Soil Data Explorer - SALMON

Official Series Description

Lab Data Summary

Aggregate lab data for the SALMON soil series. This aggregation is based on all pedons with a current taxon name of SALMON, 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 SALMON 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
142	87P0207	86NY089009	Salmon	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.6083336,-75.0583344
142	87P0210	86NY089012	Salmon	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.584446,-75.0411148
142	87P0211	86NY089013	Salmon	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.584446,-75.0408325

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SALMON 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 SALMON 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 SALMON 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 SALMON 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 SALMON 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 SALMON 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 SALMON 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 SALMON, 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 SALMON 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
Salmon silt loam, 2 to 8 percent slopes	SaB	1177	301876	b43y	me607	1960	1:20000
Salmon silt loam, 8 to 15 percent slopes	SaC	460	301877	b43z	me607	1960	1:20000
Salmon silt loam, 0 to 2 percent slopes	SaA	258	301875	b43x	me607	1960	1:20000
Salmon very fine sandy loam, sandy substratum, 3 to 8 percent slopes	297B	578	1600897	1qqvv	nh603		1:24000
Salmon very fine sandy loam, sandy substratum, 0 to 3 percent slopes	297A	245	1600895	1qqvs	nh603		1:24000
Salmon very fine sandy loam, 3 to 8 percent slopes	630B	616	280542	9dxr	nh607	2000	1:24000
Salmon very fine sandy loam, 8 to 15 percent slopes	630C	583	280543	9dxs	nh607	2000	1:24000
Salmon very fine sandy loam, 0 to 3 percent slopes	630A	412	280541	9dxq	nh607	2000	1:24000
Salmon very fine sandy loam, 15 to 35 percent slopes	630D	281	280544	9dxt	nh607	2000	1:24000
Salmon very fine sandy loam, 2 to 6 percent slopes	Sbb	1662	2677563	bmfh	ny033	2018	1:24000
Salmon stony very fine sandy loam over till, 2 to 6 percent slopes	Scb	1196	2677539	bmfl	ny033	2018	1:24000
Salmon very fine sandy loam, 6 to 12 percent slopes	Sbc	666	2677491	bmfj	ny033	2018	1:24000
Salmon stony very fine sandy loam over till, 0 to 2 percent slopes	Sca	616	2677511	bmfk	ny033	2018	1:24000
Salmon and Nicholville stony very fine sandy loams, 12 to 20 percent slopes	Sdd	501	2677440	bmfp	ny033	2018	1:24000
Salmon very fine sandy loam, 0 to 2 percent slopes	Sba	465	2677504	bmfg	ny033	2018	1:24000
Salmon stony very fine sandy loam over till, 6 to 12 percent slopes	Scc	401	2677498	bmfm	ny033	2018	1:24000
Salmon stony very fine sandy loam over till, 20 to 45 percent slopes	Sce	347	2677519	bmfn	ny033	2018	1:24000
Salmon-Nicholville complex, 0 to 8 percent slopes	390B	346	1912928	226kc	ny033	2018	1:24000
Salmon silt loam, 3 to 8 percent slopes	SyB	116	2753652	2spkn	ny033	2018	1:24000
Salmon very fine sandy loam, rolling	SaC	7	2679509	9wzl	ny033	2018	1:24000
Salmon-Nicholville complex, 0 to 8 percent slopes	390B	1121	2518240	226kc	ny043	2018	1:24000
Salmon-Nicholville complex, 0 to 8 percent slopes	390B	1724	2516800	226kc	ny049	2018	1:24000
Salmon silt loam, 2 to 8 percent slopes	36B	741	293410	9v9v	ny065	1993	1:24000
Salmon very fine sandy loam, rolling	SaC	2709	295014	9wzl	ny089	1990	1:24000
Salmon very fine sandy loam, 2 to 6 percent slopes	SaB	1222	295013	9wzk	ny089	1990	1:24000
Salmon very fine sandy loam, 2 to 6 percent slopes	SaB	279	281308	9fqg	vt001	1967	1:15840
Salmon very fine sandy loam, 12 to 50 percent slopes	SaE	237	281310	9fqj	vt001	1967	1:15840
Salmon very fine sandy loam, 6 to 12 percent slopes	SaC	118	281309	9fqh	vt001	1967	1:15840
Salmon very fine sandy loam, 25 to 50 percent slopes	7E	910	282988	9hgn	vt005	2006	1:20000
Salmon very fine sandy loam, 15 to 25 percent slopes	7D	751	282987	9hgm	vt005	2006	1:20000
Salmon-Adamant complex, 25 to 50 percent slopes, very rocky	207E	433	282855	9hbc	vt005	2006	1:20000
Salmon-Adamant complex, 15 to 25 percent slopes, very rocky	207D	420	282854	9hbb	vt005	2006	1:20000
Salmon very fine sandy loam, 8 to 15 percent slopes	7C	388	282986	9hgl	vt005	2006	1:20000
Salmon-Adamant complex, 8 to 15 percent slopes, very rocky	207C	210	282853	9hb9	vt005	2006	1:20000
Salmon very fine sandy loam, 3 to 8 percent slopes	7B	168	282985	9hgk	vt005	2006	1:20000
Salmon variant-Salmon very fine sandy loams, rocky, 15 to 25 percent slopes	SdD	1607	281941	9gcw	vt015	1979	1:20000
Salmon variant-Salmon very fine sandy loams, rocky, 8 to 15 percent slopes	SdC	1583	281940	9gcv	vt015	1979	1:20000
Salmon very fine sandy loam, 25 to 50 percent slopes, eroded	SaE2	1526	281939	9gct	vt015	1979	1:20000
Salmon very fine sandy loam, 8 to 15 percent slopes, eroded	SaC2	1205	281936	9gcq	vt015	1979	1:20000
Salmon variant-Salmon very fine sandy loams, rocky, 25 to 50 percent slopes	SdE	1143	281942	9gcx	vt015	1979	1:20000
Salmon very fine sandy loam, 15 to 25 percent slopes, eroded	SaD2	942	281938	9gcs	vt015	1979	1:20000
Salmon very fine sandy loam, 8 to 15 percent slopes	SaC	825	281935	9gcp	vt015	1979	1:20000
Salmon very fine sandy loam, 3 to 8 percent slopes, eroded	SaB2	526	281934	9gcn	vt015	1979	1:20000
Salmon very fine sandy loam, 15 to 25 percent slopes	SaD	485	281937	9gcr	vt015	1979	1:20000
Salmon very fine sandy loam, 3 to 8 percent slopes	SaB	263	281933	9gcm	vt015	1979	1:20000
Salmon very fine sandy loam, 25 to 50 percent slopes	54E	1417	283493	9hzy	vt019	2005	1:20000
Salmon very fine sandy loam, 15 to 25 percent slopes	54D	402	283492	9hzx	vt019	2005	1:20000
Salmon very fine sandy loam, 8 to 15 percent slopes	54C	343	283491	9hzw	vt019	2005	1:20000
Salmon very fine sandy loam, 3 to 8 percent slopes	54B	118	283490	9hzv	vt019	2005	1:20000
Salmon very fine sandy loam, 25 to 50 percent slopes	43E	2929	282665	9h47	vt023	1996	1:20000
Salmon-Adamant complex, 25 to 50 percent slopes, very rocky	64E	1474	282718	9h5y	vt023	1996	1:20000
Salmon-Adamant complex, 15 to 25 percent slopes, very rocky	64D	1267	282717	9h5x	vt023	1996	1:20000
Salmon very fine sandy loam, 15 to 25 percent slopes	43D	878	282664	9h46	vt023	1996	1:20000
Salmon very fine sandy loam, 3 to 8 percent slopes	43B	805	282662	9h44	vt023	1996	1:20000
Salmon very fine sandy loam, 8 to 15 percent slopes	43C	626	282663	9h45	vt023	1996	1:20000
Salmon-Adamant complex, 8 to 15 percent slopes, very rocky	64C	560	282716	9h5w	vt023	1996	1:20000

Map of Series Extent

Approximate geographic distribution of the SALMON 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).