Soil Data Explorer - HALIFAX

Official Series Description

Lab Data Summary

Aggregate lab data for the HALIFAX soil series. This aggregation is based on all pedons with a current taxon name of HALIFAX, 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 HALIFAX were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). 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 HALIFAX 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.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the HALIFAX series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-10-24), parsed OSD records (updated 2024-10-23) and snapshot of SC database (updated 2024-10-23).

Select annual climate data summaries for the HALIFAX series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).

Geomorphic description summaries for the HALIFAX 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 (updated 2024-10-23).

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

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

Competing Series

Soil series competing with HALIFAX share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2024-10-23) and snapshot of the SC database (updated 2024-10-23).

Select annual climate data summaries for the HALIFAX series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).

Geomorphic description summaries for the HALIFAX 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 (updated 2024-10-23).

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

Soil series sharing subgroup-level classification with HALIFAX, 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 (updated 2024-10-23).

Block Diagrams

No block diagrams are available.

Map Units

Map units containing HALIFAX 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
Halifax sandy loam, 2 to 8 percent slopes	HaB	5431	2973915	2wx24	nc033	2016	1:24000
Halifax sandy loam, 8 to 15 percent slopes	HaC	4667	2973916	2wx25	nc033	2016	1:24000
Halifax-Davie complex, 0 to 6 percent slopes	HcB	244	2433126	2mnvy	nc081	1975	1:20000
Halifax sandy loam, 6 to 10 percent slopes	HaC	84	2433122	2mnvt	nc081	1975	1:20000
Halifax sandy loam, 2 to 6 percent slopes	HaB	1242	2439302	2mw95	nc145	1987	1:24000
Halifax sandy loam, 6 to 10 percent slopes	HaC	522	2439303	2mw96	nc145	1987	1:24000
Halifax sandy loam, 2 to 8 percent slopes	HaB	767	2389047	2l601	nc157	1983	1:24000
Halifax fine sandy loam, 2 to 7 percent slopes	18B	606	135940	2xx66	va019	1985	1:24000
Halifax fine sandy loam, 7 to 15 percent slopes	18C	534	135941	2xx67	va019	1985	1:24000
Halifax-Delanco complex, 2 to 7 percent slopes, rarely flooded	20B	7168	2479410	2p70z	va029	2010	1:24000
Halifax gravelly fine sandy loam, 2 to 7 percent slopes	32B	106	1726389	1vyfz	va047	2006	1:24000
Nathalie-Halifax complex, 7 to 15 percent slopes	27C	4336	1587428	1q8vc	va049	2005	1:24000
Rasalo-Halifax complex, 2 to 7 percent slopes	33B	794	1587441	1q8vs	va049	2005	1:24000
Halifax sandy loam, 2 to 7 percent slopes	20B	757	1587417	1q8v0	va049	2005	1:24000
Rasalo-Halifax complex, 7 to 15 percent slopes	33C	458	1587442	1q8vt	va049	2005	1:24000
Halifax sandy loam, 7 to 15 percent slopes	20C	416	1587418	1q8v1	va049	2005	1:24000
Halifax sandy loam, 2 to 8 percent slopes	24B	12109	1472819	1lfl9	va083	2004	1:24000
Halifax sandy loam, 8 to 15 percent slopes	24C	8260	1472820	1lflb	va083	2004	1:24000
Halifax fine sandy loam, 2 to 10 percent slopes, moderately eroded	HeC2	159	119847	2z1xq	va137	1966	1:15840
Halifax fine sandy loam, 2 to 7 percent slopes	HeB	147	119846	2z1xp	va137	1966	1:15840
Halifax sandy loam, 2 to 7 percent slopes	16B	1598	119958	2yzs1	va143	1989	1:24000
Halifax sandy loam, 7 to 15 percent slopes	16C	424	119959	2yzs2	va143	1989	1:24000

Map of Series Extent

Approximate geographic distribution of the HALIFAX 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 (updated 2024-10-30).