Soil Data Explorer - VINLAND

Official Series Description

Lab Data Summary

Aggregate lab data for the VINLAND soil series. This aggregation is based on all pedons with a current taxon name of VINLAND, 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 VINLAND 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
106	04KS103503	04KS103503	Vinland	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.0545387,-95.0911789
106	04KS103968	04KS103968	Vinland	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.1425323,-95.0282516
106	07KS005001	07KS005001	Vinland	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.4703484,-95.1949158
106	07KS087021	07KS087021	Vinland	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.2591667,-95.4563904
106	07KS087022	07KS087022	Vinland	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.1094437,-95.2249985
106	07KS087024	07KS087024	Vinland	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.2588882,-95.4597244
106	07KS103008	07KS103008	Vinland	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.3379936,-95.0789719
106	08KS005012	08KS005012	Vinland	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.5946388,-95.3908615
106	08KS087013	08KS087013	Vinland	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.1151962,-95.2022247
106	08KS087014	08KS087014	Vinland	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.1152229,-95.2020798
106	08KS087016	08KS087016	Vinland	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.09161,-95.2079468
106	08KS087017	08KS087017	Vinland	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.088974,-95.2091675
106	00P0112	99KS103016	Vinland	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.1025352,-95.0574799
106	05N0493	S2005KS087004	Vinland	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.2619438,-95.460556

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the VINLAND 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 VINLAND 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 VINLAND 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 VINLAND 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 terrace figure.

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

Competing Series

Soil series competing with VINLAND 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 VINLAND 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 VINLAND 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 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 VINLAND, 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. KS-2010-09-09-03 | Hillsdale Watershed -

   Typical pattern of soils and parent material in the Woodson-Sibleyville-Summit association.

2. KS-2012-01-25-36 | Shawnee County - June 1970

   Loess-till area in the northern part of Shawnee County showing the relation of soils to the landscape in soil association 3 (Soil Survey of Shawnee County, Kansas; 1970).

3. KS-2012-01-25-37 | Shawnee County - June 1970

   Relation of soils to landscape in soil association 6 in the southwestern part of the county (Soil Survey of Shawnee County, Kansas; 1970).

Map Units

Map units containing VINLAND 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
Vinland silty clay loam, 4 to 15 percent slopes	7655	3801	1475374	2yrvs	ks005	1998	1:24000
Vinland-Rock outcrop complex, 15 to 45 percent slopes	7658	861	1475375	2yrvt	ks005	1998	1:24000
Bendena-Vinland complex, 8 to 30 percent slopes	7216	101	1480279	1lpby	ks005	1998	1:24000
Vinland-Sibleyville complex, 7 to 15 percent slopes	7666	96	2420328	2yrvz	ks005	1998	1:24000
Wamego-Vinland silty clay loams, 3 to 15 percent slopes	4834	95	1475347	2vhh3	ks005	1998	1:24000
Wallula-Vinland complex, 5 to 40 percent slopes	7672	94	2420336	2x6bv	ks005	1998	1:24000
Sogn-Vinland complex, 3 to 25 percent slopes	4752	12	1480270	2wvzj	ks005	1998	1:24000
Wamego-Vinland silty clay loams, 3 to 15 percent slopes	4834	5032	1152156	2vhh3	ks013	1994	1:24000
Bendena-Vinland complex, 8 to 30 percent slopes	7216	2295	747153	t2gq	ks043	1977	1:24000
Wamego-Vinland silty clay loams, 3 to 15 percent slopes	4834	13	747191	2vhh3	ks043	1977	1:24000
Vinland-Martin complex, 7 to 15 percent slopes	7657	18899	1468857	2yrw2	ks045	1974	1:24000
Sogn-Vinland complex, 3 to 25 percent slopes	4752	14454	1468812	2wvzj	ks045	1974	1:24000
Vinland-Rock outcrop complex, 15 to 45 percent slopes	7658	10936	1468858	2yrvt	ks045	1974	1:24000
Vinland complex, 3 to 7 percent slopes	7651	3968	1468855	2yrvp	ks045	1974	1:24000
Vinland complex, 3 to 7 percent slopes, eroded	7652	857	1468856	2yrvq	ks045	1974	1:24000
Sibleyville-Vinland loams, 3 to 7 percent slopes	7607	66	1468853	1l9gc	ks045	1974	1:24000
Vinland loam, 3 to 12 percent slopes	7654	16	1453662	1ksnb	ks073	1981	1:24000
Martin-Vinland silty clay loams, 5 to 10 percent slopes	7330	24210	1480352	2v8zy	ks085	1976	1:24000
Vinland-Sogn complex, 5 to 15 percent slopes	7660	7924	1480373	2wvzl	ks085	1976	1:24000
Vinland silty clay loam, 4 to 15 percent slopes	7655	3119	1480371	2yrvs	ks085	1976	1:24000
Vinland-Rock outcrop complex, 15 to 45 percent slopes	7658	1841	1480372	2yrvt	ks085	1976	1:24000
Sogn-Vinland complex, 3 to 25 percent slopes	4752	950	1480329	2wvzj	ks085	1976	1:24000
Vinland complex, 3 to 7 percent slopes	7651	164	1480369	2yrvp	ks085	1976	1:24000
Wamego-Vinland silty clay loams, 3 to 15 percent slopes	4834	71	1480331	2vhh3	ks085	1976	1:24000
Vinland complex, 7 to 15 percent slopes	7653	7	1480370	2yrvr	ks085	1976	1:24000
Vinland complex, 7 to 15 percent slopes	7653	20366	1480077	2yrvr	ks087	1974	1:24000
Vinland-Rock outcrop complex, 15 to 45 percent slopes	7658	16013	1480080	2yrvt	ks087	1974	1:24000
Sogn-Vinland complex, 3 to 25 percent slopes	4752	11718	1480030	2wvzj	ks087	1974	1:24000
Vinland complex, 3 to 7 percent slopes	7651	9103	1480076	2yrvp	ks087	1974	1:24000
Vinland-Sibleyville complex, 7 to 15 percent slopes	7666	1454	2420329	2yrvz	ks087	1974	1:24000
Vinland-Sibleyville complex, 3 to 7 percent slopes	7665	265	2420327	2yrvy	ks087	1974	1:24000
Vinland silty clay loam, 4 to 15 percent slopes	7655	169	1480078	2yrvs	ks087	1974	1:24000
Vinland-Martin complex, 7 to 15 percent slopes	7657	164	1480079	2yrw2	ks087	1974	1:24000
Wallula-Vinland complex, 5 to 40 percent slopes	7672	162	2420335	2x6bv	ks087	1974	1:24000
Martin-Vinland silty clay loams, 5 to 10 percent slopes	7330	25	1480059	2v8zy	ks087	1974	1:24000
Sogn-Vinland complex, 3 to 25 percent slopes	4752	13795	766074	2wvzj	ks091	1976	1:24000
Vinland-Rock outcrop complex, 15 to 45 percent slopes	7658	9069	766075	2yrvt	ks091	1976	1:24000
Sibleyville-Vinland loams, 3 to 7 percent slopes	7607	1576	766073	tq51	ks091	1976	1:24000
Martin-Vinland silty clay loams, 5 to 10 percent slopes	7330	1448	766061	2v8zy	ks091	1976	1:24000
Vinland-Sibleyville complex, 7 to 15 percent slopes	7666	4802	2420330	2yrvz	ks103	1973	1:24000
Wallula-Vinland complex, 5 to 40 percent slopes	7672	1916	2420334	2x6bv	ks103	1973	1:24000
Vinland-Sibleyville complex, 5 to 12 percent slopes	7659	1906	1862398	2yrvv	ks103	1973	1:24000
Vinland-Sibleyville complex, 3 to 7 percent slopes	7665	1453	2420326	2yrvy	ks103	1973	1:24000
Vinland-Rock outcrop complex, 15 to 40 percent slopes	7667	1417	2420332	2yrw0	ks103	1973	1:24000
Vinland loam, 3 to 12 percent slopes	7654	1095	1453727	1ksqf	ks111	1977	1:24000
Vinland variant loam, 5 to 25 percent slopes	7656	475	1406033	2yrw1	ks131	1980	1:24000
Sogn-Vinland complex, 3 to 25 percent slopes	4752	2420	1454762	2wvzj	ks139	1983	1:24000
Vinland-Martin complex, 7 to 15 percent slopes	7657	434	1454778	2yrw2	ks139	1983	1:24000
Vinland-Rock outcrop complex, 15 to 45 percent slopes	7658	188	1454779	2yrvt	ks139	1983	1:24000
Vinland-Sogn complex, 15 to 45 percent slopes	7661	167	1454780	2wvzm	ks139	1983	1:24000
Sogn-Vinland complex, 3 to 25 percent slopes	4752	30534	1473462	2wvzj	ks177	1966	1:24000
Vinland-Rock outcrop complex, 15 to 45 percent slopes	7658	5986	1473531	2yrvt	ks177	1966	1:24000
Vinland silty clay loam, 4 to 15 percent slopes	7655	1747	1473529	2yrvs	ks177	1966	1:24000
Vinland-Sogn complex, 15 to 45 percent slopes	7661	239	1532315	2wvzm	ks177	1966	1:24000
Vinland-Martin complex, 7 to 15 percent slopes	7657	69	1473530	2yrw2	ks177	1966	1:24000
Martin-Vinland silty clay loams, 5 to 10 percent slopes	7330	13	1473503	2v8zy	ks177	1966	1:24000
Sogn-Vinland complex, 3 to 25 percent slopes	4752	69	1472148	2wvzj	ks197	1988	1:24000
Vinland-Rock outcrop complex, 15 to 45 percent slopes	7658	1416	1862285	2yrvt	ks209	1973	1:24000
Vinland-Sibleyville complex, 5 to 12 percent slopes	7659	396	1862286	2yrvv	ks209	1973	1:24000

Map of Series Extent

Approximate geographic distribution of the VINLAND 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).