Soil Data Explorer - CHADAKOIN

Official Series Description

Lab Data Summary

Aggregate lab data for the CHADAKOIN soil series. This aggregation is based on all pedons with a current taxon name of CHADAKOIN, 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 CHADAKOIN 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
140	92P0038	S1991NY077004	Chadakoin	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.5683327,-74.9288864

Water Balance

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

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

Competing Series

Soil series competing with CHADAKOIN 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 CHADAKOIN 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 CHADAKOIN 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 CHADAKOIN, 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 CHADAKOIN 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
Chadakoin channery silt loam, 35 to 50 percent slopes	51F	644	299909	b22h	ny003	2013	1:24000
Chadakoin channery silt loam, 25 to 35 percent slopes	51E	299	299908	b22g	ny003	2013	1:24000
Chadakoin channery silt loam, 8 to 15 percent slopes	51C	48	299906	b22d	ny003	2013	1:24000
Chadakoin channery silt loam, 15 to 25 percent slopes	51D	47	299907	b22f	ny003	2013	1:24000
Chadakoin channery silt loam, 25 to 35 percent slopes	51E	7235	289630	9qcx	ny009	2002	1:24000
Chadakoin channery silt loam, 15 to 25 percent slopes	51D	2696	289629	9qcw	ny009	2002	1:24000
Chadakoin channery silt loam, 35 to 50 percent slopes	51F	2548	289631	9qcy	ny009	2002	1:24000
Chadakoin channery silt loam, 8 to 15 percent slopes	51C	1860	289628	9qcv	ny009	2002	1:24000
Chadakoin channery silt loam, 3 to 8 percent slopes	51B	658	289627	9qct	ny009	2002	1:24000
Chadakoin silt loam, 15 to 25 percent slopes	ChD	6821	289793	9qk5	ny013	1988	1:15840
Chadakoin silt loam, 25 to 35 percent slopes	ChE	6752	289794	9qk6	ny013	1988	1:15840
Chadakoin silt loam, 8 to 15 percent slopes	ChC	5522	289792	9qk4	ny013	1988	1:15840
Chadakoin silt loam, 35 to 50 percent slopes	ChF	3543	289795	9qk7	ny013	1988	1:15840
Chadakoin silt loam, 3 to 8 percent slopes	ChB	2417	289791	9qk3	ny013	1988	1:15840
Chadakoin silt loam, 3 to 8 percent slopes	115B	6790	293311	9v6n	ny065	1993	1:24000
Chadakoin silt loam, 8 to 15 percent slopes	115C	4575	293312	9v6p	ny065	1993	1:24000
Chadakoin silt loam, 15 to 25 percent slopes	115D	2856	293313	9v6q	ny065	1993	1:24000
Chadakoin silt loam, 25 to 45 percent slopes	115E	1170	293314	9v6r	ny065	1993	1:24000
Lordstown, Chadakoin, and Manlius soils, 25 to 50 percent slopes, very rocky	LrE	31671	294242	2zxqz	ny077	1993	1:24000
Lordstown-Chadakoin complex, 15 to 25 percent slopes	LpD	19939	294241	9w5n	ny077	1993	1:24000
Lordstown-Chadakoin complex, 8 to 15 percent slopes	LpC	17016	294240	9w5m	ny077	1993	1:24000

Map of Series Extent

Approximate geographic distribution of the CHADAKOIN 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).