| *** Andic Soil Properties Data *** |
| Pedon ID: S2012MS023002 | ( Clarke, Mississippi ) | Print Date: Nov 11 2024 10:32PM |
| Sampled as on Jun 4, 2012: | Savannah ; Fine-loamy, siliceous, semiactive, thermic Typic Fragiudults |
| Revised to correlated on Jun 4, 2012: | Savannah ; Fine-loamy, siliceous, semiactive, thermic Typic Fragiudults |
| United States Department of Agriculture | ||||
| SSL | - | Project | C2014USMS010 OSD resampling 2013 | Natural Resources Conservation Service |
| - | Site ID | 2012MS023002 Lat: 32° 1038.40" north Long: 88° 487.60" west MLRA: 133A | National Soil Survey Center | |
| - | Pedon No. | 14N0294 | Kellogg Soil Survey Laboratory | |
| - | General Methods 1B1A, 2A1, 2B | Lincoln, Nebraska 68508-3866 | ||
| Andic Soil Properties Tier 1 | -1- | -2- | -3- | -4- | -5- | -6- | -7- | -8- | -9- | -10- | -11- | -12- | -13- | -14- | -15- | -16- | -17- | -18- | -19- | -20- | -21- | |||
| Total | Fine | CaCO3 | CoSi to | Est | .1-75 | Vol >2mm | Bulk | COLE | Al+½Fe | Al+½Fe | ||||||||||||||
| Clay | Clay | Clay | VCoS | Clay | Fraction | % of | (- - - - 1500 kPa - - - -) | Density | Whole | (- - - - - - - - - - Glass Content - - - - - - - - - -) | *15.625 | *60.0 | ||||||||||||
| Depth | <.002 | <.0002 | <.002 | .02 - 2 | Content | Whole Soil | air-dry | field moist | /Clay | 33 kPa | Soil | csi | vfs | fs | ms | cs | vcs | Wt Avg | +Glass | +Glass | ||||
| Layer | (cm) | Horz | Prep | (- - - - - - - - - - - % of <2 mm - - - - - - - - -) | % of <75 mm | (- - - - - - - - % - - - - - - -) | g cm-3 | cm cm-1 | (- - - - - - - - - - - - - - - - - - - - - % - - - - - - - - - - - - - - - - - - - - -) | |||||||||||||||
| 3A1a1a | 3C2a1a | |||||||||||||||||||||||
| 14N01506 | 0-13 | Ap | S | 5.6 | 79.4 | 6.7 | 51 | 2 | 4.5 | 0.80 | ||||||||||||||
| 14N01507 | 13-25 | E | S | 6.6 | 77.2 | 9.3 | 51 | 2 | 4.5 | 0.68 | ||||||||||||||
| 14N01508 | 25-53 | Bt1 | S | 23.0 | 54.9 | 30 | tr | 10.7 | 0.47 | |||||||||||||||
| 14N01509 | 53-69 | Bt2 | S | 22.4 | 71.1 | 62 | -- | 9.7 | 0.43 | |||||||||||||||
| 14N01510 | 69-109 | Btx1 | S | 33.7 | 45.8 | 25 | -- | 16.2 | 0.48 | |||||||||||||||
| 14N01511 | 109-145 | Btx2 | S | 33.2 | 50.1 | 30 | -- | 14.8 | 0.45 | |||||||||||||||
| 14N01512 | 145-180 | Btx3 | S | 29.2 | 58.6 | 42 | -- | 12.2 | 0.42 | |||||||||||||||
| 14N01513 | 180-224 | BC | S | 22.4 | 54.0 | 30 | -- | 10.1 | 0.45 | |||||||||||||||
| Andic Soil Properties Tier 2 | -1- | -2- | -3- | -4- | -5- | -6- | -7- | -8- | -9- | -10- | -11- | -12- | -13- | -14- | -15- | -16- | -17- | -18- | -19- | |||
| CO3 | Al+ | 8*Si | Optical | KCl | NH4OAC | Sum | (- Base Sat -) | |||||||||||||||
| pH | pH | Org | Tot | as | NZ | ½Fe | 8*Si | 2*Fe | +2*Fe | Density | Extr | Sum | Bases+ | NH4OAC | Sum of | Melanic | (- Atterberg -) | |||||
| Depth | H2O | NaF | C | C | CaCO3 | P Ret | Oxal | Oxal | Oxal | Oxal | Oxal | Al | Bases | Extr Al | pH 7.0 | Cations | Index | LL | PI | |||
| Layer | (cm) | Horz | Prep | (- - - - - - - - - - - - - - - - - - - - - - - % wt - - - - - - - - - - - - - - - - - -) | cmol(+) kg-1 | (- meq 100g-1 -) | (- - - - % - - - - -) | ( % <0.4mm ) | ||||||||||||||
| 4C1a2a | 4C1a1a1 | 4H2a | 4G2 | 4B3a1a | ||||||||||||||||||
| 14N01506 | 0-13 | Ap | S | 5.4 | 7.9 | 1.82 | 0.07 | 1 | tr | 1 | 0.03 | 0.1 | 3.9 | 4.0 | 70 | 36 | ||||||
| 14N01507 | 13-25 | E | S | 5.4 | 8.2 | 0.80 | 0.09 | -- | tr | -- | 0.03 | 0.1 | 2.3 | 2.4 | 61 | 31 | ||||||
| 14N01508 | 25-53 | Bt1 | S | 5.4 | 9.2 | 0.33 | 0.07 | -- | -- | -- | 0.01 | 0.6 | 4.3 | 4.9 | 72 | 41 | ||||||
| 14N01509 | 53-69 | Bt2 | S | 4.7 | 9.0 | 0.07 | 0.10 | -- | -- | -- | tr | 4.8 | 0.5 | 5.3 | 8 | 5 | ||||||
| 14N01510 | 69-109 | Btx1 | S | 4.8 | 9.1 | 0.13 | 0.13 | -- | -- | -- | 0.01 | 4.9 | 1.8 | 6.7 | 19 | 13 | ||||||
| 14N01511 | 109-145 | Btx2 | S | 4.7 | 9.1 | 0.13 | 0.13 | -- | -- | -- | tr | 6.6 | 0.9 | 7.5 | 9 | 6 | ||||||
| 14N01512 | 145-180 | Btx3 | S | 4.8 | 9.1 | 0.09 | 0.12 | -- | -- | -- | tr | 6.2 | 0.6 | 6.8 | 7 | 5 | ||||||
| 14N01513 | 180-224 | BC | S | 4.7 | 8.7 | 0.16 | 0.14 | -- | tr | -- | 0.01 | 6.5 | 0.2 | 6.7 | 2 | 2 | ||||||