Soil Data Explorer - MORGANLAKE

Official Series Description

Lab Data Summary

Aggregate lab data for the MORGANLAKE soil series. This aggregation is based on all pedons with a current taxon name of MORGANLAKE, 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 MORGANLAKE 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
92	79P0081	S1978WI003003	Morganlake	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	46.9994431,-90.452774
92	05N0180	S2004MI131003	Morganlake	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	46.8916626,-89.0942383
94A	94P0847	S1993MI119003	Morganlake	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.9086113,-84.2266693
94A	00P0291	S1999MI135003	Morganlake	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.7758064,-84.0391922

Water Balance

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

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the MORGANLAKE 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 2D hillslope position figure.

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

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.

Soil series sharing subgroup-level classification with MORGANLAKE, 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

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

1. MI-2010-09-07-07 | Kalkaska County - 2005

   Typical pattern of soils and parent material in the Islandlake-Blue Lake-Morganlake, sandy substratum, general soil map unit (Soil Survey of Kalkaska County, Michigan; 2005).

2. MI-2010-09-07-26 | Montmorency County - 2003

   Typical pattern of soils and underlying material in the Bamfield-Menominee-Lupton association (Soil Survey of Montmorency County, Michigan; 2003).

Map Units

Map units containing MORGANLAKE 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
Morganlake loamy sand, 0 to 6 percent slopes	393B	14000	191336	6f34	mi007	1998	1:12000
Morganlake loamy sand, 6 to 12 percent slopes	393C	4816	191337	6f35	mi007	1998	1:12000
Morganlake-Ossineke, sandy substratum-Blue Lake complex, 0 to 6 percent slopes	424B	47	191378	6f4h	mi007	1998	1:12000
Morganlake-Ossineke, sandy substratum-Blue Lake complex, 6 to 12 percent slopes	424C	4	191379	6f4j	mi007	1998	1:12000
Morganlake loamy sand, 0 to 6 percent slopes	MrgaaB	101	3155935	2ytj9	mi009	1976	1:15840
Zandi-Morganlake complex, dissected, 25 to 60 percent slopes	8104F	1182	2483882	2pcp7	mi061	1989	1:20000
Morganlake loamy fine sand, 0 to 6 percent slopes	8212B	708	2484938	2pds9	mi061	1989	1:20000
Morganlake loamy fine sand, 6 to 12 percent slopes	8212C	520	2484939	2pdsb	mi061	1989	1:20000
Morganlake sand, 0 to 6 percent slopes	120B	5904	191700	6fgw	mi069	1995	1:15840
Morganlake-Nester complex, 0 to 6 percent slopes	441B	3349	191880	6fnp	mi069	1995	1:15840
Morganlake sand, 6 to 12 percent slopes	120C	747	191701	6fgx	mi069	1995	1:15840
Morganlake-Nester complex, 6 to 12 percent slopes	441C	358	191881	6fnq	mi069	1995	1:15840
Graycalm-Menominee-Morganlake sands, 6 to 18 percent slopes	434D	288	191872	6fnf	mi069	1995	1:15840
Morganlake-Graycalm sands, 0 to 6 percent slopes	433B	200	191871	6fnd	mi069	1995	1:15840
Morganlake, sandy substratum-Woodman-Blue Lake complex, 1 to 6 percent slopes	467B	2571	190723	6dgc	mi079	1998	1:12000
Morganlake, sandy substratum-Woodman-Blue Lake complex, 6 to 12 percent slopes	467C	1158	190724	6dgd	mi079	1998	1:12000
Morganlake loamy sand, sandy substratum, 0 to 6 percent slopes	472B	294	190729	6dgk	mi079	1998	1:12000
Morganlake-Ossineke, sandy substratum-Blue Lake complex, 0 to 6 percent slopes	424B	4010	192400	6g6g	mi119	1997	1:12000
Morganlake loamy sand, 0 to 6 percent slopes	393B	3787	192286	6g2s	mi119	1997	1:12000
Morganlake-Ossineke, sandy substratum-Blue Lake complex, 6 to 12 percent slopes	424C	2283	192401	6g6h	mi119	1997	1:12000
Morganlake-Iosco-Deford complex, 0 to 6 percent slopes	422B	1640	192295	6g32	mi119	1997	1:12000
Morganlake loamy sand, 6 to 12 percent slopes	393C	907	192287	6g2t	mi119	1997	1:12000
Zandi-Morganlake complex, dissected, 25 to 60 percent slopes	8104F	1076	1674821	1t6sh	mi131	2007	1:24000
Morganlake loamy fine sand, 0 to 6 percent slopes	60B	854	1456461	1kwkm	mi131	2007	1:24000
Morganlake loamy fine sand, 6 to 12 percent slopes	8212C	83	1674864	1t6tw	mi131	2007	1:24000
Morganlake loamy sand, 0 to 6 percent slopes	393B	1211	209050	70jk	mi135	2003	1:12000
Morganlake-Nester complex, 0 to 6 percent slopes	441B	885	209054	70jp	mi135	2003	1:12000
Morganlake-Ossineke, sandy substratum-Blue Lake complex, 6 to 12 percent slopes	424C	829	628170	p2nk	mi135	2003	1:12000
Morganlake-Ossineke, sandy substratum-Blue Lake complex, 0 to 6 percent slopes	424B	692	628171	p2nl	mi135	2003	1:12000
Morganlake-Nester complex, 6 to 12 percent slopes	441C	363	209055	70jq	mi135	2003	1:12000
Morganlake loamy sand, 6 to 12 percent slopes	393C	304	209052	70jm	mi135	2003	1:12000
Morganlake loamy sand, 0 to 6 percent slopes	393B	4018	191488	6f81	mi137	1998	1:12000
Morganlake loamy sand, 6 to 12 percent slopes	393C	1956	191489	6f82	mi137	1998	1:12000
Morganlake-Ossineke, sandy substratum-Blue Lake complex, 0 to 6 percent slopes	424B	1817	191497	6f8b	mi137	1998	1:12000
Morganlake-0ssineke, sandy substratum,-Blue Lake complex, 6 to 12 percent slopes	424C	1469	191498	6f8c	mi137	1998	1:12000
Morganlake-Nester complex, 0 to 6 percent slopes	441B	1774	191060	6dt7	mi143	1999	1:12000
Morganlake sand, 0 to 6 percent slopes	120B	1290	191009	6drl	mi143	1999	1:12000
Morganlake sand, 6 to 12 percent slopes	120C	459	191010	6drm	mi143	1999	1:12000
Morganlake-Nester complex, 6 to 12 percent slopes	441C	151	191081	6dtx	mi143	1999	1:12000
Morganlake loamy sand, 0 to 6 percent slopes	712B	3638	1444479	1kh33	wi003	2006	1:12000
Morganlake loamy sand, 6 to 15 percent slopes	712C	526	1444480	1kh34	wi003	2006	1:12000
Morganlake loamy sand, 0 to 6 percent slopes	712B	1691	433744	gkbr	wi007	2005	1:12000
Morganlake loamy sand, 6 to 15 percent slopes	712C	1356	433745	gkbs	wi007	2005	1:12000
Morganlake loamy sand, 0 to 6 percent slopes	712B	1216	781443	v74v	wi031	2005	1:12000
Morganlake loamy sand, 6 to 15 percent slopes	712C	442	781444	v74w	wi031	2005	1:12000
Ellwood-Iosco-Morganlake complex, 0 to 6 percent slopes	EmB	1526	430000	gffz	wi037	1995	1:12000
Morganlake loamy fine sand, 0 to 6 percent slopes	MrB	468	430016	gfgh	wi037	1995	1:12000
Morganlake loamy sand, 0 to 6 percent slopes	712B	409	782311	v81v	wi051	2006	1:12000
Morganlake loamy sand, 6 to 15 percent slopes	712C	94	782312	v81w	wi051	2006	1:12000
Morganlake loamy fine sand, 0 to 6 percent slopes	MxB	2092	395821	f8wf	wi078	1998	1:12000

Map of Series Extent

Approximate geographic distribution of the MORGANLAKE 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).