Soil Data Explorer - MASADA

Official Series Description

Lab Data Summary

Aggregate lab data for the MASADA soil series. This aggregation is based on all pedons with a current taxon name of MASADA, 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 MASADA 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
133A	81P0360	81AL101001	Masada	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	32.4044456,-86.046669
136	90P0229	89NC149001	Masada	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.2544441,-81.973053
136	90P0230	89NC149002	Masada	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.2913895,-82.1188889
136	00P1126	S2000VA047014	Masada	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.447272,-77.764667

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MASADA 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 MASADA 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 MASADA 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 MASADA 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 MASADA 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 MASADA 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 MASADA 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 flats position figure.

Soil series sharing subgroup-level classification with MASADA, 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. NC-2012-02-07-39 | Polk County - 1998

   The relationship between soils, landscape, and parent material in the Riverview-Chewacla-Buncombe general soil map unit. The Buncombe soils are in convex areas adjacent to the stream channel; the Chewacla soils are in the lower, concave areas further from the channel; and the Riverview soils occur in the remaining areas of the flood plain. The clayey Masada, Dogue, and Roanoke soils are on the higher stream terraces (Soil Survey of Polk County, North Carolina; 1998).

Map Units

Map units containing MASADA 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
Altavista and Masada silt loams, low terraces, 0 to 2 percent slopes	AaA	3228	523274	kkht	al015	1959	1:20000
Altavista and Masada silt loams, low terraces 2 to 6 percent slopes, eroded	AaB2	482	523275	kkhv	al015	1959	1:20000
Masada silt loam, 0 to 2 percent slopes	MsA	4858	328530	c0vr	al021	1967	1:20000
Masada slaty loam, 2 to 8 percent slopes	MaB	3397	523250	kkh1	al121	1969	1:20000
Masada fine sandy loam, very gently sloping phase	McB	210	124373	45f1	ga117	1957	1:20000
Masada fine sandy loam, eroded gently sloping phase	McC2	135	124374	45f2	ga117	1957	1:20000
Masada fine sandy loam, 6 to 10 percent slopes, eroded	MoC2	320	124537	45lb	ga137	1960	1:20000
Masada fine sandy loam, 6 to 10 percent slopes, severely eroded	MoC3	145	124538	45lc	ga137	1960	1:20000
Masada fine sandy loam, 2 to 6 percent slopes, eroded	MoB2	90	124536	45l9	ga137	1960	1:20000
Masada-Urban land complex, 0 to 3 percent slopes	MuA	495	124836	45wz	ga215	1980	1:15840
Masada fine sandy loam, 0 to 3 percent slopes	MaA	195	124835	45wy	ga215	1980	1:15840
Masada fine sandy loam, 2 to 6 percent slopes	MoB	505	125283	46cd	ga605	1967	1:15840
Masada fine sandy loam, 2 to 6 percent slopes	MoB	3780	125454	46jx	ga618	1966	1:15840
Masada gravelly sandy loam, 2 to 6 percent slopes	MpB	2275	125455	46jy	ga618	1966	1:15840
Masada gravelly sandy loam, 6 to 10 percent slopes, eroded	MpC2	1995	125456	46jz	ga618	1966	1:15840
Masada fine sandy loam, 2 to 6 percent slopes	MoB	3095	531353	ktxf	ga622	1967	1:20000
Masada sandy clay loam, 10 to 15 percent slopes, eroded	MyD2	1390	531356	ktxj	ga622	1967	1:20000
Masada fine sandy loam, 6 to 10 percent slopes, eroded	MoC2	1200	531354	ktxg	ga622	1967	1:20000
Masada gravelly loam, 2 to 10 percent slopes	MpC	1085	531355	ktxh	ga622	1967	1:20000
Masada fine sandy loam, 0 to 2 percent slopes	MoA	825	531352	ktxd	ga622	1967	1:20000
Masada fine sandy loam, 6 to 10 percent slopes, eroded	MoC2	2810	125678	46s4	ga632	1967	1:15840
Masada fine sandy loam, 2 to 6 percent slopes, eroded	MoB2	1030	125677	46s3	ga632	1967	1:15840
Masada fine sandy loam, 2 to 6 percent slopes	MoB	700	125676	46s2	ga632	1967	1:15840
Masada fine sandy loam, 10 to 15 percent slopes, eroded	MoD2	475	125679	46s5	ga632	1967	1:15840
Masada sandy loam, 2 to 6 percent slopes	MdB	11	2973927	2wx2j	nc033	2016	1:24000
Masada fine sandy loam, 2 to 6 percent slopes	MaB	407	2432577	2mn97	nc059	1988	1:24000
Masada fine sandy loam, 2 to 6 percent slopes	MdB	782	2424286	2mcns	nc097	2011	1:12000
Masada fine sandy loam, 6 to 10 percent slopes	MdC	177	2424287	2mcnt	nc097	2011	1:12000
Masada sandy loam, 2 to 8 percent slopes	MsB	475	113633	3t7l	nc109	1989	1:24000
Masada sandy loam, 8 to 15 percent slopes	MsC	115	113634	3t7m	nc109	1989	1:24000
Masada-Mattaponi complex, 2 to 8 percent slopes	MmB	1075	2233592	2dz7c	nc123	2007	1:24000
Masada gravelly sandy loam, 8 to 15 percent slopes	MaC	332	2233591	2dz7b	nc123	2007	1:24000
Masada fine sandy loam, 2 to 8 percent slopes	MaB	1856	113915	3tjp	nc125	1987	1:24000
Masada fine sandy loam, 8 to 15 percent slopes	MaD	824	113916	3tjq	nc125	1987	1:24000
Masada sandy loam, 2 to 8 percent slopes	MsB	1031	111095	3qlq	nc149	1992	1:24000
Masada sandy loam, 8 to 15 percent slopes	MaC	5278	114712	3vcd	nc153	1996	1:24000
Masada sandy loam, 15 to 25 percent slopes	MaD	2253	114713	3vcf	nc153	1996	1:24000
Masada and altavista soils, 2 to 6 percent slopes	MaB	1789	130310	4clk	sc057	1967	1:20000
Masada-Hornsville complex, 0 to 2 percent slopes, very rarely flooded	MdA	699	2485952	2pfv0	sc085	1969	1:20000
Masada sandy loam, 2 to 6 percent slopes	MaB	880	2513851	2lq2j	sc091	2013	1:15840
Masada loam, eroded rolling phase	Ma	154	525174	kmh3	tn059	1954	1:15840
Masada loam, undulating phase	Mb	66	525175	kmh4	tn059	1954	1:15840
Masada loam, 2 to 5 percent slopes	MaB	249	1689685	1tq7z	tn179	1955	1:15840
Masada clay loam, 5 to 12 percent slopes, eroded	MaC2	198	1689684	1tq7y	tn179	1955	1:15840
Masada clay loam, 12 to 25 percent slopes, eroded	MaD2	86	1689683	1tq7x	tn179	1955	1:15840
Masada loam, 2 to 6 percent slopes	27B	1409	117849	3yml	va036	1993	1:24000
Masada sandy clay loam, 2 to 6 percent slopes, severely eroded	28B3	264	117855	3yms	va036	1993	1:24000
Masada fine sandy loam, 6 to 15 percent slopes, eroded	MeD2	1570	118758	3zkx	va037	1970	1:15840
Masada fine sandy loam, 2 to 6 percent slopes, eroded	MeB2	1343	118757	3zkw	va037	1970	1:15840
Masada fine sandy loam, 15 to 25 percent slopes	MeE	668	118759	3zky	va037	1970	1:15840
Masada fine sandy loam, 2 to 6 percent slopes	106B	1976	118813	3zmp	va041	1974	1:15840
Masada gravelly fine sandy loam, 2 to 6 percent slopes	103B	1238	118808	3zmj	va041	1974	1:15840
Masada loam, 2 to 6 percent slopes	117B	325	118823	3zn0	va041	1974	1:15840
Masada gravelly fine sandy loam, 6 to 12 percent slopes	103C	282	118809	3zmk	va041	1974	1:15840
Masada fine sandy loam, 6 to 12 percent slopes	106C	151	118814	3zmq	va041	1974	1:15840
Masada loam, 6 to 12 percent slopes	117C	12	118824	3zn1	va041	1974	1:15840
Masada fine sandy loam, undulating phase	Mk	483	121816	42rk	va065	1950	1:15840
Masada fine sandy loam, 2 to 7 percent slopes	21B	1405	119003	3ztt	va075	1976	1:15840
Masada fine sandy loam, 7 to 15 percent slopes	21C	907	119004	3ztv	va075	1976	1:15840
Masada fine sandy loam, 2 to 7 percent slopes	44B	730	119122	3zyn	va085	1976	1:15840
Masada fine sandy loam, 2 to 7 percent slopes, eroded	MsB2	3088	119391	407b	va109	1972	1:15840
Masada fine sandy loam, 7 to 15 percent slopes, eroded	MsC2	869	119392	407c	va109	1972	1:15840
Masada fine sandy loam, 2 to 7 percent slopes	15B	659	119452	4099	va111	1979	1:20000
Masada fine sandy loam, 2 to 6 percent slopes	MdB	1333	119597	40fz	va117	1990	1:24000
Masada loam, 2 to 7 percent slopes	29B	705	120418	419g	va177	1980	1:15840
Masada loam, 7 to 15 percent slopes, eroded	29C2	552	120419	419h	va177	1980	1:15840
Masada loam, 7 to 15 percent slopes, moderately eroded	29C2	5	2376411	2krvf	va630	2008	1:12000
Masada fine sandy loam, 2 to 6 percent slopes	MpB	3722	120733	41mm	va631	1973	1:15840
Masada loam, local alluvium, 0 to 4 percent slopes	MtB	3129	120739	41mt	va631	1973	1:15840
Masada fine sandy loam, 6 to 15 percent slopes	MpC	2451	120734	41mn	va631	1973	1:15840
Masada loam, 2 to 6 percent slopes, eroded	MsB2	645	120737	41mr	va631	1973	1:15840
Masada gravelly fine sandy loam, 2 to 6 percent slopes	MrB	538	120735	41mp	va631	1973	1:15840
Masada loam, 6 to 12 percent slopes, eroded	MsC2	404	120738	41ms	va631	1973	1:15840
Masada gravelly fine sandy loam, 6 to 10 percent slopes	MrC	313	120736	41mq	va631	1973	1:15840
Masada-Urban land complex, 2 to 6 percent slopes	24B	137	140102	4psf	va760	2004	1:24000
Masada-Urban land complex, gravelly phase, 6 to 12 percent slopes	25C	97	140105	4psj	va760	2004	1:24000
Masada-Urban land complex, gravelly phase, 2 to 6 percent slopes	25B	42	140104	4psh	va760	2004	1:24000
Masada-Urban land complex, 6 to 12 percent slopes	24C	37	140103	4psg	va760	2004	1:24000

Map of Series Extent

Approximate geographic distribution of the MASADA 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).