Soil Data Explorer - BROCKPORT

Official Series Description

Lab Data Summary

Aggregate lab data for the BROCKPORT soil series. This aggregation is based on all pedons with a current taxon name of BROCKPORT, 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 BROCKPORT 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 BROCKPORT 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 BROCKPORT 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 BROCKPORT 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 BROCKPORT 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 BROCKPORT 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 BROCKPORT 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 BROCKPORT 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.

Soil series sharing subgroup-level classification with BROCKPORT, 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 BROCKPORT 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
Brockport and Lockport silty clay loams, 2 to 6 percent slopes	BlB	549	289371	9q3k	ny011	1968	1:15840
Brockport silty clay loam, 0 to 3 percent slopes	BrA	1249	290757	9rk8	ny029	1979	1:15840
Brockport silty clay loam, 3 to 8 percent slopes	BrB	588	290758	9rk9	ny029	1979	1:15840
Brockport silt loam, 3 to 8 percent slopes	30B	424	3105665	2y9vw	ny051	2019	1:24000
Brockport silty clay loam, 0 to 2 percent slopes	BrA	1820	292670	9tjz	ny055	1967	1:15840
Brockport silt loam	Br	1025	292793	9tny	ny057	1973	1:24000
Tuller-Brockport complex, 0 to 3 percent slopes	TvA	8	292892	9ts4	ny057	1973	1:24000
Tuller-Brockport complex, 3 to 8 percent slopes	TvB	5	292893	9ts5	ny057	1973	1:24000
Lockport and Brockport silty clay loams, 0 to 6 percent slopes	LvB	3939	293599	9vhy	ny067	1973	1:20000
Brockport silty clay loam, 2 to 6 percent slopes	BrB	1035	294004	9vy0	ny073	1973	1:15840
Brockport silty clay loam, 0 to 2 percent slopes	BrA	552	294003	9vxz	ny073	1973	1:15840
Brockport silty clay loam, 6 to 12 percent slopes	BrC	156	294005	9vy1	ny073	1973	1:15840
Brockport silty clay loam, 0 to 6 percent slopes	BrB	483	294099	9w12	ny075	1973	1:15840
Tuller-Brockport complex, 0 to 3 percent slopes	TvA	4295	309657	bd6y	ny093	1973	1:15840
Tuller-Brockport complex, 3 to 8 percent slopes	TvB	2014	309658	bd6z	ny093	1973	1:15840
Lockport and Brockport silty clay loams, 0 to 3 percent slopes	LoA	3573	295747	9xr7	ny117	1972	1:15840
Lockport and Brockport silty clay loams, 3 to 8 percent slopes	LoB	917	295748	9xr8	ny117	1972	1:15840
Brockport silt loam, 0 to 4 percent slopes	BrA	509	292969	9tvm	ny664	1968	1:15840

Map of Series Extent

Approximate geographic distribution of the BROCKPORT 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).