Crop Performance and Soil Properties in Two Artificially Eroded Soils in North‐Central Alberta

Abstract

Field experiments were conducted from 1991 to 1995 at Josephburg (Orthic Black Chernozem, Typic Cryoboroll) and Cooking Lake (Orthic Gray Luvisol, Typic Cryoboralf), Alberta, to determine the impact of topsoil removal on selected soil properties, N‐mineralization potential, and crop yield, and the effectiveness of various amendments for restoring the productivity of eroded soils. The simulated‐erosion levels were established in the autumn of 1990 by removing 20 cm of topsoil in 5‐cm depth increments. The four amendments were: control, addition of 5 cm of topsoil, fertilizers to supply 100 kg N ha−1 and 20 kg P ha−1, and cattle manure at 75 Mg ha−1. Topsoil and manure were applied once in the autumn of 1990, while fertilizers were applied annually from 1991 to 1995. Available N and P; total C, N, and P; and N‐mineralization potential decreased, while bulk density increased with increasing depth of topsoil removal. Tiller number, plant height, spike density, thousand‐kernel weight, and leaf area index decreased with simulated erosion. Grain yield reductions due to simulated soil erosion were either linear or curvilinear functions of nutrient removal. Application of N and P fertilizers and manure improved grain yield and reduced the impact of yield loss due to erosion. Return of 5 cm of topsoil also increased grain yield, but to a lesser extent than manure or fertilizers. Grain yields were maximized when fertilizers were also applied to organic amendment treatments. Our findings suggest the importance of integrated use of organic amendments and chemical fertilizers for best crop yields on severely eroded soils.