Soil Data Explorer - ARLAND

Official Series Description

Lab Data Summary

Aggregate lab data for the ARLAND soil series. This aggregation is based on all pedons with a current taxon name of ARLAND, 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 ARLAND were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). 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
105	40A2015	S1947WI005023	Arland	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.2938881,-91.7327805
105	98P0081	S1979WI017003	Arland	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.98336,-91.55294
105	81P0092	S1980WI017001	Arland	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.13881,-91.63779
90B	98P0083	S1979WI017005	Arland	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.20377,-91.58408
90B	81P0093	S1980WI017004	Arland	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.08943,-91.53059

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ARLAND 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 ARLAND series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-06) and snapshot of SC database (updated 2023-10-02).

Select annual climate data summaries for the ARLAND 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 2023-10-09).

Geomorphic description summaries for the ARLAND 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 2023-10-04).

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 ARLAND share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-06) and snapshot of the SC database (updated 2023-10-02).

Select annual climate data summaries for the ARLAND 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 2023-10-09).

Geomorphic description summaries for the ARLAND 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 2023-10-04).

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

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

Soil series sharing subgroup-level classification with ARLAND, 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 2023-10-02).

Block Diagrams

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

1. WI-2010-11-08-01 | Barron County - 2001

   Typical pattern of soils and parent material in the Arland-Hayriver-Freeon association (Soil Survey of Barron County, Wisconsin; 2001).

Map Units

Map units containing ARLAND 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
Arland fine sandy loam, 6 to 12 percent slopes, eroded	ApC2	11073	431273	ggs1	wi005	1993	1:20000
Arland silt loam, 2 to 6 percent slopes	AsB	7128	431275	ggs3	wi005	1993	1:20000
Arland fine sandy loam, 2 to 6 percent slopes	ApB	6535	431272	ggs0	wi005	1993	1:20000
Arland silt loam, 6 to 12 percent slopes, eroded	AsC2	5610	431276	ggs4	wi005	1993	1:20000
Arland fine sandy loam, 12 to 25 percent slopes	ApD	5406	431274	ggs2	wi005	1993	1:20000
Arland sandy loam, 6 to 12 percent slopes, eroded	ApC2	5058	421486	g4lb	wi017	1985	1:15840
Arland loam, 6 to 12 percent slopes, eroded	AsC2	3093	421489	g4lf	wi017	1985	1:15840
Arland sandy loam, 2 to 6 percent slopes	ApB	2988	421485	g4l9	wi017	1985	1:15840
Arland loam, 2 to 6 percent slopes	AsB	2957	421488	g4ld	wi017	1985	1:15840
Arland sandy loam, 12 to 20 percent slopes, eroded	ApD2	1520	421487	g4lc	wi017	1985	1:15840
Arland loam, 12 to 20 percent slopes, eroded	AsD2	821	421490	g4lg	wi017	1985	1:15840
Arland fine sandy loam, 6 to 12 percent slopes, moderately eroded, dissected	804C2	945	2518691	n5bb	wi033	2003	1:15840
Arland fine sandy loam, 12 to 25 percent slopes, dissected	804D	568	2518692	n5bc	wi033	2003	1:15840
Arland fine sandy loam, 2 to 6 percent slopes, moderately eroded, dissected	804B2	55	2518690	n5b8	wi033	2003	1:15840
Arland sandy loam, 6 to 12 percent slopes, eroded	AtC2	1166	421742	g4vl	wi035	1974	1:15840
Arland sandy loam, 2 to 6 percent slopes	AtB	382	421741	g4vk	wi035	1974	1:15840
Arland sandy loam, 12 to 20 percent slopes, eroded	AtD2	334	421743	g4vm	wi035	1974	1:15840
Arland fine sandy loam, 12 to 25 percent slopes, dissected	804D	289	3099699	n5bc	wi035	1974	1:15840
Arland fine sandy loam, 6 to 12 percent slopes, moderately eroded, dissected	804C2	158	3099698	n5bb	wi035	1974	1:15840
Arland fine sandy loam, 2 to 6 percent slopes, moderately eroded, dissected	804B2	71	3099697	n5b8	wi035	1974	1:15840
Arland loam, warm variant, 2 to 6 percent slopes, moderately eroded	ArB2	938	425197	g8g1	wi045	1969	1:12000
Arland loam, warm variant, 6 to 12 percent slopes, moderately eroded	ArC2	566	425198	g8g2	wi045	1969	1:12000
Arland loam, warm variant, 12 to 20 percent slopes, moderately eroded	ArD2	160	425199	g8g3	wi045	1969	1:12000
Arland silt loam, 2 to 6 percent slopes	AsB	4516	422110	g57g	wi109	1975	1:15840
Arland silt loam, 6 to 12 percent slopes, eroded	AsC2	3752	422111	g57h	wi109	1975	1:15840
Arland sandy loam, 12 to 25 percent slopes, eroded	ApD2	3174	422108	g57d	wi109	1975	1:15840
Arland sandy loam, 6 to 12 percent slopes, eroded	ApC2	2242	422107	g57c	wi109	1975	1:15840
Arland sandy loam, 25 to 35 percent slopes	ApF	1134	422109	g57f	wi109	1975	1:15840

Map of Series Extent

Approximate geographic distribution of the ARLAND 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 2023-10-04).