Official Series Description


Lab Data Summary

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

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HANLY 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 HANLY 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 HANLY 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 HANLY 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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Click the image to view it full size.

There are insufficient data to create the 3D mountains figure.

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Click the image to view it full size.

Competing Series

Soil series competing with HANLY 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 HANLY series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the HANLY 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 .

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

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 HANLY, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. ND-2010-09-27-01 | Billings County - 2005

    Typical pattern of soils and underlying material in the Glendive-Havre-Hanly association (Soil Survey of Billings County, North Dakota; 2005).

  2. SD-2012-03-15-48 | Harding County - December 1988

    Pattern of soils and parent material in the Hanly-Korchea-Glendive and Bullock-Parchin associations (Soil Survey of Harding County, SD; 1988).

Map Units

Map units containing HANLY 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
Hanly-Ryell fine sandy loam, 0 to 4 percent slopes7B3954343241cj59mt01119921:24000
Hanly-Glendive complex, 0 to 2 percent slopes, occasionally flooded4621A10382343473cjdsmt01719951:24000
Hanly-Glendive complex, 0 to 2 percent slopes, nonflooded462A2960343474cjdtmt01719951:24000
Hanly loamy fine sand, 0 to 2 percent slopes, rarely flooded46A772343476cjdwmt01719951:24000
Hanly loamy fine sand, 0 to 2 percent slopes, occasionally flooded461A514343470cjdpmt01719951:24000
Hanly-Glendive loams, 0 to 2 percent slopes, occasionally flooded660A8343624cjknmt01719951:24000
Hanly soils, 0 to 4 percent slopes, occasionally floodedBk6183341995cgw3mt02119711:24000
Hanly-Ryell fine sandy loams, 0 to 4 percent slopes7B2904342289ch5lmt02519911:24000
Hanly loamy fine sand, 0 to 2 percent slopes, occasionally flooded591A3369342669chkvmt03320021:24000
Hanly loamy fine sand, 0 to 2 percent slopes, rarely flooded59A1641342670chkwmt03320021:24000
Hanly loamy fine sand, 0 to 2 percent slopes, occasionally flooded241A3000343882cjtzmt04119941:24000
Hanly loamy fine sand, 0 to 2 percent slopes24A894343883cjv0mt04119941:24000
Hanly loamy fine sand792254344445ckf4mt05519811:24000
Glendive-Hanly complex, protected78724344444ckf3mt05519811:24000
Hanly-Glendive complex, 0 to 2 percent slopes671782344987ckzmmt07919861:24000
Hanly-Glendive-Havre complex, 0 to 2 percent slopes101A876345058cl1xmt10119921:24000
Havre, Hanly, and Glendive soils, channeled5935812346504cmkkmt60819761:24000
Hanly loamy fine sand489191346476cmjnmt60819761:24000
Rivra-Hanly complex, 0 to 2 percent slopes992953347015cn31mt61519921:24000
Hanly fine sandy loam, 0 to 2 percent slopes100A344347554cnnfmt64119941:24000
Hanly-Glendive loams, 0 to 2 percent slopes, occasionally flooded962159348132cp82mt64919851:24000
Hanly fine sandy loam, 0 to 6 percent slopes, occasionally floodedL4209B482127070802qxjpnd00719981:24000
Zeona-Hanly, occasionally flooded loamy fine sands, 0 to 9 percent slopesL1855C65627070412qxhxnd00719981:24000
Hanly loamy fine sand, 0 to 6 percent slopesHa241499283712b40nd01119691:20000
Hanly soils, channeled, 0 to 2 percent slopesHc140999283812b41nd01119691:20000
Hanly fine sandy loam, 0 to 6 percent slopes, occasionally floodedL4209B68625635022qxjpnd01119691:20000
Zeona-Hanly, occasionally flooded loamy fine sands, 0 to 9 percent slopesL1855C44625634722qxhxnd01119691:20000
Hanly fine sandy loam, 0 to 6 percent slopes, occasionally floodedL4209B261227071472qxjpnd02519811:20000
Hanly fine sandy loam, 0 to 6 percent slopes, occasionally floodedL4209B9827073482qxjpnd03319851:24000
Hanly fine sandy loam, 0 to 6 percent slopes, occasionally floodedL4209B473527151732qxjpnd05320031:24000
Hanly fine sandy loam, 0 to 6 percent slopes, occasionally floodedL4209B582527159542qxjpnd08719741:20000
Zeona-Hanly, occasionally flooded loamy fine sands, 0 to 9 percent slopesL1855C82827159022qxhxnd08719741:20000
Hanly loamy fine sand,Ha2340353178cvhvsd01919701:24000
Hanly-Dogiecreek fine sandy loamsHd18162355748cy5rsd06319841:24000
Hanly loamy fine sandHb4641355747cy5qsd06319841:24000
Hanly-Slickspots complexHe4484355749cy5ssd06319841:24000
Hanly fine sandy loamHa3493355746cy5psd06319841:24000
Orthents, hummocky-Hanly complex, 0 to 15 percent slopesPb538354645cx15sd10519771:24000
Hanly family-Riverwash complex, 1 to 3 percent slopes130326503978jxfcwy63819901:24000

Map of Series Extent

Approximate geographic distribution of the HANLY 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 .