Soil Data Explorer - HALL

Official Series Description

Lab Data Summary

Aggregate lab data for the HALL soil series. This aggregation is based on all pedons with a current taxon name of HALL, 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 HALL were used in the calculation. Source: KSSL snapshot (updated 2020-03-13). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Pedons used in the lab summary:

MLRA	Lab ID	Pedon ID	Taxonname	CI	NSSL / NASIS Reports	Link To SoilWeb GMap
102C	94P0110	93NE125001	Hall	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.4380569,-98.1472244
71	94P0105	01NE079001-OSD	Hall	8	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.8584409,-98.5315642
71	40A5360	1952NE079003	Hall	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.8530604,-98.5309309
71	40A2094	S1949NE079010	Hall	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.8736115,-98.6247253
71	40A2050	S1952NE079001	Hall	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.9697266,-98.6117706
71	40A2253	S1952NE079002	Hall	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.8572235,-98.5505524
73	79P0146	79NE073001	Hall	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.5900002,-99.8663864
n/a	40A2098	S1951NE079013	Hall	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	40A2099	S1951NE079014	Hall	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	40A2096	S1951NE079015	Hall	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	40A2100	S1952NE019003	Hall	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a

Water Balance

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

Competing Series

Soil series competing with HALL 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 HALL 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 HALL 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 mountains figure.

Soil series sharing subgroup-level classification with HALL, 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

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

1. NE-2012-02-10-13 | Clay County - March 1981

   Typical pattern of soils in the Geary-Holder-Uly and the Hord-Cass-Hobbs associations showing the relationship of the soils to topography and parent material (Soil Survey of Clay County, Nebraska; March 1981).

2. NE-2012-02-10-21 | Custer County - July 1982

   Typical pattern of soils in the Holdrege-Hall-Hord association and relationship of soils to topography and parent material (Soil Survey of Custer County, Nebraska; July 1982).

3. NE-2012-02-13-12 | Gosper County - February 1981

   Typical pattern of soils and parent material in the Holdrege-Hall association (Soil Survey of Gosper County, Nebraska; February 1981).

4. NE-2012-02-13-61 | Nance County - July 1960

   General soil areas of Nance County from a "bird's-eye view" (Soil Survey of Nance County, Nebraska; July 1960).

5. NE-2012-02-13-62 | Nance County - July 1960

   Principal soils of Nance County (Soil Survey of Nance County, Nebraska; July 1960).

6. NE-2012-02-13-63 | Nance County - July 1960

   A cross section along the eastern side of Nance County showing the relationship of the soils to the geological materials (Soil Survey of Nance County, Nebraska; July 1960).

7. NE-2012-02-14-19 | Wheeler County - September 1988

   Pattern of soils and parent material in the Coly-Uly association (Soil Survey of Wheeler County, Nebraska; September 1988).

Map Units

Map units containing HALL 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
Hall silt loam, 0 to 1 percent slopes	8840	1332	2605740	2pdd6	ks029	1972	1:24000
Hall silt loam, 0 to 1 percent slopes	8840	811	2605644	2pdd6	ks157	1965	1:24000
Hall silt loam, 0 to 1 percent slopes	8840	5366	1691906	1tskm	ne001	1970	1:20000
Hall silt loam, 0 to 1 percent slopes	8840	13571	427038	gbcf	ne011	1966	1:20000
Hall silt loam, 1 to 3 percent slopes	8841	3718	427039	gbcg	ne011	1966	1:20000
Hall-Gayville complex, 1 to 3 percent slopes	8851	1546	427037	gbcd	ne011	1966	1:20000
Hall silt loam, 3 to 6 percent slopes, eroded	8844	3	2401375	2lltq	ne011	1966	1:20000
Hall silt loam, 0 to 1 percent slopes	8840	2330	357627	d04c	ne015	1976	1:20000
Holdrege-Hall silt loam, 0 to 1 percent slopes	4153	25858	1700058	30rsr	ne019	1967	1:20000
Hall silt loam, 0 to 1 percent slopes	8840	14673	1700048	1v218	ne019	1967	1:20000
Hall silt loam, 1 to 3 percent slopes	8841	1084	1700049	1v219	ne019	1967	1:20000
Hall silt loam, 0 to 1 percent slopes	8840	2158	1691281	1trxg	ne023	1979	1:20000
Hall silt loam, 0 to 1 percent slopes	8840	2648	1692114	1tssb	ne035	1979	1:20000
Hall silty clay loam, sandy substratum, 0 to 1 percent slopes	8848	2076	427889	gc7w	ne037	1980	1:20000
Hall silt loam, 1 to 3 percent slopes	8841	30023	1699600	1v1kt	ne041	1980	1:20000
Hall silt loam, 0 to 1 percent slopes	8840	4637	1699599	1v1ks	ne041	1980	1:20000
Hall silt loam, 0 to 1 percent slopes	8840	12988	1699687	1v1nm	ne047	1975	1:20000
Hall silt loam, 1 to 3 percent slopes	8841	2652	1699686	1v1nl	ne047	1975	1:20000
Hall silt loam, wet substratum, 0 to 1 percent slopes	8846	1684	1699688	2zwkp	ne047	1975	1:20000
Hall silt loam, 0 to 1 percent slopes	8840	9706	1691951	1tsm2	ne061	1974	1:20000
Hall silt loam, 1 to 3 percent slopes	8841	36804	1699401	1v1cd	ne063	1973	1:20000
Hall silt loam, 0 to 1 percent slopes	8840	22467	1699400	1v1cc	ne063	1973	1:20000
Hall silt loam, 3 to 6 percent slopes	8843	2381	1699402	2zwkx	ne063	1973	1:20000
Hall silt loam, 0 to 1 percent slopes	8840	8483	1699743	1v1qf	ne065	1975	1:20000
Hall silt loam, 0 to 1 percent slopes	8840	19109	1692209	1tswd	ne073	1978	1:20000
Hall silt loam, 1 to 3 percent slopes	8841	1519	1692210	1tswf	ne073	1978	1:20000
Hall silt loam, 1 to 3 percent slopes	8841	4431	1699943	1v1xw	ne077	1987	1:20000
Hall silt loam, 0 to 1 percent slopes	8840	1665	1699942	1v1xv	ne077	1987	1:20000
Hall silt loam, sandy substratum, 0 to 1 percent slopes	8845	17797	1700133	1v240	ne079	2003	1:12000
Hall silt loam, 0 to 1 percent slopes	8840	4277	1700130	1v23x	ne079	2003	1:12000
Hall, eroded-Hobbs, silt loams, 0 to 3 perent slopes	8849	2367	1700134	1v241	ne079	2003	1:12000
Hall silt loam. 3 to 6 percent slopes, eroded	8847	1487	1700132	1v23z	ne079	2003	1:12000
Hall silt loam, 1 to 3 percent slopes, eroded	8842	791	1700131	1v23y	ne079	2003	1:12000
Hord and Hall silt loams, 0 to 1 percent slopes	8860	14625	1692248	2yl4f	ne083	1967	1:20000
Hord and Hall silt loams, 1 to 3 percent slopes	8861	4640	1692249	2yl4g	ne083	1967	1:20000
Hall silt loam, 0 to 1 percent slopes	8840	2041	99705	3br9	ne093	1968	1:12000
Hall silt loam, sandy substratum, 0 to 1 percent slopes	8845	76	2228912	2dtcd	ne093	1968	1:12000
Hall silt loam, 1 to 3 percent slopes	8841	7372	1699169	1v13x	ne111	1971	1:24000
Hall silt loam, 0 to 1 percent slopes	8840	1762	1699168	1v13w	ne111	1971	1:24000
Hall silt loam, 0 to 1 percent slopes	8840	473	1699355	1v19x	ne113	1969	1:24000
Hall silt loam, sandy substratum, 0 to 1 percent slopes	8845	2602	1709642	1vd0r	ne121	1978	1:20000
Hall silt loam, 1 to 3 percent slopes	8841	9	2401440	2llwt	ne121	1978	1:20000
Hall silt loam, 0 to 1 percent slopes	8840	20434	427469	gbtb	ne125	1958	1:20000
Hall silt loam, 1 to 3 percent slopes	8841	4832	427470	gbtc	ne125	1958	1:20000
Hall-Gayville variant silt loams, 0 to 1 percent slopes	8850	675	427468	gbt9	ne125	1958	1:20000
Hall silt loam, 3 to 6 percent slopes, eroded	8844	460	427472	gbtf	ne125	1958	1:20000
Hall silt loam, 3 to 6 percent slopes	8843	264	427471	gbtd	ne125	1958	1:20000
Hall silt loam, 0 to 1 percent slopes	8840	4113	1692064	1tsqq	ne129	1974	1:20000
Hall silt loam, 0 to 1 percent slopes	8840	67	2219477	2dhk1	ne137	1967	1:20000
Hall silt loam, 0 to 1 percent slopes	8840	318	2217211	2df5y	ne141	1984	1:20000
Hall silt loam, 0 to 1 percent slopes	8840	1629	1692290	1tsz0	ne143	1967	1:20000
Hall silt loam, 0 to 1 percent slopes	8840	3130	1691208	1trv3	ne159	1967	1:20000
Hall silt loam, 1 to 3 percent slopes	8841	1895	1691209	1trv4	ne159	1967	1:20000
Hall-Olbut complex, 1 to 3 percent slopes	8852	1573	1691218	1trvf	ne159	1967	1:20000
Hall silt loam, 0 to 1 percent slopes	8840	2227	1699991	1v1zf	ne163	1987	1:20000
Hall silt loam, 0 to 1 percent slopes	8840	172	2218734	2dgs2	ne169	1965	1:20000
Hall silt loam, 0 to 1 percent slopes	8840	439	2229065	2dtjb	ne181	1967	1:20000
Hall silt loam, 1 to 3 percent slopes	8841	238	1699843	1v1tn	ne183	1984	1:20000
Hall silt loam, 0 to 1 percent slopes	8840	741	1692331	1tt0b	ne185	1974	1:20000

Map of Series Extent

Approximate geographic distribution of the HALL 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).