Soil Data Explorer - EASTPORT

Official Series Description

Lab Data Summary

Aggregate lab data for the EASTPORT soil series. This aggregation is based on all pedons with a current taxon name of EASTPORT, 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 EASTPORT were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.

Water Balance

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

Competing Series

Soil series competing with EASTPORT 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 EASTPORT 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 EASTPORT 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 terrace figure.

Soil series sharing subgroup-level classification with EASTPORT, 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 EASTPORT 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
Eastport sand, 0 to 6 percent slopes	11B	393	190242	6cyv	mi001	1993	1:20000
Eastport sand, 0 to 6 percent slopes	11B	108	191249	6f0b	mi007	1998	1:12000
Eastport-Rubicon sands, 0 to 6 percent slopes	ErB	2829	189151	6btn	mi011	1964	1:20000
Eastport-Rubicon-Roscommon association, undulating	EtB	1915	189159	6btx	mi011	1964	1:20000
Eastport-Rubicon association, rolling	EsC	1170	189158	6btw	mi011	1964	1:20000
Eastport-Grattan sands, 6 to 12 percent slopes	EgC	873	2673440	2qz4p	mi011	1964	1:20000
Eastport-Grattan sands, 0 to 6 percent slopes	EgB	412	2673439	2qz4n	mi011	1964	1:20000
Eastport-Rubicon sands, 6 to 12 percent slopes	ErC	392	189152	6btp	mi011	1964	1:20000
Adrian-Eastport-Rubicon association, undulating	AeB	292	189107	6bs7	mi011	1964	1:20000
Eastport-Rubicon sands, 6 to 12 percent slopes, moderately eroded	ErC2	121	189153	6btq	mi011	1964	1:20000
Eastport-Grattan sands, 12 to 18 percent slopes	EgD	114	2673442	2qz4r	mi011	1964	1:20000
Eastport-Grattan association, rolling	EhC	96	2673445	2qz4v	mi011	1964	1:20000
Eastport-Grattan sands, 12 to 18 percent slopes, moderately eroded	EgD2	50	2673443	2qz4s	mi011	1964	1:20000
Eastport-Rubicon sands, 12 to 18 percent slopes	ErD	39	189154	6btr	mi011	1964	1:20000
Eastport-Grattan sands, 25 to 45 percent slopes	EgF	30	2673444	2qz4t	mi011	1964	1:20000
Eastport-Grattan sands, 6 to 12 percent slopes, moderately eroded	EgC2	27	2673441	2qz4q	mi011	1964	1:20000
Eastport-Rubicon sands, 18 to 25 percent slopes, moderately eroded	ErE2	24	189156	6btt	mi011	1964	1:20000
Eastport-Rubicon sands, 25 to 45 percent slopes	ErF	22	189157	6btv	mi011	1964	1:20000
Eastport-Rubicon sands, 12 to 18 percent slopes, moderately eroded	ErD2	7	189155	6bts	mi011	1964	1:20000
Eastport-Grattan sands, 0 to 6 percent slopes	123B	23	2673575	2qz4n	mi017	1978	1:20000
Eastport-Grattan sands, 12 to 18 percent slopes	123D	2	2673576	2qz4r	mi017	1978	1:20000
Eastport sand, 0 to 6 percent slopes	EdB	1027	190425	6d4r	mi029	1970	1:15840
Eastport sand, 6 to 12 percent slopes	EdC	512	190426	6d4s	mi029	1970	1:15840
Eastport sand, 0 to 6 percent slopes	25B	1124	190555	6d8y	mi031	1988	1:15840
Eastport sand, 12 to 25 percent slopes	25D	288	190556	6d8z	mi031	1988	1:15840
Eastport-Roscommon sands, 0 to 6 percent slopes	EeB	3386	1588048	1q9hc	mi041	1969	1:24000
Eastport sand, 0 to 6 percent slopes	EdB	2970	1588047	1q9hb	mi041	1969	1:24000
Roscommon-Eastport sands, 0 to 6 percent slopes	ReB	2028	189366	6c1l	mi047	1968	1:20000
Eastport sand, 0 to 6 percent slopes	EdB	1988	189330	6c0f	mi047	1968	1:20000
Lake beach and Eastport sand, 0 to 6 percent slopes	LeB	700	189498	6c5v	mi055	1963	1:15840
Eastport-Roscommon sands, 0 to 2 percent slopes	ErA	368	189411	6c31	mi055	1963	1:15840
Eastport sand, 0 to 6 percent slopes	EdB	6434	190791	6djk	mi089	1967	1:20000
Eastport-Leafriver complex, 0 to 35 percent slopes	38E	10503	416398	fz96	mi097	1994	1:20000
Eastport sand, 15 to 35 percent slopes	17E	4642	416362	fz81	mi097	1994	1:20000
Eastport sand, 0 to 15 percent slopes	17D	856	416361	fz80	mi097	1994	1:20000
Eastport sand, 1 to 8 percent slopes	67B	1009	190931	6dp2	mi141	1989	1:15840
Eastport sand, 0 to 6 percent slopes	EaB	1930	187413	690l	mi147	1969	1:20000
Eastport sand, 6 to 18 percent slopes	EaC	435	187414	690m	mi147	1969	1:20000
Eastport, Arenac, and Kalkaska sands, 2 to 7 percent slopes, slightly eroded	EaB1	339	188249	69wk	mi151	1955	1:15840
Eastport, Arenac, and Kalkaska sands, 0 to 2 percent slopes, slightly eroded	EaA1	181	188248	69wj	mi151	1955	1:15840
Eastport fine sand and beach sand, 0 to 2 percent slopes	EbA0	154	188251	69wm	mi151	1955	1:15840
Eastport fine sand and beach sand, 2 to 18 percent slopes	EbC0	144	188252	69wn	mi151	1955	1:15840
Eastport, Arenac, and Kalkaska sands, 7 to 14 percent slopes, slightly eroded	EaC1	106	188250	69wl	mi151	1955	1:15840
Eastport sand, 0 to 6 percent slopes	EsB	55	2508266	690l	mi151	1955	1:15840

Map of Series Extent

Approximate geographic distribution of the EASTPORT 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).