Abstract

The effects of 20 years of potassium (K) fertilization (in two treatments: 113 and 225kg K2Oha−1) on grain and stover yields, plant K concentrations, aboveground K uptake, K use efficiencies, soil K pools, and the K balance were examined in a Haplic Phaeozem soil under a rain-fed mono-cropped spring maize (Zea mays L.) system in the province of Jilin, northeast China. The indigenous K supply (zero K application) maintained an average grain yield of 7.0tha−1 per year, but the year-to-year variation was large. Application of K significantly (P<0.05) increased the average grain yields by 15.1 and 13.8% in the 113 and 225kg K2Oha−1 treatments, respectively, over the experimental period. The mean K recovery efficiency, K agronomic efficiency, and K partial factor productivity decreased from 37.3 to 28.5%, 10.8 to 4.9kgkg−1, and 86.8 to 43.1kgkg−1 when the K application rate increased from 113 to 225kg K2Oha−1. The effect of K application was larger on stover K concentrations than grain K concentrations. In the top 100cm of the soil profile, excessive or non-synchronized K application significantly (P<0.05) increased the leaching of exchangeable K in comparison with the control, but K application had little effect on soil non-exchangeable K and total K. K fertilizer, therefore, plays an important role in increasing grain yields in China, but the K application rate can be reduced if farmers return stover to the soil and make full use of K below the soil surface.

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