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Dryad

Soil properties and their interactions on organic farms in Nebraska

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Jan 13, 2022 version files 2.93 MB

Abstract

Sustainable soil productivity is a function of soil chemical, physical, and biological main and interaction effects that vary with inherent soil properties, topography, crop, location, and management. These effects were investigated using soil samples collected at geo-referenced points from 119 fields on 15 organically certified farms across Nebraska. Observations are reported for 46 variables. Most fields had adequate soil conditions for high productivity. The irrigated versus rainfed effects differed for several soil properties in western compared with eastern Nebraska. On average, about 80% of the soil was in water-stable aggregates (WSA) of >0.05 mm diameter with more aggregation and arbuscular mycorrhizal fungi (AMF) with pasture compared with cropland. Variation in soil microbial biomass (SMB) was more affected by variation in soil and climate properties than by management. Increased SOM for cropland in eastern Nebraska was positively related to SMB but not to AMF or the biomass ratios of saprophytic fungi (Fs) to bacteria and of actinomycetes to other bacteria. After accounting for the effect of SOM, SMB was most positively related to crop growth at the time of sampling, and availability of K and S. Mehlich-3 P was positively correlated with SMB but P and Zn availability were negatively correlated to AMF. Increased soil pH was associated with greater biomass of Fs and eukaryotes but not of bacteria. The SMB was generally less for pastures in western Nebraska compared with other field types. In conclusion, the soil properties of these organic farms were generally suited to high productivity and SMB had a strong, positive relationship to SOM.