Official Series Description


Lab Data Summary

Aggregate lab data for the DANVERS soil series. This aggregation is based on all pedons with a current taxon name of DANVERS, 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 DANVERS 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
43B89P016488MT031013Danvers5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.6349983,-111.2977753
4489P037277MT077324Danvers5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.3572235,-112.6483307
4640A3491S1958MT045006Danvers6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.346859,-110.1477737
4640A3492S1958MT045007Danvers6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.3582497,-110.129158
58A40A3493S1956MT111001Danvers6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.8582611,-108.1101837
58A40A3494S1956MT111002Danvers6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.8232613,-108.1093521
n/a40A5318S1957MT027001Danvers4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the DANVERS 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 DANVERS 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 DANVERS 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 DANVERS 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 DANVERS 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 DANVERS 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 DANVERS 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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Soil series sharing subgroup-level classification with DANVERS, 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 DANVERS 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
Danvers clay loam, 0 to 2 percent slopes5523936342556chg6mt02719791:24000
Danvers-Tamaneen clay loams, 0 to 2 percent slopes5810968342559chg9mt02719791:24000
Danvers clay loam, 2 to 8 percent slopes569032342557chg7mt02719791:24000
Fairfield-Danvers clay loams, 0 to 2 percent slopes938834342598chhkmt02719791:24000
Fairfield-Danvers clay loams, 2 to 4 percent slopes947700342599chhlmt02719791:24000
Danvers-Acel clay loams, 0 to 2 percent slopes571689342558chg8mt02719791:24000
Danvers silty clay loam, 2 to 4 percent slopesDa24897345704clqrmt11119661:20000
Danvers silty clay loam, 8 to 15 percent slopesDn3577345705clqsmt11119661:20000
Danvers-Shaak clay loams, 7 to 15 percent slopesDs2553345707clqvmt11119661:20000
Danvers-Judith complex, 7 to 15 percent slopesDr633345706clqtmt11119661:20000
Danvers-Judith clay loams, 0 to 2 percent slopesDm563421473404y9xmt60219631:20000
Danvers clay loam, 0 to 2 percent slopesDa171221473324y9nmt60219631:20000
Danvers-Judith clay loams, 2 to 4 percent slopesDn121221473414y9ymt60219631:20000
Danvers cobbly clay loam, 0 to 4 percent slopesDd68631473354y9rmt60219631:20000
Danvers clay loam, 2 to 4 percent slopesDb55921473334y9pmt60219631:20000
Danvers-Judith complex, 0 to 2 percent slopesDp46041473434yb0mt60219631:20000
Judith-Danvers gravelly clay loams, 0 to 4 percent slopesJp44241473794yc5mt60219631:20000
Danvers cobbly clay loam, 4 to 8 percent slopesDf28381473364y9smt60219631:20000
Danvers-Judith clay loams, shale substratum, 0 to 4 per cent slopesDo21031473424y9zmt60219631:20000
Danvers stony clay loam, 2 to 4 percent slopesDk19251473394y9wmt60219631:20000
Danvers clay loam, 4 to 8 percent slopesDc17561473344y9qmt60219631:20000
Danvers gravelly clay loam, 0 to 4 percent slopesDh11091473384y9vmt60219631:20000
Beckton-Danvers clay loamsBd9081473034y8qmt60219631:20000
Danvers cobbly clay loam, 8 to 15 percent slopesDg6851473374y9tmt60219631:20000
Danvers-Judith silty clay loams, undulatingDf5413345932clz3mt60719701:24000
Danvers silty clay loam, gently undulatingDb4665345928clyzmt60719701:24000
Danvers-Judith silty clay loams, hillyDg3599345933clz4mt60719701:24000
Danvers-Judith silty clay loams, gently undulatingDe2922345931clz2mt60719701:24000
Danvers cobbly silty clay loam, 1 to 4 percent slopesDd2563345930clz1mt60719701:24000
Danvers silty clay loam, 0 to 1 percent slopesDa2275345927clyymt60719701:24000
Danvers silty clay loam, undulatingDc1417345929clz0mt60719701:24000
Danvers silty clay loam, 0 to 2 percent slopes472289341931cgt1mt61319751:24000
Danvers-Roy complex, 8 to 15 percent slopes, moderately impacted1446D53915526256kgmt61620031:24000
Roy-Shawmut-Danvers complex, 35 to 60 percent slopes351F4781547265605mt61620031:24000
Danvers-Roy complex, 15 to 35 percent slopes, moderately impacted1446E37915526356khmt61620031:24000
Danvers-Roy complex, 4 to 8 percent slopes, moderately impacted1446C15015526156kfmt61620031:24000
Roy-Shawmut-Danvers complex, 15 to 35 percent slopes351E806095714wlbmt61620031:24000
Danvers clay loam, 2 to 4 percent slopes49B62154831563kmt61620031:24000
Danvers-Roy complex, 35 to 60 percent slopes, moderately impacted1446F5615526456kjmt61620031:24000
Roy-Shawmut-Danvers complex, 35 to 60 percent slopes, moderately impacted951F5115522356j6mt61620031:24000
Danvers-Roy complex, 2 to 4 percent slopes, moderately impacted646B4215522756jbmt61620031:24000
Danvers clay loam, 15 to 35 percent slopes49E4154833563mmt61620031:24000
Roy-Shawmut-Danvers complex, 15 to 35 percent slopes351E104341443474wlbmt62119971:24000
Danvers clay loam, 4 to 8 percent slopes49C47491444644vb4mt62119971:24000
Danvers clay loam, 0 to 4 percent slopes49B40801444634vb3mt62119971:24000
Danvers-Roy complex, 4 to 8 percent slopes446C24281444194v8pmt62119971:24000
Danvers clay loam, 8 to 15 percent slopes49D24021444654vb5mt62119971:24000
Danvers-Roy complex, 8 to 15 percent slopes446D22221444204v8qmt62119971:24000
Danvers-Coben clay loams, 4 to 8 percent slopes849C19321446174vh2mt62119971:24000
Danvers-Roy complex, 15 to 35 percent slopes446E18651444214v8rmt62119971:24000
Roy-Tolbert-Danvers complex, 8 to 15 percent slopes646D15401445404vdlmt62119971:24000
Roy-Shawmut-Danvers cobbly loams, 35 to 60 percent slopes351F14571443484v6dmt62119971:24000
Roy-Tolbert-Danvers complex, 15 to 35 percent slopes646E8531445414vdmmt62119971:24000
Danvers-Coben clay loams, 8 to 15 percent slopes849D6221446184vh3mt62119971:24000
Danvers cobbly loam, 0 to 4 percent slopes149B4261442204v28mt62119971:24000
Danvers-Roy complex, 0 to 4 percent slopes446B3591444184v8nmt62119971:24000
Danvers cobbly loam, 8 to 15 percent slopes149D3581442224v2bmt62119971:24000
Roy-Shawmut-Danvers complex, 8 to 15 percent slopes351D2501443464v6bmt62119971:24000
Danvers cobbly loam, 4 to 8 percent slopes149C2081442214v29mt62119971:24000
Danvers-Coben clay loams, 2 to 4 percent slopes849B1651446164vh1mt62119971:24000
Danvers-Roy complex, 35 to 60 percent slopes446F1261444224v8smt62119971:24000
Danvers clay loam, 15 to 35 percent slopes49E1091444664vb6mt62119971:24000
Danvers silty clay loam, 4 to 8 percent slopes58C171615560756xlmt62219971:24000
Danvers silty clay loam, 8 to 15 percent slopes58D115715560856xmmt62219971:24000
Danvers silty clay loam, 0 to 4 percent slopes58B46115560656xkmt62219971:24000
Danvers-Quagle complex, 4 to 8 percent slopes458C40115550756tcmt62219971:24000
Danvers cobbly clay loam, 8 to 15 percent slopes258D34115535356ndmt62219971:24000
Danvers-Quagle complex, 8 to 15 percent slopes458D10515550856tdmt62219971:24000
Danvers gravelly clay loam, 2 to 8 percent slopes654C467190211221v9gmt62420211:24000
Martinsdale, very stony-Danvers, extremely stony complex, 2 to 15 percent slopes708D43724874802phf9mt62420211:24000
Martinsdale, very stony-Danvers, extremely stony complex, 2 to 15 percent slopes708D31025124472phf9mt6321:24000
Roy-Shawmut-Danvers complex, 15 to 35 percent slopes351E113917032494wlbmt63520061:24000
Danvers-Roy complex, 8 to 15 percent slopes446D38117029581v524mt63520061:24000
Danvers-Roy complex, 15 to 35 percent slopes446E15417029591v525mt63520061:24000
Danvers clay loam, 8 to 15 percent slopes49D3517032391v5c6mt63520061:24000
Danvers cobbly clay loam, 1 to 4 percent slopes430B14021480294z14mt63720141:24000
Danvers clay loam, 1 to 4 percent slopes30B13671480184z0smt63720141:24000
Danvers gravelly clay loam, 1 to 4 percent slopes130B8801479844yzpmt63720141:24000
Danvers-Kiev complex, 2 to 8 percent slopes230B5011480014z07mt63720141:24000
Danvers cobbly clay loam, 4 to 8 percent slopes430C4591480304z15mt63720141:24000
Danvers gravelly clay loam, 2 to 8 percent slopes190C104314973050t0mt63920001:24000
Danvers loam, 2 to 8 percent slopes269C42214983450xcmt63920001:24000
Tamaneen-Danvers clay loams, 0 to 4 percent slopes871B6019347791cnx2mt64119941:24000
Roy-Shawmut-Danvers complex, 15 to 35 percent slopes351E413651456794wlbmt64419951:24000
Danvers clay loam, 8 to 15 percent slopes49D214741457824wpnmt64419951:24000
Danvers clay loam, 4 to 8 percent slopes49C165381457814wpmmt64419951:24000
Danvers clay loam, 0 to 4 percent slopes49B116431457804wplmt64419951:24000
Roy-Shawmut-Danvers complex, 35 to 60 percent slopes351F85611456804wlcmt64419951:24000
Danvers-Roy complex, 8 to 15 percent slopes446D76521457464wnhmt64419951:24000
Danvers cobbly clay loam, 8 to 15 percent slopes149D75801455564wgcmt64419951:24000
Danvers cobbly clay loam, 4 to 8 percent slopes149C25851455554wgbmt64419951:24000
Danvers-Roy complex, 4 to 8 percent slopes446C17491457454wngmt64419951:24000
Danvers-Roy complex, 0 to 4 percent slopes446B15741457444wnfmt64419951:24000
Danvers cobbly clay loam, 0 to 4 percent slopes149B13891455544wg9mt64419951:24000

Map of Series Extent

Approximate geographic distribution of the DANVERS 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 .