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Soil Survey Manual - Table 3-6
Illustrative water-state annual pattern
| Average - 6 years in 10 |
| Depth (cm) |
:Jan |
:Feb |
:Mar |
:Apr |
:May |
:Jun |
:Jul |
:Aug |
:Sep |
:Oct |
:Nov |
:Dec |
| Fine, montmorillonitic, mesic Typic Argiudoll
a |
| 0 - 25 |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MS |
:DS |
:DS |
:MS |
:MM |
:MM |
| |
:F |
:F |
: |
: |
: |
: |
: |
: |
: |
: |
: |
:F |
| 25 - 50 |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MS |
:MS |
:MS |
:MS |
:MM |
| |
:F |
:F |
:F |
: |
: |
: |
: |
: |
: |
: |
: |
: |
| 50 - 100 |
:MS |
:MS |
:MM |
:MM |
:MM |
:MM |
:MS |
:MS |
:MS |
:MS |
:MS |
:MS |
| 100 - 150 |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
| 150 - 200 |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
| Fine-loamy, mixed, thermic Typic Haploxeralf
b |
| 0 - 30 |
:MM |
:MS |
:MS |
:DS |
:DS |
:D1 c |
:D1 |
:D1 |
:D1 |
:D1 |
:D1 |
:MS |
| 30 - 70 |
:MM |
:MM |
:MM |
:MM |
:MS |
:DS |
:D1 |
:D1 |
:D1 |
:DS |
:MS |
:MM |
| 70 - 100 |
:MV |
:MV |
:MM |
:MM |
:MM |
:MM |
:MS |
:D1 |
:D1 |
:D1 |
:D1 |
:MS |
| 120 - 170 |
:MM |
:MM |
:MM |
:MS |
:MS |
:MS |
:MS |
:D1 |
:D1 |
:D1 |
:DS |
:MS |
| Driest 2 years in 10 |
| Depth (cm) |
:Jan |
:Feb |
:Mar |
:Apr |
:May |
:Jun |
:Jul |
:Aug |
:Sep |
:Oct |
:Nov |
:Dec |
| Fine, montmorillonitic, mesic Typic Argiudoll
a |
| 0 - 25 |
:MM |
:MM |
:MM |
:MM |
:MM |
:MS |
:DS |
:DS |
:DS |
:MS |
:MS |
:MM |
| |
:F |
:F |
: |
: |
: |
: |
: |
: |
: |
: |
: |
:F |
| 25 - 50 |
:MS |
:MS |
:MS |
:MS |
:MS |
:MS |
:MS |
:MS |
:MS |
:MS |
:MS |
:MS |
| |
:F |
:F |
:F |
: |
: |
: |
: |
: |
: |
: |
: |
: |
| 50 - 100 |
:MS |
:MS |
:MS |
:MM |
:MM |
:MS |
:MS |
:MS |
:MS |
:MS |
:MS |
:MS |
| 100 - 150 |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
| 150 - 200 |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
| Fine-loamy, mixed, thermic Typic Haploxeralf
b |
| 0 - 30 |
:MS |
:MM |
:MS |
:MS |
:DS |
:DS |
:D1 |
:D1 |
:D1 |
:D1 |
:D1 |
:DS |
| 30 - 70 |
:MM |
:MM |
:MM |
:MM |
:MS |
:DS |
:D1 |
:D1 |
:D1 |
:D1 |
:MS |
:MS |
| 70 - 100 |
:MS |
:MM |
:MM |
:MM |
:MM |
:MM |
:MS |
:D1 |
:D1 |
:D1 |
:D1 |
:DS |
| 120 - 170 |
:MS |
:MM |
:MS |
:MS |
:MS |
:MS |
:MS |
:D1 |
:D1 |
:D1 |
:D1 |
:D1 |
| Wettest 2 years in 10 |
| Depth (cm) |
:Jan |
:Feb |
:Mar |
:Apr |
:May |
:Jun |
:Jul |
:Aug |
:Sep |
:Oct |
:Nov |
:Dec |
| Fine, montmorillonitic, mesic Typic Argiudoll
a |
| 0 - 25 |
:MM |
:MM |
:MV |
:MV |
:MV |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
| |
:F |
:F |
: |
: |
: |
: |
: |
: |
: |
: |
: |
:F |
| 25 - 50 |
:MM |
:MM |
:MV |
:MV |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
| |
:F |
:F |
:F |
: |
: |
: |
: |
: |
: |
: |
: |
: |
| 50 - 100 |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
| 100 - 150 |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
| 150 - 200 |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
:MM |
| Fine-loamy, mixed, thermic Typic Haploxeralf
b |
| 0 - 30 |
:MM |
:MM |
:MM |
:MS |
:DS |
:DS |
:D1 |
:D1 |
:D1 |
:DS |
:MS |
:MM |
| 30 - 70 |
:MV |
:MV |
:MM |
:MM |
:MS |
:DS |
:D1 |
:D1 |
:D1 |
:DS |
:MM |
|
| 70 - 100 |
:MV |
:MV |
:MM |
:MM |
:MM |
:MM |
:MS |
:D1 |
:D1 |
:D1 |
:MS |
:MM |
| 120 - 170 |
:MM |
:MM |
:MS |
:MS |
:MS |
:MS |
:MS |
:D1 |
:D1 |
:D1 |
:DS |
:MS |
a. Otoe County, Nebraska (Sautter,
1982). Sharpsburg silty clay loam, 2-5 percent slopes. Corn (Zea mays)
following corn. Assume: contoured, terraced, over 20 percent residue cover.
Disk twice in April. Field cultivate once. Plant May 1-15. Cultivate once or
twice. Harvest November 1-15. Cattle graze after harvest. Based on a
discussion with H.E. Sautter, soil scientist (retired), Syracuse, Nebraska.
Monthly water states based on long-term field mapping experience and water
balance computations. The Sharpsburg soil series pertains to the map unit
illustrative of a consociation (appendix).
b. San Diego Area, California (Bowman, 1973). Mean annual precipitation at
Escondido is 344 mm and at Thornwaite potential evaporation is 840 mm. Study
area in Fallbrook sandy loam, 5 to 9 percent slopes, eroded. The study area
has slightly greater slope than the upper limit of the map unit. Vegetation
is annual range, fair condition. Generalizations were made originally for
the 1983 National Soil Survey Conference based on field measurements in 1966
by Nettleton et al (1968), as interpreted by R.A. Dierking, soil correlator,
Portland, Oregon. At the time, moderately dry and very dry were not
distinguished.
c. D1 = DV + DM. |
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