain slopes, belt geology, all aspects290291223968162lg2nid6701:24000
Pearsoncreek-Highfalls-Newbell families, complex, gentle glaciated mountain slopes, belt geology, south aspects283215723968092lg2fid6701:24000
Newbell-Dufort-Pepoon families, complex, steep glaciated mountain slopes, belt geology, south aspects258158323967872lg1qid6701:24000
Pearsoncreek-Marblecreek-Newbell families, complex, glaciated stream breaklands, metasedimentary belt geology, rain-on-snow10797823966722lfy0id6701:24000
Newbell very bouldery silt loam, 25 to 40 percent slopes59wk462293683259wkid6701:24000
Newbell-Pepoon families-Rock outcrop complex, glaciated scoured steep mountain slopes with moderate to deeply incised draws, belt geology, south aspects27532323968012lg25id6701:24000
Newbell-Dufort families, complex, glaciated scoured mountain slopes with shallow to moderately incised draws, belt geology, south aspects27723423968042lg28id6701:24000
Newbell-Dufort-Pepoon families, complex, glaciated mountain slopes, belt geology, south aspects25716123967862lg1pid6701:24000
Newbell-Dufort-Pepoon families, complex, steep dissected glacially scoured mountain slopes, belt geology, south aspects2788523968052lg29id6701:24000
Newbell-Dufort-Pepoon families, complex, glaciated mountain slopes and ridges, belt geology, south aspects2565823967852lg1nid6701:24000
Newbell cobbly ashy silt loam, 0 to 40 percent slopes, stony168467731581322tcs2wa06519781:24000
Newbell-Rock outcrop complex, 40 to 65 percent slopes171245511581362tcs4wa06519781:24000
Newbell cobbly ashy silt loam, 40 to 65 percent slopes, stony169242201581332tcs3wa06519781:24000
Newbell ashy silt loam, 25 to 40 percent slopes166152741581302tcrzwa06519781:24000
Newbell ashy silt loam, 0 to 25 percent slopes165143521581292tcrywa06519781:24000
Newbell-Rock outcrop complex, 15 to 40 percent slopes170124231581352tcs1wa06519781:24000
Newbell ashy silt loam, 40 to 65 percent slopes167113041581312tcs0wa06519781:24000
Newbell bouldery sandy loam, 30 to 60 percent slopes2129566764828d6wa60819951:24000
Newbell silt loam, dry, 40 to 65 percent slopes3145808704502c9lwa64819871:24000
Newbell silt loam, dry, 20 to 40 percent slopes3132999704492c9kwa64819871:24000
Newbell silt loam, dry, 5 to 20 percent slopes312710704482c9jwa64819871:24000
Newbell cobbly ashy silt loam, 0 to 40 percent slopes, stony89195591584552tcs2wa65119811:24000
Newbell ashy silt loam, 0 to 25 percent slopes86184551584522tcrywa65119811:24000
Newbell-Rock outcrop complex, 15 to 40 percent slopes93177481584602tcs1wa65119811:24000
Newbell-Rock outcrop complex, 40 to 65 percent slopes94162241584612tcs4wa65119811:24000
Newbell ashy silt loam, 25 to 40 percent slopes87142111584532tcrzwa65119811:24000
Newbell ashy silt loam, 40 to 65 percent slopes88135521584542tcs0wa65119811:24000
Rock outcrop-Newbell complex, 30 to 65 percent slopes118753715832659r9wa65119811:24000
Newbell cobbly ashy silt loam, 40 to 65 percent slopes, stony9038681584572tcs3wa65119811:24000
Newbell very bouldery silt loam, 25 to 40 percent slopes91199715845859wkwa65119811:24000
Newbell very bouldery silt loam, 40 to 65 percent slopes9263515845959wlwa65119811:24000
Highfalls-Pearsoncreek-Newbell families, complex, glaciated mountain slopes, belt geology, south aspects2lg1h12128509052lg1hwa65119811:24000
Pearsoncreek-Highfalls-Newbell families, complex, moderately to deeply incised glaciated mountain slopes, belt geology, south aspects2lg1m4228509192lg1mwa65119811:24000
Pearsoncreek-Highfalls-Newbell families, complex, glaciated mountain slopes, belt geology, all aspects2lg2n3228509362lg2nwa65119811:24000
Highfalls-Pearsoncreek-Newbell families, complex, steep glaciated mountain slopes, belt geology, south aspects2lg1k3028509322lg1kwa65119811:24000
Pearsoncreek-Highfalls-Newbell families, complex, shallow incised glaciated mountain slopes, belt geology, south aspects2lg1l2528509122lg1lwa65119811:24000
Highfalls-Pearsoncreek-Newbell families, complex, moderately steep glaciated mountain slopes, belt geology, south aspects2lg1j528509232lg1jwa65119811:24000
Pearsoncreek-Marblecreek-Newbell families, complex, glaciated stream breaklands, metasedimentary belt geology2lfxz428509562lfxzwa65119811:24000

Map of Series Extent

Approximate geographic distribution of the NEWBELL 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 .