Official Series Description


Lab Data Summary

Aggregate lab data for the HOMEWOOD soil series. This aggregation is based on all pedons with a current taxon name of HOMEWOOD, 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 HOMEWOOD 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
13965PA0390051973PA039001Homewood4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.65378,-79.64801
n/aKX-0281979-OH083-028Homewood5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HOMEWOOD 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 HOMEWOOD 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 HOMEWOOD 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 HOMEWOOD 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 HOMEWOOD 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 HOMEWOOD 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 HOMEWOOD 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.

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 HOMEWOOD, 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 HOMEWOOD 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
Homewood silt loam, 2 to 6 percent slopesHlB526631468p62yoh02920051:12000
Homewood silt loam, 6 to 15 percent slopesHoC574536652l0fcoh03119961:15840
Homewood silt loam, 2 to 6 percent slopesHoB550536651l0fboh03119961:15840
Homewood-Gilpin complex, 12 to 20 percent slopes, erodedHoD254451722695s82oh04519981:12000
Homewood silt loam, 6 to 12 percent slopes, erodedHnC24611722685s81oh04519981:12000
Homewood-Gilpin complex, 20 to 35 percent slopes, erodedHoE23891722705s83oh04519981:12000
Homewood silt loam, 2 to 6 percent slopesHwB17582613592nlh9oh08319831:15840
Homewood silt loam, 6 to 12 percent slopesHwC16307613593nlhboh08319831:15840
Homewood silt loam, 12 to 18 percent slopes, erodedHwD25494613594nlhcoh08319831:15840
Chili-Homewood silt loams, 6 to 12 percent slopesCnC3159613571nlgmoh08319831:15840
Chili-Homewood silt loams, 12 to 18 percent slopesCnD2248613572nlgnoh08319831:15840
Homewood silt loam, 18 to 25 percent slopes, erodedHwE2435613595nlhdoh08319831:15840
Homewood silt loam, 6 to 15 percent slopesHrC922160102dcy6oh08319831:15840
Homewood silt loam, 6 to 12 percent slopes, erodedHoC276301710395qzdoh08919861:15840
Homewood silt loam, 12 to 18 percent slopes, erodedHoD251901710405qzfoh08919861:15840
Homewood silt loam, 2 to 6 percent slopesHoB20751710385qzcoh08919861:15840
Homewood silt loam, 18 to 25 percent slopes, erodedHoE26601710415qzgoh08919861:15840
Homewood silt loam, 15 to 20 percent slopes, erodedHfD2815407691nq97oh08919861:15840
Homewood silt loam, 15 to 20 percent slopes, erodedHaD2500537898l1qkoh11919891:15840
Homewood silt loam, 8 to 15 percent slopes, erodedHaC2335537897l1qjoh11919891:15840
Homewood silt loam, 12 to 18 percent slopes, erodedHoD21814256481jvhnoh11919891:15840
Homewood silt loam, 6 to 12 percent slopes, erodedHoC2614256471jvhmoh11919891:15840
Homewood-Westmoreland silt loams, 15 to 25 percent slopes, erodedHaD28854537547l1c7oh12719841:15840
Homewood-Westmoreland silt loams, 25 to 40 percent slopes, erodedHaE24471537548l1c8oh12719841:15840
Homewood silt loam, 15 to 20 percent slopes, erodedHoD212115416641nr73oh12719841:15840
Homewood silt loam, 6 to 12 percent slopesHpC18014065391j6m7oh13919711:15840
Homewood silt loam, 2 to 6 percent slopesHpB16814065381j6m6oh13919711:15840
Homewood silt loam, 12 to 18 percent slopes, erodedHpD25814065401j6m8oh13919711:15840
Homewood silt loam, 18 to 25 percent slopes, erodedHpE21314065411j6m9oh13919711:15840

Map of Series Extent

Approximate geographic distribution of the HOMEWOOD 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 .