Official Series Description


Lab Data Summary

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

Soil series sharing subgroup-level classification with MEGONOT, 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 MEGONOT 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
Cambeth, noncalcareous-Megonot complex, 8 to 15 percent slopes297D647963433802w7p4mt01719951:24000
Cambeth, noncalcareous-Megonot complex, 2 to 8 percent slopes297C290533433792w7p3mt01719951:24000
Cambeth, noncalcareous-Megonot complex, 2 to 8 percent slopes373C1193783426352w7p3mt03320021:24000
Cambeth, noncalcareous-Megonot complex, 8 to 15 percent slopes373D732363426362w7p4mt03320021:24000
Kobase-Megonot silty clay loams, 1 to 8 percent slopes140B4236344478cghrmt06519961:24000
Megonot-Yawdim silty clay loams, 4 to 15 percent slopes68C4093344617cgkymt06519961:24000
Kobase-Megonot silty clay loams, calcareous, 1 to 8 percent slopes140C559344479cghsmt06519961:24000
Megonot-Yawdim silty clay loams, 25 to 60 percent slopes182F5058346613cmp2mt61519921:24000
Megonot-Kobase-Delpoint complex, 2 to 8 percent slopes142C2512346601cmnpmt61519921:24000
Megonot-Weingart-Delpoint complex, 0 to 4 percent slopes141B1647346600cmnnmt61519921:24000
Megonot-Yawdim complex, 4 to 15 percent slopes68D496219124342261fmt62420211:24000
Kobase-Megonot complex, calcareous, 0 to 8 percent slopes140C3524347251cnbnmt62420211:24000
Kobase-Megonot complex, calcareous, 0 to 8 percent slopes, fan474C110619126322267tmt62420211:24000
Megonot-Yawdim complex, 4 to 15 percent slopes, fan481D81419124352261gmt62420211:24000
Cabbart-Megonot complex, 8 to 15 percent slopes138D698347246cnbhmt62420211:24000
Cabbart-Megonot complex, 15 to 45 percent slopes138F39226102522r8d1mt62420211:24000
Kobase-Megonot complex, 0 to 8 percent slopes473C23119126312267smt62420211:24000
Cabbart-Megonot complex, 2 to 8 percent slopes138C166347245cnbgmt62420211:24000
Kobase-Megonot silty clay loams, 1 to 8 percent slopes140B332513995cghrmt62420211:24000
Megonot-Yawdim silty clay loams, 4 to 15 percent slopes68C152513983cgkymt62420211:24000
Megonot-Weingart complex, 8 to 35 percent slopes149D22401477064ypqmt63019911:24000
Megonot silty clay, 4 to 8 percent slopes146C1961477044ypnmt63019911:24000
Cabbart-Megonot-Kobase clay loams, 2 to 15 percent slopes138D657514965050qfmt63920001:24000
Kobase-Rentsac-Megonot complex, 4 to 25 percent slopes363E10481499215105mt63920001:24000
Megonot-Cabbart complex, 2 to 8 percent slopes365C2061499235107mt63920001:24000
Kobase-Megonot silty clay loams, 2 to 8 percent slopes322C1882347671cns6mt64119941:24000
Megonot-Kobase silty clay loams, 8 to 15 percent slopes96D741347821cny1mt64119941:24000
Megonot-Yawdim silty clay loams, 4 to 15 percent slopes68C79817125521vh1mmt65519751:24000
Kobase-Megonot silty clay loams, 1 to 8 percent slopes140B7517125631vh1zmt65519751:24000
Cabbart-Megonot-Kobase clay loams, 2 to 15 percent slopes138D20361416d42lmt65519751:24000
Megonot-Yawdim-Rock outcrop complex, 25 to 60 percent slopes589F13000348733cpwgmt65719901:24000
Megonot-Tanna clay loams, 2 to 8 percent slopes270C11697348514cpndmt65719901:24000
Megonot-Richey-Tanna clay loams, 2 to 8 percent slopes148C11363348355cph8mt65719901:24000
Megonot-Kobase-Yawdim complex, 8 to 15 percent slopes570D6381348724cpw5mt65719901:24000
Megonot-Yawdim-Crago complex, 15 to 60 percent slopes367F6282348594cpqzmt65719901:24000
Megonot silty clay loam, 0 to 4 percent slopes70B4478348784cpy3mt65719901:24000
Megonot-Yawdim silty clay loams, 4 to 15 percent slopes68C26842341711cgkymt66620081:24000
Kobase-Megonot silty clay loams, 1 to 8 percent slopes140B7633341643cghrmt66620081:24000
Kobase-Megonot silty clay loams, calcareous, 1 to 8 percent slopes140C2849341644cghsmt66620081:24000
Cabbart-Megonot-Kobase complex, 2 to 15 percent slopes138D215385691nn08mt66620081:24000
Kobase-Rentsac-Megonot complex, 4 to 25 percent slopes363E86620223ntd6mt6691:24000
Polaris-Megonot-Tabyago complex, 8 to 40 percent slopes102442316521621sg6kwy0411:24000
Delphill-Alldown-Megonot association, 3 to 25 percent slopes119552186261620j6dwy0411:24000
Delphill-Iyers-Poposhia complex, 3 to 25 percent slopes1191478503962jxdvwy63819901:24000
Megonot-Yawdim clay loams, 3 to 15 percent slopes2961578817628wft3wy70520031:24000
Pomeroy-Megonot complex, 3 to 20 percent slopes -- draft8401735226119272qst0wy7231:24000

Map of Series Extent

Approximate geographic distribution of the MEGONOT 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 .