Soil Data Explorer - MONARDA

Official Series Description

Lab Data Summary

Aggregate lab data for the MONARDA soil series. This aggregation is based on all pedons with a current taxon name of MONARDA, 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 MONARDA were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). 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
143	83P0337	82NH007002	Monarda	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.9749985,-71.3916702
143	87P0089	86NH007001	Monarda	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.2838898,-71.2847214
143	87P0090	86NH007002	Monarda	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.2552795,-71.2655563
143	09N0153	S08ME021001.Monarda	MONARDA	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	46.0244667,-69.6196833
143	10N0329	S09ME021013.Monarda	Monarda	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.6533889,-69.48675
144A	40A0519	S1968VT021007	Monarda	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.6542332,-73.0884426
144B	40A0413	1958ME019001	Monarda	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.900063,-69.2828247
144B	40A0407	1958ME019002	Monarda	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.9166667,-69.25
144B	40A0412	ME-58-09-019-05	Monarda	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.8571111,-69.2809722
146	12N7807	S11ME003025.Monarda	Monarda	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	46.14075,-67.8961389
n/a	97P0228	S1996NH007010	Monarda	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MONARDA 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 MONARDA 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 MONARDA 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 MONARDA 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 MONARDA 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 MONARDA 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 MONARDA 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 MONARDA, 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. ME-2010-09-03-02 | Franklin County Area and Part of Somerset County - 2003

   Typical pattern of the soils and underlying material in the Telos-Chesuncook-Monarda general soil map unit (Soil Survey of Franklin County Area and Part of Somerset County, Maine; 2003).

Map Units

Map units containing MONARDA 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
Monarda silt loam, 0 to 3 percent slopes, very stony	MrA	14447	284478	2t0yg	me011	1974	1:20000
Monarda silt loam, 0 to 3 percent slopes	MoA	2606	284477	2t0yk	me011	1974	1:20000
Monarda-Telos complex, 0 to 8 percent slopes, very stony	MyB	8601	284569	2slvg	me027	1979	1:20000
Monarda silt loam, 0 to 3 percent slopes	MwB	689	284568	2t0yk	me027	1979	1:20000
Monarda silt loam, 0 to 3 percent slopes, very stony	Mr	99551	284780	2t0yg	me602	1967	1:20000
Monarda silt loam, 0 to 3 percent slopes	Mo	5931	284779	2t0yk	me602	1967	1:20000
Monarda-Burnham complex, 3 to 8 percent slopes	MoB	121688	301852	2t0ym	me607	1960	1:20000
Monarda-Burnham complex, 0 to 3 percent slopes	MoA	71084	301851	2t0yl	me607	1960	1:20000
Monarda-Burnham complex, 0 to 3 percent slopes, very stony	MrB	68819	301853	2t0yn	me607	1960	1:20000
Monarda-Burnham complex, 0 to 3 percent slopes, very stony	MrB	91244	614190	2t0yn	me608	1962	1:20000
Monarda-Burnham complex, 0 to 3 percent slopes	MoA	70003	614188	2t0yl	me608	1962	1:20000
Monarda-Burnham complex, 3 to 8 percent slopes	MoB	56680	614189	2t0ym	me608	1962	1:20000
Monarda-Telos complex, 0 to 8 percent slopes, very stony	MUB	22868	285027	2slvg	me610	1992	1:20000
Monarda-Burnham complex, 0 to 3 percent slopes, very stony	MTB	5841	285026	2t0yn	me610	1992	1:20000
Telos-Monarda-Monson association, 0 to 8 percent slopes, rocky	TMB	4044	285062	2t0jp	me610	1992	1:20000
Monarda extremely flaggy silt loam, 0 to 8 percent slopes, very stony	MsB	2087	285041	2w3z3	me610	1992	1:20000
Telos-Monarda association, 0 to 8 percent slopes, rubbly	TLB	821	285061	2w3z7	me610	1992	1:20000
Monarda silt loam, 0 to 8 percent slopes	MrB	393	285040	2t0yh	me610	1992	1:20000
Monarda-Telos complex, 0 to 8 percent slopes, very stony	MOB	34419	746076	t1bz	me612	2016	1:24000
Monarda-Burnham complex, 0 to 3 percent slopes, very stony	MXA	22273	746065	t1bm	me612	2016	1:24000
Monarda-Monson-Telos association, 0 to 8 percent slopes, rocky	MMB	18403	746077	t1c0	me612	2016	1:24000
Monarda-Telos complex, 0 to 8 percent slopes, very stony	TmB	8853	1483012	1ls63	me612	2016	1:24000
Kenduskeag-Monarda complex, 0 to 8 percent slopes, very stony	KMB	6676	1483115	1ls9f	me612	2016	1:24000
Monarda-Burnham complex, 0 to 3 percent slopes, very stony	MbA	4430	741912	sx0n	me612	2016	1:24000
Monarda gravelly silt loam, 0 to 3 percent slopes	MoA	1917	741911	sx0m	me612	2016	1:24000
Telos-Monarda-Urban land association, 0 to 8 percent slopes	MuB	507	2396089	2lfb6	me612	2016	1:24000
Monarda-Burnham complex, 0 to 3 percent slopes, very stony	MrB	220798	285235	2t0yn	me614	1960	1:20000
Monarda-Burnham complex, 0 to 15 percent slopes, extremely stony	MsC	48765	285236	2w3z8	me614	1960	1:20000
Monarda silt loam, 0 to 3 percent slopes	MoB	9054	285234	2t0yk	me614	1960	1:20000
Howland-Monarda association, 0 to 8 percent slopes, very stony	HRB	47340	285332	2w3zf	me615	1994	1:24000
Monarda-Telos complex, 0 to 8 percent slopes, very stony	TMB	36044	285368	2slvg	me615	1994	1:24000
Telos-Monarda-Monson association, 0 to 8 percent slopes, rocky	TNB	28404	285369	2t0jp	me615	1994	1:24000
Monarda-Burnham complex, 0 to 3 percent slopes, very stony	MW	27286	285343	2t0yn	me615	1994	1:24000
Monarda-Howland-Thorndike complex, 3 to 15 percent slopes, very stony	MXB	20639	285344	2w3zn	me615	1994	1:24000
Monarda silt loam, 0 to 8 percent slopes	MvB	756	285349	2t0yh	me615	1994	1:24000
Monarda-Telos complex, 0 to 8 percent slopes, very stony	MWB	9499	285598	2slvg	me617	2004	1:24000
Telos-Elliottsville-Monarda complex, 0 to 8 percent slopes, very stony	TEB	1762	285625	2w3zb	me617	2004	1:24000
Monarda-Burnham complex, 0 to 3 percent slopes, very stony	MXB	656	285599	2t0yn	me617	2004	1:24000
Monarda silt loam, 0 to 8 percent slopes, very stony	MvB	585	285606	2w3z9	me617	2004	1:24000
Monarda-Telos complex, 0 to 8 percent slopes, very stony	MTB	135809	285699	2slvg	me619	2005	1:24000
Telos-Monarda-Monson association, 0 to 8 percent slopes, rocky	TMB	100857	285694	2t0jp	me619	2005	1:24000
Monarda-Burnham complex, 0 to 3 percent slopes, very stony	MOB	63990	285700	2t0yn	me619	2005	1:24000
Monarda-Knob Lock association, 1 to 12 percent slopes, very rocky	MRB	3247	285710	2w3zc	me619	2005	1:24000
Telos-Monarda-Monson association, 0 to 8 percent slopes, rocky	TRB	289118	2549919	2t0jp	me620	2011	1:24000
Monarda-Burnham complex, 0 to 3 percent slopes, very stony	MBA	184308	2549923	2t0yn	me620	2011	1:24000
Monarda-Telos complex, 0 to 8 percent slopes, very stony	TMB	145582	2549922	2slvg	me620	2011	1:24000
Telos-Monarda-Monson association, 0 to 8 percent slopes, rocky	TRB	209038	2549858	2t0jp	me621	2011	1:24000
Monarda-Burnham complex, 0 to 3 percent slopes, very stony	MBA	138484	2549863	2t0yn	me621	2011	1:24000
Monarda-Telos complex, 0 to 8 percent slopes, very stony	TMB	119749	2549862	2slvg	me621	2011	1:24000
Monarda-Telos complex, 0 to 8 percent slopes, very stony	TMB	95615	1909299	2slvg	me622	2007	1:24000
Monarda-Burnham complex, 0 to 3 percent slopes, very stony	MUB	58689	1909300	2t0yn	me622	2007	1:24000
Telos-Monarda-Monson association, 0 to 8 percent slopes, rocky	TNB	27963	1909294	2t0jp	me622	2007	1:24000
Monarda-Telos association, gently sloping, very stony	770B	1468	280742	9f46	nh607	2000	1:24000
Monarda-Burnham association, gently sloping, very stony	769B	117	280740	9f44	nh607	2000	1:24000
Lanesboro-Monarda association, strongly sloping, very stony	LmC	7300	290356	9r4b	ny021	1985	1:15840

Map of Series Extent

Approximate geographic distribution of the MONARDA 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).