Official Series Description


Lab Data Summary

Aggregate lab data for the MOBEETIE soil series. This aggregation is based on all pedons with a current taxon name of MOBEETIE, 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 MOBEETIE were used in the calculation. Source: KSSL snapshot . 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 MOBEETIE 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.

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Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the MOBEETIE series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

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Select annual climate data summaries for the MOBEETIE series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the MOBEETIE 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 .

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

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Competing Series

Soil series competing with MOBEETIE share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

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Select annual climate data summaries for the MOBEETIE series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the MOBEETIE 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 .

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Click the image to view it full size.

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

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There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with MOBEETIE, 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 .

Block Diagrams

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

  1. TX-2010-11-02-22 | Carson County -

    General relationship of the soils in Carson County (Soil Survey of Carson County, Texas).

  2. TX-2010-11-02-43 | Deaf Smith County - 2007

    Typical pattern of soils in the Plemons-Potter-Mobeetie general soil map unit (Soil Survey of Deaf Smith County, Texas; 2007).

  3. TX-2012-03-20-39 | Deaf Smith County - August 1968

    Topography and underlying material of the Mobeetie (3); Quay-Montoya-Vernon (8); and Mobeetie-Potter-Rough broken land (4) associations (Soil Survey of Deaf Smith County, TX; 1968).

  4. TX-2012-03-21-35 | Lipscomb County - December 1975

    Pattern of soils and underlying material in association 2 (Soil Survey of Lipscomb County, TX; 1975).

  5. TX-2012-03-21-37 | Lipscomb County - December 1975

    Pattern of soils and underlying material in association 4 (Soil Survey of Lipscomb County, TX; 1975).

  6. TX-2012-03-22-06 | Wheeler County - October 1975

    Relationship of soils in the Grandfield-Hardeman association to parent material and relief (Soil Survey of Wheeler County, TX; 1975).

  7. TX-2012-03-22-07 | Wheeler County - October 1975

    Relationship of soils in the Abilene-Mobeetie-Berda association to parent material and relief (Soil Survey of Wheeler County, TX; 1975).

Map Units

Map units containing MOBEETIE 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
Mobeetie-Potter association, 1 to 15 percent slopesMW11781376448dmqhnm02519671:20000
Potter-Mobeetie association, 8 to 45 percent slopesPMG2761884288f7g3nm04120141:24000
Mobeetie fine sandy loam, 1 to 5 percent slopesMO4533558961w53nm61419661:20000
Potter-Mobeetie association, 8 to 45 percent slopesPMG12918377742f7g3nm66920051:24000
Mobeetie fine sandy loam, cool, 5 to 12 percent slopesBeD136493824182tqtyok04519631:24000
Otero and Mobeetie soils, 5 to 12 percent slopes, severely erodedEr4177382432dtyjok04519631:24000
Mobeetie fine sandy loam, 3 to 5 percent slopes, coolBeC38573824172tqtpok04519631:24000
Mobeetie-Veal-Potter complex, 3 to 20 percent slopesBo409693624682tqtztx01119631:20000
Mobeetie-Veal complex, 3 to 8 percent slopesBfD239703624662w846tx01119631:20000
Mobeetie fine sandy loam, moist, 1 to 3 percent slopesMtB41729623262xrwgtx03319701:24000
Mobeetie-Veal-Potter association, 5 to 20 percent slopesMVE3032962345f6lhtx03319701:24000
Mobeetie fine sandy loam, 1 to 3 percent slopesMoB190362956f7fttx03319701:24000
Mobeetie-Veal association, 5 to 20 percent slopesMEE50523258051308q7tx04519721:20000
Mobeetie fine sandy loam, moist, 0 to 3 percent slopesMoB5923632852tw49tx04519721:20000
Mobeetie-Veal complex, 3 to 8 percent slopesMVD579943779822w846tx06520001:24000
Mobeetie-Veal-Potter complex, 3 to 20 percent slopesMVE132653779572tqtztx06520001:24000
Potter-Mobeetie association, 8 to 45 percent slopesPMG6782377964f7g3tx06520001:24000
Mobeetie-Tascosa complex, 3 to 20 percent slopesMTE37413779562w847tx06520001:24000
Mobeetie fine sandy loam, 3 to 5 percent slopes, coolMoC7703779622tqtptx06520001:24000
Mobeetie-Veal-Potter association, 5 to 20 percent slopesMVE2644393622f6lhtx11520041:24000
Potter-Mobeetie association, 8 to 45 percent slopesPMG7207378059f7g3tx11719991:24000
Mobeetie-Veal-Potter complex, 3 to 20 percent slopesMVE43933780522tqtztx11719991:24000
Mobeetie fine sandy loam, 3 to 5 percent slopes, coolMoC25513780542tqtptx11719991:24000
Mobeetie fine sandy loam, cool, 5 to 12 percent slopesMoD2863780552tqtytx11719991:24000
Mobeetie fine sandy loam, 3 to 5 percent slopesMtC3599365136f7fvtx12519651:20000
Mobeetie fine sandy loam, 1 to 3 percent slopesMtB1036365135f7fttx12519651:20000
Mobeetie-Veal-Potter complex, 3 to 20 percent slopesMxD826963651902tqtztx12919751:24000
Mobeetie-Tascosa complex, 3 to 20 percent slopesMTE339463651892w847tx12919751:24000
Mobeetie fine sandy loam, cool, 5 to 12 percent slopesMrD143043651872tqtytx12919751:24000
Mobeetie fine sandy loam, 3 to 5 percent slopes, coolMrC75983651862tqtptx12919751:24000
Badland-Mobeetie association, 15 to 50 percent slopesBa537336518830krmtx12919751:24000
Mobeetie fine sandy loam, 1 to 3 percent slopes, coolMrB16853651842tqtntx12919751:24000
Berda and Mobeetie soils, 5 to 20 percent slopesBME82566074541t2dhtx15320041:24000
Tascosa and Mobeetie soils, 3 to 30 percent slopesTMG3541695969plhhtx15320041:24000
Mobeetie fine sandy loam, 1 to 3 percent slopesMoB123695958f7fttx15320041:24000
Mobeetie fine sandy loam, 3 to 5 percent slopesMnC17054378343f7fvtx16919651:24000
Mobeetie-Potter association, 3 to 20 percent slopesMP1667137833330949tx16919651:24000
Mobeetie-Latom fine sandy loams, 2 to 20 percent slopesMoD11590378344dppntx16919651:24000
Mobeetie fine sandy loam, 1 to 3 percent slopesMnB4086378342f7fttx16919651:24000
Mobeetie-Veal-Potter complex, 3 to 20 percent slopesMxD435603919352tqtztx17919651:20000
Mobeetie fine sandy loam, cool, 5 to 12 percent slopesMoC243623919342tqtytx17919651:20000
Badland-Mobeetie association, 15 to 50 percent slopesBa295039191530krmtx17919651:20000
Veal and Mobeetie fine sandy loams, 1 to 3 percent slopesMbB741391925f4trtx17919651:20000
Potter-Mobeetie association, 8 to 45 percent slopes, coolPMG2169319484282w84dtx19520071:24000
Mobeetie-Veal-Potter complex, 3 to 20 percent slopesMVE1652919484252tqtztx19520071:24000
Mobeetie fine sandy loam, 1 to 3 percent slopes, coolMoB381819484082tqtntx19520071:24000
Mobeetie fine sandy loam, 3 to 5 percent slopes, coolMoC322319484072tqtptx19520071:24000
Mobeetie-Veal-Potter complex, 3 to 20 percent slopesMVD677863674432tqtztx20519731:24000
Mobeetie fine sandy loam, 1 to 3 percent slopes, coolMoB60413674452tqtntx20519731:24000
Mobeetie fine sandy loam, 3 to 5 percent slopes, coolMoC55933674462tqtptx20519731:24000
Mobeetie fine sandy loam, 5 to 8 percent slopes, coolMoD25193674472tqtstx20519731:24000
Mobeetie-Likes complex, 3 to 20 percent slopesMt60725367573dbh6tx21119671:20000
Mobeetie-Veal-Potter complex, 3 to 20 percent slopesMx174733675742tqtztx21119671:20000
Mobeetie fine sandy loam, 3 to 5 percent slopes, coolMrC66613675722tqtptx21119671:20000
Mobeetie fine sandy loam, 1 to 3 percent slopes, coolMrB6363675712tqtntx21119671:20000
Mobeetie fine sandy loam, 1 to 3 percent slopesMoB4677391892f7fttx22719651:24000
Mobeetie fine sandy loam, 3 to 5 percent slopesMoC4545391893f7fvtx22719651:24000
Mobeetie-Veal-Potter complex, 3 to 20 percent slopesMVE448033679292tqtztx23319721:24000
Mobeetie fine sandy loam, cool, 5 to 12 percent slopesMbD173503679282tqtytx23319721:24000
Mobeetie fine sandy loam, 3 to 5 percent slopes, coolMbC87513679272tqtptx23319721:24000
Mobeetie fine sandy loam, 1 to 3 percent slopes, coolMbB11273679262tqtntx23319721:24000
Mobeetie fine sandy loamGf342368232dc5gtx25319661:20000
Mobeetie-Veal-Potter complex, 3 to 20 percent slopesMXD360023694592tqtztx29519711:24000
Mobeetie fine sandy loam, 5 to 8 percent slopes, coolMrD234933694632tqtstx29519711:24000
Mobeetie fine sandy loam, 3 to 5 percent slopes, coolMrC161633694622tqtptx29519711:24000
Mobeetie fine sandy loam, 1 to 3 percent slopes, coolMrB53253694612tqtntx29519711:24000
Mobeetie fine sandy loam, 5 to 8 percent slopesMoD139236984930942tx30319751:20000
Mobeetie fine sandy loam, 3 to 5 percent slopesMoC958369848f7fvtx30319751:20000
Mobeetie fine sandy loam, 1 to 3 percent slopesMoB938369847f7fttx30319751:20000
Mobeetie-Veal-Potter association, 5 to 20 percent slopesMVE1607379046f7fmtx30519991:24000
Mobeetie fine sandy loam, 1 to 3 percent slopesMoB4010370344f7fttx31719681:24000
Mobeetie-Veal-Potter complex, 3 to 20 percent slopesMvC203373708262tqtztx34119681:24000
Mobeetie fine sandy loam, cool, 5 to 12 percent slopesMrD179003708252tqtytx34119681:24000
Mobeetie fine sandy loam, 3 to 5 percent slopes, coolMrC112063708242tqtptx34119681:24000
Tascosa, Mobeetie, and Springer soils, rollingTmC4469370837dfwhtx34119681:24000
Mobeetie fine sandy loam, 1 to 3 percent slopes, coolMrB44003708232tqtntx34119681:24000
Polar-Mobeetie association, hillyPME22781370886dfy2tx34519721:24000
Mobeetie fine sandy loam, 3 to 5 percent slopesMoC10298370878f7fvtx34519721:24000
Mobeetie fine sandy loam, moist, 0 to 3 percent slopesMoB33643708772tw49tx34519721:24000
Mobeetie fine sandy loam, 5 to 12 percent slopesMoE3220370879f7fwtx34519721:24000
Vona-Mobeetie complex, 2 to 8 percent slopesVmD3424371107dg56tx35719661:20000
Mobeetie fine sandy loam, 5 to 8 percent slopes, coolMoD24213710902tqtstx35719661:20000
Mobeetie-Veal-Potter complex, 3 to 20 percent slopesMVE6974431241532tqtztx35919781:24000
Mobeetie-Tascosa complex, 3 to 20 percent slopesMTE3718231241522w847tx35919781:24000
Mobeetie fine sandy loam, cool, 5 to 12 percent slopesMfD2472031241512tqtytx35919781:24000
Mobeetie fine sandy loam, 3 to 5 percent slopes, coolMfC2230631241502tqtptx35919781:24000
Mobeetie fine sandy loam, 1 to 3 percent slopes, coolMfB1476331241492tqtntx35919781:24000
Potter-Mobeetie association, 8 to 45 percent slopes, coolPMG1054031241612w84dtx35919781:24000
Mobeetie-Veal-Potter complex, 3 to 20 percent slopesMVE3268631242222tqtztx37519741:24000
Mobeetie-Tascosa complex, 3 to 20 percent slopesMTE2930631242212w847tx37519741:24000
Mobeetie fine sandy loam, cool, 5 to 12 percent slopesMfD1528531242262tqtytx37519741:24000
Potter-Mobeetie association, 8 to 45 percent slopes, coolPMG1116731242292w84dtx37519741:24000
Mobeetie fine sandy loam, 3 to 5 percent slopes, coolMfC340831242252tqtptx37519741:24000
Mobeetie fine sandy loam, 1 to 3 percent slopes, coolMfB271031242242tqtntx37519741:24000
Mobeetie-Urban land complexMoU49931242722mhwstx37519741:24000
Potter-Mobeetie association, 8 to 45 percent slopesPMG21278371399f7g3tx38119991:24000
Mobeetie-Veal-Potter complex, 3 to 20 percent slopesMVE73613713932tqtztx38119991:24000
Mobeetie fine sandy loam, 3 to 5 percent slopes, coolMoC6883714232tqtptx38119991:24000
Mobeetie-Veal-Potter urban land association, 5 to 20 percent slopesMVU244630009p4kwtx38119991:24000
Mobeetie-Veal-Potter complex, 3 to 20 percent slopesMxD998703715232tqtztx39319791:24000
Mobeetie fine sandy loam, cool, 5 to 12 percent slopesMrD281133715222tqtytx39319791:24000
Mobeetie fine sandy loam, 1 to 3 percent slopes, coolMrB42003715202tqtntx39319791:24000
Mobeetie fine sandy loam, 3 to 5 percent slopes, coolMrC35363715212tqtptx39319791:24000
Mobeetie fine sandy loam, cool, 5 to 12 percent slopesMoD126473721062tqtytx42119701:24000
Mobeetie fine sandy loam, 3 to 5 percent slopes, coolMoC82533721052tqtptx42119701:24000
Mobeetie fine sandy loam, 5 to 8 percent slopes, coolMrD50363733152tqtstx48319701:24000
Mobeetie fine sandy loam, cool, 1 to 5 percent slopesMrC365137331430qfztx48319701:24000
Mobeetie-Veal-Potter complex, 3 to 20 percent slopesMsD35763733162tqtztx48319701:24000

Map of Series Extent

Approximate geographic distribution of the MOBEETIE 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 .