*** Taxonomy Characterization Data *** |
Pedon ID: S1960CO099004 | ( Prowers, Colorado ) | Print Date: Apr 30 2025 2:02AM |
Sampled as on Mar 5, 2008: | Rocky Ford ; Fine-silty, mixed, calcareous, mesic Ustic Torriorthent |
Revised to correlated on Mar 5, 2008: | Rocky Ford ; Fine-silty, mixed, mesic Ustic Torriorthent |
United States Department of Agriculture | ||||
SSL | - | Project | NL40001 SSIR SAMPLES | Soil Conservation Service |
- | Site ID | S1960CO099004 Lat: 38° 5' 31.00" north Long: 102° 14' 48.00" west MLRA: 67B | Lincoln Soil Survey Laboratory | |
- | Pedon No. | 40A3916 | Soil Laboratory | |
- | General Methods 1B1A, 2A1, 2B | Lincoln, Nebraska |
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 | ||||||||||||
40A29985 | 0-10 | Ap | S | 33.5 | 1.0 | 0.45 | 3 | -- | |||||
40A29986 | 10-23 | A | S | 36.8 | tr | 0.43 | 2 | -- | |||||
40A29987 | 23-46 | AC | S | 24.2 | 5.0 | 0.50 | 4 | -- |
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 | 6A1a | 6E1a | 8A1a | 5D2 | |||||||||||||||
40A29985 | 0-10 | Ap | S | 7.9 | 1.66 | 7 | 100 | 0.67 | 1.20 | 2 | |||||||||
40A29986 | 10-23 | A | S | 7.9 | 1.53 | 7 | 100 | 0.62 | 0.80 | 2 | |||||||||
40A29987 | 23-46 | AC | S | 7.9 | 0.69 | 11 | 100 | 0.70 | 0.90 | 2 |