Abstract

AbstractLong‐term agricultural sustainability and productivity are controlled by the integrative effects of different management practices on the soil. Many Arkansas producers use the double‐crop system to grow soybeans [Glycine max (L.) Merr] and wheat (Triticum aestivum L.). The objective of this study was to evaluate the effects of agricultural management practices (including residue level, tillage, irrigation, and burning) and soil depth on the change in various soil properties from 2010 to 2020 in a long‐term, wheat–soybean, double‐crop system on a silt‐loam soil (Glossaquic Fraglossudalfs) in eastern Arkansas. Soil nutrients tended to accumulate over time, the most in the top 10 cm, whereas soil nutrient contents in the 10‐to‐20‐cm depth interval tended to not significantly change over time. Soil bulk density (BD) generally decreased across all treatments over time. Soil organic matter (SOM) content increased under all treatment combinations by 0.097 kg ha−1. Soil BD decreased and SOM numerically increased the most in the no‐tillage/no‐burn treatment in the top 10 cm of the soil. Total C was 9.2 times greater, whereas total N was 48 times greater in the top 10 cm of the soil. Soil pH was 1.9 times greater under irrigation than under nonirrigated treatments. Quantifying changes in soil‐properties over time will help producers to better understand the long‐term effects of various residue and water management practices and to find reasonable, more sustainable alternative practices.

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