Official Series Description


Lab Data Summary

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

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
43A92P03981991WA047006Merkel6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.8744431,-119.3166656
43A95P00681994WA047009Merkel5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.7675018,-119.1849976
694P03591994WA047001Merkel6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.6244431,-119.7869415

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MERKEL 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 MERKEL 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 MERKEL 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 MERKEL 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 MERKEL 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 MERKEL 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 MERKEL 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 hills figure.

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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 MERKEL, 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 MERKEL 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
Merkel family, 2 to 30 percent slopes.163999470384hsgpca70219841:24000
Merkel-Toadlake-Parks families complex, 5 to 40 percent slopes.193st226190599221zbmca70219841:24000
Patio deep-Gleason-Merkel families complex, 10 to 40 percent slopes.2305545470545hsmwca70319831:24000
Patip deep-Merkel families complex, 15 to 35 percent slopes.2313448470546hsmxca70319831:24000
Patio deep-Merkel families complex, 35 to 60 percent slopes.2322224470547hsmyca70319831:24000
Merkel-Toadlake-Parks families complex, 5 to 40 percent slopes.1936279470791hswtca70719831:24000
Merkel-Wintoner families complex, 50 to 80 percent slopes.1944044470792hswvca70719831:24000
Typic Cryaquolls-Merkel family, till substratum association, 0 to 20 percent slopes.3261210470924ht13ca70719831:24000
Merkel-Switchback families complex, 15 to 30 percent slopesFbE6845471642hts8ca77719811:24000
Merkel-Wapal families complex, 30 to 50 percent slopesFbF6675471643hts9ca77719811:24000
Merkel gravelly ashy sandy loam, 0 to 30 percent slopes, stony147131071581092v74fwa06519781:24000
Merkel-Rock outcrop complex, 40 to 65 percent slopes150620715811359jfwa06519781:24000
Merkel gravelly ashy sandy loam, 30 to 65 percent slopes, stony14856381581102v74gwa06519781:24000
Merkel-Rock outcrop complex, 0 to 40 percent slopes149448415811159jcwa06519781:24000
Rock outcrop-Merkel complex, 30 to 50 percent slopes19440815816159kzwa06519781:24000
Merkel sandy loam, 15 to 35 percent slopesMkE16635701142byrwa61919681:24000
Merkel-Rock land complex, 15 to 50 percent slopesMmE2686701182bywwa61919681:24000
Merkel stony sandy loam, 0 to 25 percent slopesMlD2529701162bytwa61919681:24000
Merkel stony sandy loam, 25 to 65 percent slopesMlF1877701172byvwa61919681:24000
Merkel sandy loam, 35 to 65 percent slopesMkF1843701152byswa61919681:24000
Merkel sandy loam, 0 to 15 percent slopesMkC1293701132byqwa61919681:24000
Nevine-Merkel complex, 15 to 35 percent slopes26312616026231qsnjwa61919681:24000
Merkel sandy loam, 20 to 40 percent slopes27810237704092c88wa64819871:24000
Merkel sandy loam, 40 to 65 percent slopes2794215704102c89wa64819871:24000
Merkel bouldery fine sandy loam, 5 to 20 percent slopes2802169704122c8cwa64819871:24000
Merkel sandy loam, 5 to 20 percent slopes2771903704082c87wa64819871:24000
Merkel bouldery fine sandy loam, 20 to 40 percent slopes2811563704132c8dwa64819871:24000
Nevine-Merkel complex, 15 to 35 percent slopes40516940189996021s21wa64920081:24000
Merkel ashy sandy loam, 15 to 35 percent slopes36016820189994721s1mwa64920081:24000
Merkel-Lithic Haploxerepts-Rock outcrop complex, 15 to 35 percent slopes3627920189994021s1dwa64920081:24000
Merkel cobbly ashy sandy loam, 35 to 65 percent slopes3614320189994821s1nwa64920081:24000
Merkel ashy sandy loam, 5 to 15 percent slopes3593200190157521tr4wa64920081:24000
Nevine-Merkel complex, 35 to 65 percent slopes4062495189996121s22wa64920081:24000
Merkel-Wilma complex, 35 to 65 percent slopes3632440189994321s1hwa64920081:24000
Merkel gravelly ashy sandy loam, 0 to 30 percent slopes, stony7460271584392v74fwa65119811:24000
Merkel gravelly ashy sandy loam, 30 to 65 percent slopes, stony7514911584402v74gwa65119811:24000
Merkel-Rock outcrop complex, 10 to 65 percent slopes7629415844159w0wa65119811:24000
Nevine-Merkel complex, 15 to 35 percent slopes26331328758122jwkwa74920051:24000
Merkel ashy sandy loam, 15 to 35 percent slopes2298192757982jw3wa74920051:24000
Nevine-Merkel complex, 35 to 65 percent slopes2647524758132jwlwa74920051:24000
Merkel-Lithic Haploxerepts-Rock outcrop complex, 15 to 35 percent slopes2317147757912jvwwa74920051:24000
Merkel-Wilma complex, 35 to 65 percent slopes2324925757942jvzwa74920051:24000
Merkel cobbly ashy sandy loam, 35 to 65 percent slopes2303197757992jw4wa74920051:24000
Merkel ashy sandy loam, 5 to 20 percent slopes228254614132nm1qwa74920051:24000

Map of Series Extent

Approximate geographic distribution of the MERKEL 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 .