Official Series Description


Lab Data Summary

Aggregate lab data for the HARSLOW soil series. This aggregation is based on all pedons with a current taxon name of HARSLOW, 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 HARSLOW 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
199P0176S1998OR003002Harslow6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.4652786,-123.5402756
109N1173S2009OR071011Harslow6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.301857,-123.3787003

Water Balance

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

There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with HARSLOW 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 HARSLOW 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 HARSLOW 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 HARSLOW, 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 HARSLOW 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
Klistan-Harslow complex, 30 to 60 percent slopes1023780852622vqdor00320041:24000
Klistan-Harslow-Hemcross complex, 5 to 30 percent slopes1031920852642vqgor00320041:24000
Harslow-Kilchis-Rock outcrop complex, 60 to 90 percent slopes751185854372vx1or00320041:24000
Harslow-Klistan-Rock outcrop complex, 60 to 90 percent slopes761074852492vpzor00320041:24000
Klistan-Harslow complex, 30 to 60 percent slopes31E61076087321bnor00719841:20000
Harslow-Kilchis very gravelly loams, 60 to 90 percent slopes22F52116086321bbor00719841:20000
Klistan-Harslow complex, 60 to 90 percent slopes31F7016087421bpor00719841:20000
Klistan-Harslow-Hemcross complex, 60 to 90 percent slopes43F831766720127xsor05720061:24000
Harslow-Klistan-Rock outcrop complex, 60 to 90 percent slopes44F125996718127x4or05720061:24000
Harslow-Rock outcrop-Klistan complex, 60 to 90 percent south slopes144F99686720527xxor05720061:24000
Harslow-Kilchis very gravelly medial loams, 60 to 90 percent slopes322F8186719427xkor05720061:24000
Rock outcrop-Harslow complex, 40 to 100 percent slopes145F580672732803or05720061:24000
Klistan-Harslow-Rock outcrop complex, 30 to 60 percent slopes44E1516718327x6or05720061:24000
Klistan-Harslow-Hemcross complex, 60 to 90 percent slopes64G539617236491vvllor06719751:20000
Harslow-Klistan-Rock outcrop complex, 60 to 90 percent slopes75G6017236681vvm6or06719751:20000
Harslow-Rock outcrop-Klistan complex, 60 to 90 percent south slopes74G5517236671vvm5or06719751:20000
Klistan-Harslow-Hemcross complex, 60 to 90 percent slopes43F5087271118927xsor07119671:24000
Harslow-Klistan-Rock outcrop complex, 60 to 90 percent slopes44F142271118827x4or07119671:24000
Harslow-Kilchis-Rock outcrop complex, 60 to 90 percent slopes360G12514215081jq63or63719811:20000
Klistan-Harslow complex, 30 to 60 percent slopes385F5114215121jq67or63719811:20000
Harslow-Klistan-Rock outcrop complex, 60 to 90 percent slopes365G1314215091jq64or63719811:20000
Harslow-Rock outcrop complex, 60 to 90 percent slopes24H2750646362581or63819901:20000
Klistan-Harslow very gravelly loams, 20 to 60 percent slopes31G267564658258ror63819901:20000
Kilchis-Harslow-Rock outcrop complex, 60 to 100 percent south slopes121G6086629326zhor64919941:24000

Map of Series Extent

Approximate geographic distribution of the HARSLOW 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 .