*** Taxonomy Characterization Data *** |
Pedon ID: S1990MN093002(4415) | ( Meeker, Minnesota ) | Print Date: Oct 31 2024 7:03PM |
Sampled as on Sep 16, 1990: | Canisteo |
Revised to correlated on Aug 31, 2011: | Crowriver ; Coarse-loamy, mixed, superactive, mesic Typic Calciaquolls |
State of Minnesoota | ||||
SSL | - | Project | MN201201 University of Minnesota | University of Minnesota |
- | Site ID | S1990MN093002(4415) Lat: 45° 12' 33.02" north Long: 94° 35' 55.96" west MLRA: 103 | Department of Soil Science | |
- | Pedon No. | UMN4415 | 568 Borlang Hall, 1991 Upper Buford Cr | |
- | General Methods 1B1A, 2A1, 2B | St. Paul, MN 55108 |
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 | 3A1a1a | ||||||||||||
MN441501 | 0-23 | Ap | S | 20.4 | 2.0 | ||||||||
MN441502 | 23-30 | Ak | S | 19.8 | 3.0 | ||||||||
MN441503 | 30-51 | Bkg | S | 15.5 | 4.0 | ||||||||
MN441504 | 51-152 | Bk | S | 9.3 | 1.0 |
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 | % | |||||||||||
4C1a2a | 6A1 | 4E1a1a1a1 | |||||||||||||||||
MN441501 | 0-23 | Ap | S | 7.5 | 2.70 | 5 | |||||||||||||
MN441502 | 23-30 | Ak | S | 7.6 | 1.10 | 9 | |||||||||||||
MN441503 | 30-51 | Bkg | S | 7.6 | 0.40 | 14 | |||||||||||||
MN441504 | 51-152 | Bk | S | 7.6 | 0.10 | 16 |