Official Series Description


Lab Data Summary

Aggregate lab data for the HOWLAND soil series. This aggregation is based on all pedons with a current taxon name of HOWLAND, 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 HOWLAND 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
14383P033882NH007003Howland6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.9749985,-71.3916702
144B40A0486S1962NH009004HOWLAND6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.2230568,-71.851387
n/a97P0227S1996NH007009Howland6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HOWLAND 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 HOWLAND 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 HOWLAND 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 HOWLAND 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 terrace figure.

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Competing Series

Soil series competing with HOWLAND 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 HOWLAND 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 HOWLAND 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 HOWLAND, 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 HOWLAND 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
Howland gravelly loam, 3 to 8 percent slopesHoB1252643018332w3y6me60719601:20000
Howland loam, 0 to 8 percent slopes, very stonyHvB978853018352w3y8me60719601:20000
Plaisted-Howland association, 0 to 8 percent slopes, very stonyPvB369213018702w3yrme60719601:20000
Plaisted-Howland association, 8 to 15 percent slopes, very stonyPvC360893018712w3yqme60719601:20000
Howland gravelly loam, 8 to 15 percent slopesHoC161013018342w3y7me60719601:20000
Thorndike-Howland association, 8 to 15 percent slopes, very rockyTsC144613018942wqmhme60719601:20000
Howland silt loam, 8 to 15 percent slopes, very stonyHvC83583018362w3y9me60719601:20000
Thorndike-Howland association, 0 to 8 percent slopes, very rockyTsB62173018932wqmcme60719601:20000
Howland gravelly loam, 0 to 3 percent slopesHoA8993018322t0k3me60719601:20000
Howland loam, 0 to 8 percent slopes, very stonyHvB752366141732w3y8me60819621:20000
Howland gravelly loam, 3 to 8 percent slopesHoB683526141712w3y6me60819621:20000
Plaisted-Howland association, 0 to 8 percent slopes, very stonyPvB670466142032w3yrme60819621:20000
Plaisted-Howland association, 8 to 15 percent slopes, very stonyPvC371106142042w3yqme60819621:20000
Thorndike-Howland association, 0 to 8 percent slopes, very rockyTsB243586142172wqmcme60819621:20000
Thorndike-Howland association, 8 to 15 percent slopes, very rockyTsC233296142182wqmhme60819621:20000
Howland silt loam, 8 to 15 percent slopes, very stonyHvC132816141742w3y9me60819621:20000
Howland gravelly loam, 8 to 15 percent slopesHoC58166141722w3y7me60819621:20000
Howland gravelly loam, 0 to 3 percent slopesHoA23786141702t0k3me60819621:20000
Howland loam, 0 to 8 percent slopes, very stonyHvB1065692852232w3y8me61419601:20000
Howland silt loam, 8 to 15 percent slopes, very stonyHvC269892852242w3y9me61419601:20000
Howland silt loam, 15 to 30 percent slopes, very stonyHvD32752852252w3ybme61419601:20000
Howland gravelly loam, 3 to 8 percent slopesHoB26882852212w3y6me61419601:20000
Howland gravelly loam, 8 to 15 percent slopesHoC1792852222w3y7me61419601:20000
Plaisted-Howland-Penquis association, 3 to 15 percent slopes, very stonyPWC514192853512t0k9me61519941:24000
Howland-Monarda association, 0 to 8 percent slopes, very stonyHRB473402853322w3zfme61519941:24000
Monarda-Howland-Thorndike complex, 3 to 15 percent slopes, very stonyMXB206392853442w3znme61519941:24000
Plaisted-Penquis-Howland association, 15 to 25 percent slopes, very stonyPWD30672853522w407me61519941:24000
Howland gravelly loam, 3 to 8 percent slopesHoB30522853332w3y6me61519941:24000
Cabot-Howland association, 0 to 15 percent slopesCAB82914784261lmf5me61920051:24000
Howland-Plaisted association, 15 to 35 percent slopes, very stonyHYD27814784242w3ycme61920051:24000
Howland-Cabot association, 0 to 15 percent slopesHWB24814784251lmf4me61920051:24000
Plaisted-Howland association, 3 to 15 percent slopes, very stonyPSB1914784172w3ypme61920051:24000
Plaisted-Howland association, 15 to 35 percent slopes, very stonyPSD414784182w3ynme61920051:24000
Howland-Cabot association, gently sloping, very stony964B315002807609f4snh60720001:24000
Cabot-Howland association, gently sloping, very stony965B231242807619f4tnh60720001:24000
Howland-Plaisted association, 15 to 35 percent slopes, very stony864D142852806532w3ycnh60720001:24000
Howland silt loam, 8 to 15 percent slopes, very stony567C96352805002w3y9nh60720001:24000
Plaisted-Howland association, 15 to 35 percent slopes, very stony762D82492805982w3ynnh60720001:24000
Plaisted-Howland association, 3 to 15 percent slopes, very stony762B75182805972w3ypnh60720001:24000
Howland silt loam, 15 to 30 percent slopes, very stony567D50652805012w3ybnh60720001:24000
Howland loam, 0 to 8 percent slopes, very stony567B35452804992w3y8nh60720001:24000
Howland gravelly loam, 8 to 15 percent slopes566C17092804972w3y7nh60720001:24000
Howland gravelly loam, 3 to 8 percent slopes566B11662804962w3y6nh60720001:24000
Howland silt loam, 15 to 25 percent slopes566D4292804982w3zgnh60720001:24000

Map of Series Extent

Approximate geographic distribution of the HOWLAND 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 .