Soil Data Explorer - FARLAND

Official Series Description

Lab Data Summary

Aggregate lab data for the FARLAND soil series. This aggregation is based on all pedons with a current taxon name of FARLAND, 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 FARLAND 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
44	89P0154	88MT031002	Farland	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.8144455,-111.0749969
44	89P0161	88MT031010	Farland	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.9205551,-111.0875015
44	91P0196	90MT031001	Farland	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.6587982,-110.9799957
54	40A0044	58ND089013	Farland	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	47.0030556,-102.44
54	40A0045	58ND089020	Farland	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	46.9955556,-102.4775

Water Balance

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

Competing Series

Soil series competing with FARLAND 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 FARLAND 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 FARLAND 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.

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

Soil series sharing subgroup-level classification with FARLAND, 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. ND-2010-09-27-12 | Williams County - 2002

   Typical pattern of soils and underlying material in the Lawther-Shambo-Savage association (Soil Survey of Williams County, North Dakota; 2002).

2. ND-2010-09-27-17 | Morton County - 2002

   Typical pattern of soils and underlying materials in the Farland-Savage-Amor-Belfield association (Soil Survey of Morton County, North Dakota; 2002).

3. ND-2012-02-07-35 | Dunn County - April 1982

   Typical pattern of soils and underlying material in the Straw-Velva association (Soil Survey of Dunn County, North Dakota; April 1982).

4. ND-2012-02-08-53 | Stark County - February 1968

   Diagram showinig the relationship of some of the major soils in Stark County (Soil Survey of Stark County, North Dakota; February 1968).

Map Units

Map units containing FARLAND 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
Farland silt loam, 2 to 8 percent slopes	59C	5076	343557	cjhh	mt017	1995	1:24000
Morton-Farland silt loams, 2 to 8 percent slopes	871C	2228	343725	cjnx	mt017	1995	1:24000
Farland silt loam, 0 to 4 percent slopes	63	2122	344428	ckdl	mt055	1981	1:24000
Farland and Havrelon soils, 4 to 8 percent slopes	Fm	39140	347852	cnz1	mt643	1967	1:20000
Farland-Cabba association, 8 to 20 percent slopes	Fk	18207	347850	cnyz	mt643	1967	1:20000
Farland silt loam, 4 to 8 percent slopes	Fe	10817	347848	cnyx	mt643	1967	1:20000
Farland-Rockland association, 0 to 6 percent slopes	Fl	6309	347851	cnz0	mt643	1967	1:20000
Farland-Cabba association, 4 to 8 percent slopes	Fh	5888	347849	cnyy	mt643	1967	1:20000
Farland silt loam, 2 to 4 percent slopes	Fd	5849	347847	cnyw	mt643	1967	1:20000
Farland silt loam, 0 to 2 percent slopes	Fa	1253	347846	cnyv	mt643	1967	1:20000
Farland-Cherry silt loams, 2 to 8 percent slopes	17	108358	348219	cpbw	mt661	1982	1:24000
Farland silt loam, 2 to 8 percent slopes	16	42455	348218	cpbv	mt661	1982	1:24000
Belfield-Daglum-Farland silt loams, 0 to 2 percent slopes	E0403A	7819	2563527	2r4g0	nd011	1969	1:20000
Belfield-Daglum-Farland silt loams, 2 to 6 percent slopes	E0403B	3922	2563528	2r4g1	nd011	1969	1:20000
Grail-Farland silt loams, 2 to 6 percent slopes	E0814B	941	2563557	2rdbd	nd011	1969	1:20000
Morton-Farland silt loams, 3 to 6 percent slopes	E2927B	199	2661698	1vzv5	nd015	1967	1:20000
Morton-Farland silt loams, 3 to 6 percent slopes	E2927B	17686	2707210	1vzv5	nd025	1981	1:20000
Farland silt loam, 0 to 2 percent slopes	E2203A	8197	2707203	1vztg	nd025	1981	1:20000
Belfield-Daglum-Farland silt loams, 0 to 2 percent slopes	E0403A	5701	2707165	2r4g0	nd025	1981	1:20000
Farland silt loam, 2 to 6 percent slopes	E2203B	4713	2707204	1vzth	nd025	1981	1:20000
Morton-Farland silt loams, 0 to 3 percent slopes	E2927A	1264	2707209	1vzv4	nd025	1981	1:20000
Farland silt loam, 2 to 6 percent slopes	E2203B	1939	2661780	1vzth	nd029	1979	1:20000
Farland silt loam, 0 to 6 percent slopes	C466B	208	2564344	2q6l8	nd029	1979	1:20000
Farland silt loam, 0 to 2 percent slopes	E2203A	32	2661779	1vztg	nd029	1979	1:20000
Morton-Farland silt loams, 3 to 6 percent slopes	E2927B	10	1715500	1vzv5	nd037	1985	1:20000
Farland silt loam, 6 to 9 percent slopes	E2203C	5	2759645	1vztj	nd037	1985	1:20000
Morton-Farland silt loams, 3 to 6 percent slopes	E2927B	25	2755686	1vzv5	nd041	1986	1:20000
Morton-Farland silt loams, 0 to 3 percent slopes	E2927A	19	2755685	1vzv4	nd041	1986	1:20000
Farland silt loam, 0 to 2 percent slopes	E2203A	2	2755681	1vztg	nd041	1986	1:20000
Farland silt loam, 2 to 6 percent slopes	E2203B	23002	2699163	1vzth	nd059	1998	1:20000
Morton-Farland silt loams, 3 to 6 percent slopes	E2927B	11552	1718358	1vzv5	nd059	1998	1:20000
Farland silt loam, 0 to 2 percent slopes	E2203A	10460	1718350	1vztg	nd059	1998	1:20000
Farland silt loam, 6 to 9 percent slopes	E2203C	8314	2699164	1vztj	nd059	1998	1:20000
Farland silt loam, 9 to 15 percent slopes	E2203D	1952	2699165	cdnd	nd059	1998	1:20000
Grail-Farland silt loams, 2 to 6 percent slopes	E0814B	3	2759665	2rdbd	nd059	1998	1:20000
Belfield-Daglum-Farland silt loams, 0 to 2 percent slopes	E0403A	287	2662535	2r4g0	nd061	1988	1:24000
Morton-Farland silt loams, 3 to 6 percent slopes	E2927B	9374	2525954	1vzv5	nd065	1971	1:20000
Grail-Farland silt loams, 2 to 6 percent slopes	E0814B	3103	2525911	2rdbd	nd065	1971	1:20000
Farland silt loam, 0 to 2 percent slopes	E2203A	1259	2525938	1vztg	nd065	1971	1:20000
Morton-Farland silt loams, 0 to 3 percent slopes	E2927A	717	2525953	1vzv4	nd065	1971	1:20000
Farland silt loam, 2 to 6 percent slopes	E2203B	265	2525939	1vzth	nd065	1971	1:20000
Belfield-Daglum-Farland silt loams, 0 to 2 percent slopes	E0403A	18512	2707357	2r4g0	nd087	1974	1:20000
Belfield-Daglum-Farland silt loams, 2 to 6 percent slopes	E0403B	10740	2707358	2r4g1	nd087	1974	1:20000
Morton-Farland silt loams, 3 to 6 percent slopes	E2927B	6174	2715835	1vzv5	nd087	1974	1:20000
Farland silt loam, 0 to 2 percent slopes	E2203A	3716	2707416	1vztg	nd087	1974	1:20000
Morton-Farland silt loams, 0 to 3 percent slopes	E2927A	2161	2715834	1vzv4	nd087	1974	1:20000
Grail-Farland silt loams, 2 to 6 percent slopes	E0814B	895	2707380	2rdbd	nd087	1974	1:20000
Farland silt loam, 2 to 6 percent slopes	E2203B	641	2707417	1vzth	nd087	1974	1:20000
Morton-Farland silt loams, 3 to 6 percent slopes	E2927B	1358	1713541	1vzv5	nd089	1965	1:20000
Farland silt loam, 0 to 2 percent slopes	E2203A	495	1713519	1vztg	nd089	1965	1:20000
Morton-Farland silt loams, 0 to 3 percent slopes	E2927A	305	1713540	1vzv4	nd089	1965	1:20000
Farland silt loam, 2 to 6 percent slopes	E2203B	92	1713520	1vzth	nd089	1965	1:20000
Farland silt loam, 6 to 9 percent slopes	E2203C	78	1713521	1vztj	nd089	1965	1:20000
Farland silt loam, 2 to 6 percent slopes	E2203B	3361	2662567	1vzth	nd105	1993	1:24000
Farland silt loam, 0 to 6 percent slopes	669	1533	339143	ccx3	nd105	1993	1:24000
Farland silt loam, 0 to 6 percent slopes	C466B	513	2567033	2q6l8	nd105	1993	1:24000
Morton-Farland silt loams, 0 to 2 percent slopes	MfA	4534	354211	cwl5	sd041	1972	1:24000
Farland silt loam, 0 to 2 percent slopes	FaA	2330	354190	2zr09	sd041	1972	1:24000
Farland silt loam, 2 to 6 percent slopes	FaB	991	354191	2zr0b	sd041	1972	1:24000
Farland silt loam, 0 to 2 percent slopes	FaA	2234	355840	2zr09	sd137	1985	1:24000
Farland silt loam, 2 to 6 percent slopes	FaB	1031	355841	2zr0b	sd137	1985	1:24000

Map of Series Extent

Approximate geographic distribution of the FARLAND 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).