*** Taxonomy Characterization Data *** |
Pedon ID: 1999MO203069M | ( Shannon, Missouri ) | Print Date: Nov 21 2024 1:24PM |
Sampled as on Jul 18, 1999: | Eudy |
Revised to correlated on Jan 29, 2012: | Eudy ; Fine, mixed, superactive, mesic Typic Hapludalfs |
State of Missouri | ||||
SSL | - | Project | MO201002 University of Missouri Project 2 | University of Missouri |
- | Site ID | 1999MO203069M Lat: 37° 6' 31.86" north Long: 91° 13' 44.38" west MLRA: 116A | College of Engineering | |
- | Pedon No. | M9961369 | Soil Characterization Laboratory | |
- | General Methods 1B1A, 2A1, 2B | Columbia, Missouri 65211 |
Taxonomy Tier 1 | -1- | -2- | -3- | -4- | -5- | -6- | -7- | -8- | -9- | -10- | |||
Fine | CaCO3 | 1500 | .1-75 | Bulk | Cole | Vol | Resist | ||||||
Clay | Clay | Clay | kPa | Clay | mm | Den | Whole | % of | Min | ||||
Depth | <.002 | <.0002 | <.002 | /Clay | Est | Frac | 33 kPa | Soil | Whole | % | |||
Layer | (cm) | Horz | Prep | (---------% of <2 mm-------) | (-------- % --------) | g cm-3 | cm cm-1 | ||||||
3A1a1a | |||||||||||||
MU064035 | 0-10 | A | S | 7.5 | |||||||||
MU064036 | 10-28 | Bt1 | S | 12.8 | |||||||||
MU064037 | 28-48 | 2Bt2 | S | 44.6 | |||||||||
MU064038 | 48-71 | 3Bt3 | S | 22.3 |
Taxonomy Tier 2 | -1- | -2- | -3- | -4- | -5- | -6- | -7- | -8- | -9- | -10- | -11- | -12- | -13- | -14- | -15- | -16- | |||
pH | pH | Org | Tot | Al+½ Fe | CO3 as | (--- Base Sat ---) | NZ | ECEC | CEC7 | ECEC | Al | ||||||||
Depth | H2O | NaF | C | C | Oxal | ODOE | CaCO3 | NH4 | Bases | P Ret | cmol(+) | /Clay | /Clay | Sat | E C | ESP | |||
Layer | (cm) | Horz | Prep | (------------------------------------------ % --------------------------------------------) | kg -1 | % | dS m-1 | % | |||||||||||
8C1a | 6A2d | ||||||||||||||||||
MU064035 | 0-10 | A | S | 6.3 | 1.80 | 81 | 63 | 1.15 | tr | ||||||||||
MU064036 | 10-28 | Bt1 | S | 5.2 | 0.60 | 57 | 42 | 0.60 | -- | ||||||||||
MU064037 | 28-48 | 2Bt2 | S | 6.4 | 1.00 | 95 | 78 | 0.60 | tr | ||||||||||
MU064038 | 48-71 | 3Bt3 | S | 7.5 | 0.60 | 100* | 94 | 0.66 | tr |