| *** Andic Soil Properties Data *** |
| Pedon ID: S2002LA095003 | ( St. John the BaptistParish, Louisiana ) | Print Date: Nov 12 2024 9:37AM |
| Sampled as on May 27, 2002: | Carville ; Coarse-silty, mixed, superactive, nonacid, hyperthermic Fluvaquentic Endoaquept |
| Revised to correlated: | Carville ; Coarse-silty, mixed, superactive, nonacid, thermic Fluvaquentic Endoaquepts |
| United States Department of Agriculture | ||||
| SSL | - | Project | C2002USLA135 HYPERTHERMIC STUDY | Natural Resources Conservation Service |
| - | Site ID | S2002LA095003 Lat: 30° 47.25" north Long: 90° 2750.03" west MLRA: 131 | National Soil Survey Center | |
| - | Pedon No. | 02N0335 | 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 | 3A1a1a | 3C2a1a | DbWR1 | |||||||||||||||||||||
| 02N01644 | 0-16 | Ap1 | S | 9.3 | 4.4 | 16.2 | 2 | -- | 8.0 | 0.86 | 1.36 | 0.012 | ||||||||||||
| 02N01645 | 16-32 | Ap2 | S | 9.9 | 5.2 | 4 | -- | 5.5 | 0.56 | 1.40 | 0.007 | |||||||||||||
| 02N01646 | 32-49 | C1 | S | 16.0 | 6.8 | 1 | -- | 8.7 | 0.54 | 1.50 | 0.009 | 3 | ||||||||||||
| 02N01647 | 49-70 | C2 | S | 15.3 | 7.4 | 1 | -- | 8.5 | 0.56 | 1.34 | 0.012 | |||||||||||||
| 02N01648 | 70-85 | C3 | S | 18.8 | 8.2 | tr | -- | 10.5 | 0.56 | 1.38 | 0.012 | |||||||||||||
| 02N01649 | 85-100 | C4 | S | 14.5 | 6.7 | 1 | -- | 7.7 | 0.53 | 1.30 | 0.010 | 3 | ||||||||||||
| 02N01650 | 100-114 | Cg1 | S | 14.9 | 6.8 | 1 | -- | 8.8 | 0.59 | 1.28 | 0.013 | |||||||||||||
| 02N01651 | 114-138 | Cg2 | S | 13.9 | 6.3 | 1 | -- | 8.0 | 0.58 | 1.37 | 0.010 | |||||||||||||
| 02N01652 | 138-190 | Cg3 | S | 12.7 | 5.5 | 1 | -- | 7.2 | 0.57 | 1.34 | 0.007 | |||||||||||||
| 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 | 4H2a | 4E1a1a1a1 | ||||||||||||||||||||
| 02N01644 | 0-16 | Ap1 | S | 8.2 | 1.91 | 3 | 32.5 | 100* | ||||||||||||||
| 02N01645 | 16-32 | Ap2 | S | 8.5 | 0.89 | 3 | 45.5 | 100* | ||||||||||||||
| 02N01646 | 32-49 | C1 | S | 8.3 | 0.70 | 3 | 31.8 | 100* | ||||||||||||||
| 02N01647 | 49-70 | C2 | S | 8.3 | 0.65 | 3 | 27.9 | 100* | ||||||||||||||
| 02N01648 | 70-85 | C3 | S | 8.2 | 0.70 | 2 | 27.7 | 100* | ||||||||||||||
| 02N01649 | 85-100 | C4 | S | 8.2 | 0.67 | 2 | 22.4 | 100* | ||||||||||||||
| 02N01650 | 100-114 | Cg1 | S | 8.2 | 0.73 | 3 | 25.6 | 100* | ||||||||||||||
| 02N01651 | 114-138 | Cg2 | S | 8.1 | 0.86 | 2 | 22.9 | 100* | ||||||||||||||
| 02N01652 | 138-190 | Cg3 | S | 8.0 | 0.65 | 1 | 17.5 | 100* | ||||||||||||||